A butterfly is a mainly day-flying insect of the order Lepidoptera, which includes the butterflies and moths. Like other holometabolous insects, the butterfly's life cycle consists of four parts: egg, larva, pupa and adult. Most species are diurnal. Butterflies have large, often brightly coloured wings, and conspicuous, fluttering flight. Butterflies comprise the true butterflies (superfamily Papilionoidea), the skippers (superfamily Hesperioidea) and the moth-butterflies (superfamily Hedyloidea). All the many other families within the Lepidoptera are referred to as moths. The earliest known butterfly fossils date to the mid Eocene epoch, between 40–50 million years ago.[1]

Butterflies exhibit polymorphism, mimicry and aposematism. Some, like the Monarch, will migrate over long distances. Some butterflies have evolved symbiotic and parasitic relationships with social insects such as ants. Some species are pests because in their larval stages they can damage domestic crops or trees; however, some species are agents of pollination of some plants, and caterpillars of a few butterflies (e.g., Harvesters) eat harmful insects. Culturally, butterflies are a popular motif in the visual and literary arts.

Pyrite concretions in black shale from the Pennsylvanian of Illinois, USA. (public display, National Rockhound Hall of Fame, Murdo, South Dakota, USA)

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5500 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

The sulfide minerals contain one or more sulfide anions (S-2). The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals. Many sulfides are economically significant, as they occur commonly in ores. The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc. Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size. These minerals will not form in the presence of free oxygen. Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals.

Pyrite is a common iron sulfide mineral (FeS2). It’s nickname is “fool's gold”. Pyrite has a metallic luster, brassy gold color (in contrast to the deep rich yellow gold color of true gold - www.flickr.com/photos/jsjgeology/sets/72157651325153769/), dark gray to black streak, is hard (H=6 to 6.5), has no cleavage, and is moderately heavy for its size. It often forms cubic crystals or pyritohedrons (crystals having pentagonal faces).

Pyrite is common in many hydrothermal veins, shales, coals, various metamorphic rocks, and massive sulfide deposits.

The pyrite specimens shown above are "pyrite suns" - discoidal concretions developed along a bedding plane in black shale (which is probably restored or reconstructed or fabricated for the retail market). Texturally, the concretions have outward-radiating crystals with moderately-developed concentricity. Mineralogically, they are principally composed of pyrite, plus minor marcasite (also FeS2 - iron sulfide; marcasite is a polymorph of pyrite).

Stratigraphy: Anna Shale (= roof shale of the Herrin Coal), upper Carbondale Formation, Desmoinesian Series, upper Middle Pennsylvanian

Locality: coal mine near Sparta, Randolph County, southwestern Illinois, USA

------------------------

Photo gallery of pyrite:

www.mindat.org/gallery.php?min=3314

Mohs 7.

Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon–oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical formula of SiO2. Quartz is the second most abundant mineral in Earth's continental crust, behind feldspar.

Quartz exists in two forms, the normal α-quartz and the high-temperature β-quartz, both of which are chiral. The transformation from α-quartz to β-quartz takes place abruptly at 573 °C (846 K; 1,063 °F). Since the transformation is accompanied by a significant change in volume, it can easily induce microfracturing of ceramics or rocks passing through this temperature threshold.

There are many different varieties of quartz, several of which are classified as gemstones. Since antiquity, varieties of quartz have been the most commonly used minerals in the making of jewelry and hardstone carvings, especially in Eurasia.

Quartz is the mineral defining the value of 7 on the Mohs scale of hardness, a qualitative scratch method for determining the hardness of a material to abrasion.

Etymology

The word "quartz" is derived from the German word "Quarz", which had the same form in the first half of the 14th century in Middle High German and in East Central German] and which came from the Polish dialect term kwardy, which corresponds to the Czech term tvrdý ("hard")

The Ancient Greeks referred to quartz as κρύσταλλος (krustallos) derived from the Ancient Greek κρύος (kruos) meaning "icy cold", because some philosophers (including Theophrastus) apparently believed the mineral to be a form of supercooled ice. Today, the term rock crystal is sometimes used as an alternative name for transparent coarsely crystalline quartz.

Crystal habit and structure

Quartz belongs to the trigonal crystal system at room temperature, and to the hexagonal crystal system above 573 °C (846 K; 1,063 °F). The ideal crystal shape is a six-sided prism terminating with six-sided pyramids at each end. In nature quartz crystals are often twinned (with twin right-handed and left-handed quartz crystals), distorted, or so intergrown with adjacent crystals of quartz or other minerals as to only show part of this shape, or to lack obvious crystal faces altogether and appear massive.[16][17] Well-formed crystals typically form as a druse (a layer of crystals lining a void), of which quartz geodes are particularly fine examples.The crystals are attached at one end to the enclosing rock, and only one termination pyramid is present. However, doubly terminated crystals do occur where they develop freely without attachment, for instance, within gypsum.

Although many of the varietal names historically arose from the color of the mineral, current scientific naming schemes refer primarily to the microstructure of the mineral. Color is a secondary identifier for the cryptocrystalline minerals, although it is a primary identifier for the macrocrystalline varieties.[24]

Major varieties of quartz

TypeColor and descriptionTransparency

Herkimer diamondColorlessTransparent

Rock crystalColorlessTransparent

AmethystPurple to violet colored quartzTransparent

CitrineYellow quartz ranging to reddish-orange or brown (Madera quartz), and occasionally greenish yellowTransparent

AmetrineA mix of amethyst and citrine with hues of purple/violet and yellow or orange/brownTransparent

Rose quartzPink, may display diasterismTransparent

ChalcedonyFibrous, variously translucent, cryptocrystalline quartz occurring in many varieties.

The term is often used for white, cloudy, or lightly colored material intergrown with moganite.

Otherwise more specific names are used.

CarnelianReddish orange chalcedonyTranslucent

AventurineQuartz with tiny aligned inclusions (usually mica) that shimmer with aventurescenceTranslucent to opaque

AgateMulti-colored, curved or concentric banded chalcedony (cf. Onyx)Semi-translucent to translucent

OnyxMulti-colored, straight banded chalcedony or chert (cf. Agate)Semi-translucent to opaque

JasperOpaque cryptocrystalline quartz, typically red to brown but often used for other colorsOpaque

Milky quartzWhite, may display diasterismTranslucent to opaque

Smoky quartzLight to dark gray, sometimes with a brownish hueTranslucent to opaque

Tiger's eyeFibrous gold, red-brown or bluish colored chalcedony, exhibiting chatoyancy.

PrasioliteGreenTransparent

Rutilated quartzContains acicular (needle-like) inclusions of rutile

Dumortierite quartzContains large amounts of blue dumortierite crystalsTranslucent

Varieties (according to color)[edit]

Pure quartz, traditionally called rock crystal or clear quartz, is colorless and transparent or translucent, and has often been used for hardstone carvings, such as the Lothair Crystal. Common colored varieties include citrine, rose quartz, amethyst, smoky quartz, milky quartz, and others. These color differentiations arise from the presence of impurities which change the molecular orbitals, causing some electronic transitions to take place in the visible spectrum causing colors.

The most important distinction between types of quartz is that of macrocrystalline (individual crystals visible to the unaided eye) and the microcrystalline or cryptocrystalline varieties (aggregates of crystals visible only under high magnification). The cryptocrystalline varieties are either translucent or mostly opaque, while the transparent varieties tend to be macrocrystalline. Chalcedony is a cryptocrystalline form of silica consisting of fine intergrowths of both quartz, and its monoclinic polymorph moganite] Other opaque gemstone varieties of quartz, or mixed rocks including quartz, often including contrasting bands or patterns of color, are agate, carnelian or sard, onyx, heliotrope, and jasper

Amethyst

Clear (regular) quartz

Amethyst

Blue quartz

Dumortierite quartz

Citrine quartz (natural)

Citrine quartz (heat-altered amethyst)

Milky quartz

Rose quartz

Smoky quartz

Prasiolite

Amethyst is a form of quartz that ranges from a bright vivid violet to a dark or dull lavender shade. The world's largest deposits of amethysts can be found in Brazil, Mexico, Uruguay, Russia, France, Namibia, and Morocco. Sometimes amethyst and citrine are found growing in the same crystal. It is then referred to as ametrine. Amethyst derives its color from traces of iron in its structure.[27]

Blue quartz

Blue quartz contains inclusions of fibrous magnesio-riebeckite or crocidolite.

Dumortierite quartz]

Inclusions of the mineral dumortierite within quartz pieces often result in silky-appearing splotches with a blue hue. Shades of purple or grey sometimes also are present. "Dumortierite quartz" (sometimes called "blue quartz") will sometimes feature contrasting light and dark color zones across the material.[29][30] "Blue quartz" is a minor gemstone.[29][31]

Citrine

Citrine is a variety of quartz whose color ranges from pale yellow to brown due to a submicroscopic distribution of colloidal ferric hydroxide impurities.[32] Natural citrines are rare; most commercial citrines are heat-treated amethysts or smoky quartzes. However, a heat-treated amethyst will have small lines in the crystal, as opposed to a natural citrine's cloudy or smoky appearance. It is nearly impossible to differentiate between cut citrine and yellow topaz visually, but they differ in hardness. Brazil is the leading producer of citrine, with much of its production coming from the state of Rio Grande do Sul. The name is derived from the Latin word citrina which means "yellow" and is also the origin of the word "citron". Sometimes citrine and amethyst can be found together in the same crystal, which is then referred to as ametrine.[33] Citrine has been referred to as the "merchant's stone" or "money stone", due to a superstition that it would bring prosperity.[34]

Citrine was first appreciated as a golden-yellow gemstone in Greece between 300 and 150 BC, during the Hellenistic Age. Yellow quartz was used prior to that to decorate jewelry and tools but it was not highly sought after.

Milky quartz

Milk quartz or milky quartz is the most common variety of crystalline quartz. The white color is caused by minute fluid inclusions of gas, liquid, or both, trapped during crystal formation, making it of little value for optical and quality gemstone applications.

Rose quartz

Rose quartz is a type of quartz that exhibits a pale pink to rose red hue. The color is usually considered as due to trace amounts of titanium, iron, or manganese, in the material. Some rose quartz contains microscopic rutile needles that produce asterism in transmitted light. Recent X-ray diffraction studies suggest that the color is due to thin microscopic fibers of possibly dumortierite within the quartz.

Additionally, there is a rare type of pink quartz (also frequently called crystalline rose quartz) with color that is thought to be caused by trace amounts of phosphate or aluminium. The color in crystals is apparently photosensitive and subject to fading. The first crystals were found in a pegmatite found near Rumford, Maine, US and in Minas Gerais, Brazil.[39] The crystals found are more transparent and euhedral, due to the impurities of phosphate and aluminium that formed crystalline rose quartz, unlike the iron and microscopic dumortierite fibers that formed rose quartz.

Smoky quartz

Smoky quartz is a gray, translucent version of quartz. It ranges in clarity from almost complete transparency to a brownish-gray crystal that is almost opaque. Some can also be black. The translucency results from natural irradiation acting on minute traces of aluminum in the crystal structure.[41]

Prasiolite

Not to be confused with Praseolite.

Prasiolite, also known as vermarine, is a variety of quartz that is green in color. Since 1950, almost all natural prasiolite has come from a small Brazilian mine, but it is also seen in Lower Silesia in Poland. Naturally occurring prasiolite is also found in the Thunder Bay area of Canada. It is a rare mineral in nature; most green quartz is heat-treated amethyst]

Synthetic and artificial treatments

A synthetic quartz crystal grown by the hydrothermal method, about 19 cm long and weighing about 127 grams

Not all varieties of quartz are naturally occurring. Some clear quartz crystals can be treated using heat or gamma-irradiation to induce color where it would not otherwise have occurred naturally. Susceptibility to such treatments depends on the location from which the quartz was mined.

Prasiolite, an olive colored material, is produced by heat treatment;[44] natural prasiolite has also been observed in Lower Silesia in Poland] Although citrine occurs naturally, the majority is the result of heat-treating amethyst or smoky quartz. Carnelian has been heat-treated to deepen its color since prehistoric times.

Because natural quartz is often twinned, synthetic quartz is produced for use in industry. Large, flawless, single crystals are synthesized in an autoclave via the hydrothermal process.

Like other crystals, quartz may be coated with metal vapors to give it an attractive sheen

Occurrence

Granite rock in the cliff of Gros la Tête on Aride Island, Seychelles. The thin (1–3 cm wide) brighter layers are quartz veins, formed during the late stages of crystallization of granitic magmas. They are sometimes called "hydrothermal veins".

Quartz is a defining constituent of granite and other felsic igneous rocks. It is very common in sedimentary rocks such as sandstone and shale. It is a common constituent of schist, gneiss, quartzite and other metamorphic rocks.[16] Quartz has the lowest potential for weathering in the Goldich dissolution series and consequently it is very common as a residual mineral in stream sediments and residual soils. Generally a high presence of quartz suggests a "mature" rock, since it indicates the rock has been heavily reworked and quartz was the primary mineral that endured heavy weathering

While the majority of quartz crystallizes from molten magma, quartz also chemically precipitates from hot hydrothermal veins as gangue, sometimes with ore minerals like gold, silver and copper. Large crystals of quartz are found in magmatic pegmatites. Well-formed crystals may reach several meters in length and weigh hundreds of kilograms

Elemental impurity incorporation strongly influences the ability to process and utilize quartz. Naturally occurring quartz crystals of extremely high purity, necessary for the crucibles and other equipment used for growing silicon wafers in the semiconductor industry, are expensive and rare. These high-purity quartz are defined containing less than 50 ppm of impurity elements. A major mining location for high purity quartz is the Spruce Pine Gem Mine in Spruce Pine, North Carolina, United States. Quartz may also be found in Caldoveiro Peak, in Asturias, Spain.

The largest documented single crystal of quartz was found near Itapore, Goiaz, Brazil; it measured approximately 6.1 m × 1.5 m × 1.5 m and weighed 39,916 kilograms.

Mining

Quartz is extracted from open pit mines. Miners occasionally use explosives to expose deep pockets of quartz. More frequently, bulldozers and backhoes are used to remove soil and clay and expose quartz veins, which are then worked using hand tools. Care must be taken to avoid sudden temperature changes that may damage the crystals.

Almost all the industrial demand for quartz crystal (used primarily in electronics) is met with synthetic quartz produced by the hydrothermal process. However, synthetic crystals are less prized for use as gemstones. The popularity of crystal healing has increased the demand for natural quartz crystals, which are now often mined in developing countries using primitive mining methods, sometimes involving child labor.[60]

Related silica minerals

Tridymite and cristobalite are high-temperature polymorphs of SiO2 that occur in high-silica volcanic rocks. Coesite is a denser polymorph of SiO2 found in some meteorite impact sites and in metamorphic rocks formed at pressures greater than those typical of the Earth's crust. Stishovite is a yet denser and higher-pressure polymorph of SiO2 found in some meteorite impact sites. Lechatelierite is an amorphous silica glass SiO2 which is formed by lightning strikes in quartz sand]

Safety

As quartz is a form of silica, it is a possible cause for concern in various workplaces. Cutting, grinding, chipping, sanding, drilling, and polishing natural and manufactured stone products can release hazardous levels of very small, crystalline silica dust particles into the air that workers breathe.Crystalline silica of respirable size is a recognized human carcinogen and may lead to other diseases of the lungs such as silicosis and pulmonary fibrosis.

From Wikipedia

Chairlift @ Lollapalooza 2016, Grant Park, Chicago, IL, on Saturday, July 30, 2016.

Lollapalooza 2016 Setlist:

Look Up

Polymorphing

Amanaemonesia

I Belong in Your Arms

Show U Off

Romeo

Crying In Public

Moth to the Flame

Ch-Ching

Get Real

Opening night of the show "Polymorph" by Katya Usvitsky, at The One Well, Greenpoint, Brooklyn, NYC. See press coverage here. The work will be on display/for sale through November 4th.

Artist's website.

As borboletas são insectos da ordem Lepidoptera classificados nas super-famílias Hesperioidea e Papilionoidea, que constituem o grupo informal Rhopalocera.

As borboletas têm dois pares de asas membranosas cobertas de escamas e peças bucais adaptadas a sucção. Distinguem-se das traças (mariposas) pelas antenas rectilíneas que terminam numa bola, pelos hábitos de vida diurnos, pela metamorfose que decorre dentro de uma crisálida rígida e pelo abdómen fino e alongado. Quando em repouso, as borboletas dobram as suas asas para cima.

As borboletas são importantes polinizadores de diversas espécies de plantas.

O ciclo de vida das borboletas engloba as seguintes etapas:

1) ovo→ fase pré-larval

2) larva→ chamada também de lagarta ou taturana,

3) pupa→ que se desenvolve dentro da crisálida (ou casulo)

4) imago→ fase adulta

_______________________

A butterfly is any of several groups of mainly day-flying insects of the order Lepidoptera, the butterflies and moths. Like other holometabolous insects, butterflies' life cycle consists of four parts, egg, larva, pupa and adult. Most species are diurnal. Butterflies have large, often brightly coloured wings, and conspicuous, fluttering flight. Butterflies comprise the true butterflies (superfamily Papilionoidea), the skippers (superfamily Hesperioidea) and the moth-butterflies (superfamily Hedyloidea). All the many other families within the Lepidoptera are referred to as moths.

Butterflies exhibit polymorphism, mimicry and aposematism. Some, like the Monarch, will migrate over long distances. Some butterflies have evolved symbiotic and parasitic relationships with social insects such as ants. Butterflies are important economically as agents of pollination. The caterpillars of some butterflies eat harmful insects. A few species are pests because in their larval stages they can damage domestic crops or trees. Culturally, butterflies are a popular motif in the visual and literary arts.

Gujba

Carbonaceous chondrites CBa

Nigeria

Fall: 1984

TKW: 100 kg / OBJ: 2,1 g

Gujba is a bencubbinite (carbonaceous chondrite). At 6:30 in the evening, a bright fireball approaching from the west was seen and heard by local residents. The cone-shaped mass that landed in a corn field near the village of Bogga Dingare in Yobe, Nigeria, was estimated to have weighed ~100 kg, but most of the mass was broken up into small pieces and dispersed.

To date, Gujba is the only witnessed bencubbinite fall.

Bencubbinites are unusual stony-iron meteorites composed of roughly equal amounts of Fe, Ni metal and ferromagnesian silicates. Gujba is classified as a bencubbinite (CBa); meteorites in the CBa group are primitive, metal-rich chondrites. The bencubbinites represent some of the most fascinating meteorites, recording evidence of violent planetary-sized impacts, and containing some of the most primitive solar system materials. Their primitive characteristics make the CBa chondrites valuable recorders of early nebular processes.

Gujba is a primitive, polymict, chondritic breccia, the first fall of the bencubbinite group. It contains 0.4–8 mm-diameter, rounded, metallic globules (~41 vol%) and 0.8–15 mm-diameter silicate globules (~20 vol%), cemented together by a dark-colored, silicate-rich, impact-melt matrix composed of mm-sized fragments of both silicate and metal globules (~39 vol%).

Metal globules can contain up to ~1 vol% troilite, which is positively correlated with the abundance of volatile siderophile elements. Fractionation of siderophile elements in Gujba was controlled by volatility rather than by oxidation/sulfidation processes or magmatic crystallization (Krot et al., 2002). Siderophile element correlations are inconsistent with a nebular condensation model. It is generally assumed that a protoplanetary impact gave rise to a vapor cloud with high enough partial pressures to generate a metal-enriched gas. The metal globules then condensed as liquids from this gas and were sorted by size and density, thereby establishing the high metal/silicate ratio of the group. The CB group reflects a sequence of increasingly lighter Fe isotopes from Gujba through HaH 237 to Isheyevo (Zipfel and Weyer, 2006). This wide Fe isotopic range provides further evidence of a formation within an impact vapor plume rather than in a nebula setting. See the HaH 237 page for a more detailed scenario of the CB group formation process ascertained by Fedkin et al. (2015) through kinetic condensation modeling.

In a nm-scale study of Gujba, a two-phase (kamacite and taenite) metal particle was observed comprising ~30 individual grains that demonstrate a reheating episode occurred at temperatures of ~675°C (Goldstein et al, 2011). It is estimated that a subsequent cooling to ~550°C occurred within a time period of a month. A similar metal particle having a similar thermal history was found in the CBb bencubbinite HaH 237. Through 3-D mapping of Gujba at a µm scale, at least five types of metal particles of differing Ni content (~5 to ~8.2 wt%) and sulfide content were identified (Berlin et al., 2013). These metal particles are consistent with an origin in an impact plume, followed by accretion to a secondary parent body, where they experienced impact-associated secondary heating. Based on their examination of sulfide phases embedded in metal grains within the Gujba and Weatherford CBa meteorites, and through comparisons of Fe–S–Cr phase diagrams, Srinivasan et al. (2013) concluded that both the reheating of these sulfide phases and the injection of silicate melt into metal and silicate host components were likely concurrent with this impact.

Hydrocode modeling employing a homogeneous nucleation theory demonstrates that the very high densities and temperatures that would lead to the formation of mm- to cm-sized metal globules are consistent with an impact vapor plume origin rather than a nebular origin (Anic et al., 2005). A high velocity collision is most likely to produce those conditions conducive to producing the particle size that exists in Gujba. An alternative model has been described whereby the metal was melted to form globules, while S and volatile siderophiles were subsequently evaporated out. The metal globules have varying Ni contents and exhibit quench textures (Rubin et al., 2003), and since no diffusion has occurred among globules in contact with each other, it can be inferred that they were accreted at cold temperatures after being isolated from the hot condensation region.

The silicate globules in Gujba exhibit skeletal olivine textures, contain no FeNi-metal or troilite, and have low concentrations of volatile elements, features indicative of quenching from a molten state; i.e., condensation from a hot, impact-generated vapor plume (Krot et al., 2004). CAIs have been found in some bencubbinites including HaH 237, QUE 94411, and Gujba, as well as the transitional member Isheyevo; however, since their O-isotopic values plot along the CCAM line instead of the CR trend line, they represent solar nebula material rather than condensates from the impact vapor plume (Fedkin et al., 2015).

Raman spectra have identified the first carbonaceous chondrite occurrence of several high pressure phases within barred olivine fragments and the matrix components of Gujba; these include majorite garnet, majorite-pyrope solid solution, and wadsleyite, along with minor grossular-pyrope solid solution and coesite (Weisberg and Kimura, 2010). These high pressure phases formed either from solid-state transformation of pyroxene or crystallization from an impact melt during a heterogeneous, planetesimal wide impact shock event reaching minimum pressures of ~19 GPa and temperatures of ~2000°C. The investigators argue that these high pressure phases are inconsistent with the subsequent formation of chondrules within an impact plume since at such high temperatures these phases would be rapidly back-transformed to their low temperature polymorphs. Moreover, the measured cooling rates of chondrules (ave. 100K/hr) are much too slow than that at which shock veins with high pressure polymorphs would survive (~1000K/hr). Therefore, they determined that the barred chondrules and metal in CB chondrites were formed prior to the impact event that produced the high pressure polymorphs.

The bencubbinites constitute a small group having similar oxygen and nitrogen isotopic compositions as well as similar petrologic characteristics. They have highly reduced silicates, bulk metal abundances of 60–70 vol%, Cr-bearing troilite, metal with near solar Ni/Co ratios, and similar elemental abundances. Among chondrite groups, the bencubbinites show a significant enrichment of 15N, with Gujba having an intermediate content within the group. The bencubbinites have been divided into two petrologic subgroups, CBa and CBb, representing those with cm-sized metal and silicate globules, and those with mm-sized globules, respectively. Further information on the formation of bencubbinites can be found on the Bencubbin, Isheyevo, and NWA 1814 pages.

Based on the U–Pb isotopic chronometer using the Shallowater standard (at that time corrected to 4.5613 [±0.0008] b.y. by Connelly et al., 2012), the chondrules in Gujba (CBa) and HaH 237 (CBb) were calculated to have formed simultaneously 4.56168 (±0.00051) b.y. ago; this age reflects a more recent formation event in comparison to other chondrite groups. Employing the corrected I–Xe data from Gilmour et al. (2009) for Gujba and that from Pravdivtseva et al. (2014) for HaH 237, respective closure ages of 4.5632 (±0.0013) b.y. and 4.56101 (±0.00087) b.y. were obtained. The age difference between these CBa and CBb chondrules was attributed to possible heterogeneity of the I-isotopic compositions in the two meteorites' respective formation regions within the impact vapor-melt plume (Bollard et al., 2015). Furthermore, other chronometers have provided ages consistent with those cited above, with a Hf–W age anchored to CAIs of 4.5622 (±0.0024) b.y., and a Mn–Cr age anchored to D'Orbigny of 4.5633 (±0.001) b.y. (Bollard et al., 2015). In their high-precision study of four Gujba chondrules, Bollard et al. (2015) derived a weighted average age of 4.56249 (±0.00021) b.y.; this equates to 4.8 (±0.3) m.y. after CAIs, or 1.2 (±0.6) m.y. after the formation of the youngest known nebular chondrule. Subsequent to this, high precision isotopic studies involving HaH 237 were conducted by Pravdivtseva et al. (2015, 2016), which led them to suggest a refinement in the absolute I–Xe age for the Shallowater standard of 4.5624 (±0.0002) b.y. Based on this new refinement, the age of HaH 237 relative to Shallowater was ascertained to be 4.5621 (±0.0003) m.y., which is consistent with the U-corrected Pb–Pb age determined for Gujba chondrules by Bollard et al. (2015) above, as well as that determined for HaH 237 silicates by Krot et al. (2005) of 4.5619 (±0.0009) b.y. All of these ages attest to a relatively late formation of the CB-group chondrites from a vapor-melt plume following a catastrophic impact between two planetary embryos.

The CRE age of Gujba (26 ±7 m.y.) is identical within uncertainties to that of Bencubbin (27.3 m.y.), and both have similar noble gas concentrations (also similar in some respects to the enstatite chondrites; Nakashima and Nagao, 2009), which attests to a common ejection event on their parent body. However, while the metal and silicate globules in Gujba are mostly complete, undistorted spheres, those in Bencubbin and Weatherford are fragmented and distorted. Gujba and other CB chondrites exhibit multiple characteristics that are consistent with a severe shock subsequent to its formation, including melting, brecciation, and deformation. The presence of certain high-pressure phases in Gujba—majorite and wadsleyite, produced by the conversion of low-Ca pyroxene and olivine, respectively—attests to the occurrence of a significant shock event of ~19 GPa at 2000°C (Weisberg and Kimura, 2004) consistent with a shock stage of S2. As in Bencubbin, shock-associated structures identified in Gujba include stishovite, amorphous to poorly graphitized carbon, ordered graphite, rounded to euhedral diamonds, nanodiamond clumps, and rare bucky-diamonds, along with carbonaceous nanoglobules (Garvie et al., 2011).

The CB, CH, and CR chondrites constitute the CR clan, comprising groups which likely formed in the same isotopic reservoir under similar conditions in the solar nebula; current evidence argues for an origin of the metal-rich carbonaceous chondrites in a common collision between planetary embryos (Krot et al., 2009). The Gujba specimen pictured above is an 18.1 g polished slice sectioned from a 282 g fragment that was originally purchased in 2000 in Gidan Wire, Nigeria. See also a most spectacular 81.05 g full slice of this special bencubbinite, courtesy of the Stephan Kambach collection, which exhibits the finest details of both metallic and silicate chondrules. A beautiful high-resolution exterior view of Gujba, courtesy of Paul Swartz (Meteorite Picture of the Day, 1 Oct 2014), can be seen here. The photo below shows an awesome 2,365 g end piece, part of the Jay Piatek Collection, that was sectioned from a 3,440 g complete Gujba mass.

Vug with aragonite & calcite crystals in arenaceous, ferruginous, fossiliferous limestone from the Mississippian of Ohio, USA (photograph taken & provided by James Cheshire).

This unusual sedimentary rock has small vugs containing clear to whitish aragonite crystals (CaCO3 - calcium carbonate) and whitish, blocky calcite crystals (also CaCO3). Aragonite is a less common polymorph of calcite. Aragonite is rarely found in Ohio. The host rock is an arenaceous, ferruginous, fossiiferous limestone with dolomitized crinoid stem columnals.

Stratigraphy: Vinton Member (horizon occurs at the boundary between massive, thick-bedded Vinton below & thin-bedded, flaggy Vinton above), upper Logan Formation, Osagean Stage, upper Lower Mississippian

Locality: Mt. Calvary Cemetery Outcrop - roadcut along eastern side of Jacksontown Road (Rt. 13), immediately adjacent to (east of) Mt. Calvary Catholic Cemetery, ~0.15 miles south of intersection with Hopewell Drive, Heath, south-central Licking County, east-central Ohio, USA (40° 02’ 00.8” North, 82° 24” 10.5” West)

As borboletas são insectos da ordem Lepidoptera classificados nas super-famílias Hesperioidea e Papilionoidea, que constituem o grupo informal Rhopalocera.

As borboletas têm dois pares de asas membranosas cobertas de escamas e peças bucais adaptadas a sucção. Distinguem-se das traças (mariposas) pelas antenas rectilíneas que terminam numa bola, pelos hábitos de vida diurnos, pela metamorfose que decorre dentro de uma crisálida rígida e pelo abdómen fino e alongado. Quando em repouso, as borboletas dobram as suas asas para cima.

As borboletas são importantes polinizadores de diversas espécies de plantas.

O ciclo de vida das borboletas engloba as seguintes etapas:

1) ovo→ fase pré-larval

2) larva→ chamada também de lagarta ou taturana,

3) pupa→ que se desenvolve dentro da crisálida (ou casulo)

4) imago→ fase adulta

_______________________

A butterfly is any of several groups of mainly day-flying insects of the order Lepidoptera, the butterflies and moths. Like other holometabolous insects, butterflies' life cycle consists of four parts, egg, larva, pupa and adult. Most species are diurnal. Butterflies have large, often brightly coloured wings, and conspicuous, fluttering flight. Butterflies comprise the true butterflies (superfamily Papilionoidea), the skippers (superfamily Hesperioidea) and the moth-butterflies (superfamily Hedyloidea). All the many other families within the Lepidoptera are referred to as moths.

Butterflies exhibit polymorphism, mimicry and aposematism. Some, like the Monarch, will migrate over long distances. Some butterflies have evolved symbiotic and parasitic relationships with social insects such as ants. Butterflies are important economically as agents of pollination. The caterpillars of some butterflies eat harmful insects. A few species are pests because in their larval stages they can damage domestic crops or trees. Culturally, butterflies are a popular motif in the visual and literary arts.

Botryoidal marcasite from Peru.

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 6000 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

The sulfide minerals contain one or more sulfide anions (S-2). The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals. Many sulfides are economically significant, as they occur commonly in ores. The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc. Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size. These minerals will not form in the presence of free oxygen. Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals.

Marcasite is an iron sulfide mineral, FeS2, which is the same chemical formula as pyrite. Different minerals having the same chemical formula are called polymorphs. Other examples of polymorphs are graphite-diamond (both C) and calcite-aragonite (both CaCO3). Pyrite and marcasite both have a metallic luster, a brassy gold color, and a dark gray to black streak. They both lack cleavage, and they have the same hardness (H = 6 to 6.5). Marcasite tends to have a paler brass color than pyrite. Some marcasites are almost silvery-colored.

How does one visually distinguish marcasite from pyrite? Apart from color, marcasite crystals are typically plates, or sharp & pointed, and marcasite tends to twin, resulting in cockscomb masses (www.mindat.org/photo-408969.html). Marcasite also more readily breaks down into whitish powder (FeSO4).

Pyrite can convert to marcasite naturally, and vice versa. Pyrite concretions may have preserved needle-shaped crystals of marcasite, but the marcasite is gone. X-ray analysis may be needed to determine which polymorph is present.

Locality: Julcani Mining District, Angaraes Province, Huancavelica Department, southern Peru

-----------------

Photo gallery of marcasite:

www.mindat.org/gallery.php?min=2571

Obsidian in the Pleistocene of Wyoming, USA.

Obsidian is a glassy-textured, extrusive igneous rock. Glassy-textured rocks have no crystals at all. They form by very rapid cooling of lava or by cooling of high-viscosity lava. Most obsidians form by the latter. Obsidian can be felsic, intermediate, mafic, or alkaline in chemistry. Most are felsic to intermediate.

A famous locality in North America is Obsidian Cliff at Yellowstone, Wyoming. It is a Pleistocene-aged lava flow with the chemistry of rhyolite (= a light-colored, felsic, aphanitic, extrusive igneous rock). The cliff itself shows columnar jointing, which formed by cooling and contraction. The rocks principally range from black-colored, aphyric rhyolitic obsidian to partially devitrified rhyolitic obsidian. Lithophysae are sometimes present. Extremely small, microscopic crystals are present - they can be seen in thin sections. Some samples are reported to have small olivine phenocrysts. Small clusters of crystals, composed of plagioclase feldspar, pyroxene, and olivine, are sometimes present.

Many of the whitish-colored spots and bands running through most Obsidian Cliff rock samples are areas of devitrification. Glass is unstable on geologic times scales and it slowly crystallizes. The light-colored spots and bands are now non-glassy. Spotted, partially devitrified obsidian is known by the rockhound term "snowflake obsidian" (see: www.flickr.com/photos/jsjgeology/16561606417). The spots are composed of silica (SiO2), but are not quartz. Rather, they are composed of a polymorph of quartz - cristobalite.

Why does Obsidian Cliff here not look black and glassy? The rocks are weathered, partially devitrified, and considerably lichen-covered. Classic, black, glassy obsidian can be seen in some of the boulders along the road.

Stratigraphy: Roaring Mountain Member, Plateau Rhyolite, Upper Pleistocene, ~59 ka

Locality: Obsidian Cliff, eastern edge of Obsidian Creek Valley, Yellowstone National Park, northwestern Wyoming, USA

----------------------

Age & some lithologic info. from:

Wooton (2010) - Age and Petrogenesis of the Roaring Mountain Rhyolites, Yellowstone Volcanic Field, Wyoming. M.S. thesis. University of Nevada at Las Vegas. 296 pp.

The Term Morph Is Inappropriate

As if we didn’t know, we asked a solitary roadside birder, “Looking for something?”

“The Gyrfalcon.”

“Have you seen it?”

“No.”

“Why isn’t anybody else looking?”

“They’re all at Grace Lake, waiting and hoping.”

Well, Maggie and I spent a little time in the parking lot overlooking Grace Lake from the southwest side. There were gulls: Herrings, Ring-bills and Lesser Black-backs, as well as some Canadas, Mallards and Common Mergs, but no falcon, just distant birders standing with their scopes on the east side of the lake.

A falcon of the tundra, one that perches on the ground or on low human-made objects, needs extensive unobstructed views, a place with wide open spaces, low-cut grass. So we went to the airport.

It was about 3:20 PM. We couldn’t ask for better timing. On the airport’s south side, we immediately drove up to a juvenile Gyrfalcon, a brown bird, perched on the snow not more than 50-60 feet from the road. Though the direction of light was almost just right, photography was not ideal. The falcon was on the other side of the airport’s chain-linked fence. Nevertheless, my camera knew what it had to do.

Seemingly indifferent to us, the Gyr was leaning over, using its beak to clean its toes, followed by facial combing with its talons. Afterwards it gazed in all directions as though seeking something, perhaps out of hunger. Then lifting its wings, it took to the air, keeping just a few feet above the ground and was quickly lost in the airport’s distant expanse of snow shadow and glare--my fourth Gyr in southeast Michigan, my ninth in the State as of today, 16 November 2019.

Alan

Tom J. Cade (1928-2019, a world renowned conservationist and co-founder of the Peregrine Fund, had this to say: “In the old literature naturalists wrote about white, grey and black ‘color phases’ of the gyrfalcon and even different species of gyrs. In fact, the different plumage types grade imperceptibly into one another, with every kind of intermediate condition represented in different individuals. . . . The Ungava region of northern Quebec is especially interesting as the whitest and blackest varieties breed together in the same area along with every kind of grey intermediate. (p. 76, The Falcons of the World, 1980).”

Eugene Potapov, assistant professor, Bryn Athyn College, is a raptor specialist and the notable author of The Gyrfalcon 2005, a definitive work: “Cade et al quite rightly state that . . . the Gyrfalcon has complete gradation rendering the term ‘morph’ inappropriate (p. 23).”

“Gyrfalcons also have shades of brown and gray in their feathers, and worn plumage may be tan-brown; Gyrs may or may not have a barred tail and moustachial stripes (p. 47).

“. . . some authors classify the birds on the basis of their background color (Cade et al. 1998). Gray form can then be a bird with gray color in the background or bird with a white background but with a lot of dark gray or brown streaks, spots or bars. The degree of the coverage of these spots can then divide the white and gray morphs. As a consequence, it is often difficult to classify Gyrs with excessive numbers or spots and a true white background ( p. 47)

“. . . Palmer (1988) considered that the division of the Gyrfalcons ‘into two or three color morphs . . . is misleading, and ‘any attempt to categorize Gyrs is subjective’, ‘because of variations from nearly (entirely?) white to almost or entirely black. Flann (2003) suggested that the Gyrfalcon has ‘continuous polymorphism’ and so does not have morphs (p.47).

“Another process is the coloration of the background, which may perhaps be independent of, but is parallel with, the variation in coloration and size of dark spots. So, . . . we have two axes of variation in coloration. One is the color as such, including both the color of the background and the color of dark spots. The second axis is the size and pattern of the dark/light spots. Interestingly, there have been no attempts to analyze this two-dimensional variation using objective criteria. In the following section we make an attempt to measure Gyrfalcon colors using a new approach (p. 47).”

To those who wish to pursue this new approach to the color patterns of the Gyrfalcon, I suggest read Potapov’s book.

www.globalraptors.org/grin/ResearcherResults.asp?lresID=412

Les Sources Occultes 008/999

Un film de Laurent Courau, d'après un scénario de Thierry Ehrmann.

Un hommage à Norman Spinrad

Comédienne : Élora Bessey

Effets pyrotechniques : Thierry Loir

Images, textes et montage : Laurent Courau

Photographe de plateau : Kurt Ehrmann

Bande-son originale : Cheerleader 69

Remerciements à Jolan Bessey, Carine Dubois, Rodolphe Bessey et Vincent Kindred Véhixe.

© Les Amis de l'Esprit de la Salamandre 1999

Entre effroi et merveilles, une zone mouvante aux portes du futur et des enfers...

Les Sources Occultes vous entraînent au coeur d'un univers polymorphe dont les clés et les motifs se révéleront au fur et à mesure des épisodes de cette série de fictions. En attendant un final apocalyptique, au sens premier du terme, qui révélera la structure générale sous la forme d'un long-métrage...

Les Sources Occultes offrent aussi une nouvelle porte d'entrée dans le labyrinthe multidimensionnel de la Demeure du Chaos à celles et ceux qui postulent à notre casting, une occasion unique de pénétrer les arcanes de l'esprit de la Salamandre.

Secrets revealed of the Abode of Chaos (112 pages, adult only) >>>

Faceted diamonds - "Cumulus" brooch with 8 carat diamond at top. (public display, Field Museum of Natural History, Chicago, Illinois, USA)

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5200 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

Elements are fundamental substances of matter - matter that is composed of the same types of atoms. At present, 118 elements are known (four of them are still unnamed). Of these, 98 occur naturally on Earth (hydrogen to californium). Most of these occur in rocks & minerals, although some occur in very small, trace amounts. Only some elements occur in their native elemental state as minerals.

To find a native element in nature, it must be relatively non-reactive and there must be some concentration process. Metallic, semimetallic (metalloid), and nonmetallic elements are known in their native state.

The element carbon occurs principally in its native state as graphite (C) and diamond (C). Graphite is the common & far less valuable polymorph of carbon. A scarce polymorph of carbon is diamond. The physical properties of diamond and graphite couldn’t be more different, considering they have the same chemistry. Diamond has a nonmetallic, adamantine luster, typically occurs in cubic or octahedral (double-pyramid) crystals, or subspherical to irregularly-shaped masses, and is extremely hard (H≡10). Diamonds can be almost any color, but are typically clearish, grayish, or yellowish. Many diamonds are noticeably fluorescent under black light (ultraviolet light), but the color and intensity of fluorescence varies. Some diamonds are phosphorescent - under certain conditions, they glow for a short interval on their own.

Very rarely, diamond is a rock-forming mineral (see diamondite - www.flickr.com/photos/jsjgeology/14618393527).

Pyrite concretion in shale from the Pennsylvanian of Illinois, USA. (public display, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania, USA)

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5500 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

The sulfide minerals contain one or more sulfide anions (S-2). The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals. Many sulfides are economically significant, as they occur commonly in ores. The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc. Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size. These minerals will not form in the presence of free oxygen. Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals.

Pyrite is a common iron sulfide mineral (FeS2). It’s nickname is “fool's gold”. Pyrite has a metallic luster, brassy gold color (in contrast to the deep rich yellow gold color of true gold - www.flickr.com/photos/jsjgeology/sets/72157651325153769/), dark gray to black streak, is hard (H=6 to 6.5), has no cleavage, and is moderately heavy for its size. It often forms cubic crystals or pyritohedrons (crystals having pentagonal faces).

Pyrite is common in many hydrothermal veins, shales, coals, various metamorphic rocks, and massive sulfide deposits.

The pyrite specimen shown above is a "pyrite sun" - a discoidal concretion developed along a bedding plane in black shale. Texturally, the concretion has outward-radiating crystals with moderately-developed concentricity. Mineralogically, pyrite suns are principally composed of pyrite, plus minor marcasite (also FeS2 - iron sulfide; marcasite is a polymorph of pyrite).

Stratigraphy: Anna Shale (= roof shale of the Herrin Coal), upper Carbondale Formation, Desmoinesian Series, upper Middle Pennsylvanian

Locality: coal mine near Sparta, Randolph County, southwestern Illinois, USA

------------------------

Photo gallery of pyrite:

www.mindat.org/gallery.php?min=3314

As borboletas são insectos da ordem Lepidoptera classificados nas super-famílias Hesperioidea e Papilionoidea, que constituem o grupo informal Rhopalocera.

As borboletas têm dois pares de asas membranosas cobertas de escamas e peças bucais adaptadas a sucção. Distinguem-se das traças (mariposas) pelas antenas rectilíneas que terminam numa bola, pelos hábitos de vida diurnos, pela metamorfose que decorre dentro de uma crisálida rígida e pelo abdómen fino e alongado. Quando em repouso, as borboletas dobram as suas asas para cima.

As borboletas são importantes polinizadores de diversas espécies de plantas.

O ciclo de vida das borboletas engloba as seguintes etapas:

1) ovo→ fase pré-larval

2) larva→ chamada também de lagarta ou taturana,

3) pupa→ que se desenvolve dentro da crisálida (ou casulo)

4) imago→ fase adulta

_______________________

A butterfly is any of several groups of mainly day-flying insects of the order Lepidoptera, the butterflies and moths. Like other holometabolous insects, butterflies' life cycle consists of four parts, egg, larva, pupa and adult. Most species are diurnal. Butterflies have large, often brightly coloured wings, and conspicuous, fluttering flight. Butterflies comprise the true butterflies (superfamily Papilionoidea), the skippers (superfamily Hesperioidea) and the moth-butterflies (superfamily Hedyloidea). All the many other families within the Lepidoptera are referred to as moths.

Butterflies exhibit polymorphism, mimicry and aposematism. Some, like the Monarch, will migrate over long distances. Some butterflies have evolved symbiotic and parasitic relationships with social insects such as ants. Butterflies are important economically as agents of pollination. The caterpillars of some butterflies eat harmful insects. A few species are pests because in their larval stages they can damage domestic crops or trees. Culturally, butterflies are a popular motif in the visual and literary arts.

The Hominidae, whose members are known as the great apes or hominids, are a taxonomic family of primates that includes eight extant species in four genera: Pongo (the Bornean, Sumatran and Tapanuli orangutan); Gorilla (the eastern and western gorilla); Pan (the chimpanzee and the bonobo); and Homo, of which only modern humans (Homo sapiens) remain.

Numerous revisions in classifying the great apes have caused the use of the term hominid to change over time. The original meaning of "hominid" referred only to humans (Homo) and their closest extinct relatives. However, by the 1990s humans, apes, and their ancestors were considered to be "hominids".

The earlier restrictive meaning has now been largely assumed by the term hominin, which comprises all members of the human clade after the split from the chimpanzees (Pan). The current meaning of "hominid" includes all the great apes including humans. Usage still varies, however, and some scientists and laypersons still use "hominid" in the original restrictive sense; the scholarly literature generally shows the traditional usage until the turn of the 21st century.

Within the taxon Hominidae, a number of extant and extinct genera are grouped with the humans, chimpanzees, and gorillas in the subfamily Homininae; others with orangutans in the subfamily Ponginae (see classification graphic below). The most recent common ancestor of all Hominidae lived roughly 14 million years ago, when the ancestors of the orangutans speciated from the ancestral line of the other three genera. Those ancestors of the family Hominidae had already speciated from the family Hylobatidae (the gibbons), perhaps 15 to 20 million years ago.

Due to the close genetic relationship between humans and the other great apes, certain animal rights organizations, such as the Great Ape Project, argue that nonhuman great apes are persons and should be given basic human rights. Twenty-nine countries have instituted research bans to protect great apes from any kind of scientific testing.

Evolution

See also: Human evolution

Sumatran orangutan (Pongo abelii)

In the early Miocene, about 22 million years ago, there were many species of arboreally adapted primitive catarrhines from East Africa; the variety suggests a long history of prior diversification. Fossils from 20 million years ago include fragments attributed to Victoriapithecus, the earliest Old World monkey. Among the genera thought to be in the ape lineage leading up to 13 million years ago are Proconsul, Rangwapithecus, Dendropithecus, Limnopithecus, Nacholapithecus, Equatorius, Nyanzapithecus, Afropithecus, Heliopithecus, and Kenyapithecus, all from East Africa.

At sites far distant from East Africa, the presence of other generalized non-cercopithecids, that is, non-monkey primates, of middle Miocene age—Otavipithecus from cave deposits in Namibia, and Pierolapithecus and Dryopithecus from France, Spain and Austria—is further evidence of a wide diversity of ancestral ape forms across Africa and the Mediterranean basin during the relatively warm and equable climatic regimes of the early and middle Miocene. The most recent of these far-flung Miocene apes (hominoids) is Oreopithecus, from the fossil-rich coal beds in northern Italy and dated to 9 million years ago.

Molecular evidence indicates that the lineage of gibbons (family Hylobatidae), the "lesser apes", diverged from that of the great apes some 18–12 million years ago, and that of orangutans (subfamily Ponginae) diverged from the other great apes at about 12 million years. There are no fossils that clearly document the ancestry of gibbons, which may have originated in a still-unknown South East Asian hominoid population; but fossil proto-orangutans, dated to around 10 million years ago, may be represented by Sivapithecus from India and Griphopithecus from Turkey. Species close to the last common ancestor of gorillas, chimpanzees and humans may be represented by Nakalipithecus fossils found in Kenya and Ouranopithecus fossils found in Greece. Molecular evidence suggests that between 8 and 4 million years ago, first the gorillas (genus Gorilla), and then the chimpanzees (genus Pan) split off from the line leading to humans. Human DNA is approximately 98.4% identical to that of chimpanzees when comparing single nucleotide polymorphisms (see human evolutionary genetics). The fossil record, however, of gorillas and chimpanzees is limited; both poor preservation—rain forest soils tend to be acidic and dissolve bone—and sampling bias probably contribute most to this problem.

Other hominins probably adapted to the drier environments outside the African equatorial belt; and there they encountered antelope, hyenas, elephants and other forms becoming adapted to surviving in the East African savannas, particularly the regions of the Sahel and the Serengeti. The wet equatorial belt contracted after about 8 million years ago, and there is very little fossil evidence for the divergence of the hominin lineage from that of gorillas and chimpanzees—which split was thought to have occurred around that time. The earliest fossils argued by some to belong to the human lineage are Sahelanthropus tchadensis (7 Ma) and Orrorin tugenensis (6 Ma), followed by Ardipithecus (5.5–4.4 Ma), with species Ar. kadabba and Ar. ramidus.

Taxonomy

Further information: Human taxonomy

Terminology

Humans are one of the four extant hominid genera.

The classification of the great apes has been revised several times in the last few decades; these revisions have led to a varied use of the word "hominid" over time. The original meaning of the term referred to only humans and their closest relatives—what is now the modern meaning of the term "hominin". The meaning of the taxon Hominidae changed gradually, leading to a modern usage of "hominid" that includes all the great apes including humans.

A number of very similar words apply to related classifications:

A hominoid, sometimes called an ape, is a member of the superfamily Hominoidea: extant members are the gibbons (lesser apes, family Hylobatidae) and the hominids.

A hominid is a member of the family Hominidae, the great apes: orangutans, gorillas, chimpanzees and humans.

A hominine is a member of the subfamily Homininae: gorillas, chimpanzees, and humans (excludes orangutans).

A hominin is a member of the tribe Hominini: chimpanzees and humans.

A homininan, following a suggestion by Wood and Richmond (2000), would be a member of the subtribe Hominina of the tribe Hominini: that is, modern humans and their closest relatives, including Australopithecina, but excluding chimpanzees.

A human is a member of the genus Homo, of which Homo sapiens is the only extant species, and within that Homo sapiens sapiens is the only surviving subspecies.

Extant and fossil relatives of humans

Hominidae was originally the name given to the family of humans and their (extinct) close relatives, with the other great apes (that is, the orangutans, gorillas and chimpanzees) all being placed in a separate family, the Pongidae. However, that definition eventually made Pongidae paraphyletic because at least one great ape species (the chimpanzees) proved to be more closely related to humans than to other great apes. Most taxonomists today encourage monophyletic groups—this would require, in this case, the use of Pongidae to be restricted to just one closely related grouping. Thus, many biologists now assign Pongo (as the subfamily Ponginae) to the family Hominidae. The taxonomy shown here follows the monophyletic groupings according to the modern understanding of human and great ape relationships.

Humans and close relatives including the tribes Hominini and Gorillini form the subfamily Homininae (see classification graphic below). (A few researchers go so far as to refer the chimpanzees and the gorillas to the genus Homo along with humans.) But, those fossil relatives more closely related to humans than the chimpanzees represent the especially close members of the human family, and without necessarily assigning subfamily or tribal categories.

Many extinct hominids have been studied to help understand the relationship between modern humans and the other extant hominids. Some of the extinct members of this family include Gigantopithecus, Orrorin, Ardipithecus, Kenyanthropus, and the australopithecines Australopithecus and Paranthropus.

The exact criteria for membership in the tribe Hominini under the current understanding of human origins are not clear, but the taxon generally includes those species that share more than 97% of their DNA with the modern human genome, and exhibit a capacity for language or for simple cultures beyond their 'local family' or band. The theory of mind concept—including such faculties as empathy, attribution of mental state, and even empathetic deception—is a controversial criterion; it distinguishes the adult human alone among the hominids. Humans acquire this capacity after about four years of age, whereas it has not been proven (nor has it been disproven) that gorillas or chimpanzees ever develop a theory of mind. This is also the case for some New World monkeys outside the family of great apes, as, for example, the capuchin monkeys.

However, even without the ability to test whether early members of the Hominini (such as Homo erectus, Homo neanderthalensis, or even the australopithecines) had a theory of mind, it is difficult to ignore similarities seen in their living cousins. Orangutans have shown the development of culture comparable to that of chimpanzees, and some say the orangutan may also satisfy those criteria for the theory of mind concept. These scientific debates take on political significance for advocates of great ape personhood.

See also: List of hominoids

There are eight living species of great ape which are classified in four genera. The following classification is commonly accepted:

Family Hominidae: humans and other great apes; extinct genera and species excluded

Subfamily Ponginae

Tribe Pongini

Genus Pongo

Bornean orangutan, Pongo pygmaeus

Pongo pygmaeus pygmaeus

Pongo pygmaeus morio

Pongo pygmaeus wurmbii

Sumatran orangutan, Pongo abelii

Tapanuli orangutan, Pongo tapanuliensis

Subfamily Homininae

Tribe Gorillini

Genus Gorilla

Western gorilla, Gorilla gorilla

Western lowland gorilla, Gorilla gorilla gorilla

Cross River gorilla, Gorilla gorilla diehli

Eastern gorilla, Gorilla beringei

Mountain gorilla, Gorilla beringei beringei

Eastern lowland gorilla, Gorilla beringei graueri

Tribe Hominini

Subtribe Panina

Genus Pan

Chimpanzee, Pan troglodytes

Central chimpanzee, Pan troglodytes troglodytes

Western chimpanzee, Pan troglodytes verus

Nigeria-Cameroon chimpanzee, Pan troglodytes ellioti

Eastern chimpanzee, Pan troglodytes schweinfurthii

Bonobo, Pan paniscus

Subtribe Hominina

Genus Homo

Human, Homo sapiens

Anatomically modern human, Homo sapiens sapiens

Fossil

In addition to the extant species and subspecies, archaeologists, paleontologists, and anthropologists have discovered and classified numerous extinct great ape species as below, based on the taxonomy shown.

Tribe Lufengpithecini †

Lufengpithecus

Lufengpithecus lufengensis

Lufengpithecus keiyuanensis

Lufengpithecus hudienensis

Meganthropus

Meganthropus palaeojavanicus

Tribe Sivapithecini†

Ankarapithecus

Ankarapithecus meteai

Sivapithecus

Sivapithecus brevirostris

Sivapithecus punjabicus

Sivapithecus parvada

Sivapithecus sivalensis

Sivapithecus indicus

Gigantopithecus

Gigantopithecus bilaspurensis

Gigantopithecus blacki

Gigantopithecus giganteus

Tribe Pongini

Khoratpithecus†

Khoratpithecus ayeyarwadyensis

Khoratpithecus piriyai

Khoratpithecus chiangmuanensis

Pongo (orangutans)

Pongo hooijeri†

Subfamily Homininae

Tribe Dryopithecini †

Kenyapithecus

Kenyapithecus wickeri

Danuvius

Danuvius guggenmosi

Pierolapithecus

Pierolapithecus catalaunicus

Udabnopithecus

Udabnopithecus garedziensis

Ouranopithecus

Ouranopithecus macedoniensis

Otavipithecus

Otavipithecus namibiensis

Morotopithecus (placement disputed)

Morotopithecus bishopi

Oreopithecus (placement disputed)

Oreopithecus bambolii

Nakalipithecus

Nakalipithecus nakayamai

Anoiapithecus

Anoiapithecus brevirostris

Hispanopithecus

Hispanopithecus laietanus

Hispanopithecus crusafonti

Dryopithecus

Dryopithecus wuduensis

Dryopithecus fontani

Dryopithecus brancoi

Dryopithecus laietanus

Dryopithecus crusafonti

Rudapithecus

Rudapithecus hungaricus

Samburupithecus

Samburupithecus kiptalami

Tribe Gorillini

Chororapithecus † (placement debated)

Chororapithecus abyssinicus

Tribe Hominini

Subtribe Panina

Subtribe Hominina

Graecopithecus †

Graecopithecus freybergi

Sahelanthropus†

Sahelanthropus tchadensis

Orrorin†

Orrorin tugenensis

Ardipithecus†

Ardipithecus ramidus

Ardipithecus kadabba

Kenyanthropus†

Kenyanthropus platyops

Praeanthropus†

Praeanthropus bahrelghazali

Praeanthropus anamensis

Praeanthropus afarensis

Australopithecus†

Australopithecus africanus

Australopithecus garhi

Australopithecus sediba

Australopithecus deyiremeda

Paranthropus†

Paranthropus aethiopicus

Paranthropus robustus

Paranthropus boisei

Homo – close relatives of modern humans

Homo gautengensis† (also classified as H. habilis)

Homo rudolfensis† (membership in Homo uncertain)

Homo habilis† (membership in Homo uncertain)

Homo naledi†

Dmanisi Man, Homo georgicus† (thought by some to be an early subspecies of Homo erectus)

Homo ergaster† (considered by some to be an early subspecies of Homo erectus)

Homo erectus†

Homo erectus bilzingslebenensis †

Java Man, Homo erectus erectus †

Lantian Man, Homo erectus lantianensis †

Nanjing Man, Homo erectus nankinensis †

Peking Man, Homo erectus pekinensis †

Solo Man, Homo erectus soloensis †

Tautavel Man, Homo erectus tautavelensis †

Yuanmou Man, Homo erectus yuanmouensis †

Flores Man or Hobbit, Homo floresiensis†

Homo luzonensis †

Homo antecessor† (thought by some to be a late H. erectus or early H. heidelbergensis)

Homo heidelbergensis† (also classified as H. sapiens heidelbergensis)

Homo cepranensis† (also classified as H. heidelbergensis)

Homo helmei† (also classified as late H. heidelbergensis or early H. sapiens)

Homo tsaichangensis† (thought by some to be a subspecies of H. erectus or a Denisovan)

Denisovans (scientific name not yet assigned)†

Neanderthal, Homo neanderthalensis† (sometimes called Homo sapiens neanderthalensis)

Homo rhodesiensis† (thought by some to be an African subspecies of H. heidelbergensis or an early H. sapiens)

Modern human, Homo sapiens (sometimes called Homo sapiens sapiens)

Homo sapiens idaltu†

Archaic Homo sapiens†

Description

The great apes are tailless primates, with the smallest living species being the bonobo at 30 to 40 kilograms (66 to 88 lb) in weight, and the largest being the eastern gorillas, with males weighing 140 to 180 kilograms (310 to 400 lb). In all great apes, the males are, on average, larger and stronger than the females, although the degree of sexual dimorphism varies greatly among species. Hominid teeth are similar to those of the Old World monkeys and gibbons, although they are especially large in gorillas. The dental formula is

2.1.2.3

2.1.2.3

. Human teeth and jaws are markedly smaller for their size than those of other apes, which may be an adaptation to not only having supplanted with extensive tool use the role of jaws in hunting and fighting, but also eating cooked food since the end of the Pleistocene.

Behavior

Although most living species are predominantly quadrupedal, they are all able to use their hands for gathering food or nesting materials, and, in some cases, for tool use. They build complex sleeping platforms, also called nests, in trees to sleep in at night, but chimpanzees and gorillas also build terrestrial nests, and gorillas can also sleep on the bare ground.

All species are omnivorous, although chimpanzees and orangutans primarily eat fruit. When gorillas run short of fruit at certain times of the year or in certain regions, they resort to eating shoots and leaves, often of bamboo, a type of grass. Gorillas have extreme adaptations for chewing and digesting such low-quality forage, but they still prefer fruit when it is available, often going miles out of their way to find especially preferred fruits. Humans, since the Neolithic revolution, have consumed mostly cereals and other starchy foods, including increasingly highly processed foods, as well as many other domesticated plants (including fruits) and meat.

Gestation in great apes lasts 8–9 months, and results in the birth of a single offspring, or, rarely, twins. The young are born helpless, and require care for long periods of time. Compared with most other mammals, great apes have a remarkably long adolescence, not being weaned for several years, and not becoming fully mature for eight to thirteen years in most species (longer in orangutans and humans). As a result, females typically give birth only once every few years. There is no distinct breeding season.

Gorillas and chimpanzees live in family groups of around five to ten individuals, although much larger groups are sometimes noted. Chimpanzees live in larger groups that break up into smaller groups when fruit becomes less available. When small groups of female chimpanzees go off in separate directions to forage for fruit, the dominant males can no longer control them and the females often mate with other subordinate males. In contrast, groups of gorillas stay together regardless of the availability of fruit. When fruit is hard to find, they resort to eating leaves and shoots.

This fact is related to gorillas' greater sexual dimorphism relative to that of chimpanzees; that is, the difference in size between male and female gorillas is much greater than that between male and female chimpanzees. This enables gorilla males to physically dominate female gorillas more easily. In both chimpanzees and gorillas, the groups include at least one dominant male, and young males leave the group at maturity.

Legal status

Main articles: Great ape personhood, Great Ape Project, and Countries banning non-human ape experimentation

Due to the close genetic relationship between humans and the other great apes, certain animal rights organizations, such as the Great Ape Project, argue that nonhuman great apes are persons and, per the Declaration on Great Apes, should be given basic human rights. In 1999, New Zealand was the first country to ban any great ape experimentation, and now 29 countries have currently instituted a research ban to protect great apes from any kind of scientific testing.

On 25 June 2008, the Spanish parliament supported a new law that would make "keeping apes for circuses, television commercials or filming" illegal. On 8 September 2010, the European Union banned the testing of great apes.

Common guillemot (Uria aalge) on Lunga, Treshnish Isles. The white ring around the eye extending back as a white line is a polymorphism.

The swivel base is made with the headset of an old kiddies bike from a dumpster The handlebar post happens to be the right size to take a saddle frame (stripped of the upper). This gives the chair a fair bit of springiness. Unfortunately it is impractical to use the saddle tilt mechanism, as it has to be adjusted with a spanner, and pulled really tight. This would strip the serrated washers in no time, and is hard work and inconvenient. Nevertheless, the tilt mech does at least allow for some tilt, even if fixed.

The headset has a collar of Polymorph to fit snuggly into the conical hole of the chair base.

The whole assembly allows for normal swivel, and is also height adjustable (albeit with an allan key, awkwardly). The reason I did not use the gas lift base of the office chair was that it would not go low enough to allow for the extra padding of the seat and allow my feet to sit flat on the ground.

A lovely white version of Thysanotus arenarius

This image was taken during my trip in January 2012 to Mono Lake in California.

The subject in the foreground is called Tufa, which incase you're wondering to yourself "What the hell is Tufa?", here comes the school bit...

Tufa columns are an unusual form of tufa typically associated with saline lakes. They are distinct from most tufa deposits in that they lack any significant macrophyte component - this is due to the salinity excluding mesophilic organisms. Some tufa columns may actually form from hot-springs and therefore actually be a form of travertine. It is generally thought that such features form from CaCO3 precipitated when carbonate rich source waters emerge into alkaline soda lakes.

Modern tufa is formed from supersaturated alkaline waters, with raised pCO2. On emergence, waters degas CO2 due to the lower atmospheric pCO2, resulting in an increase in pH. Since carbonate solubility decreases with increased pH, precipitation is induced. Supersaturation may be enhanced by factors leading to a reduction in pCO2, for example increased air-water interactions at waterfalls may be important, as may photosynthesis.

Calcite is the dominant mineral precipitate found, however the polymorph aragonite is also found in the columns.

Got it? OK, quick version - it's a type of limestone which grows in super salty water, such as Mono Lake has :)

Marcasite from Shullsburg, Wisconsin, USA. (public display, Seaman Mineral Museum, Michigan Technological University, Houghton, Michigan, USA)

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 6000 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

The sulfide minerals contain one or more sulfide anions (S-2). The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals. Many sulfides are economically significant, as they occur commonly in ores. The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc. Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size. These minerals will not form in the presence of free oxygen. Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals.

Marcasite is an iron sulfide mineral, FeS2, which is the same chemical formula as pyrite. Different minerals having the same chemical formula are called polymorphs. Other examples of polymorphs are graphite-diamond (both C) and calcite-aragonite (both CaCO3). Pyrite and marcasite both have a metallic luster, a brassy gold color, and a dark gray to black streak. They both lack cleavage, and they have the same hardness (H = 6 to 6.5). Marcasite tends to have a paler brass color than pyrite. Some marcasites are almost silvery-colored.

How does one visually distinguish marcasite from pyrite? Apart from color, marcasite crystals are typically plates, or sharp & pointed, and marcasite tends to twin, resulting in cockscomb masses (www.mindat.org/photo-408969.html). Marcasite also more readily breaks down into whitish powder (FeSO4).

Pyrite can convert to marcasite naturally, and vice versa. Pyrite concretions may have preserved needle-shaped crystals of marcasite, but the marcasite is gone. X-ray analysis may be needed to determine which polymorph is present.

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Photo gallery of marcasite:

www.mindat.org/gallery.php?min=2571

Green orthoclase feldspar (field of view ~9 centimeters across) from Southern Cross, ~11-12 km N of the city of Broken Hill, Broken Hill Block, far-western New South Wales, southeastern Australia.

--------------

Greenish-colored potassium feldspar is uncommon, but specimens are readily available in the mineral trade. The traditional variety of green feldspar is amazonite, a greenish microcline feldspar. Green orthoclase feldspar is exceedingly rare, and is known from few localities on Earth. Some may be tempted to call this stuff amazonite, but it isn’t. Amazonite only refers to (it’s supposed to refer to) green microcline. Orthoclase feldspar is KAlSi3O8 (potassium aluminosilicate), an abundant rock-forming mineral and a polymorph of microcline (also KAlSi3O8). Published chemical analysis indicates that the green coloration is due to lead impurity.

Here’s a large mass of Precambrian-aged green orthoclase feldspar, from what is traditionally the only known occurrence in the world. This is from the Broken Hill Block of western New South Wales in Australia.

Faceted diamonds - "Cumulus" brooch with 8 carat diamond at top. (public display, Field Museum of Natural History, Chicago, Illinois, USA)

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5200 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

Elements are fundamental substances of matter - matter that is composed of the same types of atoms. At present, 118 elements are known (four of them are still unnamed). Of these, 98 occur naturally on Earth (hydrogen to californium). Most of these occur in rocks & minerals, although some occur in very small, trace amounts. Only some elements occur in their native elemental state as minerals.

To find a native element in nature, it must be relatively non-reactive and there must be some concentration process. Metallic, semimetallic (metalloid), and nonmetallic elements are known in their native state.

The element carbon occurs principally in its native state as graphite (C) and diamond (C). Graphite is the common & far less valuable polymorph of carbon. A scarce polymorph of carbon is diamond. The physical properties of diamond and graphite couldn’t be more different, considering they have the same chemistry. Diamond has a nonmetallic, adamantine luster, typically occurs in cubic or octahedral (double-pyramid) crystals, or subspherical to irregularly-shaped masses, and is extremely hard (H≡10). Diamonds can be almost any color, but are typically clearish, grayish, or yellowish. Many diamonds are noticeably fluorescent under black light (ultraviolet light), but the color and intensity of fluorescence varies. Some diamonds are phosphorescent - under certain conditions, they glow for a short interval on their own.

Very rarely, diamond is a rock-forming mineral (see diamondite - www.flickr.com/photos/jsjgeology/14618393527).

These beautiful snails have common names such as banded, grove or brown-lipped snails and despite looking very different in colour, they are all members of the same species - Cepaea nemoralis - and this is known as polymorphism.

I was busy trimming the ivy and these were just some of the different morphs I saved as I went about the gardening!

Les Sources Occultes 008/999

Un film de Laurent Courau, d'après un scénario de Thierry Ehrmann.

Réalisation : Laurent Courau

Scénario : Thierry Ehrmann

Comédienne : Elora Bessey

Artificier : Thierry Loir

Remerciements à Jolan Bessey, Carine Dubois et Rodolphe Bessey.

© Les Amis de l'Esprit de la Salamandre 1999

Entre effroi et merveilles, une zone mouvante aux portes du futur et des enfers...

Les Sources Occultes vous entraînent au coeur d'un univers polymorphe dont les clés et les motifs se révéleront au fur et à mesure des épisodes de cette série de fictions. En attendant un final apocalyptique, au sens premier du terme, qui révélera la structure générale sous la forme d'un long-métrage...

Les Sources Occultes offrent aussi une nouvelle porte d'entrée dans le labyrinthe multidimensionnel de la Demeure du Chaos à celles et ceux qui postulent à notre casting, une occasion unique de pénétrer les arcanes de l'esprit de la Salamandre.

Secrets revealed of the Abode of Chaos (112 pages, adult only) >>>

(~2.7 centimeters across at its widest)

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Igneous rocks form by the cooling & crystallization of hot, molten rock (magma & lava). If this happens at or near the land surface, or on the seafloor, they are extrusive igneous rocks. If this happens deep underground, they are intrusive igneous rocks. Most igneous rocks have a crystalline texture, but some are clastic, vesicular, frothy, or glassy.

Obsidian is readily identifiable. It is a glassy-textured, extrusive igneous rock. Obsidian is natural glass - it lacks crystals, and therefore lacks minerals. Obsidian is typically black in color, but most obsidians have a felsic to intermediate chemistry. Felsic igneous rocks are generally light-colored, so a felsic obsidian seems a paradox. Mafic obsidians are scarce, but they are also black and glassy.

Obsidian is an uncommon rock, but can be examined at several famous localities in America, such as Obsidian Cliff at the Yellowstone Hotspot (northwestern Wyoming, USA) and Big Obsidian Flow at the Newberry Volcano (central Oregon, USA).

Obsidian is moderately hard and has a conchoidal fracture (smooth and curved fracture surface), with sharp broken edges. Freshly-broken obsidian has the sharpest edges of any material known, natural or man-made (as seen under a scanning electron microscope).

Obsidian forms two ways: 1) very rapid cooling of lava, which prevents the formation of crystals; 2) cooling of high-viscosity lava, which prevents easy movement of atoms to form crystals. An example of obsidian that formed the first way is along the margins of basaltic lava flows at Kilaeua Volcano (Hawaii Hotspot, central Pacific Ocean). The obsidian sample seen here formed the second way.

Obsidian is unstable on geologic time scales - it will slowly convert to material that is not obsidian. A partially-converted obsidian is a distinctive rock called snowflake obsidian. The black portions of the rock seen here are rhyolitic obsidian (glass). The white patches ("snowflakes") are devitrification spots composed of cristobalite (SiO2, a polymorph of quartz).

Faceted diamond, illuminated by four light sources. (5.5 mm across at its widest; 0.75 carats)

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5200 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

Elements are fundamental substances of matter - matter that is composed of the same types of atoms. At present, 118 elements are known (four of them are still unnamed). Of these, 98 occur naturally on Earth (hydrogen to californium). Most of these occur in rocks & minerals, although some occur in very small, trace amounts. Only some elements occur in their native elemental state as minerals.

To find a native element in nature, it must be relatively non-reactive and there must be some concentration process. Metallic, semimetallic (metalloid), and nonmetallic elements are known in their native state.

The element carbon occurs principally in its native state as graphite (C) and diamond (C). Graphite is the common & far less valuable polymorph of carbon. A scarce polymorph of carbon is diamond. The physical properties of diamond and graphite couldn’t be more different, considering they have the same chemistry. Diamond has a nonmetallic, adamantine luster, typically occurs in cubic or octahedral (double-pyramid) crystals, or subspherical to irregularly-shaped masses, and is extremely hard (H≡10). Diamonds can be almost any color, but are typically clearish, grayish, or yellowish. Many diamonds are noticeably fluorescent under black light (ultraviolet light), but the color and intensity of fluorescence varies. Some diamonds are phosphorescent - under certain conditions, they glow for a short interval on their own.

Very rarely, diamond is a rock-forming mineral (see diamondite - www.flickr.com/photos/jsjgeology/14618393527).

Pseudomorphs are minerals that have replaced other minerals, while retaining the crystal shape of the original mineral.

The tetraradiate crystalline structure seen here was originally marcasite (FeS2), a brassy gold-colored iron sulfide mineral that is a polymorph of pyrite. The marcasite was replaced by black-colored iron oxide. People disagree on what the iron oxide mineral is - I've seen it referred to as hematite, limonite, or goethite.

Geologic context: eroded from the Khoman Formation, Maastrichtian Stage, upper Upper Cretaceous

Locality: unrecorded / undisclosed site in the White Desert, supposedly near Farafra Oasis, western Egypt

Graphite-pyroxene-scapolite skarn from New York State, USA. (3.4 centimeters across at its foreground widest)

This is a polymineralic, coaresely-crystalline textured, contact metamorphic rock - a skarn. It occurs in the contact zone between a limestone and a pegmatitic granite. Three minerals are present: 1) dark green-colored augite pyroxene; 2) whitish-gray colored meionite scapolite; and 3) silvery-gray graphite.

Meionite scapolite is a feldspathoid mineral, Ca4Al6Si6O24CO3 - calcium aluminosilicate-carbonate. It fluoresces a dull red color under ultraviolet light (UV light; black light).

Graphite is carbon (C), which is one of two widespread polymorphs of carbon (the other is diamond). This rock comes from a graphite mine in New York State - graphite occurs there are relatively rich "veins" along the contact metamorphic zone between the limestone and the granite. The graphite content of the rock shown here is too low to be a graphite ore. Graphite has a silvery-gray color and streak, a metallic luster, a greasy feel, and a hardness of 1 (it is very soft).

This sample is consistent with the "pyroxene contact rock with graphite" of Alling (1917).

Age: Proterozoic ?

Locality: unrecorded pit/working at Chilson Hill Mines (= Lead Hill Mines), likely from the southern or southeastern sides of Lead Hill (Chilson Hill), north of Chilson Brook, ~2.75 air miles east-southeast of the town of Chilson & ~2.75 air miles west-northwest of the town of Ticonderoga, southeastern Essex County, eastern Adirondack Mountains, northeastern New York State, USA

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Lead Hill Mines references:

Alling (1917) - Lead Hill. pp. 23-31 in The Adirondack graphite deposits. New York State Museum Bulletin 199.

Lauf & Pasto (1983) - Graphite from the Lead Hill Mine, Ticonderoga, New York. Mineralogical Record 14: 25-30.

Note: We would love to know how you are re-using our graphics, especially if you are a teacher using them in the classroom. Send us an email: knowablemagazine AT annualreviews DOT org

There are millions of places in the human genome where a DNA letter can vary from one person to the next. These differences are known as SNPs (single nucleotide polymorphisms). Researchers are looking for SNPs linked to an elevated risk of breast cancer in order to help explain cases where breast cancer runs in families but no genetic cause is yet known. In this example, Person 1 has a SNP that has been linked to elevated breast cancer risk in population studies; the other two individuals have SNPs that are not.

An illustration depicting the millions of places in the human genome where a DNA letter can vary from one person to the next. These differences are known as SNPs (single nucleotide polymorphisms). Researchers are looking for SNPs linked to an elevated risk of breast cancer in order to help explain cases where breast cancer runs in families but no genetic cause is yet known.

Read more: "Unraveling breast cancer risk"

A text In English:

The Swallow-tailed Hummingbird, so called from its forked tail, is one of the largest hummingbirds in cities and gardens, but it also occurs in gallery forests, bushy pastures and edges of woods or coppices. It is green, except for the blue head and upper breast, turning to iridescent purple according to the direction of light; it has dark wings and a heavy black bill. The tail is dark blue with the external feathers longer than central ones. It is very aggressive and attacks other hummingbirds that dare to visit flowers in certain trees. Where the flowers are available for many months, the individual is fiercely territorial, but generally needs to search soon for other flowering plants. It flies to catch small insets on or under leaves in the gallery forests or woodlands. The female builds a small cup-shaped nest saddled on a branch, not far from the main trunk in the shade of leaves. Perched on favorite branches, the male can utter long but low chirps. Once in a while, it interrupts these singing sessions to feed, and flies back for more song or to clean the plumage. They occur from the Guianas and Amazon River to Paraguay and southeastern Peru. They can get along with partially deforested zones, but may disappear with intensive agriculture and with the development of treeless cities.

Um texto em Português:

Beija-flor Tesoura (Eupetomena macroura), fotografado em Brasília-DF, Brasil.

Eupetomena macroura (Gmelin, 1788): tesoura; swallow-tailed hummingbird c.

Destaca-se das espécies estudadas pelo maior porte e pela cauda comprida e bifurcada, o que lhe valeu o nome popular. Como é comum entre os beija-flores, é uma espécie agressiva que disputa com outras o seu território e fontes de alimento.

Nidificação: o ninho, em forma de tigela, é assentado numa forquilha de arbusto ou árvores, a cerca de 2 a 3 m do solo. O material utilizado na construção é composto por fibras vegetais incluindo painas, musgos e liquens, aderidos externamente com teias de aranhas.

Hábitat: capoeiras, cerrados, borda de matas e jardins.

Tamanho: 17,0 cm

A SEGUIR UM TEXTO ENCONTRADO E REPRODUZIDO DO ENDEREÇO nationalgeographic.abril.uol.com.br/ng/edicoes/83/reporta... DA NATIONAL GEOGRAFIC:

Prodígios da micro-engenharia, os beija-flores são os campeões dos pesos-leves entre as aves

Uma faísca safira, um frêmito de asas, e o minúsculo pássaro - ou seria um inseto? - some como miragem fugaz. Reaparece instantes depois, agora num ângulo melhor. É pássaro mesmo, um dervixe do tamanho do meu polegar com asas que batem 80 vertiginosas vezes por segundo, produzindo um zumbido quase inaudível. As penas da cauda, à guisa de leme, delicadamente direcionam o vôo em três direções. Ele fita a trombeta de uma vistosa flor alaranjada e do bico fino como agulha projeta uma língua delgada feito linha. Um raio de Sol ricocheteia de suas penas iridescentes. A cor refletida deslumbra como uma pedra preciosa contra uma janela ensolarada. Não admira que os beija-flores sejam tão queridos e que tanta gente já tenha tropeçado ao tentar descrevê-los. Nem mesmo circunspectos cientistas resistem a termos como "belo", "magnífico", "exótico".

Surpresa maior é o fato de o aparentemente frágil beija-flor ser uma das mais resistentes criaturas do reino animal. Cerca de 330 espécies prosperam em ambientes diversos, muitos deles brutais: do Alasca à Argentina, do deserto do Arizona à costa de Nova Scotia, da Amazônia à linha nevada acima dos 4,5 mil metros nos Andes (misteriosamente, essas aves só são encontradas no Novo Mundo).

"Eles vivem no limite do que é possível aos vertebrados, e com maestria", diz Karl Schuchmann, ornitólogo do Instituto Zoológico Alexander Koenig e do Fundo Brehm, na Alemanha. Schuchmann ouviu falar de um beija-flor que viveu 17 anos em cativeiro. "Imagine a resistência de um organismo de 5 ou 6 gramas para viver tanto tempo!", diz ele espantado. Em média, o minúsculo coração de um beija-flor bate cerca de 500 vezes por minuto (em repouso!). Assim, o desse pequeno cativo teria batido meio bilhão de vezes, quase o dobro do total de uma pessoa de 70 anos.

Mas esses passarinhos são duráveis apenas em vida. Quando morrem, seus ossos delicados e ocos quase nunca se fossilizam. Daí o assombro causado pela recente descoberta de um amontoado de fósseis de aves que talvez inclua um beija-flor ancestral de 30 milhões de anos. Como os beija-flores modernos, os espécimes fósseis tinham o bico longo e fino e os ossos superiores das asas mais curtos, terminando em uma saliência arredondada que talvez lhes permitisse fazer a rotação na articulação do ombro e parar no ar.

A outra surpresa foi o local do achado: no sul da Alemanha, longe do território dos beija-flores atuais. Para alguns cientistas, essa descoberta mostra que já existiram beija-flores fora das Américas, mas se extinguiram. Ou quem sabe os fósseis não fossem de beija-flor. Os céticos, entre eles Schuchmann, afirmam que muitas vezes, ao longo da evolução, outros grupos de aves adquiriram características semelhantes às do beija-flor. Os verdadeiros beija-flores, diz Schuchmann, evoluíram nas florestas do leste do Brasil, onde competiam com insetos pelo néctar das flores.

"O Brasil foi o laboratório do protótipo", diz o ornitólogo. "E o modelo funcionou." O beija-flor tornou-se a obra-prima da microengenharia da natureza. Aperfeiçoou sua habilidade de parar no ar há dezenas de milhões de anos para competir por parte das flores do Novo Mundo.

"Eles são uma ponte entre o mundo das aves e o dos insetos", diz Doug Altshuler, da Universidade da Califórnia em Riverside. Altshuler, que estuda o vôo dos beija-flores, examinou os movimentos das asas do pássaro. Observou que, nele, os impulsos elétricos propulsores dos músculos das asas lembram mais os dos insetos que os das aves. Talvez por isso o beija-flor produza tanta energia por batida de asas: mais, por unidade de massa, que qualquer outro vertebrado. Altshuler também analisou os trajetos neurais do beija-flor, que funcionam com a mesma vertiginosa velocidade encontrada nas aves mais ágeis, como seu primo mais próximo, o andorinhão. "São incríveis; uns pequenos Frankesteins", compara.

Certamente eles sabem intimidar: grama por grama, talvez sejam os maiores confrontadores da natureza. "O vocabulário do beija-flor deve ser 100% composto de palavrões", graceja Sheri Williamson, naturalista do Southeastern Arizona Bird Observatory. A agressão do beija-flor nasce de ferozes instintos territoriais moldados à necessidade de sugar néctar a cada poucos minutos. Os beija-flores competem desafiando e ameaçando uns aos outros. Postam-se face a face no ar, rodopiam, mergulham na direção da grama e voam de ré, em danças de dominância que terminam tão subitamente quanto começam.

O melhor lugar para vermos tais batalhas é nas montanhas, especialmente no Equador, em que ricos ecossistemas se apresentam em suas várias altitudes. Sheri supõe que o sentido norte-sul das cordilheiras americanas também crie rotas favoráveis à migração para onde haja constante suprimento de flores. O que contrasta, diz ela, com as barreiras naturais que se estendem de leste a oeste na África, como o Saara e o Mediterrâneo.

Algumas espécies de beija-flor, porém, adaptaram-se a atravessar vastidões planas, onde o alimento é escasso. Antes de sua intrépida migração da primavera para os Estados Unidos e o Canadá, os beija-flores-de-garganta-vermelha reúnem-se no México e empanturram-se de insetos e néctar. Armazenam gordura e duplicam de peso em uma semana. Em seguida, atravessam o golfo do México, voando 800 quilômetros sem escalas por 20 horas, até a costa distante.

A região próxima à linha do equador é um reino de beija-flores. Quem sai do aeroporto de Quito, no Equador, pode ser logo saudado por um cintilante beija-flor-violeta, com pintura de guerra de manchas púrpura iridescentes nos lados da face. A leste da cidade, nas cabeceiras da bacia Amazônica, o beija-flor-bico-de-espada esvoaça na mata portando o bico mais longo de todas as aves em proporção a seu tamanho: mais de metade do comprimento total do animal. Nas encostas do Cotopaxi, um vulcão ao sul de Quito, o beija-flor-do-chimborazo foi avistado acima dos 4,5 mil metros. Ali ele passa a noite entorpecido em cavernas, pois desacelera seu ritmo metabólico o suficiente para não morrer de fome antes de amanhecer. Mais tarde, aquecido pelo Sol, ele recomeça a se alimentar.

"Quem estuda beija-flores fica irremediavelmente enfeitiçado", diz Sheri Williamson. "São criaturinhas sedutoras. Tentei resistir, mas agora tenho sangue de beija-flor correndo nas veias."

Canon EOS 50D

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Ipê Amarelo, Tabebuia [chrysotricha or ochracea].

Text, in english, from Wikipedia, the free encyclopedia

"Trumpet tree" redirects here. This term is occasionally used for the Shield-leaved Pumpwood (Cecropia peltata).

Tabebuia

Flowering Araguaney or ipê-amarelo (Tabebuia chrysantha) in central Brazil

Scientific classification

Kingdom: Plantae

(unranked): Angiosperms

(unranked): Eudicots

(unranked): Asterids

Order: Lamiales

Family: Bignoniaceae

Tribe: Tecomeae

Genus: Tabebuia

Gomez

Species

Nearly 100.

Tabebuia is a neotropical genus of about 100 species in the tribe Tecomeae of the family Bignoniaceae. The species range from northern Mexico and the Antilles south to northern Argentina and central Venezuela, including the Caribbean islands of Hispaniola (Dominican Republic and Haiti) and Cuba. Well-known common names include Ipê, Poui, trumpet trees and pau d'arco.

They are large shrubs and trees growing to 5 to 50 m (16 to 160 ft.) tall depending on the species; many species are dry-season deciduous but some are evergreen. The leaves are opposite pairs, complex or palmately compound with 3–7 leaflets.

Tabebuia is a notable flowering tree. The flowers are 3 to 11 cm (1 to 4 in.) wide and are produced in dense clusters. They present a cupular calyx campanulate to tubular, truncate, bilabiate or 5-lobed. Corolla colors vary between species ranging from white, light pink, yellow, lavender, magenta, or red. The outside texture of the flower tube is either glabrous or pubescentThe fruit is a dehiscent pod, 10 to 50 cm (4 to 20 in.) long, containing numerous—in some species winged—seeds. These pods often remain on the tree through dry season until the beginning of the rainy.

Species in this genus are important as timber trees. The wood is used for furniture, decking, and other outdoor uses. It is increasingly popular as a decking material due to its insect resistance and durability. By 2007, FSC-certified ipê wood had become readily available on the market, although certificates are occasionally forged.

Tabebuia is widely used as ornamental tree in the tropics in landscaping gardens, public squares, and boulevards due to its impressive and colorful flowering. Many flowers appear on still leafless stems at the end of the dry season, making the floral display more conspicuous. They are useful as honey plants for bees, and are popular with certain hummingbirds. Naturalist Madhaviah Krishnan on the other hand once famously took offense at ipé grown in India, where it is not native.

Lapacho teaThe bark of several species has medical properties. The bark is dried, shredded, and then boiled making a bitter or sour-tasting brownish-colored tea. Tea from the inner bark of Pink Ipê (T. impetiginosa) is known as Lapacho or Taheebo. Its main active principles are lapachol, quercetin, and other flavonoids. It is also available in pill form. The herbal remedy is typically used during flu and cold season and for easing smoker's cough. It apparently works as expectorant, by promoting the lungs to cough up and free deeply embedded mucus and contaminants. However, lapachol is rather toxic and therefore a more topical use e.g. as antibiotic or pesticide may be advisable. Other species with significant folk medical use are T. alba and Yellow Lapacho (T. serratifolia)

Tabebuia heteropoda, T. incana, and other species are occasionally used as an additive to the entheogenic drink Ayahuasca.

Mycosphaerella tabebuiae, a plant pathogenic sac fungus, was first discovered on an ipê tree.

Tabebuia alba

Tabebuia anafensis

Tabebuia arimaoensis

Tabebuia aurea – Caribbean Trumpet Tree

Tabebuia bilbergii

Tabebuia bibracteolata

Tabebuia cassinoides

Tabebuia chrysantha – Araguaney, Yellow Ipê, tajibo (Bolivia), ipê-amarelo (Brazil), cañaguate (N Colombia)

Tabebuia chrysotricha – Golden Trumpet Tree

Tabebuia donnell-smithii Rose – Gold Tree, "Prima Vera", Cortez blanco (El Salvador), San Juan (Honduras), palo blanco (Guatemala),duranga (Mexico)

A native of Mexico and Central Americas, considered one of the most colorful of all Central American trees. The leaves are deciduous. Masses of golden-yellow flowers cover the crown after the leaves are shed.

Tabebuia dubia

Tabebuia ecuadorensis

Tabebuia elongata

Tabebuia furfuracea

Tabebuia geminiflora Rizz. & Mattos

Tabebuia guayacan (Seem.) Hemsl.

Tabebuia haemantha

Tabebuia heptaphylla (Vell.) Toledo – tajy

Tabebuia heterophylla – roble prieto

Tabebuia heteropoda

Tabebuia hypoleuca

Tabebuia impetiginosa – Pink Ipê, Pink Lapacho, ipê-cavatã, ipê-comum, ipê-reto, ipê-rosa, ipê-roxo-damata, pau d'arco-roxo, peúva, piúva (Brazil), lapacho negro (Spanish); not "brazilwood"

Tabebuia incana

Tabebuia jackiana

Tabebuia lapacho – lapacho amarillo

Tabebuia orinocensis A.H. Gentry[verification needed]

Tabebuia ochracea

Tabebuia oligolepis

Tabebuia pallida – Cuban Pink Trumpet Tree

Tabebuia platyantha

Tabebuia polymorpha

Tabebuia rosea (Bertol.) DC.[verification needed] (= T. pentaphylla (L.) Hemsley) – Pink Poui, Pink Tecoma, apama, apamate, matilisguate

A popular street tree in tropical cities because of its multi-annular masses of light pink to purple flowers and modest size. The roots are not especially destructive for roads and sidewalks. It is the national tree of El Salvador and the state tree of Cojedes, Venezuela

Tabebuia roseo-alba – White Ipê, ipê-branco (Brazil), lapacho blanco

Tabebuia serratifolia – Yellow Lapacho, Yellow Poui, ipê-roxo (Brazil)

Tabebuia shaferi

Tabebuia striata

Tabebuia subtilis Sprague & Sandwith

Tabebuia umbellata

Tabebuia vellosoi Toledo

Ipê-do-cerrado

Texto, em português, da Wikipédia, a enciclopédia livre.

Ipê-do-cerrado

Classificação científica

Reino: Plantae

Divisão: Magnoliophyta

Classe: Magnoliopsida

Subclasse: Asteridae

Ordem: Lamiales

Família: Bignoniaceae

Género: Tabebuia

Espécie: T. ochracea

Nome binomial

Tabebuia ochracea

(Cham.) Standl. 1832

Sinónimos

Bignonia tomentosa Pav. ex DC.

Handroanthus ochraceus (Cham.) Mattos

Tabebuia chrysantha (Jacq.) G. Nicholson

Tabebuia hypodictyon A. DC.) Standl.

Tabebuia neochrysantha A.H. Gentry

Tabebuia ochracea subsp. heteropoda (A. DC.) A.H. Gentry

Tabebuia ochracea subsp. neochrysantha (A.H. Gentry) A.H. Gentry

Tecoma campinae Kraenzl.

ecoma grandiceps Kraenzl.

Tecoma hassleri Sprague

Tecoma hemmendorffiana Kraenzl.

Tecoma heteropoda A. DC.

Tecoma hypodictyon A. DC.

Tecoma ochracea Cham.

Ipê-do-cerrado é um dos nomes populares da Tabebuia ochracea (Cham.) Standl. 1832, nativa do cerrado brasileiro, no estados de Amazonas, Pará, Maranhão, Piauí, Ceará, Pernambuco, Bahia, Espírito Santo, Goiás, Mato Grosso, Mato Grosso do Sul, Minas Gerais, Rio de Janeiro, São Paulo e Paraná.

Está na lista de espécies ameaçadas do estado de São Paulo, onde é encontrda também no domínio da Mata Atlântica[1].

Ocorre também na Argentina, Paraguai, Bolívia, Equador, Peru, Venezuela, Guiana, El Salvador, Guatemala e Panamá[2].

Há uma espécie homônima descrita por A.H. Gentry em 1992.

Outros nomes populares: ipê-amarelo, ipê-cascudo, ipê-do-campo, ipê-pardo, pau-d'arco-do-campo, piúva, tarumã.

Características

Altura de 6 a 14 m. Tronco tortuso com até 50 cm de diâmetro. Folhas pilosas em ambas as faces, mais na inferior, que é mais clara.

Planta decídua, heliófita, xerófita, nativa do cerrado em solos bem drenados.

Floresce de julho a setembro. Os frutos amadurecem de setembro a outubro.

FloresProduz grande quantidade de sementes leves, aladas com pequenas reservas, e que perdem a viabilidade em menos de 90 dias após coleta. A sua conservação vem sendo estudada em termos de determinação da condição ideal de armazenamento, e tem demonstrado a importância de se conhecer o comportamento da espécie quando armazenada com diferentes teores de umidade inicial, e a umidade de equilíbrio crítica para a espécie (KANO; MÁRQUEZ & KAGEYAMA, 1978). As levíssimas sementes aladas da espécie não necessitam de quebra de dormência. Podem apenas ser expostas ao sol por cerca de 6 horas e semeadas diretamente nos saquinhos. A germinação ocorre após 30 dias e de 80%. As sementes são ortodoxas e há aproximadamente 72 000 sementes em cada quilo.

O desenvolvimento da planta é rápido.

Como outros ipês, a madeira é usada em tacos, assoalhos, e em dormentes e postes. Presta-se também para peças torneadas e instrumento musicais.

Tabebuia alba (Ipê-Amarelo)

Texto, em português, produzido pela Acadêmica Giovana Beatriz Theodoro Marto

Supervisão e orientação do Prof. Luiz Ernesto George Barrichelo e do Eng. Paulo Henrique Müller

Atualizado em 10/07/2006

O ipê amarelo é a árvore brasileira mais conhecida, a mais cultivada e, sem dúvida nenhuma, a mais bela. É na verdade um complexo de nove ou dez espécies com características mais ou menos semelhantes, com flores brancas, amarelas ou roxas. Não há região do país onde não exista pelo menos uma espécie dele, porém a existência do ipê em habitat natural nos dias atuais é rara entre a maioria das espécies (LORENZI,2000).

A espécie Tabebuia alba, nativa do Brasil, é uma das espécies do gênero Tabebuia que possui “Ipê Amarelo” como nome popular. O nome alba provém de albus (branco em latim) e é devido ao tomento branco dos ramos e folhas novas.

As árvores desta espécie proporcionam um belo espetáculo com sua bela floração na arborização de ruas em algumas cidades brasileiras. São lindas árvores que embelezam e promovem um colorido no final do inverno. Existe uma crença popular de que quando o ipê-amarelo floresce não vão ocorrer mais geadas. Infelizmente, a espécie é considerada vulnerável quanto à ameaça de extinção.

A Tabebuia alba, natural do semi-árido alagoano está adaptada a todas as regiões fisiográficas, levando o governo, por meio do Decreto nº 6239, a transformar a espécie como a árvore símbolo do estado, estando, pois sob a sua tutela, não mais podendo ser suprimida de seus habitats naturais.

Taxonomia

Família: Bignoniaceae

Espécie: Tabebuia Alba (Chamiso) Sandwith

Sinonímia botânica: Handroanthus albus (Chamiso) Mattos; Tecoma alba Chamisso

Outros nomes vulgares: ipê-amarelo, ipê, aipê, ipê-branco, ipê-mamono, ipê-mandioca, ipê-ouro, ipê-pardo, ipê-vacariano, ipê-tabaco, ipê-do-cerrado, ipê-dourado, ipê-da-serra, ipezeiro, pau-d’arco-amarelo, taipoca.

Aspectos Ecológicos

O ipê-amarelo é uma espécie heliófita (Planta adaptada ao crescimento em ambiente aberto ou exposto à luz direta) e decídua (que perde as folhas em determinada época do ano). Pertence ao grupo das espécies secundárias iniciais (DURIGAN & NOGUEIRA, 1990).

Abrange a Floresta Pluvial da Mata Atlântica e da Floresta Latifoliada Semidecídua, ocorrendo principalmente no interior da Floresta Primária Densa. É característica de sub-bosques dos pinhais, onde há regeneração regular.

Informações Botânicas

Morfologia

As árvores de Tabebuia alba possuem cerca de 30 metros de altura. O tronco é reto ou levemente tortuoso, com fuste de 5 a 8 m de altura. A casca externa é grisáceo-grossa, possuindo fissuras longitudinais esparas e profundas. A coloração desta é cinza-rosa intenso, com camadas fibrosas, muito resistentes e finas, porém bem distintas.

Com ramos grossos, tortuosos e compridos, o ipê-amarelo possui copa alongada e alargada na base. As raízes de sustentação e absorção são vigorosas e profundas.

As folhas, deciduais, são opostas, digitadas e compostas. A face superior destas folhas é verde-escura, e, a face inferior, acinzentada, sendo ambas as faces tomentosas. Os pecíolos das folhas medem de 2,5 a 10 cm de comprimento. Os folíolos, geralmente, apresentam-se em número de 5 a 7, possuindo de 7 a 18 cm de comprimento por 2 a 6 cm de largura. Quando jovem estes folíolos são densamente pilosos em ambas as faces. O ápice destes é pontiagudo, com base arredondada e margem serreada.

As flores, grandes e lanceoladas, são de coloração amarelo-ouro. Possuem em média 8X15 cm.

Quanto aos frutos, estes possuem forma de cápsula bivalvar e são secos e deiscentes. Do tipo síliqua, lembram uma vagem. Medem de 15 a 30 cm de comprimento por 1,5 a 2,5 cm de largura. As valvas são finamente tomentosas com pêlos ramificados. Possuem grande quantidade de sementes.

As sementes são membranáceas brilhantes e esbranquiçadas, de coloração marrom. Possuem de 2 a 3 cm de comprimento por 7 a 9 mm de largura e são aladas.

Reprodução

A espécie é caducifólia e a queda das folhas coincide com o período de floração. A floração inicia-se no final de agosto, podendo ocorrer alguma variação devido a fenômenos climáticos. Como a espécie floresce no final do inverno é influenciada pela intensidade do mesmo. Quanto mais frio e seco for o inverno, maior será a intensidade da florada do ipê amarelo.

As flores por sua exuberância, atraem abelhas e pássaros, principalmente beija-flores que são importantes agentes polinizadores. Segundo CARVALHO (2003), a espécie possui como vetor de polinização a abelha mamangava (Bombus morio).

As sementes são dispersas pelo vento.

A planta é hermafrodita, e frutifica nos meses de setembro, outubro, novembro, dezembro, janeiro e fevereiro, dependendo da sua localização. Em cultivo, a espécie inicia o processo reprodutivo após o terceiro ano.

Ocorrência Natural

Ocorre naturalmente na Floresta Estaciobal Semidecicual, Floresta de Araucária e no Cerrado.

Segundo o IBGE, a Tabebuia alba (Cham.) Sandw. é uma árvore do Cerrado, Cerradão e Mata Seca. Apresentando-se nos campos secos (savana gramíneo-lenhosa), próximo às escarpas.

Clima

Segundo a classificação de Köppen, o ipê-amarelo abrange locais de clima tropical (Aw), subtropical úmido (Cfa), sutropical de altitude (Cwa e Cwb) e temperado.

A T.alba pode tolerar até 81 geadas em um ano. Ocorre em locais onde a temperatura média anual varia de 14,4ºC como mínimo e 22,4ºC como máximo.

Solo

A espécie prefere solos úmidos, com drenagem lenta e geralmente não muito ondulados (LONGHI, 1995).

Aparece em terras de boa à média fertilidade, em solos profundos ou rasos, nas matas e raramente cerradões (NOGUEIRA, 1977).

Pragas e Doenças

De acordo com CARVALHO (2003), possui como praga a espécie de coleópteros Cydianerus bohemani da família Curculionoideae e um outro coleóptero da família Chrysomellidae. Apesar da constatação de elevados índices populacionais do primeiro, os danos ocasionados até o momento são leves. Nas praças e ruas de Curitiba - PR, 31% das árvores foram atacadas pela Cochonilha Ceroplastes grandis.

ZIDKO (2002), ao estudar no município de Piracicaba a associação de coleópteros em espécies arbóreas, verificou a presença de insetos adultos da espécie Sitophilus linearis da família de coleópteros, Curculionidae, em estruturas reprodutivas. Os insetos adultos da espécie emergiram das vagens do ipê, danificando as sementes desta espécie nativa.

ANDRADE (1928) assinalou diversas espécies de Cerambycidae atacando essências florestais vivas, como ingazeiro, cinamomo, cangerana, cedro, caixeta, jacarandá, araribá, jatobá, entre outras como o ipê amarelo.

A Madeira

A Tabebuia alba produz madeira de grande durabilidade e resistência ao apodrecimento (LONGHI,1995).

MANIERI (1970) caracteriza o cerne desta espécie como de cor pardo-havana-claro, pardo-havan-escuro, ou pardo-acastanhado, com reflexos esverdeados. A superfície da madeira é irregularmente lustrosa, lisa ao tato, possuindo textura media e grã-direita.

Com densidade entre 0,90 e 1,15 grama por centímetro cúbico, a madeira é muito dura (LORENZI, 1992), apresentando grande dificuldade ao serrar.

A madeira possui cheiro e gosto distintos. Segundo LORENZI (1992), o cheiro característico é devido à presença da substância lapachol, ou ipeína.

Usos da Madeira

Sendo pesada, com cerne escuro, adquire grande valor comercial na marcenaria e carpintaria. Também é utilizada para fabricação de dormentes, moirões, pontes, postes, eixos de roda, varais de carroça, moendas de cana, etc.

Produtos Não-Madeireiros

A entrecasca do ipê-amarelo possui propriedades terapêuticas como adstringente, usada no tratamento de garganta e estomatites. É também usada como diurético.

O ipê-amarelo possui flores melíferas e que maduras podem ser utilizadas na alimentação humana.

Outros Usos

É comumente utilizada em paisagismo de parques e jardins pela beleza e porte. Além disso, é muito utilizada na arborização urbana.

Segundo MOREIRA & SOUZA (1987), o ipê-amarelo costuma povoar as beiras dos rios sendo, portanto, indicado para recomposição de matas ciliares. MARTINS (1986), também cita a espécie para recomposição de matas ciliares da Floresta Estacional Semidecidual, abrangendo alguns municípios das regiões Norte, Noroeste e parte do Oeste do Estado do Paraná.

Aspectos Silviculturais

Possui a tendência a crescer reto e sem bifurcações quando plantado em reflorestamento misto, pois é espécie monopodial. A desrrama se faz muito bem e a cicatrização é boa. Sendo assim, dificilmente encopa quando nova, a não ser que seja plantado em parques e jardins.

Ao ser utilizada em arborização urbana, o ipê amarelo requer podas de condução com freqüência mediana.

Espécie heliófila apresenta a pleno sol ramificação cimosa, registrando-se assim dicotomia para gema apical. Deve ser preconizada, para seu melhor aproveitamento madeireiro, podas de formação usuais (INQUE et al., 1983).

Produção de Mudas

A propagação deve realizada através de enxertia.

Os frutos devem ser coletados antes da dispersão, para evitar a perda de sementes. Após a coleta as sementes são postas em ambiente ventilado e a extração é feita manualmente. As sementes do ipê amarelo são ortodoxas, mantendo a viabilidade natural por até 3 meses em sala e por até 9 meses em vidro fechado, em câmara fria.

A condução das mudas deve ser feita a pleno sol. A muda atinge cerca de 30 cm em 9 meses, apresentando tolerância ao sol 3 semanas após a germinação.

Sementes

Os ipês, espécies do gênero Tabebuia, produzem uma grande quantidade de sementes leves, aladas com pequenas reservas, e que perdem a viabilidade em poucos dias após a sua coleta. A sua conservação vem sendo estudada em termos de determinação da condição ideal de armazenamento, e tem demonstrado a importância de se conhecer o comportamento da espécie quando armazenada com diferentes teores de umidade inicial, e a umidade de equilíbrio crítica para a espécie (KANO; MÁRQUEZ & KAGEYAMA, 1978).

As levíssimas sementes aladas da espécie não necessitam de quebra de dormência. Podem apenas ser expostas ao sol por cerca de 6 horas e semeadas diretamente nos saquinhos. A quebra natural leva cerca de 3 meses e a quebra na câmara leva 9 meses. A germinação ocorre após 30 dias e de 80%.

As sementes são ortodoxas e há aproximadamente 87000 sementes em cada quilo.

Preço da Madeira no Mercado

O preço médio do metro cúbico de pranchas de ipê no Estado do Pará cotado em Julho e Agosto de 2005 foi de R$1.200,00 o preço mínimo, R$ 1509,35 o médio e R$ 2.000,00 o preço máximo (CEPEA,2005).

Sandy got a good shot of these guys too: www.flickr.com/photos/sandybird/17142281/

Chairlift @ Lollapalooza 2016, Grant Park, Chicago, IL, on Saturday, July 30, 2016.

Lollapalooza 2016 Setlist:

Look Up

Polymorphing

Amanaemonesia

I Belong in Your Arms

Show U Off

Romeo

Crying In Public

Moth to the Flame

Ch-Ching

Get Real

Faceted diamond, illuminated by one light source and showing the famous "fire" of gem-quality diamond. (4.75 mm across at its widest)

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5200 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

Elements are fundamental substances of matter - matter that is composed of the same types of atoms. At present, 118 elements are known (four of them are still unnamed). Of these, 98 occur naturally on Earth (hydrogen to californium). Most of these occur in rocks & minerals, although some occur in very small, trace amounts. Only some elements occur in their native elemental state as minerals.

To find a native element in nature, it must be relatively non-reactive and there must be some concentration process. Metallic, semimetallic (metalloid), and nonmetallic elements are known in their native state.

The element carbon occurs principally in its native state as graphite (C) and diamond (C). Graphite is the common & far less valuable polymorph of carbon. A scarce polymorph of carbon is diamond. The physical properties of diamond and graphite couldn’t be more different, considering they have the same chemistry. Diamond has a nonmetallic, adamantine luster, typically occurs in cubic or octahedral (double-pyramid) crystals, or subspherical to irregularly-shaped masses, and is extremely hard (H≡10). Diamonds can be almost any color, but are typically clearish, grayish, or yellowish. Many diamonds are noticeably fluorescent under black light (ultraviolet light), but the color and intensity of fluorescence varies. Some diamonds are phosphorescent - under certain conditions, they glow for a short interval on their own.

Very rarely, diamond is a rock-forming mineral (see diamondite - www.flickr.com/photos/jsjgeology/14618393527).

As borboletas são insectos da ordem Lepidoptera classificados nas super-famílias Hesperioidea e Papilionoidea, que constituem o grupo informal Rhopalocera.

As borboletas têm dois pares de asas membranosas cobertas de escamas e peças bucais adaptadas a sucção. Distinguem-se das traças (mariposas) pelas antenas rectilíneas que terminam numa bola, pelos hábitos de vida diurnos, pela metamorfose que decorre dentro de uma crisálida rígida e pelo abdómen fino e alongado. Quando em repouso, as borboletas dobram as suas asas para cima.

As borboletas são importantes polinizadores de diversas espécies de plantas.

O ciclo de vida das borboletas engloba as seguintes etapas:

1) ovo→ fase pré-larval

2) larva→ chamada também de lagarta ou taturana,

3) pupa→ que se desenvolve dentro da crisálida (ou casulo)

4) imago→ fase adulta

_______________________

A butterfly is any of several groups of mainly day-flying insects of the order Lepidoptera, the butterflies and moths. Like other holometabolous insects, butterflies' life cycle consists of four parts, egg, larva, pupa and adult. Most species are diurnal. Butterflies have large, often brightly coloured wings, and conspicuous, fluttering flight. Butterflies comprise the true butterflies (superfamily Papilionoidea), the skippers (superfamily Hesperioidea) and the moth-butterflies (superfamily Hedyloidea). All the many other families within the Lepidoptera are referred to as moths.

Butterflies exhibit polymorphism, mimicry and aposematism. Some, like the Monarch, will migrate over long distances. Some butterflies have evolved symbiotic and parasitic relationships with social insects such as ants. Butterflies are important economically as agents of pollination. The caterpillars of some butterflies eat harmful insects. A few species are pests because in their larval stages they can damage domestic crops or trees. Culturally, butterflies are a popular motif in the visual and literary arts.

As borboletas são insectos da ordem Lepidoptera classificados nas super-famílias Hesperioidea e Papilionoidea, que constituem o grupo informal Rhopalocera.

As borboletas têm dois pares de asas membranosas cobertas de escamas e peças bucais adaptadas a sucção. Distinguem-se das traças (mariposas) pelas antenas rectilíneas que terminam numa bola, pelos hábitos de vida diurnos, pela metamorfose que decorre dentro de uma crisálida rígida e pelo abdómen fino e alongado. Quando em repouso, as borboletas dobram as suas asas para cima.

As borboletas são importantes polinizadores de diversas espécies de plantas.

O ciclo de vida das borboletas engloba as seguintes etapas:

1) ovo→ fase pré-larval

2) larva→ chamada também de lagarta ou taturana,

3) pupa→ que se desenvolve dentro da crisálida (ou casulo)

4) imago→ fase adulta

_______________________

A butterfly is any of several groups of mainly day-flying insects of the order Lepidoptera, the butterflies and moths. Like other holometabolous insects, butterflies' life cycle consists of four parts, egg, larva, pupa and adult. Most species are diurnal. Butterflies have large, often brightly coloured wings, and conspicuous, fluttering flight. Butterflies comprise the true butterflies (superfamily Papilionoidea), the skippers (superfamily Hesperioidea) and the moth-butterflies (superfamily Hedyloidea). All the many other families within the Lepidoptera are referred to as moths.

Butterflies exhibit polymorphism, mimicry and aposematism. Some, like the Monarch, will migrate over long distances. Some butterflies have evolved symbiotic and parasitic relationships with social insects such as ants. Butterflies are important economically as agents of pollination. The caterpillars of some butterflies eat harmful insects. A few species are pests because in their larval stages they can damage domestic crops or trees. Culturally, butterflies are a popular motif in the visual and literary arts.

Chairlift @ Lollapalooza 2016, Grant Park, Chicago, IL, on Saturday, July 30, 2016.

Lollapalooza 2016 Setlist:

Look Up

Polymorphing

Amanaemonesia

I Belong in Your Arms

Show U Off

Romeo

Crying In Public

Moth to the Flame

Ch-Ching

Get Real

www.desertmuseum.org/kids/oz/long-fact-sheets/Desert%20Ce...

Les Sources Occultes 008/999

Un film de Laurent Courau, d'après un scénario de Thierry Ehrmann.

Réalisation : Laurent Courau

Scénario : Thierry Ehrmann

Comédienne : Elora Bessey

Artificier : Thierry Loir

Remerciements à Jolan Bessey, Carine Dubois et Rodolphe Bessey.

© Les Amis de l'Esprit de la Salamandre 1999

Entre effroi et merveilles, une zone mouvante aux portes du futur et des enfers...

Les Sources Occultes vous entraînent au coeur d'un univers polymorphe dont les clés et les motifs se révéleront au fur et à mesure des épisodes de cette série de fictions. En attendant un final apocalyptique, au sens premier du terme, qui révélera la structure générale sous la forme d'un long-métrage...

Les Sources Occultes offrent aussi une nouvelle porte d'entrée dans le labyrinthe multidimensionnel de la Demeure du Chaos à celles et ceux qui postulent à notre casting, une occasion unique de pénétrer les arcanes de l'esprit de la Salamandre.

Secrets revealed of the Abode of Chaos (112 pages, adult only) >>>

Faceted diamonds - "Cumulus" brooch with 8 carat diamond at top. (public display, Field Museum of Natural History, Chicago, Illinois, USA)

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5200 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

Elements are fundamental substances of matter - matter that is composed of the same types of atoms. At present, 118 elements are known (four of them are still unnamed). Of these, 98 occur naturally on Earth (hydrogen to californium). Most of these occur in rocks & minerals, although some occur in very small, trace amounts. Only some elements occur in their native elemental state as minerals.

To find a native element in nature, it must be relatively non-reactive and there must be some concentration process. Metallic, semimetallic (metalloid), and nonmetallic elements are known in their native state.

The element carbon occurs principally in its native state as graphite (C) and diamond (C). Graphite is the common & far less valuable polymorph of carbon. A scarce polymorph of carbon is diamond. The physical properties of diamond and graphite couldn’t be more different, considering they have the same chemistry. Diamond has a nonmetallic, adamantine luster, typically occurs in cubic or octahedral (double-pyramid) crystals, or subspherical to irregularly-shaped masses, and is extremely hard (H≡10). Diamonds can be almost any color, but are typically clearish, grayish, or yellowish. Many diamonds are noticeably fluorescent under black light (ultraviolet light), but the color and intensity of fluorescence varies. Some diamonds are phosphorescent - under certain conditions, they glow for a short interval on their own.

Very rarely, diamond is a rock-forming mineral (see diamondite - www.flickr.com/photos/jsjgeology/14618393527).

Canon EOS R5 Mark II, Canon RF 800mm f/11 IS STM, processed in Lightroom.

Uria aalge, Common Guillemot (in the US Common Murre). The common name in German is insulting.

Wikipedia: "Some individuals in the North Atlantic, known as "bridled guillemots", have a white ring around the eye extending back as a white line. This is not a distinct subspecies, but a polymorphism that becomes more common the farther north the birds breed."

Taken on Billy Shiel's Boat Tour of the Farne Islands, after landing on Inner Farne.

en.wikipedia.org/wiki/Common_murre

A butterfly is an insect of the order Lepidoptera. Like all Lepidoptera, butterflies are notable for their unusual life cycle with a larval caterpillar stage, an inactive pupal stage, and a spectacular metamorphosis into a familiar and colourful winged adult form. Most species are day-flying so they regularly attract attention. The diverse patterns formed by their brightly coloured wings and their erratic yet graceful flight have made butterfly watching a hobby.

Butterflies comprise the true butterflies (superfamily Papilionoidea), the skippers (superfamily Hesperioidea) and the moth-butterflies (superfamily Hedyloidea). Butterflies exhibit polymorphism, mimicry and aposematism. Some migrate over long distances. Some butterflies have evolved symbiotic and parasitic relationships with social insects such as ants. Butterflies are important economically as agents of pollination. In addition, a few species are pests, because they can damage domestic crops and trees in their larval stage.

Culturally, butterflies are a popular motif in the visual and literary arts.

Pyrite concretion from the Pennsylvanian of Illinois, USA. (6.7 centimeters across at its widest)

A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 5500 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates.

The sulfide minerals contain one or more sulfide anions (S-2). The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals. Many sulfides are economically significant, as they occur commonly in ores. The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc. Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size. These minerals will not form in the presence of free oxygen. Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals.

Pyrite is a common iron sulfide mineral (FeS2). It’s nickname is “fool's gold”. Pyrite has a metallic luster, brassy gold color (in contrast to the deep rich yellow gold color of true gold - www.flickr.com/photos/jsjgeology/sets/72157651325153769/), dark gray to black streak, is hard (H=6 to 6.5), has no cleavage, and is moderately heavy for its size. It often forms cubic crystals or pyritohedrons (crystals having pentagonal faces).

Pyrite is common in many hydrothermal veins, shales, coals, various metamorphic rocks, and massive sulfide deposits.

The pyrite specimen shown above is a "pyrite sun" - a discoidal concretion that was developed along a bedding plane in black shale. Texturally, the concretion has outward-radiating crystals with moderately-developed concentricity. Mineralogically, pyrite suns are principally composed of pyrite, plus minor marcasite (also FeS2 - iron sulfide; marcasite is a polymorph of pyrite).

Stratigraphy: Anna Shale (= roof shale of the Herrin Coal), upper Carbondale Formation, Desmoinesian Series, upper Middle Pennsylvanian

Locality: coal mine near Sparta, Randolph County, southwestern Illinois, USA

------------------------

Photo gallery of pyrite:

www.mindat.org/gallery.php?min=3314

Alchemilla glaucescens Wallr., syn.: Alchemilla hybrida L.

A Lady's-mantle, DE.:Filz Frauenmantel, Weichhaar Frauenmantel

Slo.:puhasta plahtica

Dat.: May 3. 2014

Lat.: 46°21'37.68"N Long.: 13°42'9.34"E

Code: Bot_795/2014_DSC0765

Habitat: former pasture with some scattered trees, old overgrown scree slope, slightly southeast inclined; calcareous ground; dry, nutrients poor, shallow soil layer, among low grasses and mosses; partly sunny, exposed to direct rain, average precipitations ~ 3.000 mm/year, average temperature 7-9 deg C, elevation 600 m (1.970 feet),alpine phytogeographical region.

Substratum: soil.

Place: Lower Trenta valley, between villages Soča and Trenta, right bank of river Soča, near Trenta 2b cottage, East Julian Alps, Posočje, Slovenia EC.

Comment: The genus Alchemilla is, along with the genera Hieracium and, may be also, Rubus, probably the most difficult of all in terms of correct species determination. Nobody really knows how many species it comprises. Some estimate the total number to be about 250. Amateur or semiprofessional botanical books usually 'skip' this problem by describing two or three species or groups (aggregates) only. This, of cause, makes field determination almost hopeless for a botanical amateur. But also in standard botanical works like Ref.: (1), (2), (3) and, for my country, Ref.: (4) authors treat this genus widely differently. To illustrate this, look at the number of species and/or aggregates of this genus described in these works. In Ref.:(1), for example, describing in total about 4.500 plants on over 2.600 printed pages only 12 species and/or aggregates are treated, while, on the other side, over 120 species are described in Ref.:(2) for Austria territory only. The reasons for extreme polymorphism in this genus, causing these ambiguities, are frequent hybrids along with obligate apogam (nonsexual) propagation, resulting in countless morphologically different and stable hybrids. Also insufficient knowledge about the distribution of all these individual 'species' contributes its part to the confusion. So, in spite the fact that I am trying to do my best, don't believe too much in my determinations in this genus.

Description: the whole plant, including inner and outer calyx with flower base, flower stalks, main stalk, ground leaf stalks and leaves (upper and lower side and edges) are densely hairy (lower side denser). Hairs shiny, pilose to villous mostly oriented off and up the stalks. Larger leaves have diameter 3-3.5(4) cm (in May). Flower stalks are up to 10 (15) cm tall. Many plants were present among low grasses and mosses.

Ref.:

(1) D. Aeschimann, K. Lauber, D.M. Moser, J.P. Theurillat, Flora Alpina, Vol. 1., Haupt (2004), p 786.

(2) M.A. Fischer, W. Adler, K. Oswald, Exkursionsflora Österreich Liechtenstein, Südtirol, LO Landesmuseen, Linz, Austria (2005), p 501.

(3) Rothmaler 3, Exkursionsflora von Deutschland, 11. Aufl., Elsevier, Spectrum (2007), p 242.

(4) A. Martinči et all., Mala Flora Slovenije, Tehnična Založba Slovenije (2007) (in Slovene), p 262.

Combination of NGW, DHB and TRS products with a polymorph catsuit

As borboletas são insectos da ordem Lepidoptera classificados nas super-famílias Hesperioidea e Papilionoidea, que constituem o grupo informal Rhopalocera.

As borboletas têm dois pares de asas membranosas cobertas de escamas e peças bucais adaptadas a sucção. Distinguem-se das traças (mariposas) pelas antenas rectilíneas que terminam numa bola, pelos hábitos de vida diurnos, pela metamorfose que decorre dentro de uma crisálida rígida e pelo abdómen fino e alongado. Quando em repouso, as borboletas dobram as suas asas para cima.

As borboletas são importantes polinizadores de diversas espécies de plantas.

O ciclo de vida das borboletas engloba as seguintes etapas:

1) ovo→ fase pré-larval

2) larva→ chamada também de lagarta ou taturana,

3) pupa→ que se desenvolve dentro da crisálida (ou casulo)

4) imago→ fase adulta

_______________________

A butterfly is any of several groups of mainly day-flying insects of the order Lepidoptera, the butterflies and moths. Like other holometabolous insects, butterflies' life cycle consists of four parts, egg, larva, pupa and adult. Most species are diurnal. Butterflies have large, often brightly coloured wings, and conspicuous, fluttering flight. Butterflies comprise the true butterflies (superfamily Papilionoidea), the skippers (superfamily Hesperioidea) and the moth-butterflies (superfamily Hedyloidea). All the many other families within the Lepidoptera are referred to as moths.

Butterflies exhibit polymorphism, mimicry and aposematism. Some, like the Monarch, will migrate over long distances. Some butterflies have evolved symbiotic and parasitic relationships with social insects such as ants. Butterflies are important economically as agents of pollination. The caterpillars of some butterflies eat harmful insects. A few species are pests because in their larval stages they can damage domestic crops or trees. Culturally, butterflies are a popular motif in the visual and literary arts.

Ipê-amarelo

Classificação científica

Reino: Plantae

Divisão: Magnoliophyta

Classe: Magnoliopsida

Subclasse: Asteridae

Ordem: Lamiales

Família: Bignoniaceae

Género: Tabebuia

Espécie: ver texto

Nome binomial: Tabebuia spp

Ipê-amarelo é o nome popular de algumas espécies de árvores da região Sul e Sudeste do Brasil, pertencentes à família botânica Bignoniaceae, gênero Tabebuia, que também compreende espécies com flores de cor branca, roxa, rosa ou lilás. Em outras regiões brasileiras, os ipês recebem outras denominações.O nome científico Tabebuia, de origem tupi-guarani, significa pau ou madeira que flutua. É denominada, pelos índios, de caxeta, árvore que nasce na zona litorânea do Brasil, cuja madeira íntegra (inatacável) resiste ao apodrecimento.

Entre as epécies conhecidas pelo nome popular Ipê Amarelo estão:

Tabebuia alba, da Mata Atlântica, considerada a árvore símbolo do Brasil.

T. aurea, do cerrado, da caatinga e do Pantanal

T. chrysotricha, da Mata Atlântica

T. ochracea. do cerrado

T. serratifolia, da Amazônia e da Mata Atlântica

T. umbellata, das matas ciliares da Mata Atlântica

T. vellosoi, da Mata Atlântica

T. caraiba Ipê-amarelo-do-cerrado, caroba-do-campo, craibeira

Algumas destas espécies estão ameaçadas:

OUTRAS ESPECIES DE IPES

IPÊ-ROXO ou IPÊ-roxo-da-mata(tabebuia avellandae)

É o primeiro dos Ipês a florir no ano, inicia a floração em Junho, e pode durar até Agosto, conforme a árvore. Esta espécie se confunde bastante com outras também de flor roxa, como a Tabebuia impetiginosa e a Tabebuia heptaphylla, sendo considerado por alguns autores que a T. avellanedae e a T. impetiginosa seriam a mesma espécie. São muito utilizadas no paisagismo urbano, por sua beleza e desenvolvimento

Ipê-Roxo Bola (Tabebuia impetiginosa)

Recebe este nome em razão da forma de seus cachos de flores. Chega a atingir cerca de 8 a 12 metros de altura, dotada de copa alongada, tronco ereto de 60-90 cm de diâmetro com folhas compostas 5-folioladas e quando florido perde suas folhas. É encontrado desde o Piauí até Minas Gerais, Goiás e São Paulo, em geral nas regiões de cerrado e caatinga. Floresce nos meses de maio a agosto. Existem, ainda, outras espécies de ipê roxo, como o T. heptaphylla. Sua Madeira é muito pesada (densidade 0,96g/cm3) muito dura ao corte, resistente ao ataque de organismos xilófagos.

Utilidades

A madeira é apropriada para construções externas, como dormentes, postes etc. Trabalhos de torno, acabamentos internos, como tacos e tábuas para assoalhos, degraus de escada, carrocerias, instrumentos musicais entre outros usos. A Árvore é extremamente ornamental quando em floração prestando-se admiravelmente bem para o paisagismo em geral. Esta é uma das espécies de ipê-roxo mais cultivada para arborização urbana. É também ótima para compor reflorestamentos destinados a recomposição vegetal de áreas degradadas de preservação permanente. Floresce principalmente durante os meses de maio-agosto com a planta totalmente despida de folhagem! Os frutos amadurecem a partir de outubro.

Ipê-rosa(tabebuia pentaphilla)

De crescimento bem rápido em regiões livres de geadas, (em 2 anos ela atinge 3,5 metros), podendo atingir até 35 m. a Tabebuia impetiginosa é originária da Bacia do Paraná. Floresce abundantemente de Junho a Agosto, e prefere climas mais quentes, porem num Inverno seco e ameno, ela oferece também uma linda florada no começo da Primavera. Ideal para áreas isoladas, ou paisagismo de grandes avenidas, o Ipê Rosa prefere solos férteis e bem drenados. Sabe-se que o ipê-roxo é a Tabebuia avellanedae, porém é muito comum haver confusão com a Tabebuia pentaphylla (ipê-rosa).

Totalizam-se 246 espécies de Ipês:

T. acrophylla ,T. actinophylla ,T. acunana ,T. affinis ,T. alba ,T. anafensis ,T. angustata ,T. anisophylla ,T. apiculata ,T. aquatilis ,T. araliacea ,T. arenicola ,T. argentea ,T. arianeae ,T. arimaoensis ,T. aesculifolia ,T. atrovirens ,T. aurea ,T. avellanedae ,T. bahamensis ,T. barbata ,T. berterii ,T. beyeri ,T. bibracteolata ,T. billbergii ,T. botelhensis ,T. brevipes ,T. brigandina ,T. brooksiana ,T. buchii ,T. bullata ,T. bureauvii ,T. bureavii ,T. calcicola ,T. calderoni ,T. calderonii ,T. caleticana ,T. camagueyensis ,T. candicans ,T. capitata ,T. capotei ,T. caraiba ,T. cassinoides ,T. catarinensis ,T. chapadensis ,T. chrysantha ,T. chrysea ,T. chrysotricha ,T. citrifolia ,T. clementis ,T. coartata ,T. conferta ,T. coralibe ,T. cordata ,T. cowellii ,T. crassifolia ,T. crispiflora ,T. cristata ,T. cuneifolia ,T. curtissii ,T. del ,T. densifolia ,T. dentata ,T. dictyophyllaT. diluvialis T. dolichopoda T. domingensis T. dominicensis T. donnell T. donell-smithii T.dracocephaloides T. dubia T. dugandii T. dura T. ecuadorensis T. ekmanii T. elegansT. ellipticaT. eT. fallax T. flavescens T. floccosa T. fluviatilis T. furfuraceaT. fuscata T. gemmifloraT. geroT. glaucescens T. globiflora T. glomerata T. gonavensisT. gracilipes T. grisebachiiT. guayacan T. haemantha T. heptaphylla T. heterophylla T. heteropoda T. heterotricha T. hotteana T. hypodictyon T. hypolepra T. hypoleuca T. ilicifolia T. impetiginosaT. inaequipes T. incana T. insignis T. ipe T. jackiana T. jamaicensisT. japurensis T. jaucoensis T. jojoana T. lanceolata T. lapacho T. latifolia T. lapacho T. latifolia T. leonis T. lepidophylla T. lepidota T. leptoneura T. leptopoda T. leucoxyla T. libanensis T. lindahlii T. linearis T. litoralis T. longiflora T. longpes T. lopezii T. lucida T. magnolioides T. mansoana T. maestrensis T. maxonii T. mexicana T. micrantha T. microphylla T. millsii T. moaensis T. mogotensis T. multinervis T. myrtifolia T. neochrysantha T. nervosa T. neurophylla T. nicaraguensis T. nigripes T. nipensis T. nivea T. nodosa T. obovata T. obscura T. obtusifolia T. ochracea T. odontodiscus T. oligolepis T. ophiolithica T. ophiticola T. orinocensis T. ostenfeldii T. ovatifolia T. pachyphylla T. pallida T. palmeri T. palustris T. paniculata T. papyrophloios T. pedicellata T. pentaphylla T. perelegans T. perfae T. pergracilis T. petrophila T. picotensis T. pilosa T. pinetorum T. pisoniana T. piutinga T. platyantha T. polyantha T. polymorpha T. potamophila T. pulcherrima T. pulverulenta T. pumila T. punctatissima T. pyramidata T. reticulata T. revoluta T. ricardii T. richardiana T. rigida T. riodocensis T. riparia T. roraimae T. rosea T. roseo-alba T. rubriflora T. rufescens T. rufinervis T. rugosa T. sagraei T. samanensis T. sanguinea T. sauvallei T. savannarum T. saxicola T. schumanniana T. schunkevigoi T. selachidentata T. serratifolia T. sessifolia T. sessilifolia T. setulosa T. shaferi T. simplicifolia T. speciosa T. spectabilis T. spongiosa T. stenocalyx T. striata T. subcordata T. suberosa T. subsessilis T. subtilis T. tortuensis T. trachycarpa T. trinitensis T. triorbicularis T. triphylla T. truncata T. turquinensis T. uleana T. uliginosa T. umbellata T. vellosoi T. vinosa T. wrightii T. xanthophylla T. zanonii T. zolyomiana

O ipê e a Lei, no Brasil

Embora o ipê seja considerado árvore símbolo do Brasil, pela Lei 6.607 de 7 de Dezembro de 1978 o pau-brasil foi declarado Árvore Nacional.

Pelos projetos de lei PL-2293/1974 e PL-882/1975, tentou-se instituir a flor do ipê como flor nacional do Brasil. Ambos os projetos foram arquivados na Câmara dos Deputados. O projeto de lei PL-3380/1961 visava declarar o pau-brasil e o ipê-amarelo, respectivamente, Árvore e Flor Nacionais, mas este projeto não foi aprovado.

A text In English:

The Swallow-tailed Hummingbird, so called from its forked tail, is one of the largest hummingbirds in cities and gardens, but it also occurs in gallery forests, bushy pastures and edges of woods or coppices. It is green, except for the blue head and upper breast, turning to iridescent purple according to the direction of light; it has dark wings and a heavy black bill. The tail is dark blue with the external feathers longer than central ones. It is very aggressive and attacks other hummingbirds that dare to visit flowers in certain trees. Where the flowers are available for many months, the individual is fiercely territorial, but generally needs to search soon for other flowering plants. It flies to catch small insets on or under leaves in the gallery forests or woodlands. The female builds a small cup-shaped nest saddled on a branch, not far from the main trunk in the shade of leaves. Perched on favorite branches, the male can utter long but low chirps. Once in a while, it interrupts these singing sessions to feed, and flies back for more song or to clean the plumage. They occur from the Guianas and Amazon River to Paraguay and southeastern Peru. They can get along with partially deforested zones, but may disappear with intensive agriculture and with the development of treeless cities.

Um texto em Português:

Beija-flor Tesoura (Eupetomena macroura), fotografado em Brasília-DF, Brasil.

Eupetomena macroura (Gmelin, 1788): tesoura; swallow-tailed hummingbird c.

Destaca-se das espécies estudadas pelo maior porte e pela cauda comprida e bifurcada, o que lhe valeu o nome popular. Como é comum entre os beija-flores, é uma espécie agressiva que disputa com outras o seu território e fontes de alimento.

Nidificação: o ninho, em forma de tigela, é assentado numa forquilha de arbusto ou árvores, a cerca de 2 a 3 m do solo. O material utilizado na construção é composto por fibras vegetais incluindo painas, musgos e liquens, aderidos externamente com teias de aranhas.

Hábitat: capoeiras, cerrados, borda de matas e jardins.

Tamanho: 17,0 cm

A SEGUIR UM TEXTO ENCONTRADO E REPRODUZIDO DO ENDEREÇO nationalgeographic.abril.uol.com.br/ng/edicoes/83/reporta... DA NATIONAL GEOGRAFIC:

Prodígios da micro-engenharia, os beija-flores são os campeões dos pesos-leves entre as aves

Uma faísca safira, um frêmito de asas, e o minúsculo pássaro - ou seria um inseto? - some como miragem fugaz. Reaparece instantes depois, agora num ângulo melhor. É pássaro mesmo, um dervixe do tamanho do meu polegar com asas que batem 80 vertiginosas vezes por segundo, produzindo um zumbido quase inaudível. As penas da cauda, à guisa de leme, delicadamente direcionam o vôo em três direções. Ele fita a trombeta de uma vistosa flor alaranjada e do bico fino como agulha projeta uma língua delgada feito linha. Um raio de Sol ricocheteia de suas penas iridescentes. A cor refletida deslumbra como uma pedra preciosa contra uma janela ensolarada. Não admira que os beija-flores sejam tão queridos e que tanta gente já tenha tropeçado ao tentar descrevê-los. Nem mesmo circunspectos cientistas resistem a termos como "belo", "magnífico", "exótico".

Surpresa maior é o fato de o aparentemente frágil beija-flor ser uma das mais resistentes criaturas do reino animal. Cerca de 330 espécies prosperam em ambientes diversos, muitos deles brutais: do Alasca à Argentina, do deserto do Arizona à costa de Nova Scotia, da Amazônia à linha nevada acima dos 4,5 mil metros nos Andes (misteriosamente, essas aves só são encontradas no Novo Mundo).

"Eles vivem no limite do que é possível aos vertebrados, e com maestria", diz Karl Schuchmann, ornitólogo do Instituto Zoológico Alexander Koenig e do Fundo Brehm, na Alemanha. Schuchmann ouviu falar de um beija-flor que viveu 17 anos em cativeiro. "Imagine a resistência de um organismo de 5 ou 6 gramas para viver tanto tempo!", diz ele espantado. Em média, o minúsculo coração de um beija-flor bate cerca de 500 vezes por minuto (em repouso!). Assim, o desse pequeno cativo teria batido meio bilhão de vezes, quase o dobro do total de uma pessoa de 70 anos.

Mas esses passarinhos são duráveis apenas em vida. Quando morrem, seus ossos delicados e ocos quase nunca se fossilizam. Daí o assombro causado pela recente descoberta de um amontoado de fósseis de aves que talvez inclua um beija-flor ancestral de 30 milhões de anos. Como os beija-flores modernos, os espécimes fósseis tinham o bico longo e fino e os ossos superiores das asas mais curtos, terminando em uma saliência arredondada que talvez lhes permitisse fazer a rotação na articulação do ombro e parar no ar.

A outra surpresa foi o local do achado: no sul da Alemanha, longe do território dos beija-flores atuais. Para alguns cientistas, essa descoberta mostra que já existiram beija-flores fora das Américas, mas se extinguiram. Ou quem sabe os fósseis não fossem de beija-flor. Os céticos, entre eles Schuchmann, afirmam que muitas vezes, ao longo da evolução, outros grupos de aves adquiriram características semelhantes às do beija-flor. Os verdadeiros beija-flores, diz Schuchmann, evoluíram nas florestas do leste do Brasil, onde competiam com insetos pelo néctar das flores.

"O Brasil foi o laboratório do protótipo", diz o ornitólogo. "E o modelo funcionou." O beija-flor tornou-se a obra-prima da microengenharia da natureza. Aperfeiçoou sua habilidade de parar no ar há dezenas de milhões de anos para competir por parte das flores do Novo Mundo.

"Eles são uma ponte entre o mundo das aves e o dos insetos", diz Doug Altshuler, da Universidade da Califórnia em Riverside. Altshuler, que estuda o vôo dos beija-flores, examinou os movimentos das asas do pássaro. Observou que, nele, os impulsos elétricos propulsores dos músculos das asas lembram mais os dos insetos que os das aves. Talvez por isso o beija-flor produza tanta energia por batida de asas: mais, por unidade de massa, que qualquer outro vertebrado. Altshuler também analisou os trajetos neurais do beija-flor, que funcionam com a mesma vertiginosa velocidade encontrada nas aves mais ágeis, como seu primo mais próximo, o andorinhão. "São incríveis; uns pequenos Frankesteins", compara.

Certamente eles sabem intimidar: grama por grama, talvez sejam os maiores confrontadores da natureza. "O vocabulário do beija-flor deve ser 100% composto de palavrões", graceja Sheri Williamson, naturalista do Southeastern Arizona Bird Observatory. A agressão do beija-flor nasce de ferozes instintos territoriais moldados à necessidade de sugar néctar a cada poucos minutos. Os beija-flores competem desafiando e ameaçando uns aos outros. Postam-se face a face no ar, rodopiam, mergulham na direção da grama e voam de ré, em danças de dominância que terminam tão subitamente quanto começam.

O melhor lugar para vermos tais batalhas é nas montanhas, especialmente no Equador, em que ricos ecossistemas se apresentam em suas várias altitudes. Sheri supõe que o sentido norte-sul das cordilheiras americanas também crie rotas favoráveis à migração para onde haja constante suprimento de flores. O que contrasta, diz ela, com as barreiras naturais que se estendem de leste a oeste na África, como o Saara e o Mediterrâneo.

Algumas espécies de beija-flor, porém, adaptaram-se a atravessar vastidões planas, onde o alimento é escasso. Antes de sua intrépida migração da primavera para os Estados Unidos e o Canadá, os beija-flores-de-garganta-vermelha reúnem-se no México e empanturram-se de insetos e néctar. Armazenam gordura e duplicam de peso em uma semana. Em seguida, atravessam o golfo do México, voando 800 quilômetros sem escalas por 20 horas, até a costa distante.

A região próxima à linha do equador é um reino de beija-flores. Quem sai do aeroporto de Quito, no Equador, pode ser logo saudado por um cintilante beija-flor-violeta, com pintura de guerra de manchas púrpura iridescentes nos lados da face. A leste da cidade, nas cabeceiras da bacia Amazônica, o beija-flor-bico-de-espada esvoaça na mata portando o bico mais longo de todas as aves em proporção a seu tamanho: mais de metade do comprimento total do animal. Nas encostas do Cotopaxi, um vulcão ao sul de Quito, o beija-flor-do-chimborazo foi avistado acima dos 4,5 mil metros. Ali ele passa a noite entorpecido em cavernas, pois desacelera seu ritmo metabólico o suficiente para não morrer de fome antes de amanhecer. Mais tarde, aquecido pelo Sol, ele recomeça a se alimentar.

"Quem estuda beija-flores fica irremediavelmente enfeitiçado", diz Sheri Williamson. "São criaturinhas sedutoras. Tentei resistir, mas agora tenho sangue de beija-flor correndo nas veias."

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Ipê Amarelo, Tabebuia [chrysotricha or ochracea].

Text, in english, from Wikipedia, the free encyclopedia

"Trumpet tree" redirects here. This term is occasionally used for the Shield-leaved Pumpwood (Cecropia peltata).

Tabebuia

Flowering Araguaney or ipê-amarelo (Tabebuia chrysantha) in central Brazil

Scientific classification

Kingdom: Plantae

(unranked): Angiosperms

(unranked): Eudicots

(unranked): Asterids

Order: Lamiales

Family: Bignoniaceae

Tribe: Tecomeae

Genus: Tabebuia

Gomez

Species

Nearly 100.

Tabebuia is a neotropical genus of about 100 species in the tribe Tecomeae of the family Bignoniaceae. The species range from northern Mexico and the Antilles south to northern Argentina and central Venezuela, including the Caribbean islands of Hispaniola (Dominican Republic and Haiti) and Cuba. Well-known common names include Ipê, Poui, trumpet trees and pau d'arco.

They are large shrubs and trees growing to 5 to 50 m (16 to 160 ft.) tall depending on the species; many species are dry-season deciduous but some are evergreen. The leaves are opposite pairs, complex or palmately compound with 3–7 leaflets.

Tabebuia is a notable flowering tree. The flowers are 3 to 11 cm (1 to 4 in.) wide and are produced in dense clusters. They present a cupular calyx campanulate to tubular, truncate, bilabiate or 5-lobed. Corolla colors vary between species ranging from white, light pink, yellow, lavender, magenta, or red. The outside texture of the flower tube is either glabrous or pubescentThe fruit is a dehiscent pod, 10 to 50 cm (4 to 20 in.) long, containing numerous—in some species winged—seeds. These pods often remain on the tree through dry season until the beginning of the rainy.

Species in this genus are important as timber trees. The wood is used for furniture, decking, and other outdoor uses. It is increasingly popular as a decking material due to its insect resistance and durability. By 2007, FSC-certified ipê wood had become readily available on the market, although certificates are occasionally forged.

Tabebuia is widely used as ornamental tree in the tropics in landscaping gardens, public squares, and boulevards due to its impressive and colorful flowering. Many flowers appear on still leafless stems at the end of the dry season, making the floral display more conspicuous. They are useful as honey plants for bees, and are popular with certain hummingbirds. Naturalist Madhaviah Krishnan on the other hand once famously took offense at ipé grown in India, where it is not native.

Lapacho teaThe bark of several species has medical properties. The bark is dried, shredded, and then boiled making a bitter or sour-tasting brownish-colored tea. Tea from the inner bark of Pink Ipê (T. impetiginosa) is known as Lapacho or Taheebo. Its main active principles are lapachol, quercetin, and other flavonoids. It is also available in pill form. The herbal remedy is typically used during flu and cold season and for easing smoker's cough. It apparently works as expectorant, by promoting the lungs to cough up and free deeply embedded mucus and contaminants. However, lapachol is rather toxic and therefore a more topical use e.g. as antibiotic or pesticide may be advisable. Other species with significant folk medical use are T. alba and Yellow Lapacho (T. serratifolia)

Tabebuia heteropoda, T. incana, and other species are occasionally used as an additive to the entheogenic drink Ayahuasca.

Mycosphaerella tabebuiae, a plant pathogenic sac fungus, was first discovered on an ipê tree.

Tabebuia alba

Tabebuia anafensis

Tabebuia arimaoensis

Tabebuia aurea – Caribbean Trumpet Tree

Tabebuia bilbergii

Tabebuia bibracteolata

Tabebuia cassinoides

Tabebuia chrysantha – Araguaney, Yellow Ipê, tajibo (Bolivia), ipê-amarelo (Brazil), cañaguate (N Colombia)

Tabebuia chrysotricha – Golden Trumpet Tree

Tabebuia donnell-smithii Rose – Gold Tree, "Prima Vera", Cortez blanco (El Salvador), San Juan (Honduras), palo blanco (Guatemala),duranga (Mexico)

A native of Mexico and Central Americas, considered one of the most colorful of all Central American trees. The leaves are deciduous. Masses of golden-yellow flowers cover the crown after the leaves are shed.

Tabebuia dubia

Tabebuia ecuadorensis

Tabebuia elongata

Tabebuia furfuracea

Tabebuia geminiflora Rizz. & Mattos

Tabebuia guayacan (Seem.) Hemsl.

Tabebuia haemantha

Tabebuia heptaphylla (Vell.) Toledo – tajy

Tabebuia heterophylla – roble prieto

Tabebuia heteropoda

Tabebuia hypoleuca

Tabebuia impetiginosa – Pink Ipê, Pink Lapacho, ipê-cavatã, ipê-comum, ipê-reto, ipê-rosa, ipê-roxo-damata, pau d'arco-roxo, peúva, piúva (Brazil), lapacho negro (Spanish); not "brazilwood"

Tabebuia incana

Tabebuia jackiana

Tabebuia lapacho – lapacho amarillo

Tabebuia orinocensis A.H. Gentry[verification needed]

Tabebuia ochracea

Tabebuia oligolepis

Tabebuia pallida – Cuban Pink Trumpet Tree

Tabebuia platyantha

Tabebuia polymorpha

Tabebuia rosea (Bertol.) DC.[verification needed] (= T. pentaphylla (L.) Hemsley) – Pink Poui, Pink Tecoma, apama, apamate, matilisguate

A popular street tree in tropical cities because of its multi-annular masses of light pink to purple flowers and modest size. The roots are not especially destructive for roads and sidewalks. It is the national tree of El Salvador and the state tree of Cojedes, Venezuela

Tabebuia roseo-alba – White Ipê, ipê-branco (Brazil), lapacho blanco

Tabebuia serratifolia – Yellow Lapacho, Yellow Poui, ipê-roxo (Brazil)

Tabebuia shaferi

Tabebuia striata

Tabebuia subtilis Sprague & Sandwith

Tabebuia umbellata

Tabebuia vellosoi Toledo

Ipê-do-cerrado

Texto, em português, da Wikipédia, a enciclopédia livre.

Ipê-do-cerrado

Classificação científica

Reino: Plantae

Divisão: Magnoliophyta

Classe: Magnoliopsida

Subclasse: Asteridae

Ordem: Lamiales

Família: Bignoniaceae

Género: Tabebuia

Espécie: T. ochracea

Nome binomial

Tabebuia ochracea

(Cham.) Standl. 1832

Sinónimos

Bignonia tomentosa Pav. ex DC.

Handroanthus ochraceus (Cham.) Mattos

Tabebuia chrysantha (Jacq.) G. Nicholson

Tabebuia hypodictyon A. DC.) Standl.

Tabebuia neochrysantha A.H. Gentry

Tabebuia ochracea subsp. heteropoda (A. DC.) A.H. Gentry

Tabebuia ochracea subsp. neochrysantha (A.H. Gentry) A.H. Gentry

Tecoma campinae Kraenzl.

ecoma grandiceps Kraenzl.

Tecoma hassleri Sprague

Tecoma hemmendorffiana Kraenzl.

Tecoma heteropoda A. DC.

Tecoma hypodictyon A. DC.

Tecoma ochracea Cham.

Ipê-do-cerrado é um dos nomes populares da Tabebuia ochracea (Cham.) Standl. 1832, nativa do cerrado brasileiro, no estados de Amazonas, Pará, Maranhão, Piauí, Ceará, Pernambuco, Bahia, Espírito Santo, Goiás, Mato Grosso, Mato Grosso do Sul, Minas Gerais, Rio de Janeiro, São Paulo e Paraná.

Está na lista de espécies ameaçadas do estado de São Paulo, onde é encontrda também no domínio da Mata Atlântica[1].

Ocorre também na Argentina, Paraguai, Bolívia, Equador, Peru, Venezuela, Guiana, El Salvador, Guatemala e Panamá[2].

Há uma espécie homônima descrita por A.H. Gentry em 1992.

Outros nomes populares: ipê-amarelo, ipê-cascudo, ipê-do-campo, ipê-pardo, pau-d'arco-do-campo, piúva, tarumã.

Características

Altura de 6 a 14 m. Tronco tortuso com até 50 cm de diâmetro. Folhas pilosas em ambas as faces, mais na inferior, que é mais clara.

Planta decídua, heliófita, xerófita, nativa do cerrado em solos bem drenados.

Floresce de julho a setembro. Os frutos amadurecem de setembro a outubro.

FloresProduz grande quantidade de sementes leves, aladas com pequenas reservas, e que perdem a viabilidade em menos de 90 dias após coleta. A sua conservação vem sendo estudada em termos de determinação da condição ideal de armazenamento, e tem demonstrado a importância de se conhecer o comportamento da espécie quando armazenada com diferentes teores de umidade inicial, e a umidade de equilíbrio crítica para a espécie (KANO; MÁRQUEZ & KAGEYAMA, 1978). As levíssimas sementes aladas da espécie não necessitam de quebra de dormência. Podem apenas ser expostas ao sol por cerca de 6 horas e semeadas diretamente nos saquinhos. A germinação ocorre após 30 dias e de 80%. As sementes são ortodoxas e há aproximadamente 72 000 sementes em cada quilo.

O desenvolvimento da planta é rápido.

Como outros ipês, a madeira é usada em tacos, assoalhos, e em dormentes e postes. Presta-se também para peças torneadas e instrumento musicais.

Tabebuia alba (Ipê-Amarelo)

Texto, em português, produzido pela Acadêmica Giovana Beatriz Theodoro Marto

Supervisão e orientação do Prof. Luiz Ernesto George Barrichelo e do Eng. Paulo Henrique Müller

Atualizado em 10/07/2006

O ipê amarelo é a árvore brasileira mais conhecida, a mais cultivada e, sem dúvida nenhuma, a mais bela. É na verdade um complexo de nove ou dez espécies com características mais ou menos semelhantes, com flores brancas, amarelas ou roxas. Não há região do país onde não exista pelo menos uma espécie dele, porém a existência do ipê em habitat natural nos dias atuais é rara entre a maioria das espécies (LORENZI,2000).

A espécie Tabebuia alba, nativa do Brasil, é uma das espécies do gênero Tabebuia que possui “Ipê Amarelo” como nome popular. O nome alba provém de albus (branco em latim) e é devido ao tomento branco dos ramos e folhas novas.

As árvores desta espécie proporcionam um belo espetáculo com sua bela floração na arborização de ruas em algumas cidades brasileiras. São lindas árvores que embelezam e promovem um colorido no final do inverno. Existe uma crença popular de que quando o ipê-amarelo floresce não vão ocorrer mais geadas. Infelizmente, a espécie é considerada vulnerável quanto à ameaça de extinção.

A Tabebuia alba, natural do semi-árido alagoano está adaptada a todas as regiões fisiográficas, levando o governo, por meio do Decreto nº 6239, a transformar a espécie como a árvore símbolo do estado, estando, pois sob a sua tutela, não mais podendo ser suprimida de seus habitats naturais.

Taxonomia

Família: Bignoniaceae

Espécie: Tabebuia Alba (Chamiso) Sandwith

Sinonímia botânica: Handroanthus albus (Chamiso) Mattos; Tecoma alba Chamisso

Outros nomes vulgares: ipê-amarelo, ipê, aipê, ipê-branco, ipê-mamono, ipê-mandioca, ipê-ouro, ipê-pardo, ipê-vacariano, ipê-tabaco, ipê-do-cerrado, ipê-dourado, ipê-da-serra, ipezeiro, pau-d’arco-amarelo, taipoca.

Aspectos Ecológicos

O ipê-amarelo é uma espécie heliófita (Planta adaptada ao crescimento em ambiente aberto ou exposto à luz direta) e decídua (que perde as folhas em determinada época do ano). Pertence ao grupo das espécies secundárias iniciais (DURIGAN & NOGUEIRA, 1990).

Abrange a Floresta Pluvial da Mata Atlântica e da Floresta Latifoliada Semidecídua, ocorrendo principalmente no interior da Floresta Primária Densa. É característica de sub-bosques dos pinhais, onde há regeneração regular.

Informações Botânicas

Morfologia

As árvores de Tabebuia alba possuem cerca de 30 metros de altura. O tronco é reto ou levemente tortuoso, com fuste de 5 a 8 m de altura. A casca externa é grisáceo-grossa, possuindo fissuras longitudinais esparas e profundas. A coloração desta é cinza-rosa intenso, com camadas fibrosas, muito resistentes e finas, porém bem distintas.

Com ramos grossos, tortuosos e compridos, o ipê-amarelo possui copa alongada e alargada na base. As raízes de sustentação e absorção são vigorosas e profundas.

As folhas, deciduais, são opostas, digitadas e compostas. A face superior destas folhas é verde-escura, e, a face inferior, acinzentada, sendo ambas as faces tomentosas. Os pecíolos das folhas medem de 2,5 a 10 cm de comprimento. Os folíolos, geralmente, apresentam-se em número de 5 a 7, possuindo de 7 a 18 cm de comprimento por 2 a 6 cm de largura. Quando jovem estes folíolos são densamente pilosos em ambas as faces. O ápice destes é pontiagudo, com base arredondada e margem serreada.

As flores, grandes e lanceoladas, são de coloração amarelo-ouro. Possuem em média 8X15 cm.

Quanto aos frutos, estes possuem forma de cápsula bivalvar e são secos e deiscentes. Do tipo síliqua, lembram uma vagem. Medem de 15 a 30 cm de comprimento por 1,5 a 2,5 cm de largura. As valvas são finamente tomentosas com pêlos ramificados. Possuem grande quantidade de sementes.

As sementes são membranáceas brilhantes e esbranquiçadas, de coloração marrom. Possuem de 2 a 3 cm de comprimento por 7 a 9 mm de largura e são aladas.

Reprodução

A espécie é caducifólia e a queda das folhas coincide com o período de floração. A floração inicia-se no final de agosto, podendo ocorrer alguma variação devido a fenômenos climáticos. Como a espécie floresce no final do inverno é influenciada pela intensidade do mesmo. Quanto mais frio e seco for o inverno, maior será a intensidade da florada do ipê amarelo.

As flores por sua exuberância, atraem abelhas e pássaros, principalmente beija-flores que são importantes agentes polinizadores. Segundo CARVALHO (2003), a espécie possui como vetor de polinização a abelha mamangava (Bombus morio).

As sementes são dispersas pelo vento.

A planta é hermafrodita, e frutifica nos meses de setembro, outubro, novembro, dezembro, janeiro e fevereiro, dependendo da sua localização. Em cultivo, a espécie inicia o processo reprodutivo após o terceiro ano.

Ocorrência Natural

Ocorre naturalmente na Floresta Estaciobal Semidecicual, Floresta de Araucária e no Cerrado.

Segundo o IBGE, a Tabebuia alba (Cham.) Sandw. é uma árvore do Cerrado, Cerradão e Mata Seca. Apresentando-se nos campos secos (savana gramíneo-lenhosa), próximo às escarpas.

Clima

Segundo a classificação de Köppen, o ipê-amarelo abrange locais de clima tropical (Aw), subtropical úmido (Cfa), sutropical de altitude (Cwa e Cwb) e temperado.

A T.alba pode tolerar até 81 geadas em um ano. Ocorre em locais onde a temperatura média anual varia de 14,4ºC como mínimo e 22,4ºC como máximo.

Solo

A espécie prefere solos úmidos, com drenagem lenta e geralmente não muito ondulados (LONGHI, 1995).

Aparece em terras de boa à média fertilidade, em solos profundos ou rasos, nas matas e raramente cerradões (NOGUEIRA, 1977).

Pragas e Doenças

De acordo com CARVALHO (2003), possui como praga a espécie de coleópteros Cydianerus bohemani da família Curculionoideae e um outro coleóptero da família Chrysomellidae. Apesar da constatação de elevados índices populacionais do primeiro, os danos ocasionados até o momento são leves. Nas praças e ruas de Curitiba - PR, 31% das árvores foram atacadas pela Cochonilha Ceroplastes grandis.

ZIDKO (2002), ao estudar no município de Piracicaba a associação de coleópteros em espécies arbóreas, verificou a presença de insetos adultos da espécie Sitophilus linearis da família de coleópteros, Curculionidae, em estruturas reprodutivas. Os insetos adultos da espécie emergiram das vagens do ipê, danificando as sementes desta espécie nativa.

ANDRADE (1928) assinalou diversas espécies de Cerambycidae atacando essências florestais vivas, como ingazeiro, cinamomo, cangerana, cedro, caixeta, jacarandá, araribá, jatobá, entre outras como o ipê amarelo.

A Madeira

A Tabebuia alba produz madeira de grande durabilidade e resistência ao apodrecimento (LONGHI,1995).

MANIERI (1970) caracteriza o cerne desta espécie como de cor pardo-havana-claro, pardo-havan-escuro, ou pardo-acastanhado, com reflexos esverdeados. A superfície da madeira é irregularmente lustrosa, lisa ao tato, possuindo textura media e grã-direita.

Com densidade entre 0,90 e 1,15 grama por centímetro cúbico, a madeira é muito dura (LORENZI, 1992), apresentando grande dificuldade ao serrar.

A madeira possui cheiro e gosto distintos. Segundo LORENZI (1992), o cheiro característico é devido à presença da substância lapachol, ou ipeína.

Usos da Madeira

Sendo pesada, com cerne escuro, adquire grande valor comercial na marcenaria e carpintaria. Também é utilizada para fabricação de dormentes, moirões, pontes, postes, eixos de roda, varais de carroça, moendas de cana, etc.

Produtos Não-Madeireiros

A entrecasca do ipê-amarelo possui propriedades terapêuticas como adstringente, usada no tratamento de garganta e estomatites. É também usada como diurético.

O ipê-amarelo possui flores melíferas e que maduras podem ser utilizadas na alimentação humana.

Outros Usos

É comumente utilizada em paisagismo de parques e jardins pela beleza e porte. Além disso, é muito utilizada na arborização urbana.

Segundo MOREIRA & SOUZA (1987), o ipê-amarelo costuma povoar as beiras dos rios sendo, portanto, indicado para recomposição de matas ciliares. MARTINS (1986), também cita a espécie para recomposição de matas ciliares da Floresta Estacional Semidecidual, abrangendo alguns municípios das regiões Norte, Noroeste e parte do Oeste do Estado do Paraná.

Aspectos Silviculturais

Possui a tendência a crescer reto e sem bifurcações quando plantado em reflorestamento misto, pois é espécie monopodial. A desrrama se faz muito bem e a cicatrização é boa. Sendo assim, dificilmente encopa quando nova, a não ser que seja plantado em parques e jardins.

Ao ser utilizada em arborização urbana, o ipê amarelo requer podas de condução com freqüência mediana.

Espécie heliófila apresenta a pleno sol ramificação cimosa, registrando-se assim dicotomia para gema apical. Deve ser preconizada, para seu melhor aproveitamento madeireiro, podas de formação usuais (INQUE et al., 1983).

Produção de Mudas

A propagação deve realizada através de enxertia.

Os frutos devem ser coletados antes da dispersão, para evitar a perda de sementes. Após a coleta as sementes são postas em ambiente ventilado e a extração é feita manualmente. As sementes do ipê amarelo são ortodoxas, mantendo a viabilidade natural por até 3 meses em sala e por até 9 meses em vidro fechado, em câmara fria.

A condução das mudas deve ser feita a pleno sol. A muda atinge cerca de 30 cm em 9 meses, apresentando tolerância ao sol 3 semanas após a germinação.

Sementes

Os ipês, espécies do gênero Tabebuia, produzem uma grande quantidade de sementes leves, aladas com pequenas reservas, e que perdem a viabilidade em poucos dias após a sua coleta. A sua conservação vem sendo estudada em termos de determinação da condição ideal de armazenamento, e tem demonstrado a importância de se conhecer o comportamento da espécie quando armazenada com diferentes teores de umidade inicial, e a umidade de equilíbrio crítica para a espécie (KANO; MÁRQUEZ & KAGEYAMA, 1978).

As levíssimas sementes aladas da espécie não necessitam de quebra de dormência. Podem apenas ser expostas ao sol por cerca de 6 horas e semeadas diretamente nos saquinhos. A quebra natural leva cerca de 3 meses e a quebra na câmara leva 9 meses. A germinação ocorre após 30 dias e de 80%.

As sementes são ortodoxas e há aproximadamente 87000 sementes em cada quilo.

Preço da Madeira no Mercado

O preço médio do metro cúbico de pranchas de ipê no Estado do Pará cotado em Julho e Agosto de 2005 foi de R$1.200,00 o preço mínimo, R$ 1509,35 o médio e R$ 2.000,00 o preço máximo (CEPEA,2005).