domingo, 21 de fevereiro de 2016

Jade

Jade


A selection of antique, hand-craftedChinese jade buttons
Unworked jade
Jade on display in Jade City, British Columbia, Canada
Jade is an ornamental rock. The term jade is applied to two different metamorphic rocks that are composed of different silicate minerals:
  • Nephrite consists of a microcrystalline interlocking fibrous matrix of the calcium, magnesium-iron rich amphibole mineral seriestremolite (calcium-magnesium)-ferroactinolite (calcium-magnesium-iron). The middle member of this series with an intermediate composition is called actinolite (the silky fibrous mineral form is one form of asbestos). The higher the iron content, the greener the colour.
  • Jadeite is a sodium- and aluminium-rich pyroxene. The gem form of the mineral is a microcrystalline interlocking crystal matrix.

Etymology[edit]

The English word jade is derived (via French l'ejade and Latin ilia "flanks, kidney area")[1] from the Spanish term piedra de ijada (first recorded in 1565) or "loin stone", from its reputed efficacy in curing ailments of the loins and kidneys. Nephrite is derived from lapis nephriticus, the Latin version of the Spanish piedra de ijada.[2]

Overview[edit]

Nephrite and jadeite[edit]

Nephrite and jadeite were used from prehistoric periods for hardstone carving. Jadeite has about the same hardness as quartz. Nephrite is slightly softer, but is tougher (more resistant to breakage) than jadeite. It was not until the 19th century that a French mineralogist, Alexis Damour (1808-1902), determined that "jade" was in fact two different minerals.[citation needed]
Among the earliest known jade artifacts excavated from prehistoric sites are simple ornaments with bead, button, and tubular shapes.[3] Additionally, jade was used for adzeheads, knives, and other weapons, which can be delicately shaped. As metal-working technologies became available, the beauty of jade made it valuable for ornaments and decorative objects. Jadeite measures between 6.0 and 7.0 Mohs hardness, and nephrite between 6.0 and 6.5, so it can be worked with quartz or garnet sand, and polished with bamboo or even ground jade.[citation needed]

Unusual varieties[edit]

Nephrite can be found in a creamy white form (known in China as "mutton fat" jade) as well as in a variety of green colours, whereas jadeite shows more colour variations, including blue, lavender-mauve, pink, and emerald-green colours.[citation needed] Of the two, jadeite is rarer, documented in fewer than 12 places worldwide. Translucent emerald-green jadeite is the most prized variety, both historically and today. As "quetzal" jade, bright green jadeite from Guatemala was treasured by Mesoamerican cultures, and as "kingfisher" jade, vivid green rocks from Burma became the preferred stone of post-1800 Chinese imperial scholars and rulers. Burma (Myanmar) and Guatemala are the principal sources of modern gem jadeite. In the area of Mogaung in the Myitkyina District of Upper Burma, jadeite formed a layer in the dark-green serpentine, and has been quarried and exported for well over a hundred years.[4] Canada provides the major share of modern lapidary nephrite. Nephrite jade was used mostly in pre-1800 China as well as in New Zealand, the Pacific Coast and Atlantic Coasts of North America, Neolithic Europe, and Southeast Asia. In addition to Mesoamerica, jadeite was used by Neolithic Japanese and European cultures.

History[edit]

Prehistoric and historic China[edit]

Main article: Chinese jade
Jade dragon, Western Han Dynasty (202 BC – 9 AD)
Large "mutton fat" nephrite jade displayed in Hotan Cultural Museumlobby.
Collecting jade in the White Jade River at Khotanin 2011
Jade rocks in truck in Khotan in 2011
During Neolithic times, the key known sources of nephrite jade in China for utilitarian and ceremonial jade items were the now depleted deposits in the Ningshao area in the Yangtze River Delta (Liangzhu culture3400–2250 BC) and in an area of the Liaoning province and Inner Mongolia (Hongshan culture 4700–2200 BC).[5] Dushan Jade was being mined as early as 6000 BC. In the Yin Ruins of the Shang Dynasty (1600 to 1050 BC) in Anyang, Dushan Jade ornaments were unearthed in the tomb of the Shang kings. Jade was used to create many utilitarian and ceremonial objects, from indoor decorative items to jade burial suits. Jade was considered the "imperial gem". From the earliest Chinese dynasties to the present, the jade deposits most in use were not only those of Khotan in the Western Chinese province of Xinjiangbut other parts of China as well, such as Lantian, Shaanxi. There, white and greenish nephrite jade is found in small quarries and as pebbles and boulders in the rivers flowing from the Kuen-Lun mountain range eastward into the Takla-Makan desert area. The river jade collection is concentrated in the Yarkand, the White Jade (Yurungkash) and Black Jade (Karakash) Rivers. From the Kingdom of Khotan, on the southern leg of the Silk Road, yearly tribute payments consisting of the most precious white jade were made to the Chinese Imperial court and there worked into objets d'art by skilled artisans as jade had a status-value exceeding that of gold or silver. Jade became a favourite material for the crafting of Chinese scholars' objects, such as rests for calligraphy brushes, as well as the mouthpieces of some opium pipes, due to the belief that breathing through jade would bestow longevity upon smokers who used such a pipe.[6]
Jadeite, with its bright emerald-green, pink, lavender, orange and brown colours was imported from Burma to China only after about 1800. The vivid green variety became known as Feicui (翡翠) or Kingfisher (feathers) Jade. It quickly became almost as popular as nephrite and a favorite of Qing Dynasty's nouveau riche, while scholars still had strong attachment to nephrite (white jade, or Khotan), which they deemed to be the symbol of a nobleman.
In the history of the art of the Chinese empire, jade has had a special significance, comparable with that of gold anddiamonds in the West.[7] Jade was used for the finest objects and cult figures, and for grave furnishings for high-ranking members of the imperial family.[7] Due to that significance and the rising middle class in China, today the finest jade when found in nuggets of “mutton fat” jade — so-named for its marbled white consistency — can fetch $3,000 an ounce, a tenfold increase from a decade ago.[8]
The Chinese character 玉[9] is used to denote the several types of stone known in English as "jade" (e.g. 玉器, jadewares), such as jadeite (硬玉, 'hard jade', another name for 翡翠) and nephrite (軟玉, 'soft jade'). But because of the value added culturally to jades throughout Chinese history, the word has also come to refer more generally to precious or ornamental stones,[10] and is very common in more symbolic usage as in phrases like 拋磚引玉/抛砖引玉 (lit. 'casting a brick (i.e. the speaker's own words) to draw a jade (i.e. pearls of wisdom from the other party)'), 玉容 (a beautiful face; 'jade countenance'), and 玉立 (slim and graceful; 'jade standing upright'). The character has a similar range of meanings when appearing as a radical as parts of other characters.

Prehistoric and historic India[edit]

Dagger with Jade hilt, India, 17th–18th century.Louvre
The Jain temple of Kolanpak in the Nalgonda district, Andhra Pradesh, India is home to a 5-foot (1.5 m) high sculpture ofMahavira that is carved entirely out of jade. It is the largest sculpture made from a single jade rock in the world. India is also noted for its craftsman tradition of using large amounts of green serpentine or false jade obtained primarily from Afghanistan in order to fashion jewellery and ornamental items such as sword hilts and dagger handles.[4]

Prehistoric and early historic Korea[edit]

Golden crown with jade pendants from Silla, fifth or sixth century AD, in the National Museum of Korea.
The use of jade and other greenstone was a long-term tradition in Korea (c. 850 BC – AD 668). Jade is found in small numbers of pit-houses andburials. The craft production of small comma-shaped and tubular "jades" using materials such as jade, microcline, jasper, etc., in southern Korea originates from the Middle Mumun Pottery Period (c. 850–550 BC).[11] Comma-shaped jades are found on some of the gold crowns of Silla royalty (c. 300/400–668 AD) and sumptuous elite burials of the Korean Three Kingdoms. After the state of Silla united the Korean Peninsula in 668, the widespread popularisation of death rituals related to Buddhism resulted in the decline of the use of jade in burials as prestige mortuary goods.

Southeast Asia[edit]

Archaeologists have discovered two forms of jade that can be found across Taiwan through the Philippines, East Malaysia, central and southern Vietnam, and even extending to eastern Cambodia and peninsular Thailand. These two forms are called linling-o penannular earring with three pointed circumferential projections and the double animal-headed ear pendant. The forms are very similar in size and range from about 30-35mm in diameter. Furthermore, radiocarbon dates have dated these forms in Southeast Asia from around 500 BC to 500 AD.[12] The electron probe microanalysis shows that the raw material of these two types of artifacts was nephrite jade from Taiwan called Fengtian nephrite. Evidence recovered from multiple sites from Taiwan, the Philippines, and the mainland southeast Asia suggests that Taiwan was the main source of the exchange of this kind jade. During the Iron Age of Southeast Asia, there may have been skilled craftsmen traveling from Taiwan to southeast Asia along the coastline of the South China Sea, making jade ornaments for local inhabitants.[13]

Māori[edit]

Nephrite jade in New Zealand is known as pounamu in the Māori language (often called "greenstone" in New Zealand English), and plays an important role in Māori culture. It is considered a taonga, or treasure, and therefore protected under the Treaty of Waitangi, and the exploitation of it is restricted and closely monitored. It is found only in the South Island of New Zealand, known as Te Wai Pounamu inMāori—"The [land of] Greenstone Water", or Te Wahi Pounamu—"The Place of Greenstone".
Tools, weapons and ornaments were made of it; in particular adzes, the 'mere' (short club), and the Hei-tiki (neck pendant). These were believed to have their own mana, handed down as valuable heirlooms, and often given as gifts to seal important agreements. Nephritejewellery of Maori design is widely popular with locals and tourists, although some of the jade used for these is now imported from British Columbia and elsewhere.[14]

Canada[edit]

Jade was first identified in Canada by Chinese settlers in 1886 in British Columbia. At this time jade was considered worthless as they were searching for gold. Jade was not commercialized in Canada until the 1970s. The mining business Loex James Ltd., which was started by two Californians, began commercial mining of Canadian jade in 1972.[15]

Mining[edit]

Mining is done from large boulders that contain bountiful deposits of jade. Jade is exposed using diamond-tipped core drills in order to extract samples. This is done to ensure that the jade meets requirements. Hydraulic spreaders are then inserted into cleavage points in the rock so that the jade can be broken away. Once the boulders are removed and the jade is accessible, it is broken down into more manageable 10-tonne pieces using water-cooled diamond saws. The jade is then loaded onto trucks and transported to the proper storage facilities.[16]

Mesoamerica[edit]

Main article: Jade use in Mesoamerica
Jadeite pectoral from the MayanClassic period (195 mm or 7.7 in high)
Jade was a rare and valued material in pre-Columbian Mesoamerica. The only source from which the various indigenous cultures, such as the Olmec and Maya, could obtain jade was located in the Motagua River valley in Guatemala. Jade was largely an elite good, and was usually carved in various ways, whether serving as a medium upon which hieroglyphs were inscribed, or shaped into symbolic figurines. Generally, the material was highly symbolic, and it was often employed in the performance of ideological practices and rituals.

Enhancement[edit]

Jade may be enhanced (sometimes called "stabilized"). Note that some merchants will refer to these as grades, but it is important to bear in mind that degree of enhancement is different from colour and texture quality. In other words, Type A jadeite is not enhanced but can have poor colour and texture. There are three main methods of enhancement, sometimes referred to as the ABC Treatment System:[17]
  • Type A jadeite has not been treated in any way except surface waxing.
  • Type B treatment involves exposing a promising but stained piece of jadeite to chemical bleaches and/or acids and impregnating it with a clear polymer resin. This results in a significant improvement of transparency and colour of the material. Currently, infrared spectroscopy is the most accurate test for the detection of polymer in jadeite.
  • Type C jade has been artificially stained or dyed. The effects are somewhat uncontrollable and may result in a dull brown. In any case, translucency is usually lost.
  • B+C jade is a combination of B and C: it has been both impregnated and artificially stained.
  • Type D jade refers to a composite stone such as a doublet comprising a jade top with a plastic backing.

Rhodochrosite

Rhodochrosite


Rhodochrosite
Rhodochrosite-261714.jpg
General
CategoryCarbonate minerals
Formula
(repeating unit)
MnCO3
Strunz classification05.AB.05
Crystal symmetryTrigonal hexagonal scalenohedral
H-M symbol: (32/m)
Space group: R3c
Unit cella = 4.777 Å, c = 15.67 Å; Z=6
Identification
Formula mass114.95 g/mol
ColorPink, rose-red, cherry-red, yellow, yellowish gray, cinnamon-brown, may be banded
Crystal habitRhombohedral and scalenohedral crystals; also commonly bladed, columnar, stalactitic, botryoidal, granular or massive
Crystal systemTrigonal
TwinningOn {1012} as contact and lamellar
CleavageOn {1011} perfect; parting on {1012}
FractureUneven, conchoidal
TenacityBrittle
Mohs scalehardness3.5-4
LusterVitreous to pearly
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity3.7
Optical propertiesUniaxial (-)
Refractive indexnω = 1.814 - 1.816 nε = 1.596 - 1.598
Birefringenceδ = 0.218
Pleochroismweak
UltravioletfluorescenceNone
References[1][2][3]
Rhodochrosite is a manganese carbonate mineral with chemical composition MnCO3. In its (rare) pure form, it is typically a rose-red color, but impure specimens can be shades of pink to pale brown. It streaks white, and its Mohs hardness varies between 3.5 and 4. Its specific gravity is between 3.5 and 3.7. It crystallizes in the trigonal system, and cleaves with rhombohedral carbonate cleavage in three directions. Crystal twinning often is present. It is transparent to translucent with refractive indices of =1.814 to 1.816, =1.596 to 1.598. It is often confused with the manganese silicate, rhodonite, but is distinctly softer.
Rhodochrosite forms a complete solid solution series with iron carbonate (siderite). Calcium, (as well as magnesium and zinc, to a limited extent) frequently substitutes for manganese in the structure, leading to lighter shades of red and pink, depending on the degree of substitution. It is for this reason that the most common color encountered is pink

Occurrence and discovery

Rhodochrosite occurs as a hydrothermal vein mineral along with other manganese minerals in low temperature ore deposits as in the silver mines of Romania where it was first found. Banded rhodochrosite is mined in Capillitas, Argentina.
It was first described in 1813 in reference to a sample from Cavnic, Maramureş, present-day Romania. According to Dimitrescu and Radulescu, 1966 and to Papp, 1997, this mineral was described for the first time in Sacaramb, Romania, not in Cavnic, Romania. The name is derived from the Greek word ῥοδόχρως meaning rose-colored.

Use

Its main use is as an ore of manganese which is a key component of low-cost stainless steel formulations and certain aluminiumalloys. Quality banded specimens are often used for decorative stones and jewelry. Due to its being relatively soft, and having perfect cleavage, it is very difficult to cut, and therefore rarely found faceted in jewelry.

Rhodochrosite and silver mining

Manganese carbonate is extremely destructive to the amalgamation process used in the concentration of silver ores, and so until quality mineral specimens became highly sought after by collectors, they were often discarded on the mine dump.

Culture

Stereo image

[hide]Right frame 
Rhodochrosite3d.jpg
Small Rhodochrosite specimen featured in a mineral kit, from Wuton mine, Guangxi prov, China.
Rhodochrosite is Argentina's "national gemstone".[4][5] Colorado officially named rhodochrosite as its state mineral in 2002.[6] Large specimens have been found in the Sweet Home Mine near Alma, Colorado.
It is sometimes called "Rosa del Inca", "Inca Rose" or Rosinca.[7]

Gallery

Rhodonite

Rhodonite


Rhodonite
Rodonita2EZ.jpg
Rhodonite crystals in rock
General
CategoryInosilicate
Formula
(repeating unit)
(Mn2+,Fe2+,Mg,Ca)SiO3
Strunz classification09.DK.05
Dana classification65.04.01.01
Crystal symmetryTriclinic 1 pinacoidal
Unit cella = 9.758 Å, b = 10.499 Å, c = 12.205 Å; α = 108.58°, β = 102.92°, γ = 82.52°; Z = 20
Identification
ColorRose-pink to brownish red, gray, or yellow
Crystal habitTabular crystals, massive, granular
Crystal systemTriclinic - Pinacoidal H-M Symbol (1) Space Group: P1
TwinningLamellar, composition plane {010}
CleavagePerfect on {110} and {110}, (110) ^ (110) = 92.5°; good on {001}
FractureConchoidal to uneven
Mohs scalehardness5.5 - 6.5
LusterVitreous to pearly
StreakWhite
DiaphaneityTransparent to translucent
Specific gravity3.57 - 3.76
Optical propertiesBiaxial (+)
Refractive indexnα = 1.711 - 1.738 nβ = 1.714 - 1.741 nγ = 1.724 - 1.751
Birefringenceδ = 0.013
PleochroismWeak
2V angleMeasured: 58° to 73°, Calculated: 58°
Alters toExterior commonly black from manganese oxides
References[1][2][3]
Rhodonite is a manganese inosilicate, (Mn, Fe, Mg, Ca)SiO3 and member of the pyroxenoid group of minerals, crystallizing in thetriclinic system. It commonly occurs as cleavable to compact masses with a rose-red color (the name comes from the Greek ῥόδοςrhodos, rosy), often tending to brown because of surface oxidation.
Rhodonite crystals often have a thick tabular habit, but are rare. It has a perfect, prismatic cleavage, almost at right angles. Thehardness is 5.5–6.5, and the specific gravity 3.4–3.7; luster is vitreous, being less frequently pearly on cleavage surfaces. Themanganese is often partly replaced by iron, magnesium, calcium, and sometimes zinc which may sometimes be present in considerable amounts; a greyish-brown variety containing as much as 20% of calcium oxide is called bustamite; fowlerite is a zinciferous variety containing 7% of zinc oxide.
Pink rhodonite contrasting with black manganese oxides is sometimes used as gemstone material as seen in this specimen from Humboldt County,Nevada.
The inosilicate (chain silicate) structure of rhodonite has a repeat unit of five silica tetrahedra. The rare polymorph pyroxmangite, formed at different conditions of pressure and temperature, has the same chemical composition but a repeat unit of seven tetrahedra.
Rhodonite has also been worked as an ornamental stone. In the iron and manganese mines at Pajsberg near Filipstad and Långban in Värmland, Sweden, small brilliant and translucent crystals (pajsbergite) and cleavage masses occur. Fowlerite occurs as large, rough crystals, somewhat resembling pink feldspar, with franklinite and zinc ores in granular limestone atFranklin Furnace in New Jersey.
Rhodonite is the official gemstone of Commonwealth of Massachusetts

O potencial aurífero em território brasileiro é de significativa expressão

Reservas Brasileiras

O potencial aurífero em território brasileiro é de significativa
expressão. Os distritos auríferos, definidos pela ocorrência de uma
ou mais jazidas, além de ocorrências e depósitos de menor relevância,
apresentam-se nas mais diversas tipologias, mas, no entanto,
concentram-se em determinadas áreas. Essas áreas estão encaixadas
principalmente em regiões cratônicas e em cinturões móveis associados,relacionados ao ciclo tectônico Brasiliano, cujas idades mais recentes são da ordem de 450 milhões de anos.
A estimativa de cálculo das reservas de ouro no Brasil é um
exercício de difícil realização, uma vez que significativa parte dos
depósitos conhecidos não tem suas reservas convenientemente avaliadas.
As reservas que possuem um melhor nível de detalhamento e
maior confiabilidade nos resultados das cubagens são as reservas que
estão em fase de produção ou em posse de empresas de mineração.
Esses depósitos são considerados as reservas oficiais de ouro do Brasil
e estão devidamente registradas junto ao Departamento Nacional de
Produção Mineral – DNPM. Através da consolidação dos dados e informações
declaradas pelas empresas de mineração por meio do Relatório
Anual de Lavra – RAL pode-se inferir que as reservas de ouro no País
estão devidamente quantificadas e distribuídas.
No decorrer do período 1995-2007, as reservas brasileiras apresentaram
um crescimento anual médio de 5,9% a.a. Em 1996, ocorreu
um expressivo incremento de 112,5% nas jazidas auríferas perfazendo
cerca de 1.700 t de ouro contido. No ano seguinte, um novo acréscimo
de 11,8% elevou as reservas para o patamar de 1.900 t, estabilizandose
nesses níveis até o ano de 2000. A partir de 2001 ocorreu um
decréscimo de 11,1%, com as reservas situando-se em torno de 1.600
t até o ano seguinte. Em 2003, um novo recuo de 20,6% derrubou as
reservas nacionais para 1.270 t.
As taxas negativas de reposição de recursos e reservas verificadas
ao longo dos anos de 1999 a 2003 foram ocasionadas principalmente
pelas expressivas quedas nos preços do ouro nos mercados
internacionais. Esse período recessivo restringiu fortemente a alocação
de recursos em pesquisa mineral, prospecção e explotação em
depósitos auríferos, não só no Brasil, mas em todo o mundo.
A recuperação das cotações, iniciada a partir do biênio 2002-
2003, trouxe de volta os investidores internacionais ao mercado nacional
ocasionando uma retomada de investimentos na indústria aurífera
brasileira.
Os resultados desse aquecimento no mercado propiciaram incremento
nas reservas nacionais, voltando a atingir, em 2007, aproximadamente,
1.590 t de ouro contido representando cerca de 1,8% do
total das reservas mundiais.
Mapa do Brasil com pontos de depósitos auríferos
Atualmente, as reservas nacionais (medida + indicada) de Au
primário contido representam 98,6% do total das reservas legalmente
registradas no País, perfazendo um total de 1.568 t. O gráfico 02
mostra a distribuição das reservas auríferas nos estados brasileiros
tendo Pará como principal representante, com 650 t de ouro contido
equivalentes a 41,5%, seguido por Minas Gerais com 580 t (37,0%),
Goiás (103 t, 6,5%), Bahia (99 t, 6,3%), Mato Grosso (61 t, 3,9%),
Amapá (33 t, 2,1%), Maranhão (18 t, 1,2%) e outros (23 t, 1,5%).
Cabe ressaltar que as reservas auríferas do Pará obtiveram expressivo
incremento com a cubagem dos depósitos de Cu-Au de Salobo
e Sossego/Sequeirinho localizados na Província Mineral de Carajás e
pertencentes à VALE. As reservas (medida + indicada) de Sossego avaliadas
em 517 t de Au contido foram responsáveis por alçar o Pará ao
posto de maior estado detentor de reservas de ouro do Brasil passando
a frente de Minas Gerais. Dados da tabela 04 apontam as reservas de
Minas Gerais com baixos teores médios de Au contido. Contudo, esses
teores estão fortemente distorcidos em razão das reservas da empresa
Rio Paracatu Mineração S/A, que são as mais expressivas do estado e
operam com o menor teor de corte do mundo. Ao se excluir essa reserva
do cálculo, têm-se os seguintes valores para o estado de Minas Gerais:
reserva medida de 14 milhões t de minério ROM com 106 t de Au contido
e teor de 7,50 g/t; reserva indicada de 20 milhões t de minério ROM
com 129 t de Au contido e teor de 6,33 g/t e reserva inferida de 25
milhões t de minério ROM com 188 t de Au contido e teor de 7,54 g/t.

Febre do ouro acelera desmatamento na América do Sul, afirma estudo

Febre do ouro acelera desmatamento na América do Sul, afirma estudo

Em 12 anos, 1.680 km² de florestas foram derrubados para mineração.
Brasil está entre as regiões mais afetadas, de acordo com os cientistas.


Garimpo ilegal localizado no meio da floresta amazônica, na fronteira entre a Bolívia e Brasil (Foto: Jorge Silva/Reuters)Garimpo ilegal localizado no meio da floresta amazônica, na fronteira entre a Bolívia e Brasil (Foto: Jorge Silva/Reuters)
A proliferação das minas de ouro, às vezes ilegais, observada nos últimos anos em várias regiões da América Latina acelera o desmatamento, ameaça a biodiversidade dessas áreas e contribui para a emissão de gases causadores do efeito estufa - alerta estudo na revista "Environnemental Research Letters".
"A febre do ouro mundial conduziu a um aumento significativo do desflorestamento das selvas tropicais na América do Sul", escrevem os autores.
Entre 2001 e 2015, pelo menos 1.680 km² de florestas tropicais foram derrubados para a exploração das minas de ouro, relatam os especialistas. Isso representa uma pequena parte dos milhões de quilômetros quadrados de floresta tropical de todo o planeta, mas a riqueza biológica das áreas exploradas pelos garimpeiros é excepcional.
"Embora a perda das florestas, devido à exploração das minas, seja menos importante do que o desmatamento causado pela agricultura, ele acontece nas regiões tropicais com a biodiversidade mais rica", destaca Nora Alvarez-Berrios, uma das autoras do estudo.
Floresta Amazônica (Foto: AFP)Trechos compartilhados entre Guiana, Venezuela,
Suriname, Guiana Francesa, Brasil e Colômbia
é o mais afetado (Foto: AFP)
Brasil é um dos países mais afetados
Na região de Madres de Dios, no Peru, por exemplo, um hectare de selva pode conter "até 300 espécies de árvores", explica a pesquisadora da Universidade de Porto Rico. O agravante é que 90% da destruição detectada desde 2001 ocorre em apenas quatro regiões que fazem ecossistemas e, com frequência, perto de zonas protegidas.
As regiões mais afetadas são os trechos compartilhados entre Guiana, Venezuela, Suriname, Guiana Francesa, Brasil, Colômbia, sudoeste amazônico (Peru, Bolívia, Brasil), região Tapajós-Xingu (Brasil) e região do vale Magdalena-Uraba, no norte da Colômbia.
Embora os espaços protegidos pareçam, em geral, em bom estado, os autores do estudo estimam que um terço do desflorestamento aconteceu a menos de 10 km dessas zonas, que estão expostas à contaminação química.
Em função da alta demanda, a produção mundial de ouro passou de 2.445 toneladas, em 2000, para 3.770 toneladas, em 2015.
O preço do ouro também registrou fortes altas nos últimos anos, de US$ 250 a US$ 1.300 a onça (28,3 gramas), entre 2000 e 2015. Isso contribuiu para a abertura de novas minas no mundo inteiro, incluindo em plena selva, em áreas de difícil acesso.