The Amazon
The Amazon
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Amazon rainforest
The Amazon rainforest, also known in English as Amazonia or the Amazon Jungle, is a moist broadleaf forest in the Amazon biome that covers most of the

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"The Amazon" and "Amazonia" redirect here. For the river, see Amazon River. For other uses, see Amazon and Amazonia (disambiguation). rainforest in South America

Amazon rainforest
Portuguese: Floresta amazônica
Spanish: Selva amazónicaAmazon rainforest, near Manaus, BrazilGeographyMap of the Amazon rainforest ecoregions as delineated by the WWF. The yellow line approximately encloses the Amazon drainage basin. National boundaries are shown in black.
(Satellite image from NASA)LocationBrazil, Peru, Colombia, Venezuela, Ecuador, Bolivia, Guyana, Suriname, France (French Guiana)CoordinatesCoordinates: 3°S 60°W / 3°S 60°W / -3; -60Area5,500,000 km2 (2,100,000 sq mi)

The Amazon rainforest,[a] also known in English as Amazonia or the Amazon Jungle, is a moist broadleaf forest in the Amazon biome that covers most of the Amazon basin of South America. This basin encompasses 7,000,000 km2 (2,700,000 sq mi), of which 5,500,000 km2 (2,100,000 sq mi) are covered by the rainforest. This region includes territory belonging to nine nations.

The majority of the forest is contained within Brazil, with 60% of the rainforest, followed by Peru with 13%, Colombia with 10%, and with minor amounts in Venezuela, Ecuador, Bolivia, Guyana, Suriname and France (French Guiana). Four nations have "Amazonas" as the name of one of their first-level administrative regions. The Amazon represents over half of the planet's remaining rainforests,[1] and comprises the largest and most biodiverse tract of tropical rainforest in the world, with an estimated 390 billion individual trees divided into 16,000 species.[2]

  • 1 Etymology
  • 2 History
    • 2.1 Natural
      • 2.1.1 Sahara Desert dust windblown to the Amazon
    • 2.2 Human activity
  • 3 Biodiversity
  • 4 Deforestation
  • 5 Conservation and climate change
    • 5.1 Remote sensing
    • 5.2 Impact of early 21st-century Amazon droughts
  • 6 See also
  • 7 Notes and references
  • 8 Further reading
  • 9 External links

The name Amazon is said to arise from a war Francisco de Orellana fought with the Tapuyas and other tribes. The women of the tribe fought alongside the men, as was their custom.[3] Orellana derived the name Amazonas from the Amazons of Greek mythology, described by Herodotus and Diodorus.[3]

History See also: History of South America § Amazon Natural Aerial view of the Amazon rainforest, near Manaus

The rainforest likely formed during the Eocene era (from 56 million years to 33.9 million years ago). It appeared following a global reduction of tropical temperatures when the Atlantic Ocean had widened sufficiently to provide a warm, moist climate to the Amazon basin. The rainforest has been in existence for at least 55 million years, and most of the region remained free of savanna-type biomes at least until the current ice age, when the climate was drier and savanna more widespread.[4][5]

Following the Cretaceous–Paleogene extinction event, the extinction of the dinosaurs and the wetter climate may have allowed the tropical rainforest to spread out across the continent. From 66–34 Mya, the rainforest extended as far south as 45°. Climate fluctuations during the last 34 million years have allowed savanna regions to expand into the tropics. During the Oligocene, for example, the rainforest spanned a relatively narrow band. It expanded again during the Middle Miocene, then retracted to a mostly inland formation at the last glacial maximum.[6] However, the rainforest still managed to thrive during these glacial periods, allowing for the survival and evolution of a broad diversity of species.[7]

Aerial view of the Amazon rainforest.

During the mid-Eocene, it is believed that the drainage basin of the Amazon was split along the middle of the continent by the Purus Arch. Water on the eastern side flowed toward the Atlantic, while to the west water flowed toward the Pacific across the Amazonas Basin. As the Andes Mountains rose, however, a large basin was created that enclosed a lake; now known as the Solimões Basin. Within the last 5–10 million years, this accumulating water broke through the Purus Arch, joining the easterly flow toward the Atlantic.[8][9]

There is evidence that there have been significant changes in Amazon rainforest vegetation over the last 21,000 years through the Last Glacial Maximum (LGM) and subsequent deglaciation. Analyses of sediment deposits from Amazon basin paleolakes and from the Amazon Fan indicate that rainfall in the basin during the LGM was lower than for the present, and this was almost certainly associated with reduced moist tropical vegetation cover in the basin.[10] There is debate, however, over how extensive this reduction was. Some scientists argue that the rainforest was reduced to small, isolated refugia separated by open forest and grassland;[11] other scientists argue that the rainforest remained largely intact but extended less far to the north, south, and east than is seen today.[12] This debate has proved difficult to resolve because the practical limitations of working in the rainforest mean that data sampling is biased away from the center of the Amazon basin, and both explanations are reasonably well supported by the available data.

Sahara Desert dust windblown to the Amazon

More than 56% of the dust fertilizing the Amazon rainforest comes from the Bodélé depression in Northern Chad in the Sahara desert. The dust contains phosphorus, important for plant growth. The yearly Sahara dust replaces the equivalent amount of phosphorus washed away yearly in Amazon soil from rains and floods.[13]

NASA's CALIPSO satellite has measured the amount of dust transported by wind from the Sahara to the Amazon: an average 182 million tons of dust are windblown out of the Sahara each year, at 15 degrees west longitude, across 1,600 miles (2,600 km) over the Atlantic Ocean (some dust falls into the Atlantic), then at 35 degrees West longitude at the eastern coast of South America, 27.7 million tons (15%) of dust fall over the Amazon basin (22 million tons of it consisting of phosphorus), 132 million tons of dust remain in the air, 43 million tons of dust are windblown and falls on the Caribbean Sea, past 75 degrees west longitude.[14]

CALIPSO uses a laser range finder to scan the Earth's atmosphere for the vertical distribution of dust and other aerosols. CALIPSO regularly tracks the Sahara-Amazon dust plume. CALIPSO has measured variations in the dust amounts transported – an 86 percent drop between the highest amount of dust transported in 2007 and the lowest in 2011.

A possibility causing the variation is the Sahel, a strip of semi-arid land on the southern border of the Sahara. When rain amounts in the Sahel are higher, the volume of dust is lower. The higher rainfall could make more vegetation grow in the Sahel, leaving less sand exposed to winds to blow away.[15]

Amazon phosphorus also comes as smoke due to biomass burning in Africa.[16][17]

Human activity Members of an uncontacted tribe encountered in the Brazilian state of Acre in 2009.

Based on archaeological evidence from an excavation at Caverna da Pedra Pintada, human inhabitants first settled in the Amazon region at least 11,200 years ago.[18] Subsequent development led to late-prehistoric settlements along the periphery of the forest by AD 1250, which induced alterations in the forest cover.[19]

Geoglyphs on deforested land in the Amazon rainforest, Acre.

For a long time, it was thought that the Amazon rainforest was only ever sparsely populated, as it was impossible to sustain a large population through agriculture given the poor soil. Archeologist Betty Meggers was a prominent proponent of this idea, as described in her book Amazonia: Man and Culture in a Counterfeit Paradise. She claimed that a population density of 0.2 inhabitants per square kilometre (0.52/sq mi) is the maximum that can be sustained in the rainforest through hunting, with agriculture needed to host a larger population.[20] However, recent anthropological findings have suggested that the region was actually densely populated. Some 5 million people may have lived in the Amazon region in AD 1500, divided between dense coastal settlements, such as that at Marajó, and inland dwellers.[21] By 1900, the population had fallen to 1 million and by the early 1980s it was less than 200,000.[21]

The first European to travel the length of the Amazon River was Francisco de Orellana in 1542.[22] The BBC's Unnatural Histories presents evidence that Orellana, rather than exaggerating his claims as previously thought, was correct in his observations that a complex civilization was flourishing along the Amazon in the 1540s. It is believed that the civilization was later devastated by the spread of diseases from Europe, such as smallpox.[23]

Since the 1970s, numerous geoglyphs have been discovered on deforested land dating between AD 1–1250, furthering claims about Pre-Columbian civilizations.[24][25] Ondemar Dias is accredited with first discovering the geoglyphs in 1977, and Alceu Ranzi is credited with furthering their discovery after flying over Acre.[23][26] The BBC's Unnatural Histories presented evidence that the Amazon rainforest, rather than being a pristine wilderness, has been shaped by man for at least 11,000 years through practices such as forest gardening and terra preta.[23] Terra preta is found over large areas in the Amazon forest; and is now widely accepted as a product of indigenous soil management. The development of this fertile soil allowed agriculture and silviculture in the previously hostile environment; meaning that large portions of the Amazon rainforest are probably the result of centuries of human management, rather than naturally occurring as has previously been supposed.[27] In the region of the Xingu tribe, remains of some of these large settlements in the middle of the Amazon forest were found in 2003 by Michael Heckenberger and colleagues of the University of Florida. Among those were evidence of roads, bridges and large plazas.[28]

On 3 September 1989, Varig Flight 254 crashed into the Amazon, killing 13 out of the 54 people on board.[29] On 26 September 2006, Gol Transportes Aéreos Flight 1907, a Boeing 737-800, collided with an embraer Legacy 600 above the amazon. The legacy jet landed safely, but flight 1907 lost control, broke up in mid-air, and crashed into the Amazon, killing all 154 people onboard.[30]

Biodiversity Deforestation in the Amazon rainforest threatens many species of tree frogs, which are very sensitive to environmental changes (pictured: giant leaf frog) Scarlet macaw, which is indigenous to the American tropics.

Wet tropical forests are the most species-rich biome, and tropical forests in the Americas are consistently more species rich than the wet forests in Africa and Asia.[31] As the largest tract of tropical rainforest in the Americas, the Amazonian rainforests have unparalleled biodiversity. One in ten known species in the world lives in the Amazon rainforest.[32] This constitutes the largest collection of living plants and animal species in the world.

The region is home to about 2.5 million insect species,[33] tens of thousands of plants, and some 2,000 birds and mammals. To date, at least 40,000 plant species, 2,200 fishes,[34] 1,294 birds, 427 mammals, 428 amphibians, and 378 reptiles have been scientifically classified in the region.[35] One in five of all bird species are found in the Amazon rainforest, and one in five of the fish species live in Amazonian rivers and streams. Scientists have described between 96,660 and 128,843 invertebrate species in Brazil alone.[36]

The biodiversity of plant species is the highest on Earth with one 2001 study finding a quarter square kilometer (62 acres) of Ecuadorian rainforest supports more than 1,100 tree species.[37] A study in 1999 found one square kilometer (247 acres) of Amazon rainforest can contain about 90,790 tonnes of living plants. The average plant biomass is estimated at 356 ± 47 tonnes per hectare.[38] To date, an estimated 438,000 species of plants of economic and social interest have been registered in the region with many more remaining to be discovered or catalogued.[39] The total number of tree species in the region is estimated at 16,000.[2]

A giant, bundled liana in western Brazil

The green leaf area of plants and trees in the rainforest varies by about 25% as a result of seasonal changes. Leaves expand during the dry season when sunlight is at a maximum, then undergo abscission in the cloudy wet season. These changes provide a balance of carbon between photosynthesis and respiration.[40]

The rainforest contains several species that can pose a hazard. Among the largest predatory creatures are the black caiman, jaguar, cougar, and anaconda. In the river, electric eels can produce an electric shock that can stun or kill, while piranha are known to bite and injure humans.[41] Various species of poison dart frogs secrete lipophilic alkaloid toxins through their flesh. There are also numerous parasites and disease vectors. Vampire bats dwell in the rainforest and can spread the rabies virus.[42] Malaria, yellow fever and Dengue fever can also be contracted in the Amazon region.

Deforestation Deforestation in the Maranhão state of Brazil, 2016 Main articles: Deforestation of the Amazon rainforest, Trans-Amazonian highway, and Trans-Amazonian Railway

Deforestation is the conversion of forested areas to non-forested areas. The main sources of deforestation in the Amazon are human settlement and development of the land.[43] In 2018, about 17% of the Amazon rainforest was already destroyed. Research suggests that upon reaching about 20%-25% (hence 3% - 8% more), the tipping point to flip it into a non-forest ecosystems -degraded savannah- (in eastern, southern and central Amazonia) will be reached.[44][45]

Prior to the early 1960s, access to the forest's interior was highly restricted, and the forest remained basically intact.[46] Farms established during the 1960s were based on crop cultivation and the slash and burn method. However, the colonists were unable to manage their fields and the crops because of the loss of soil fertility and weed invasion.[47] The soils in the Amazon are productive for just a short period of time, so farmers are constantly moving to new areas and clearing more land.[47] These farming practices led to deforestation and caused extensive environmental damage.[48] Deforestation is considerable, and areas cleared of forest are visible to the naked eye from outer space.

In the 1970s, construction began on the Trans-Amazonian highway. This highway represented a major threat to the Amazon rainforest.[49] The highway still has not been completed, limiting the environmental damage.

Between 1991 and 2000, the total area of forest lost in the Amazon rose from 415,000 to 587,000 square kilometres (160,000 to 227,000 sq mi), with most of the lost forest becoming pasture for cattle.[50] Seventy percent of formerly forested land in the Amazon, and 91% of land deforested since 1970, have been used for livestock pasture.[51][52] Currently, Brazil is the second-largest global producer of soybeans after the United States. New research however, conducted by Leydimere Oliveira et al., has shown that the more rainforest is logged in the Amazon, the less precipitation reaches the area and so the lower the yield per hectare becomes. So despite the popular perception, there has been no economical advantage for Brazil from logging rainforest zones and converting these to pastoral fields.[53]

The needs of soy farmers have been used to justify many of the controversial transportation projects that are currently developing in the Amazon. The first two highways successfully opened up the rainforest and led to increased settlement and deforestation. The mean annual deforestation rate from 2000 to 2005 (22,392 km2 or 8,646 sq mi per year) was 18% higher than in the previous five years (19,018 km2 or 7,343 sq mi per year).[54] Although deforestation declined significantly in the Brazilian Amazon between 2004 and 2014, there has been an increase to the present day.[55]

Since the discovery of fossil fuel reservoirs in the Amazon rainforest, oil drilling activity has steadily increased, peaking in the Western Amazon in the 1970s and ushering another drilling boom in the 2000s.[56] As oil companies have to set up their operations by opening roads through forests, which often contributes to deforestation in the region.[57]

Conservation and climate change See also: Gaviotas Amazon rainforest

Environmentalists are concerned about loss of biodiversity that will result from destruction of the forest, and also about the release of the carbon contained within the vegetation, which could accelerate global warming. Amazonian evergreen forests account for about 10% of the world's terrestrial primary productivity and 10% of the carbon stores in ecosystems[58] – of the order of 1.1 × 1011 metric tonnes of carbon.[59] Amazonian forests are estimated to have accumulated 0.62 ± 0.37 tons of carbon per hectare per year between 1975 and 1996.[59]

One computer model of future climate change caused by greenhouse gas emissions shows that the Amazon rainforest could become unsustainable under conditions of severely reduced rainfall and increased temperatures, leading to an almost complete loss of rainforest cover in the basin by 2100.[60][61] However, simulations of Amazon basin climate change across many different models are not consistent in their estimation of any rainfall response, ranging from weak increases to strong decreases.[62] The result indicates that the rainforest could be threatened though the 21st century by climate change in addition to deforestation.

In 1989, environmentalist C.M. Peters and two colleagues stated there is economic as well as biological incentive to protecting the rainforest. One hectare in the Peruvian Amazon has been calculated to have a value of $6820 if intact forest is sustainably harvested for fruits, latex, and timber; $1000 if clear-cut for commercial timber (not sustainably harvested); or $148 if used as cattle pasture.[63]

As indigenous territories continue to be destroyed by deforestation and ecocide, such as in the Peruvian Amazon[64] indigenous peoples' rainforest communities continue to disappear, while others, like the Urarina continue to struggle to fight for their cultural survival and the fate of their forested territories. Meanwhile, the relationship between non-human primates in the subsistence and symbolism of indigenous lowland South American peoples has gained increased attention, as have ethno-biology and community-based conservation efforts.

From 2002 to 2006, the conserved land in the Amazon rainforest almost tripled and deforestation rates dropped up to 60%. About 1,000,000 square kilometres (250,000,000 acres) have been put onto some sort of conservation, which adds up to a current amount of 1,730,000 square kilometres (430,000,000 acres).[65]

In April 2019 the court in Ecuador stopped oil exploration activities in 1,800 square kilometers of the Amazon rainforest[66]

In July 2019 the court on Equador, forbade the government to sell territory with forests to oil companies[67]

A 2009 study found that a 4 °C rise (above pre-industrial levels) in global temperatures by 2100 would kill 85% of the Amazon rainforest while a temperature rise of 3 °C would kill some 75% of the Amazon.[68]

Deforestation in the Amazon rainforest region has a negative impact on local climate. It was one of the main causes of the severe Drought of 2014-2015 in Brazil.[69][70] This is because the moisture from the forests is important to the rainfall in Brazil, Paraguay and Argentina. Half of the rainfall in the Amazon area is produced by the forests.[71]

Remote sensing This image reveals how the forest and the atmosphere interact to create a uniform layer of "popcorn-shaped" cumulus clouds.

The use of remotely sensed data is dramatically improving conservationists' knowledge of the Amazon basin. Given the objectivity and lowered costs of satellite-based land cover analysis, it appears likely that remote sensing technology will be an integral part of assessing the extent and damage of deforestation in the basin.[72] Furthermore, remote sensing is the best and perhaps only possible way to study the Amazon on a large scale.[73]

The use of remote sensing for the conservation of the Amazon is also being used by the indigenous tribes of the basin to protect their tribal lands from commercial interests. Using handheld GPS devices and programs like Google Earth, members of the Trio Tribe, who live in the rainforests of southern Suriname, map out their ancestral lands to help strengthen their territorial claims.[74] Currently, most tribes in the Amazon do not have clearly defined boundaries, making it easier for commercial ventures to target their territories.

To accurately map the Amazon's biomass and subsequent carbon related emissions, the classification of tree growth stages within different parts of the forest is crucial. In 2006, Tatiana Kuplich organized the trees of the Amazon into four categories: (1) mature forest, (2) regenerating forest , (3) regenerating forest , and (4) regenerating forest .[75] The researcher used a combination of Synthetic aperture radar (SAR) and Thematic Mapper (TM) to accurately place the different portions of the Amazon into one of the four classifications.

Impact of early 21st-century Amazon droughts

In 2005, parts of the Amazon basin experienced the worst drought in one hundred years,[76] and there were indications that 2006 may have been a second successive year of drought.[77] A 23 July 2006 article in the UK newspaper The Independent reported the Woods Hole Research Center results, showing that the forest in its present form could survive only three years of drought.[78][79] Scientists at the Brazilian National Institute of Amazonian Research argued in the article that this drought response, coupled with the effects of deforestation on regional climate, are pushing the rainforest towards a "tipping point" where it would irreversibly start to die. It concluded that the forest is on the brink of being turned into savanna or desert, with catastrophic consequences for the world's climate.

According to the World Wide Fund for Nature, the combination of climate change and deforestation increases the drying effect of dead trees that fuels forest fires.[80]

In 2010, the Amazon rainforest experienced another severe drought, in some ways more extreme than the 2005 drought. The affected region was approximately 1,160,000 square miles (3,000,000 km2) of rainforest, compared with 734,000 square miles (1,900,000 km2) in 2005. The 2010 drought had three epicenters where vegetation died off, whereas in 2005, the drought was focused on the southwestern part. The findings were published in the journal Science. In a typical year, the Amazon absorbs 1.5 gigatons of carbon dioxide; during 2005 instead 5 gigatons were released and in 2010 8 gigatons were released.[81][82] Additional severe droughts occurred in 2010, 2015, and 2016.[83]

In 2019 Brazil's protections of the Amazon Rain Forest were slashed, resulting in a severe loss of trees.[84]

See also
  • Amanyé
  • Amazon Conservation Association
  • Amazon Conservation Team (ACT)
  • Amazonian manatee
  • Amazon Surveillance System (Sistema de Vigilância da Amazônia)
  • Amazon Watch
  • Atlantic Forest
  • Bandeirantes
  • Coordinator of Indigenous Organizations of the Amazon River Basin (COICA)
  • Jungle
  • List of plants of Amazon Rainforest vegetation of Brazil
  • Rainforest Action Network
  • Rainforest Alliance
  • Rainforest Foundation Fund
  • Save the Amazon Rainforest Organisation (STARO)
  • Tapiche Ohara's Reserve
Notes and references
  1. ^ Portuguese: Floresta amazônica or Amazônia; Spanish: Selva amazónica, Amazonía or usually Amazonia; French: Forêt amazonienne; Dutch: Amazoneregenwoud
  1. ^ "WNF: Places: Amazon". Retrieved June 4, cite.citation{font-style:inherit}.mw-parser-output .citation q{quotes:"\"""\"""'""'"}.mw-parser-output .citation .cs1-lock-free a{background:url("//")no-repeat;background-position:right .1em center}.mw-parser-output .citation .cs1-lock-limited a,.mw-parser-output .citation .cs1-lock-registration a{background:url("//")no-repeat;background-position:right .1em center}.mw-parser-output .citation .cs1-lock-subscription a{background:url("//")no-repeat;background-position:right .1em center}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration{color:#555}.mw-parser-output .cs1-subscription span,.mw-parser-output .cs1-registration span{border-bottom:1px dotted;cursor:help}.mw-parser-output .cs1-ws-icon a{background:url("//")no-repeat;background-position:right .1em center}.mw-parser-output code.cs1-code{color:inherit;background:inherit;border:inherit;padding:inherit}.mw-parser-output .cs1-hidden-error{display:none;font-size:100%}.mw-parser-output .cs1-visible-error{font-size:100%}.mw-parser-output .cs1-maint{display:none;color:#33aa33;margin-left:0.3em}.mw-parser-output .cs1-subscription,.mw-parser-output .cs1-registration,.mw-parser-output .cs1-format{font-size:95%}.mw-parser-output .cs1-kern-left,.mw-parser-output .cs1-kern-wl-left{padding-left:0.2em}.mw-parser-output .cs1-kern-right,.mw-parser-output .cs1-kern-wl-right{padding-right:0.2em}
  2. ^ a b "Field Museum scientists estimate 16,000 tree species in the Amazon". Field Museum. October 17, 2013. Retrieved October 18, 2013.
  3. ^ a b Taylor, Isaac (1898). Names and Their Histories: A Handbook of Historical Geography and Topographical Nomenclature. London: Rivingtons. ISBN 978-0-559-29668-0. Retrieved October 12, 2008.
  4. ^ Morley, Robert J. (2000). Origin and Evolution of Tropical Rain Forests. Wiley. ISBN 978-0-471-98326-2.
  5. ^ Burnham, Robyn J.; Johnson, Kirk R. (2004). "South American palaeobotany and the origins of neotropical rainforests". Philosophical Transactions of the Royal Society. 359 (1450): 1595–1610. doi:10.1098/rstb.2004.1531. PMC 1693437. PMID 15519975.
  6. ^ Maslin, Mark; Malhi, Yadvinder; Phillips, Oliver; Cowling, Sharon (2005). "New views on an old forest: assessing the longevity, resilience and future of the Amazon rainforest" (PDF). Transactions of the Institute of British Geographers. 30 (4): 477–499. doi:10.1111/j.1475-5661.2005.00181.x. Archived from the original (PDF) on October 1, 2008. Retrieved September 25, 2008.
  7. ^ Malhi, Yadvinder; Phillips, Oliver (2005). Tropical Forests & Global Atmospheric Change. Oxford University Press. ISBN 978-0-19-856706-6.
  8. ^ Costa, João Batista Sena; Bemerguy, Ruth Léa; Hasui, Yociteru; Borges, Maurício da Silva (2001). "Tectonics and paleogeography along the Amazon river". Journal of South American Earth Sciences. 14 (4): 335–347. Bibcode:2001JSAES..14..335C. doi:10.1016/S0895-9811(01)00025-6.
  9. ^ Milani, Edison José; Zalán, Pedro Victor (1999). "An outline of the geology and petroleum systems of the Paleozoic interior basins of South America" (PDF). Episodes. 22 (3): 199–205. Archived from the original (PDF) on October 1, 2008. Retrieved September 25, 2008.
  10. ^ Colinvaux, Paul A.; Oliveira, Paulo E. De (2000). "Palaeoecology and climate of the Amazon basin during the last glacial cycle". Journal of Quaternary Science. 15 (4): 347–356. Bibcode:2000JQS....15..347C. doi:10.1002/1099-1417(200005)15:4<347::AID-JQS537>3.0.CO;2-A.
  11. ^ Van Der Hammen, Thomas; Hooghiemstra, Henry (2000). "Neogene and Quaternary history of vegetation, climate, and plant diversity in Amazonia". Quaternary Science Reviews. 19 (8): 725. Bibcode:2000QSRv...19..725V. CiteSeerX doi:10.1016/S0277-3791(99)00024-4.
  12. ^ Colinvaux, P.A.; De Oliveira, P.E.; Bush, M.B. (January 2000). "Amazonian and neotropical plant communities on glacial time-scales: The failure of the aridity and refuge hypotheses". Quaternary Science Reviews. 19 (1–5): 141–169. Bibcode:2000QSRv...19..141C. doi:10.1016/S0277-3791(99)00059-1.
  13. ^ Yu, Hongbin (2015). "The fertilizing role of African dust in the Amazon rainforest: A first multiyear assessment based on data from Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observations". Geophysical Research Letters. 42 (6): 1984–1991. Bibcode:2015GeoRL..42.1984Y. doi:10.1002/2015GL063040.
  14. ^ Garner, Rob (February 24, 2015). "Saharan Dust Feeds Amazon's Plants". NASA.
  15. ^ "Desert Dust Feeds Amazon Forests – NASA Science".
  16. ^ Barkley, Anne E.; Prospero, Joseph M.; Mahowald, Natalie; Hamilton, Douglas S.; Popendorf, Kimberly J.; Oehlert, Amanda M.; Pourmand, Ali; Gatineau, Alexandre; Panechou-Pulcherie, Kathy; Blackwelder, Patricia; Gaston, Cassandra J. (August 13, 2019). "African biomass burning is a substantial source of phosphorus deposition to the Amazon, Tropical Atlantic Ocean, and Southern Ocean". Proceedings of the National Academy of Sciences. 116 (33): 16216–16221. doi:10.1073/pnas.1906091116.
  17. ^ "Smoke from Africa fertilizes the Amazon and tropical ocean regions with soluble phosphorous".
  18. ^ Roosevelt, A.C.; da Costa, M. Lima; Machado, C. Lopes; Michab, M.; Mercier, N.; Valladas, H.; Feathers, J.; Barnett, W.; da Silveira, M. Imazio; Henderson, A.; Sliva, J.; Chernoff, B.; Reese, D.S.; Holman, J.A.; Toth, N.; Schick, K. (April 19, 1996). "Paleoindian Cave Dwellers in the Amazon: The Peopling of the Americas". Science. 272 (5260): 373–384. Bibcode:1996Sci...272..373R. doi:10.1126/science.272.5260.373.
  19. ^ Heckenberger, Michael J.; Kuikuro, Afukaka; Kuikuro, Urissapá Tabata; Russell, J. Christian; Schmidt, Morgan; Fausto, Carlos; Franchetto, Bruna (September 19, 2003). "Amazonia 1492: Pristine Forest or Cultural Parkland?". Science. 301 (5640): 1710–1714. Bibcode:2003Sci...301.1710H. doi:10.1126/science.1086112. PMID 14500979.
  20. ^ Meggers, Betty J. (December 19, 2003). "Revisiting Amazonia Circa 1492". Science. 302 (5653): 2067–2070. doi:10.1126/science.302.5653.2067b. PMID 14684803.
  21. ^ a b Chris C. Park (2003). Tropical Rainforests. Routledge. p. 108. ISBN 978-0-415-06239-8.
  22. ^ Smith, A (1994). Explorers of the Amazon. Chicago: University of Chicago Press. ISBN 978-0-226-76337-8.
  23. ^ a b c "Unnatural Histories – Amazon". BBC Four.
  24. ^ Simon Romero (January 14, 2012). "Once Hidden by Forest, Carvings in Land Attest to Amazon's Lost World". The New York Times.
  25. ^ Martti Pärssinen; Denise Schaan; Alceu Ranzi (2009). "Pre-Columbian geometric earthworks in the upper Purús: a complex society in western Amazonia". Antiquity. 83 (322): 1084–1095. doi:10.1017/s0003598x00099373.
  26. ^ Junior, Gonçalo (October 2008). "Amazonia lost and found". Pesquisa (ed.220).
  27. ^ The influence of human alteration has been generally underestimated, reports Darna L. Dufour: "Much of what has been considered natural forest in Amazonia is probably the result of hundreds of years of human use and management." "Use of Tropical Rainforests by Native Amazonians," BioScience 40, no. 9 (October 1990):658. For an example of how such peoples integrated planting into their nomadic lifestyles, see Rival, Laura (1993). "The Growth of Family Trees: Understanding Huaorani Perceptions of the Forest". Man. 28 (4): 635–652. doi:10.2307/2803990. JSTOR 2803990.
  28. ^ Heckenberger, M.J.; Kuikuro, A; Kuikuro, UT; Russell, JC; Schmidt, M; Fausto, C; Franchetto, B (September 19, 2003), "Amazonia 1492: Pristine Forest or Cultural Parkland?", Science (published 2003), 301 (5640), pp. 1710–14, Bibcode:2003Sci...301.1710H, doi:10.1126/science.1086112, PMID 14500979
  29. ^ Ranter, Harro. "ASN Aircraft accident Boeing 737-241 PP-VMK São José do Xingu, MT".
  30. ^ Ranter, Harro. "ASN Aircraft accident Boeing 737-8EH PR-GTD Peixoto Azevedo, MT".
  31. ^ Turner, I.M. 2001. The ecology of trees in the tropical rain forest. Cambridge University Press, Cambridge. ISBN 0-521-80183-4
  32. ^ "Amazon Rainforest, Amazon Plants, Amazon River Animals". World Wide Fund for Nature. Archived from the original on May 17, 2008. Retrieved May 6, 2008.
  33. ^ "Photos / Pictures of the Amazon Rainforest". Archived from the original on December 17, 2008. Retrieved December 18, 2008.
  34. ^ James S. Albert; Roberto E. Reis (March 8, 2011). Historical Biogeography of Neotropical Freshwater Fishes. University of California Press. p. 308. Archived from the original on June 30, 2011. Retrieved June 28, 2011.
  35. ^ Da Silva; Jose Maria Cardoso; et al. (2005). "The Fate of the Amazonian Areas of Endemism". Conservation Biology. 19 (3): 689–694. doi:10.1111/j.1523-1739.2005.00705.x.
  36. ^ Lewinsohn, Thomas M.; Paulo Inácio Prado (June 2005). "How Many Species Are There in Brazil?". Conservation Biology. 19 (3): 619–624. doi:10.1111/j.1523-1739.2005.00680.x.
  37. ^ Wright, S. Joseph (October 12, 2001). "Plant diversity in tropical forests: a review of mechanisms of species coexistence". Oecologia. 130 (1): 1–14. Bibcode:2002Oecol.130....1W. doi:10.1007/s004420100809. PMID 28547014.
  38. ^ Laurance, William F.; Fearnside, Philip M.; Laurance, Susan G.; Delamonica, Patricia; Lovejoy, Thomas E.; Rankin-de Merona, Judy M.; Chambers, Jeffrey Q.; Gascon, Claude (June 14, 1999). "Relationship between soils and Amazon forest biomass: a landscape-scale study". Forest Ecology and Management. 118 (1–3): 127–138. doi:10.1016/S0378-1127(98)00494-0.
  39. ^ "Amazon Rainforest". South AmericaTravel Guide. Archived from the original on August 12, 2008. Retrieved August 19, 2008.
  40. ^ Mynenia, Ranga B.; et al. (March 13, 2007). "Large seasonal swings in leaf area of Amazon rainforests". Proceedings of the National Academy of Sciences. 104 (12): 4820–4823. Bibcode:2007PNAS..104.4820M. doi:10.1073/pnas.0611338104. PMC 1820882. PMID 17360360.
  41. ^ "Piranha 'less deadly than feared'". BBC News. July 2, 2007. Archived from the original on July 7, 2007. Retrieved July 2, 2007.
  42. ^ da Rosa; Elizabeth S. T.; et al. (August 2006). "Bat-transmitted Human Rabies Outbreaks, Brazilian Amazon". Emerging Infectious Diseases. 12 (8): 1197–1202. doi:10.3201/eid1708.050929. PMC 3291204. PMID 16965697.
  43. ^ Various (2001). Bierregaard, Richard; Gascon, Claude; Lovejoy, Thomas E.; Mesquita, Rita (eds.). Lessons from Amazonia: The Ecology and Conservation of a Fragmented Forest. Yale University Press. ISBN 978-0-300-08483-2.
  44. ^ Amazon Rainforest 'heading to point of no return'
  45. ^ Amazon Tipping Point
  46. ^ Kirby, Kathryn R.; Laurance, William F.; Albernaz, Ana K.; Schroth, Götz; Fearnside, Philip M.; Bergen, Scott; M. Venticinque, Eduardo; Costa, Carlos da (2006). "The future of deforestation in the Brazilian Amazon" (PDF). Futures. 38 (4): 432–453. CiteSeerX doi:10.1016/j.futures.2005.07.011.
  47. ^ a b Watkins and Griffiths, J. (2000). Forest Destruction and Sustainable Agriculture in the Brazilian Amazon: a Literature Review (Doctoral dissertation, The University of Reading, 2000). Dissertation Abstracts International, 15–17
  48. ^ Williams, M. (2006). Deforesting the Earth: From Prehistory to Global Crisis (Abridged ed.). Chicago: The University of Chicago Press. ISBN 978-0-226-89947-3.
  49. ^ "Impacts and Causes of Deforestation in the Amazon Basin".
  50. ^ Centre for International Forestry Research (CIFOR) (2004)
  51. ^ Steinfeld, Henning; Gerber, Pierre; Wassenaar, T.D.; Castel, Vincent (2006). Livestock's Long Shadow: Environmental Issues and Options. Food and Agriculture Organization of the United Nations. ISBN 978-92-5-105571-7. Archived from the original on July 26, 2008. Retrieved August 19, 2008.
  52. ^ Margulis, Sergio (2004). Causes of Deforestation of the Brazilian Amazon (PDF). World Bank Working Paper No. 22. Washington, DC: The World Bank. ISBN 978-0-8213-5691-3. Archived (PDF) from the original on September 10, 2008. Retrieved September 4, 2008.
  53. ^ "Research paper of Leydimere Oliveira on the amazon". Archived from the original on August 3, 2013.
  54. ^ Barreto, P.; Souza Jr. C.; Noguerón, R.; Anderson, A. & Salomão, R. 2006. Human Pressure on the Brazilian Amazon Forests[permanent dead link]. Imazon. Retrieved 28 September 2006. (The Imazon web site contains many resources relating to the Brazilian Amazonia.)
  55. ^ "INPE: Estimativas Anuais desde 1988 até 2009".
  56. ^ "Oil Drilling Contaminated Western Amazon".
  57. ^ "Oil and Gas Extraction in the Amazon".
  58. ^ Melillo, J.M.; McGuire, A.D.; Kicklighter, D.W.; Moore III, B.; Vörösmarty, C.J.; Schloss, A.L. (May 20, 1993). "Global climate change and terrestrial net primary production". Nature. 363 (6426): 234–240. Bibcode:1993Natur.363..234M. doi:10.1038/363234a0.
  59. ^ a b Tian, H.; Melillo, J.M.; Kicklighter, D.W.; McGuire, A.D.; Helfrich III, J.; Moore III, B.; Vörösmarty, C.J. (July 2000). "Climatic and biotic controls on annual carbon storage in Amazonian ecosystems". Global Ecology and Biogeography. 9 (4): 315–335. doi:10.1046/j.1365-2699.2000.00198.x.
  60. ^ Cox, Betts, Jones, Spall and Totterdell. 2000. "Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model". Nature, 9 November 2000. (subscription required)
  61. ^ Radford, T. 2002. "World may be warming up even faster". The Guardian.
  62. ^ Houghton, J.T. et al. 2001. "Climate Change 2001: The Scientific Basis" Archived 7 May 2006 at the Wayback Machine. Intergovernmental Panel on Climate Change.
  63. ^ Peters, C.M.; Gentry, A.H.; Mendelsohn, R. O. (1989). "Valuation of an Amazonian forest". Nature. 339 (6227): 656–657. Bibcode:1989Natur.339..655P. doi:10.1038/339655a0.
  64. ^ Dean, Bartholomew. (2003) State Power and Indigenous Peoples in Peruvian Amazonia: A Lost Decade, 1990–2000. In The Politics of Ethnicity Indigenous Peoples in Latin American States David Maybury-Lewis, Ed. Harvard University Press
  65. ^ Cormier, L. (April 16, 2006). "A Preliminary Review of Neotropical Primates in the Subsistence and Symbolism of Indigenous Lowland South American Peoples". Ecological and Environmental Anthropology. 2 (1): 14–32. Archived from the original on December 21, 2008. Retrieved September 4, 2008.
  66. ^ "Ecuador Amazon tribe win first victory against oil companies". Devdiscourse. April 27, 2019. Retrieved April 28, 2019.
  67. ^ "Ecuador court rules Amazon rainforest can't be sold to oil companies". Newshub. Reuters. July 13, 2019. Retrieved July 19, 2019.
  68. ^ David Adam (March 11, 2009). "Amazon could shrink by 85% due to climate change, scientists say". the Guardian.
  69. ^ Watts, Jonathan (November 28, 2017). "The Amazon effect: how deforestation is starving São Paulo of water". The Guardian. Retrieved November 8, 2018.
  70. ^ Verchot, Louis (January 29, 2015). "The science is clear: Forest loss behind Brazil's drought". Center for International Forestry Research (CIFOR). Retrieved November 8, 2018.
  71. ^ E. Lovejoy, Thomas; Nobre, Carlos (February 21, 2018). "Amazon Tipping Point". Science Advances. 4 (2): eaat2340. Bibcode:2018SciA....4.2340L. doi:10.1126/sciadv.aat2340. PMC 5821491. PMID 29492460.
  72. ^ Wynne, R.H.; Joseph, K.A.; Browder, J.O.; Summers, P.M. (2007). "A Preliminary Review of Neotropical Primates in the Subsistence and Symbolism of Indigenous Lowland South American Peoples". International Journal of Remote Sensing. 28 (6): 1299–1315. Bibcode:2007IJRS...28.1299W. doi:10.1080/01431160600928609. Archived from the original on December 21, 2008. Retrieved September 4, 2008.
  73. ^ Asner, Gregory P.; Knapp, David E.; Cooper, Amanda N.; Bustamante, Mercedes M.C.; Olander, Lydia P. (June 2005). "Ecosystem Structure throughout the Brazilian Amazon from Landsat Observations and Automated Spectral Unmixing". Earth Interactions. 9 (1): 1–31. Bibcode:2005EaInt...9g...1A. doi:10.1175/EI134.1.
  74. ^ Isaacson, Andy. 2007. With the Help of GPS, Amazonian Tribes Reclaim the Rain Forest. Wired 15.11:
  75. ^ Kuplich, Tatiana M. (October 2006). "Classifying regenerating forest stages in Amazônia using remotely sensed images and a neural network". Forest Ecology and Management. 234 (1–3): 1–9. doi:10.1016/j.foreco.2006.05.066.
  76. ^ "Amazon Drought Worst in 100 Years".
  77. ^ Drought Threatens Amazon Basin – Extreme conditions felt for second year running, Paul Brown, The Guardian, 16 July 2006. Retrieved 23 August 2014
  78. ^ "Amazon rainforest 'could become a desert'" Archived 6 August 2006 at the Wayback Machine, The Independent, 23 July 2006. Retrieved 28 September 2006.
  79. ^ "Dying Forest: One year to save the Amazon", The Independent, 23 July 2006. Retrieved 23 August 2014.
  80. ^ "Climate change a threat to Amazon rainforest, warns WWF", World Wide Fund for Nature, 22 March 2006. Retrieved 23 August 2014.
  81. ^ 2010 Amazon drought record: 8 Gt extra CO2, Rolf Schuttenhelm, Bits Of Science, 4 February 2011. Retrieved 23 August 2014
  82. ^ "Amazon drought 'severe' in 2010, raising warming fears", BBC News, 3 February 2011. Retrieved 23 August 2014
  83. ^ Abraham, John (August 3, 2017). "Study finds human influence in the Amazon's third 1-in-100 year drought since 2005". the Guardian.
  84. ^ Casado, Letícia; Londoño, Ernesto (July 28, 2019). "Under Brazil's Far Right Leader, Amazon Protections Slashed and Forests Fall". The New York Times. Retrieved July 28, 2019.
Further reading
  • Bunker, S.G. (1985) Underdeveloping the Amazon: Extraction, Unequal Exchange, and the Failure of the Modern State. University of Illinois Press.
  • Cleary, David. (2000) “Towards an Environmental History of the Amazon: From Pre-history to the Nineteenth Century.” Latin American Research Review 36:2, 64-96
  • Dean, Warren. (1976) Rio Claro: A Brazilian Plantation System, 1820-1920. Stanford University Press.
  • Dean, Warren. (1997) Brazil and the Struggle for Rubber: A Study in Environmental History. Cambridge University Press.
  • Hecht, Susanna and Alexander Cockburn (1990). The Fate of the Forest: Developers, Destroyers, and Defenders of the Amazon. New York: Harper Perennial.
  • Hochstetler, K. and M. Keck (2007) Greening Brazil: Environmental Activism in State and Society. Duke University Press.
  • Revkin, A. (1990) The Burning Season: The Murder of Chico Mendes and the Fight for the Amazon Rain Forest. Houghton Mifflin.
  • Wade, Lizzie. (2015). "Drones and satellites spot lost civilizations in unlikely places." Science (American Association for the Advancement of Science), doi:10.1126/science.aaa7864
  • Weinstein, Barbara (1983) The Amazon Rubber Boom 1850-1920. Stanford University Press.
  • Sheil, D.; Wunder, S. (2002). "The value of tropical forest to local communities: complications, caveats, and cautions". Conservation Ecology. 6 (2): 9. doi:10.5751/ES-00458-060209. hdl:10535/2768.
External links Wikivoyage has a travel guide for Amazonia.

Media related to Amazon Rainforest at Wikimedia Commons

  • Journey Into Amazonia
  • The Amazon: The World's Largest Rainforest
  • WWF in the Amazon rainforest
  • Good daily updated Amazon information database on the web, held by Friends of The Earth – Brazilian Amazon.
  • Sustainable Development in the Extractive Reserve of the Baixo Rio Branco – Rio Jauaperi – Brazilian Amazon.
  • Amazon Rainforest News Original news updates on the Amazon.
  • Information about the Amazon rainforest, its people, places of interest, and how everyone can help.
  • Conference: Climate change and the fate of the Amazon. Podcasts of talks given at Oriel College, University of Oxford, 20–22 March 2007.
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  • Alpine states
  • Alpide belt
  • Visegrád Group
  • Rhineland
  • Eastphalia
  • Westphalia
  • Prussia
  • Lusatia
  • Bohemia
  • Moravia
  • Silesia
    • Czech Silesia
  • Pomerania
    • Pomerelia
    • Kashubia
  • Bukovina
  • Istria
  • Transdanubia
  • Polesia
  • Germania
    • Germania Slavica
  • Benelux
  • Low Countries
  • Northwest
  • British Isles
  • English Channel
  • Channel Islands
  • Cotentin Peninsula
  • Upper Rhine Plain
    • Upper Rhine
  • Gaul
  • Normandy
  • Brittany
  • Batavia
  • Gulf of Lion
  • Iberia
    • Al-Andalus
    • Baetic System
  • Pyrenees
  • Alpide belt
  • Po Valley (Padania)
  • Italian Peninsula
    • Tuscan Archipelago
  • Insular Italy
    • Aegadian Islands
  • Iberia
    • Al-Andalus
    • Baetic System
  • Gibraltar Arc
  • Southeastern
  • Mediterranean
  • Alpide belt
  • Germanic
  • Romance
  • Celtic
  • Slavic countries
  • Uralic
  • European Plain
  • Eurasian Steppe
  • Pontic–Caspian steppe
  • Wild Fields
  • Pannonian Basin
    • Great Hungarian Plain
    • Little Hungarian Plain
    • Eastern Slovak Lowland
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Regions of North AmericaNorth
  • Central Canada
  • Atlantic Canada
    • Atlantic Northeast
      • The Maritimes
  • Great Lakes region
  • Pacific Northwest
  • Prairie Pothole Region
  • Canadian Arctic Archipelago
  • Greenland
  • Canadian Prairies
  • The Maritimes
  • French Canada
  • English Canada
  • Acadia
    • Acadian Peninsula
  • Quebec City–Windsor Corridor
  • Peace River Country
  • Cypress Hills
  • Palliser's Triangle
  • Canadian Shield
  • Interior Alaska-Yukon lowland taiga
  • Kodiak Island
  • Newfoundland (island)
  • Vancouver Island
  • Gulf Islands
  • Strait of Georgia
  • Labrador Peninsula
  • Gaspé Peninsula
  • Avalon Peninsula
    • Bay de Verde Peninsula
  • Brodeur Peninsula
  • Melville Peninsula
  • Bruce Peninsula
  • Banks Peninsula (Nunavut)
  • Cook Peninsula
  • Gulf of Boothia
  • Georgian Bay
  • Hudson Bay
  • James Bay
(United States)Arctic
  • Aleutian Arc
    • Aleutian Range
    • Alaska Peninsula
    • Aleutian Islands
  • Gulf of Alaska
  • East Coast
  • Northeast
    • Atlantic Northeast
      • The Maritimes
    • New England
    • Mid-Atlantic
    • Commonwealth
  • Northeast
  • West Coast
  • Mountain states
  • Intermountain West
  • Basin and Range Province
  • Northwestern United States
    • Inland Northwest
    • Pacific Northwest
  • Southwest
    • Old Southwest
    • Four Corners
  • Great Lakes
  • Tallgrass prairie
  • Midwest
    • Upper Midwest
  • South Central
    • Gulf Coast
  • Deep South
  • Upland South
  • Santa Fe de Nuevo México
  • Pacific Coast Ranges
  • Oregon Trail
  • Mormon Corridor
  • Calumet Region
  • Llano Estacado
  • Third Coast
  • Backcountry
  • Trans-Mississippi
  • Great North Woods
  • Great Plains
  • Interior Plains
  • Great Basin
    • Great Basin Desert
  • Acadia
  • Ozarks
  • Ark-La-Tex
  • Waxhaws
  • Siouxland
  • Twin Tiers
  • Driftless Area
  • Palouse
  • Piedmont
  • Atlantic coastal plain
  • Outer Lands
  • Black Dirt Region
  • Blackstone Valley
  • Piney Woods
  • Rocky Mountains
  • Mojave Desert
  • The Dakotas
  • The Carolinas
  • Shawnee Hills
  • San Fernando Valley
  • Tornado Alley
  • North Coast
  • Lost Coast
  • Emerald Triangle
  • San Francisco Bay Area
    • San Francisco Bay
    • North Bay
    • East Bay
    • Silicon Valley
  • Interior Alaska-Yukon lowland taiga
  • Gulf of Mexico
  • Lower Colorado River Valley
  • Sacramento–San Joaquin River Delta
  • Yukon–Kuskokwim Delta
  • Colville Delta
  • Arkansas Delta
  • Mobile–Tensaw River Delta
  • Mississippi Delta
  • Mississippi River Delta
  • Columbia River Estuary
  • Great Basin
  • High Desert
  • Monterey Peninsula
  • Upper Peninsula of Michigan
  • Lower Peninsula of Michigan
  • Virginia Peninsula
  • Keweenaw Peninsula
  • Middle Peninsula
  • Delmarva Peninsula
  • Alaska Peninsula
  • Kenai Peninsula
  • Niagara Peninsula
  • Bering Strait
  • "Belt" regions
    • Bible Belt
    • Black Belt
    • Corn Belt
    • Cotton Belt
    • Frost Belt
    • Rice Belt
    • Rust Belt
    • Sun Belt
    • Snow Belt
  • Basin and Range Province
  • Baja California Peninsula
  • Gulf of California
    • Colorado River Delta
  • Gulf of Mexico
  • Soconusco
  • Tierra Caliente
  • La Mixteca
  • La Huasteca
  • Bajío
  • Valley of Mexico
  • Mezquital Valley
  • Sierra Madre de Oaxaca
  • Yucatán Peninsula
  • Gulf of Mexico
  • Northern Triangle of Central America
  • Western Caribbean Zone
  • Isthmus of Panama
  • Gulf of Panama
    • Pearl Islands
  • Azuero Peninsula
  • Mosquito Coast
  • Antilles
    • Greater Antilles
    • Lesser Antilles
      • Leeward
      • Leeward Antilles
      • Windward
  • Lucayan Archipelago
  • Southern Caribbean
  • West Indies
  • Aridoamerica
  • Mesoamerica
  • Oasisamerica
  • Anglo
  • Latin
    • French
    • Hispanic
  • American Cordillera
  • Ring of Fire
  • LAC
  • v
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Regions of OceaniaAustralasia
  • Gulf of Carpentaria
  • Zealandia
    • Kula Gulf
  • Australia
    • Capital Country
    • Eastern Australia
    • Lake Eyre basin
    • Murray–Darling basin
    • Northern Australia
    • Nullarbor Plain
    • Outback
    • Southern Australia
      • Maralinga
    • Sunraysia
    • Great Victoria Desert
    • Gulf of Carpentaria
    • Gulf St Vincent
    • Lefevre Peninsula
    • Fleurieu Peninsula
    • Yorke Peninsula
    • Eyre Peninsula
    • Mornington Peninsula
    • Bellarine Peninsula
    • Mount Henry Peninsula
  • Islands Region
    • Bismarck Archipelago
  • Solomon Islands
    • North Solomon Islands
    • Solomon Islands
  • Fiji
  • New Caledonia
  • New Guinea
    • Papua New Guinea
    • Republic of West Papua
  • Vanuatu
  • Caroline Islands
    • Federated States of Micronesia
    • Palau
  • Kiribati
  • Mariana Islands
    • Guam
    • Northern Mariana Islands
  • Marshall Islands
  • Nauru
  • Wake Island
  • Easter Island
  • Hawaiian Islands
  • Cook Islands
  • French Polynesia
    • Austral Islands
    • Gambier Islands
    • Mangareva Islands
    • Marquesas Islands
    • Society Islands
    • Tuamotus
  • Kermadec Islands
  • New Zealand
    • South Island
    • North Island
  • Niue
  • Pitcairn Islands
  • Samoan Islands
    • American Samoa
    • Independent State of Samoa
  • Tokelau
  • Tonga
  • Tuvalu
  • Asia-Pacific
  • Ring of Fire
  • v
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Regions of South AmericaEast
  • Amazon basin
  • Atlantic Forest
  • Caatinga
  • Cerrado
  • Caribbean South America
  • West Indies
  • Los Llanos
  • The Guianas
  • Amazon basin
    • Amazon rainforest
  • Gulf of Paria
  • Paria Peninsula
  • Paraguaná Peninsula
  • Orinoco Delta
  • Tierra del Fuego
  • Patagonia
  • Pampas
  • Pantanal
  • Gran Chaco
  • Chiquitano dry forests
  • Valdes Peninsula
  • Triple Frontier
  • Andes
    • Tropical Andes
    • Wet Andes
    • Dry Andes
    • Pariacaca mountain range
  • Altiplano
  • Atacama Desert
  • Latin
  • Hispanic
  • Bolivarian
  • American Cordillera
  • Ring of Fire
  • LAC
  • v
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Earth's polar regionsAntarctic
  • Antarctic Peninsula
  • East Antarctica
  • West Antarctica
  • Eklund Islands
  • Ecozone
  • Extreme points
  • Islands
  • Arctic Alaska
  • British Arctic Territories
  • Canadian Arctic Archipelago
  • Finnmark
  • Greenland
  • Northern Canada
  • Northwest Territories
  • Nunavik
  • Nunavut
  • Russian Arctic
  • Sakha
  • Sápmi
  • Yukon
  • North American Arctic
  • v
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  • e
Earth's oceans and seasArctic Ocean
  • Amundsen Gulf
  • Barents Sea
  • Beaufort Sea
  • Chukchi Sea
  • East Siberian Sea
  • Greenland Sea
  • Gulf of Boothia
  • Kara Sea
  • Laptev Sea
  • Lincoln Sea
  • Prince Gustav Adolf Sea
  • Pechora Sea
  • Queen Victoria Sea
  • Wandel Sea
  • White Sea
Atlantic Ocean
  • Adriatic Sea
  • Aegean Sea
  • Alboran Sea
  • Archipelago Sea
  • Argentine Sea
  • Baffin Bay
  • Balearic Sea
  • Baltic Sea
  • Bay of Biscay
  • Bay of Bothnia
  • Bay of Campeche
  • Bay of Fundy
  • Black Sea
  • Bothnian Sea
  • Caribbean Sea
  • Celtic Sea
  • English Channel
  • Foxe Basin
  • Greenland Sea
  • Gulf of Bothnia
  • Gulf of Finland
  • Gulf of Lion
  • Gulf of Guinea
  • Gulf of Maine
  • Gulf of Mexico
  • Gulf of Saint Lawrence
  • Gulf of Sidra
  • Gulf of Venezuela
  • Hudson Bay
  • Ionian Sea
  • Irish Sea
  • Irminger Sea
  • James Bay
  • Labrador Sea
  • Levantine Sea
  • Libyan Sea
  • Ligurian Sea
  • Marmara Sea
  • Mediterranean Sea
  • Myrtoan Sea
  • North Sea
  • Norwegian Sea
  • Sargasso Sea
  • Sea of Åland
  • Sea of Azov
  • Sea of Crete
  • Sea of the Hebrides
  • Thracian Sea
  • Tyrrhenian Sea
  • Wadden Sea
Indian Ocean
  • Andaman Sea
  • Arabian Sea
  • Bali Sea
  • Bay of Bengal
  • Flores Sea
  • Great Australian Bight
  • Gulf of Aden
  • Gulf of Aqaba
  • Gulf of Khambhat
  • Gulf of Kutch
  • Gulf of Oman
  • Gulf of Suez
  • Java Sea
  • Laccadive Sea
  • Mozambique Channel
  • Persian Gulf
  • Red Sea
  • Timor Sea
Pacific Ocean
  • Arafura Sea
  • Banda Sea
  • Bering Sea
  • Bismarck Sea
  • Bohai Sea
  • Bohol Sea
  • Camotes Sea
  • Celebes Sea
  • Ceram Sea
  • Chilean Sea
  • Coral Sea
  • East China Sea
  • Gulf of Alaska
  • Gulf of Anadyr
  • Gulf of California
  • Gulf of Carpentaria
  • Gulf of Fonseca
  • Gulf of Panama
  • Gulf of Thailand
  • Gulf of Tonkin
  • Halmahera Sea
  • Koro Sea
  • Mar de Grau
  • Molucca Sea
  • Moro Gulf
  • Philippine Sea
  • Salish Sea
  • Savu Sea
  • Sea of Japan
  • Sea of Okhotsk
  • Seto Inland Sea
  • Shantar Sea
  • Sibuyan Sea
  • Solomon Sea
  • South China Sea
  • Sulu Sea
  • Tasman Sea
  • Visayan Sea
  • Yellow Sea
Southern Ocean
  • Amundsen Sea
  • Bellingshausen Sea
  • Cooperation Sea
  • Cosmonauts Sea
  • Davis Sea
  • D'Urville Sea
  • King Haakon VII Sea
  • Lazarev Sea
  • Mawson Sea
  • Riiser-Larsen Sea
  • Ross Sea
  • Scotia Sea
  • Somov Sea
  • Weddell Sea
Endorheic basins
  • Aral Sea
  • Caspian Sea
  • Dead Sea
  • Salton Sea
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