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Amazon River Basin

As a drainage basin, the Amazon covers more than 7 million square kilometers in South America, making it the largest in the world. The Amazon basin encompasses portions of Bolivia, Brazil, Colombia, Ecuador, Suriname, Peru, and Venezuela, and roughly two thirds of this area fall within Brazil. Many of the main rivers of the basin are more than 2 kilometers wide, and the Amazon itself discharges roughly 175,000 m3 of water per second into the Atlantic.

Climate in the Amazon is eminently tropical with limited variation in temperatures and more seasonal variability in rainfall, which is generally greater from November to May. Soils in the Amazon were once believed to be very fertile, but most of the basin has relatively old, weathered soils that are nutrient-poor and unsuitable for sustained agriculture. The Amazon watershed consists of different kinds of rivers. Whitewater rivers, such as the Amazon itself, are very turbid because they carry greater sediment loads, transported from clay soils by heavy rainfall during the wet season. By contrast, clearwater rivers are more transparent, but sediment-poor, and blackwater rivers have the color of tea due to plant tannins in the water. During the rainy season, river levels rise, inundating lowland forests; many fish then come into the flooded forests to feed and reproduce. Whitewater rivers deposit considerable sediments in lowland soils, and due to these nutrients, whitewater rivers have particularly abundant fish populations. The nutrient deposits also raise lowland soil fertility, and when river levels decline in the dry season, the exposed lowlands are farmed due to their relatively high productivity.

The Amazon has very high biodiversity, and as a result, the countries sharing the basin are among the most biodiverse in the world. Brazil alone holds between 10% and 20% of the 1.5 million species catalogued thus far. These numbers are low, however, since new species in the Amazon are regularly being discovered and described.

Human Occupation

Understanding of the initial human occupation in the Amazon is changing. It now appears that humans arrived in the Amazon at least 11,500 years ago, judging from pottery shards. Debate continues concerning Amazon's pre-Columbian populations, which informs estimates of the basin's human carrying capacity. Scholars who emphasize lower numbers call attention to the basin's limited protein sources, and note evidence of higher population concentrations near whitewater rivers.

However, archaeological evidence of sizeable pre-Columbian earthworks, roads, and centralized settlement designs in the uplands suggests larger populations than previously estimated. Similarly, ethnobotanical evidence indicates that many areas of “pristine” forest in the Amazon were modified by human use over long periods. And patches of “Black Indian soils,” which resulted from disposal of large quantities of organic waste by indigenous groups, have been found in many places across the basin.

Indigenous peoples in the Amazon largely resided along rivers, which they intensively exploited. In the uplands, indigenous groups cut and burned vegetation to form small clearings, where they cultivated food crops. Such clearings were only temporarily used, as tribal groups subsequently moved on, allowing the forest to reclaim cleared patches.

European colonization of the Amazon began in the 16th century with Portuguese incursions westward from the Atlantic, and Spanish expeditions eastward from the Andes. Impressed with the luxuriant vegetation and considerable indigenous populations along the rivers, Europeans went in search of exotic commodities. This led to river-based trade in dyes, seeds, animal hides, and numerous other products, which were exported to Europe. This system was based in part on indigenous labor, often in missionary settlements. As a result, indigenous populations declined, and the Amazon economy became increasingly focused on specific commodities, leading to boom-bust economic cycles.

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