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Terras pretas (Amazonian Dark Earths) are a remarkable kind of archaeological site found in the Amazon region. Rich in cultural artifacts and other occupational debris, these dark anthropogenic soil matrices are very fertile, presenting high levels of organic carbon, phosphorus, calcium, magnesium, zinc, and manganese. Their high nutrient levels come from decomposed organic matter, including remains of fish, shellfish, game, and other refuse, while their dark color has been linked to residual charcoal from intentional fires associated with daily activities and landscape management. Studies of anthropogenic earths in the Amazon have a deep history, as much in the geosciences as in archaeology and other historical sciences. Terras pretas have been studied as evidence of a major shift in human–environment relations, but also within the lens of environmental resiliency and sustainability. We review representative studies from various disciplinary fields and trace the development of knowledge about terra preta. We present a growing consensus with regard to the origin and significance of anthropogenic soils, concomitant with increased efforts toward interdisciplinary study. We argue that terras pretas constitute a genuinely interdisciplinary research topic that bridges scientific and traditional knowledge and applied contexts.

Several archaeological black earth (ABE) sites occur in the Amazon region. They contain fragments of ceramic artifacts, which are very important for the archaeological purpose. In order to improve the archaeological study in the region we carried out a detailed mineralogical and chemical study of the fragments of ceramic artifacts found in the two ABE sites of CachoeiraPorteira, in the Lower Amazon Region. Their ceramics comprise the following tempers: cauixi, cariapé, sand, sand +feldspars, crushed ceramic and so on and are composed of quartz, clay equivalent material (mainly burned kaolinite), feldspars, hematite, goethite, maghemite, phosphates, anatase, and minerals of Mn and Ba. Cauixi and cariapé, siliceous organic compounds, were found too. The mineralogical composition and the morphology of their grains indicate a saprolite (clayey material rich on quartz) derived from fine-grained felsic igneous rocks or sedimentary rocks as source material for ceramic artifacts, where silica-rich components such cauixi, cariapé and/or sand (feldspar and rock fragments) were intentionally added to them. The high content of (Al,Fe)-phosphates, amorphous to low crystalline, must be product of the contact between the clayey matrix of pottery wall and the hot aqueous solution formed during the daily cooking of animal foods (main source of phosphor). The phosphate crystallization took place during the discharge of the potteries put together with waste of organic material from animal and vegetal origin, and leaving to the formation of the ABE-soil profile. KEY WORDSTerra Preta, Black Earth, Archaeological ceramic fragment, Lower Amazon, Phosphates, Mineralogy.Artefatos cerâmicos em sítios arqueológios com terra preta na região do baixo Amazonas, Brasil: Mineralogia. RESUMO Sítios arqueológicos com Terra Preta, denominados de Terra Preta de Índio ou ainda Terra Preta

The present study aims to interpret the occupation of terra firme (nonflooded uplands) archeological sites located at Tapirapé-Aquiri National Forest in the Brazilian state of Pará, through an integrated analysis of pedological, archeological, and geochemical data. We focus on seven archaeological sites, selected among 22 identified in the region. Radiocarbon and thermoluminescence dating indicate distinct periods of occupation over the past ß6000 years, and the pedo-geochemical data identify intra-and inter-site differences in soil. Archaeological, chronometric, and pedo-geochemical data provide a basis for the functional classification of archeological sites found in the region and help to identify specific human activity areas. The results lead us to infer that many of the archeological sites were the result of multiple occupations that left a persistent pedological signature on the landscape. C 2015 Wiley Periodicals, Inc.