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| Registros recuperados : 51 | |
| 21. |  | MELO, V. de; SILVEIRA, J. V. A.; SAMPAIO, J. B. M. de; OLIVEIRA, C. A. de. Levantamento conservacionista dos solos de Sape, Mari e parte de Mamanguape, Mulungu e Caldas Brandao. In: CONGRESSO BRASILEIRO DE CIENCIA DO SOLO, 15., Campinas, SP. Anais... Campinas: Sociedade Brasileira de Ciencia do Solo, 1976. p.585-590. (SUDENE. Recurso de Solos, 3)| Biblioteca(s): Embrapa Semiárido. |
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| 26. | | HANKE, D.; MELO, V. de F.; DIECKOW, J.; DICK, D. P.; BOGNOLA, I. A. Influência da matéria orgânica no diâmetro médio de minerais da fração argila de solos desenvolvidos de basalto no sul do Brasil. Revista Brasileira de Ciência do Solo, Viçosa, MG, v. 39, n. 6, p. 1611-1622, nov./dez. 2015.| Biblioteca(s): Embrapa Florestas. |
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| 29. | | RAMOS, M. R.; UHLMANN, A.; MELO, V. de F.; CURCIO, G. R.; CAGLIONI, E. Atributos de solos coesos e não coesos no Complexo Petroquímico do Rio de Janeiro, Itaboraí - RJ. Enciclopédia Biosfera, Goiânia, v. 11 n. 22, p. 360-375, 2015.| Biblioteca(s): Embrapa Florestas. |
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| 30. | | HANKE, D.; DICK, D. P.; DIECKOW, J.; MELO, V. de F.; BOGNOLA, I. A. Matéria orgânica e mineralogia de solos de uma toposseqüência do Terceiro Planalto Paranaense. In: ENCONTRO BRASILEIRO DE SUBSTÂNCIAS HÚMICAS, 10., 2013, Santo Antônio de Goiás. Matéria orgânica e qualidade ambiental: anais. Brasília, DF: Embrapa, 2013. p. 190-193| Biblioteca(s): Embrapa Florestas. |
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| 33. | | BARROS, Y. J.; SAUTTER, K. D.; MELO, V. de F.; BUSCHLE, B. Soil Mesofauna in an old mining area in Adrianópolis (PR), Brazil. In: INTERNATIONAL COLLOQUIUM ON SOIL ZOOLOGY, 15; INTERNATIONAL COLLOQUIUM ON APTERYGOTA, 12., 2008, Curitiba. Biodiversity, conservation and sustainabele management of soil animal: abstracts. Colombo: Embrapa Florestas. Editors: George Gardner Brown; Klaus Dieter Sautter; Renato Marques; Amarildo Pasini. 1 CD-ROM.| Biblioteca(s): Embrapa Florestas. |
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| 36. | | OLIVEIRA, V. R.; OLIVEIRA JUNIOR, R. S. de; MELO, V. de F.; PELUZIO, J. M.; FONTES, P. C. R. Distribuicao da producao de frutos nos cachos de cinco cultivares de tomateiro em dois sistemas de conducao. Revista Ceres, Vicosa, v.42, n.244, p.644-657, nov./dez. 1995.| Biblioteca(s): Embrapa Hortaliças. |
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| 38. | | MELO, V. de F.; FONTES, M. P. F.; BARROS, N. F. de; COSTA, L. M. da; NOVAIS, R. F. de. Extração de ferro com ditionito e oxalato em alguns solos do Estado do Rio Grande do Sul. IN: CONGRESSO BRASILEIRO DE CIÊNÇIA DO SOLO, 25., 1995, Viçosa, MG. Resumos expandidos. Viçosa: UFV, 1995. v.1, p. 265-267.| Biblioteca(s): Embrapa Tabuleiros Costeiros. |
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Registro Completo
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Biblioteca(s): |
Embrapa Amazônia Ocidental. |
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Data corrente: |
04/01/2021 |
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Data da última atualização: |
17/09/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
A - 1 |
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Autoria: |
SILVA, L. C. R.; CORRÊA, R. S.; WRIGHT, J. L.; BOMFIM, B.; HENDRICKS, L.; GAVIN, D. G.; MUNIZ, A. W.; MARTINS, G. C.; MOTTA, A. C. V.; BARBOSA, J. Z.; MELO, V. de F.; YOUNG, S. D.; BROADLEY, M. R.; SANTOS, R. V. |
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Afiliação: |
Lucas C. R. Silva, University of Oregon; Rodrigo Studart Corrêa; Jamie L. Wright; Barbara Bomfim; Lauren Hendricks; Daniel G. Gavin; ALEKSANDER WESTPHAL MUNIZ, CPAA; GILVAN COIMBRA MARTINS, CPAA; Antônio Carlos Vargas Motta; Julierme Zimmer Barbosa; Vander de Freitas Melo; Scott D. Young; Martin R. Broadley; Roberto Ventura Santos. |
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Título: |
A new hypothesis for the origin of Amazonian Dark Earths. |
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Ano de publicação: |
2021 |
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Fonte/Imprenta: |
Nature Communications, v. 12, Art. 127, 2021. |
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DOI: |
https://doi.org/10.1038/s41467-020-20184-2 |
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Idioma: |
Inglês |
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Conteúdo: |
Amazonian Dark Earths (ADEs) are unusually fertile soils characterised by elevated concentrations of microscopic charcoal particles, which confer their distinctive colouration. Frequent occurrences of pre-Columbian artefacts at ADE sites led to their ubiquitous classification as Anthrosols (soils of anthropic origin). However, it remains unclear how indigenous peoples created areas of high fertility in one of the most nutrient-impoverished environments on Earth. Here, we report new data from a well-studied ADE site in the Brazilian Amazon, which compel us to reconsider its anthropic origin. The amounts of phosphorus and calcium - two of the least abundant macronutrients in the region - are orders of magnitude higher in ADE profiles than in the surrounding soil. The elevated levels of phosphorus and calcium, which are often interpreted as evidence of human activity at other sites, correlate spatially with trace elements that indicate exogenous mineral sources rather than in situ deposition. Stable isotope actios of neodymium, strontium, and radiocarbon activity of microcharcoal particles also indicate exogenous inputs from alluvial deposition of carbon and mineral elements to ADE profiles, beginning several thousands of years before the earliest evidence of soil management for plant cultivation in the region. Our data suggest that indigenous peoples harnessed natural processes of landscape formation, which led to the unique properties of ADEs, but were not responsible for their genesis. If corroborated elsewhere, this hypothesis would transform our understanding of human influence in Amazonia, opening new frontiers for the sustainable use of tropical landscapes going forward. MenosAmazonian Dark Earths (ADEs) are unusually fertile soils characterised by elevated concentrations of microscopic charcoal particles, which confer their distinctive colouration. Frequent occurrences of pre-Columbian artefacts at ADE sites led to their ubiquitous classification as Anthrosols (soils of anthropic origin). However, it remains unclear how indigenous peoples created areas of high fertility in one of the most nutrient-impoverished environments on Earth. Here, we report new data from a well-studied ADE site in the Brazilian Amazon, which compel us to reconsider its anthropic origin. The amounts of phosphorus and calcium - two of the least abundant macronutrients in the region - are orders of magnitude higher in ADE profiles than in the surrounding soil. The elevated levels of phosphorus and calcium, which are often interpreted as evidence of human activity at other sites, correlate spatially with trace elements that indicate exogenous mineral sources rather than in situ deposition. Stable isotope actios of neodymium, strontium, and radiocarbon activity of microcharcoal particles also indicate exogenous inputs from alluvial deposition of carbon and mineral elements to ADE profiles, beginning several thousands of years before the earliest evidence of soil management for plant cultivation in the region. Our data suggest that indigenous peoples harnessed natural processes of landscape formation, which led to the unique properties of ADEs, but were not responsible for the... Mostrar Tudo |
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Palavras-Chave: |
Amazonian Dark Earths; Terra Preta de Índio. |
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Thesagro: |
Solo. |
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Categoria do assunto: |
-- |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/item/219845/1/s41467-020-20184-2.pdf
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Marc: |
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024 7 $ahttps://doi.org/10.1038/s41467-020-20184-2$2DOI
100 1 $aSILVA, L. C. R.
245 $aA new hypothesis for the origin of Amazonian Dark Earths.$h[electronic resource]
260 $c2021
520 $aAmazonian Dark Earths (ADEs) are unusually fertile soils characterised by elevated concentrations of microscopic charcoal particles, which confer their distinctive colouration. Frequent occurrences of pre-Columbian artefacts at ADE sites led to their ubiquitous classification as Anthrosols (soils of anthropic origin). However, it remains unclear how indigenous peoples created areas of high fertility in one of the most nutrient-impoverished environments on Earth. Here, we report new data from a well-studied ADE site in the Brazilian Amazon, which compel us to reconsider its anthropic origin. The amounts of phosphorus and calcium - two of the least abundant macronutrients in the region - are orders of magnitude higher in ADE profiles than in the surrounding soil. The elevated levels of phosphorus and calcium, which are often interpreted as evidence of human activity at other sites, correlate spatially with trace elements that indicate exogenous mineral sources rather than in situ deposition. Stable isotope actios of neodymium, strontium, and radiocarbon activity of microcharcoal particles also indicate exogenous inputs from alluvial deposition of carbon and mineral elements to ADE profiles, beginning several thousands of years before the earliest evidence of soil management for plant cultivation in the region. Our data suggest that indigenous peoples harnessed natural processes of landscape formation, which led to the unique properties of ADEs, but were not responsible for their genesis. If corroborated elsewhere, this hypothesis would transform our understanding of human influence in Amazonia, opening new frontiers for the sustainable use of tropical landscapes going forward.
650 $aSolo
653 $aAmazonian Dark Earths
653 $aTerra Preta de Índio
700 1 $aCORRÊA, R. S.
700 1 $aWRIGHT, J. L.
700 1 $aBOMFIM, B.
700 1 $aHENDRICKS, L.
700 1 $aGAVIN, D. G.
700 1 $aMUNIZ, A. W.
700 1 $aMARTINS, G. C.
700 1 $aMOTTA, A. C. V.
700 1 $aBARBOSA, J. Z.
700 1 $aMELO, V. de F.
700 1 $aYOUNG, S. D.
700 1 $aBROADLEY, M. R.
700 1 $aSANTOS, R. V.
773 $tNature Communications$gv. 12, Art. 127, 2021.
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Embrapa Amazônia Ocidental (CPAA) |
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