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| Registros recuperados : 20 | |
| 1. |  | SILVA, V. M.; NARDELI, A. J.; MENDES, N. A. de C.; ROCHA, M. de M.; WILSON, L.; YOUNG, S. D.; BROADLEY, M. R.; WHITE, P. J.; REIS, A. R. dos. Agronomic biofortification of cowpea with zinc: variation in primary metabolism responses and grain nutritional quality among 29 diverse genotypes. Plant Physiology and Biochemistry, v. 162, p. 378-387, 2021.| Biblioteca(s): Embrapa Meio-Norte. |
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| 2. | | SILVA, V. M.; NARDELI, A. J.; MENDES, N. A. C.; ALCOCK, T. D.; ROCHA, M. de M.; PUTTI, F. F.; WILSON, L.; YOUNG, S. D.; BROADLEY, M. R.; WHITE, P. J.; REIS, A. R. dos. Application of sodium selenate to cowpea (Vigna unguiculata L.) increases shoot and grain Se partitioning with strong genotypic interactions. Journal of Trace Elements in Medicine and Biology, v. 67, 12678, 2021.| Biblioteca(s): Embrapa Meio-Norte. |
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| 4. | | SILVA JÚNIOR, E. C. da; GUILHERME, L. R. G.; LOPES, G.; SOUZA, G. A. de; SILVA, K. E. da; LIMA, R. M. B. de; GUEDES, M. C.; WADT, L. H. de O.; REIS, A. R. dos. Are all Brazil nuts selenium-rich? In: INTERNATIONAL CONFERENCE ON SELENIUM IN THE ENVIRONMENT AND HUMAN HEALTH, 4., 2015, São Paulo. Global advances in selenium research from theory to application: proceedings. Londres: Taylor & Francis Group, 2016. p. 133-134. Editores: Gary S. Banuelos, Zhi-Qing Lin, Milton Ferreira Moraes, Luiz Roberto Guimarães Guilherme, Andre Rodrigues dos Reis.| Biblioteca(s): Embrapa Amapá; Embrapa Rondônia. |
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| 5. | | SILVA JÚNIOR, E. C. da; GUILHERME, L. R. G.; LOPES, G.; SOUZA, G. A. de; SILVA, K. E. da; LIMA, R. M. B. de; GUEDES, M. C.; WADT, L. H. de O.; REIS, A. R. dos. Are all Brazil nuts selenium-rich? In: INTERNATIONAL CONFERENCE ON SELENIUM IN THE ENVIRONMENT AND HUMAN HEALTH, 4., 2015, São Paulo. Global advances in selenium research from theory to application: Proceedings....Londres: Taylor & Francis Group, 2016. p. 133-134. Editores Gary S. Banuelos, Zhi-Qing Lin, Milton Ferreira Moraes, Luiz Roberto Guimarães Guilherme, Andre Rodrigues dos Reis.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 6. | | STEFANINI, T. F.; REIS, A. R. dos; PESSOA, J. D. C.; CALBO, A. G. Avaliação da vida útil da couve-manteiga em hidroconservador de aspersão. Horticultura brasileira, Brasília, DF, v. 26, n. 2, p. S4154-S4159, 2008. Edição dos Anais do 48 Congresso Brasileiro de Olericultura, Maringá, PR, 2008. suplemento CD -ROM. Disponível em: . Acesso em: 11 dez. 2008.| Biblioteca(s): Embrapa Instrumentação. |
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| 7. | | PASCOALINO, J. A. L.; MORAES, M. F.; SANTOS, C. L. R. dos; REIS, A. R. dos; SCHEEREN, P. L.; FRANCO, F. de A.; EVANGELISTA, A. Biofortificação agronômica com zinco em trigo. In: REUNIÃO DE BIOFORTIFICAÇÃO NO BRASIL, 5., 2015, São Paulo. [Anais...]. Brasília, DF: Embrapa, 2015. T101, p. 18-20.| Biblioteca(s): Embrapa Trigo. |
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| 9. | | TOMAZELA, A. L.; FAVARIN, J. L.; FANCELLI, A. L.; MARTIN, T. N.; DOURADO NETO, D.; REIS, A. R. dos. Doses de nitrogênio e fontes de Cu e Mn suplementar sobre a severidade da ferrugem e atributos morfológicos do milho. Revista Brasileira de Milho e Sorgo, Sete Lagoas, v. 5, n. 2, p. 192-201, 2006.| Biblioteca(s): Embrapa Milho e Sorgo. |
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| 10. | | SANTOS, L. F. de M.; LAPAZ, A. de M.; TOMAZ, R. S.; LIRA, M. V. da S.; MOREIRA, A.; REIS, A. R. dos; HEINRICHS, R. Evaluation of sulfur source and dose on the nutritional state and production of piatã forage. Semina: Ciências Agrárias, Londrina, v. 40, n. 3, p. 1237-1248, maio/jun. 2019. Título em português: Avaliação de fonte e dose de enxofre no estado nutricional e produção de forragem do piatã.| Biblioteca(s): Embrapa Soja. |
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| 11. | | SILVA JÚNIOR, E. C. da; WADT, L. H. de O.; SILVA, K. E. da; LIMA, R. M. B. de; BATISTA, K. D.; GUEDES, M. C.; OLIVEIRA JUNIOR, R. C. de; REIS, A. R. dos; LOPES, G.; BROADLEY, M. R.; YOUNG, S. D.; GUILHERME, L. R. G. Geochemistry of selenium, barium, and iodine in representative soils of the Brazilian Amazon rainforest. Science of The Total Environment, v. 828, 154426, July 2022.| Biblioteca(s): Embrapa Amazônia Ocidental; Embrapa Amazônia Oriental; Embrapa Rondônia; Embrapa Roraima. |
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| 12. | | PAIVA, A. S. de; PESSOA, J. D. C.; ALBINO, A. L. S.; REIS, A. R. dos. Injúrias de compressão em frutos de açaizeiro armazenados a baixa temperatura e tratados com zeína e cloreto de cálcio. In: CONGRESSO BRASILEIRO DE FISIOLOGIA VEGETAL - CBFV, 12., 2009, Fortaleza, CE. Desafios para produção de alimentos e bioenergia: livro de resumos. Fortaleza, CE: Embrapa Agroindústria Tropical, 2009. p. 365.| Biblioteca(s): Embrapa Instrumentação. |
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| 13. | | PAIVA, A. S. de; ALBINO, A. L. S.; PESSOA, J. D. C.; REIS, A. R. dos. Manufatura e padronização de sensores termoelásticos para medidas de turgor celular. In: CONGRESSO BRASILEIRO DE FISIOLOGIA VEGETAL - CBFV, 12., 2009, Fortaleza, CE. Desafios para produção de alimentos e bioenergia: livro de resumos. Fortaleza, CE: Embrapa Agroindústria Tropical, 2009. p. 365.| Biblioteca(s): Embrapa Instrumentação. |
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| 15. | | MORAES, M. F. de; REIS, A. R. dos; MORAES, L. A. C.; LAVRES JUNIOR, J.; VIVIAN, R.; CABRAL, C. P.; MALAVOLTA, E. Molybdenum, nickel and nitrogen sources on the mineral nutrition of rice plants. In: CONGRESSO BRASILEIRO DE CIÊNCIA DO SOLO, 32., 2009, Fortaleza. O solo e a produção de bioenergia: perspectivas e desafios. [Viçosa, MG]: SBCS; Fortaleza: UFC, 2009. 1 CD-ROM.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 16. | | PAULA NETO, A.; FAVARIN, J. L.; REIS, A. R. dos; TEZOTTO, T.; ALMEIDA, R. E. M. de; LAVRES JUNIOR, J.; GALLO, L. A. Nitrogen metabolism in coffee plants in response to nitrogen supply by fertigation. Theoretical and Experimental Plant Physiology, v. 27, n. 1, p. 41-50, Mar. 2015.| Biblioteca(s): Embrapa Pesca e Aquicultura. |
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| 17. | | IBAÑEZ, T. B.; SANTOS, L. F. de M.; LAPAZ, A. de M.; RIBEIRO, I. V.; RIBEIRO, F. V.; REIS, A. R. dos; MOREIRA, A.; HEINRICHS, R. Sulfur modulates yield and storage proteins in soybean grains. Scientia Agricola, v. 78, n. 1, e20190020, 2021. 9 p.| Biblioteca(s): Embrapa Soja. |
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| 18. | | MOREIRA, A.; MORAES, L. A. C.; REIS, A. R. dos. The molecular genetics of zinc uptake and utilization efficiency in crop plants. In: HOSSAIN, M. A.; KAMIYA, T.; BURRITT, D. J.; TRAN, L.-S. P.; FUJIWARA, T. (Ed.). Plant micronutrient use efficiency: molecular and genomic perspectives in crop plants. London: AP, c2018. cap. 5, p. 87-108.| Biblioteca(s): Embrapa Soja. |
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| 19. | | SILVA JUNIOR, E. C. da; DURAN, N. M.; LESSA, J. H. de L.; RIBEIRO, P. G.; WADT, L. H. de O.; SILVA, K. E. da; LIMA, R. M. B. de; BATISTA, K. D.; GUEDES, M. C.; OLIVEIRA JUNIOR, R. C. de; CARVALHO, H. W. P. de; REIS, A. R. dos; LOPES, G.; GUILHERME, L. R. G. Unraveling the accumulation and localization of selenium and barium in Brazil nuts using spectroanalytical techniques. Journal of Food Composition and Analysis, v. 106, art. 104329, March 2022.| Biblioteca(s): Embrapa Amapá; Embrapa Amazônia Ocidental; Embrapa Amazônia Oriental; Embrapa Rondônia; Embrapa Roraima. |
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| Registros recuperados : 20 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Florestas; Embrapa Solos. |
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Data corrente: |
20/06/2022 |
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Data da última atualização: |
10/11/2022 |
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Tipo da produção científica: |
Nota Técnica/Nota Científica |
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Autoria: |
LOMBARDO, U.; ARROYO-KALIN, M.; SCHMIDT, M.; HUISMAN, H.; LIMA, H. P.; MORAES, M. de P.; NEVES, E. G.; CLEMENT, C. R.; FONSECA, J. A. da; ALMEIDA, F. O. de; ALHO, C. F. B. V.; RAMSEY, C. B.; BROWN, G. G.; CAVALLINI, M. S.; COSTA, M. L. da; CUNHA, L.; ANJOS, L. H. C. dos; DENEVAN, W. M.; FAUSTO, C.; CAROMANO, C. F.; FONTANA, A.; FRANCHETTO, B.; GLASER, B.; HECKENBERGER, M. J.; HECHT, S.; HONORATO, V.; JAROSCH, K. A.; JUNQUEIRA, A. B.; KATER, T.; TAMANAHA, E. K.; KUYPER, T. W.; LEHMANN, J.; MADELLA, M.; MAEZUMI, S. Y.; CASCON, L. M.; MAYLE, F. E.; MCKEY, D.; MORAES, B.; MORCOTE-RÍOS, G.; BARBOSA, C. A. P.; MAGALHÃES, M. P.; PRESTES-CARNEIRO, G.; PUGLIESE, F.; PUPIM, F. N.; RACZKA, M. F.; PY-DANIEL, A. R.; ROCHA, B. C. da; RODRIGUES, L.; ROSTAIN, S.; MACEDO, R. S.; SHOCK, M. P.; SPRAFKE, T.; BASSI, F. S.; VALLE, R.; VIDAL-TORRADO, P.; VILLAGRÁN, X. S.; WATLING, J.; WEBER, S. L.; TEIXEIRA, W. G. |
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Afiliação: |
UMBERTO LOMBARDO, Institut de Ciència i Tecnologia Ambientals, Universitat Autònoma de Barcelona (ICTA-UAB); MANUEL ARROYO-KALIN, Institute of Archaeology; MORGAN SCHMIDT, Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology; HANS HUISMAN, University of Groningen; HELENA P. LIMA, Museu Paraense Emílio Goeldi; CLAIDE DE PAULA MORAES, Universidade Federal do Oeste do Pará; EDUARDO G. NEVES, University of São Paulo; CHARLES R. CLEMENT, Instituto Nacional de Pesquisas da Amazônia; JOÃO AIRES DA FONSECA, ArqueoMaquina; FERNANDO OZORIO DE ALMEIDA, Universidade do Estado do Rio de Janeiro; CARLOS FRANCISCO BRAZÃO VIEIRA ALHO, Wageningen University & Research; CHRISTOPHER BRONK RAMSEY, University of Oxford; GEORGE GARDNER BROWN, CNPF; MARTA S. CAVALLINI, University of São Paulo; MARCONDES LIMA DA COSTA, Federal University of Pará; LUÍS CUNHA, Universidade de Coimbra; LÚCIA HELENA C. DOS ANJOS, Federal Rural University of Rio de Janeiro; WILLIAM M. DENEVAN, University of Wisconsin-Madison; CARLOS FAUSTO, Universidade Federal do Rio de Janeiro; CAROLINE FERNANDES CAROMANO, Naturalis Biodiversity Center; ADEMIR FONTANA, CNPS; BRUNA FRANCHETTO, Universidade Federal do Rio de Janeiro; BRUNO GLASER, Martin-Luther-Universität Halle-Wittenberg; MICHAEL J. HECKENBERGER, University of Florida; SUSANNA HECHT, School of Public Affairs, UCLA; VINICIUS HONORATO, Universidade Federal do Oeste do Pará; KLAUS A. JAROSCH, University of Bern; ANDRÉ BRAGA JUNQUEIRA, Universitat Autònoma de Barcelona (ICTA-UAB); THIAGO KATER, University of São Paulo; EDUARDO K. TAMANAHA, Instituto de Desenvolvimento Sustentável Mamirauá; THOMAS W. KUYPER, Wageningen University & Research, Wageningen; JOHANNES LEHMANN, Cornell University; MARCO MADELLA, Institució Catalana de Recerca i Estudis Avançats (ICREA); S. YOSHI MAEZUMI, University of Amsterdam; LEANDRO MATTHEWS CASCON, Leiden University; FRANCIS E. MAYLE, University of Reading; DOYLE MCKEY, Univ Paul-Valéry Montpellier; BRUNO MORAES, Amazon Hopes Collective; GASPAR MORCOTE-RÍOS, Universidad Nacional de Colombia; CARLOS A. PALHETA BARBOSA, Institute of National Historic and Artistic Heritage; MARCOS PEREIRA MAGALHÃES, Museu Paraense Emílio Goeldi; GABRIELA PRESTES-CARNEIRO, Universidade Federal do Oeste do Pará; FRANCISCO PUGLIESE, University of São Paulo; FABIANO N. PUPIM, Universidade Federal de São Paulo; MARCO F. RACZKA, University of Reading; ANNE RAPP PY-DANIEL, Universidade Federal do Oeste do Pará; BRUNA CIGARAN DA ROCHA, Universidade Federal do Oeste do Pará; LEONOR RODRIGUES, Agroscope; STÉPHEN ROSTAIN, French National Centre for Scientific Research; RODRIGO SANTANA MACEDO, Instituto Nacional do Semiárido; MYRTLE P. SHOCK, Universidade Federal do Oeste do Pará; TOBIAS SPRAFKE, Center of Competence for Soils; FILIPPO STAMPANONI BASSI, Museu da Amazônia; RAONI VALLE, Universidade Federal do Oeste do Pará; PABLO VIDAL-TORRADO, University of São Paulo; XIMENA S. VILLAGRÁN, University of São Paulo; JENNIFER WATLING, University of São Paulo; SADIE L. WEBER, University of São Paulo; WENCESLAU GERALDES TEIXEIRA, CNPS. |
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Título: |
Evidence confirms an anthropic origin of Amazonian Dark Earths. |
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Ano de publicação: |
2022 |
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Fonte/Imprenta: |
Nature Communications, v. 13, n. 3444, 2022. |
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Páginas: |
6 p. |
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DOI: |
https://doi.org/10.1038/s41467-022-31064-2 |
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Idioma: |
Inglês
Português |
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Conteúdo: |
First described over 120 years ago in Brazil, Amazonian Dark Earths (ADEs) are expanses of dark soil that are exceptionally fertile and contain large quantities of archaeological artefacts. The elevated fertility of the dark and often deep A horizon of ADEs is widely regarded as an outcome of pre-Columbian human influence1. Archaeological research provides clear evidence that their widespread formation in lowland South America was concentrated in the Late Holocene, an outcome of sharp human population growth that peaked towards 1000 BP2,3,4. In their recent paper Silva et al.5 argue that the higher fertility of ADEs is principally a result of fluvial deposition and, as a corollary, that pre-Columbian peoples just made use of these locales, contributing little to their enhanced nutrient status.
Soil formation is inherently complex and often difficult to interpret, requiring a combination of geochemical data, stratigraphy, and dating. Although Silva et al. use this combination of methods to make their case5, their hypothesis, based on the analysis of a single ADE site and its immediate surroundings (Caldeirão, see maps in Silva et al.5), is too limited to distinguish among the multiple possible mechanisms for ADE formation. Moreover, it disregards or misreads a wealth of evidence produced by archaeologists, soil scientists, geographers and anthropologists, showing that ADEs are anthropic soils formed on land surfaces enriched by inputs associated with pre-Columbian sedentary settlement6,7,8,9. To be accepted, and be pertinent at a regional level, Silva et al.’s hypothesis5 would need to be supported by solid evidence (from numerous ADE sites), which we demonstrate is lacking. MenosFirst described over 120 years ago in Brazil, Amazonian Dark Earths (ADEs) are expanses of dark soil that are exceptionally fertile and contain large quantities of archaeological artefacts. The elevated fertility of the dark and often deep A horizon of ADEs is widely regarded as an outcome of pre-Columbian human influence1. Archaeological research provides clear evidence that their widespread formation in lowland South America was concentrated in the Late Holocene, an outcome of sharp human population growth that peaked towards 1000 BP2,3,4. In their recent paper Silva et al.5 argue that the higher fertility of ADEs is principally a result of fluvial deposition and, as a corollary, that pre-Columbian peoples just made use of these locales, contributing little to their enhanced nutrient status.
Soil formation is inherently complex and often difficult to interpret, requiring a combination of geochemical data, stratigraphy, and dating. Although Silva et al. use this combination of methods to make their case5, their hypothesis, based on the analysis of a single ADE site and its immediate surroundings (Caldeirão, see maps in Silva et al.5), is too limited to distinguish among the multiple possible mechanisms for ADE formation. Moreover, it disregards or misreads a wealth of evidence produced by archaeologists, soil scientists, geographers and anthropologists, showing that ADEs are anthropic soils formed on land surfaces enriched by inputs associated with pre-Columbian sedentary ... Mostrar Tudo |
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Palavras-Chave: |
Amazonian Dark Earths; Arqueologia; Ciencias ambientais; Environmental sciences. |
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Thesagro: |
Microbiologia do Solo; Solo. |
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Thesaurus NAL: |
Amazonia; Archaeology; Terra preta. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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URL: |
https://ainfo.cnptia.embrapa.br/digital/bitstream/doc/1144138/1/NatureCommunications-2022-EvidenceConfirmAmazonDarkEarths.pdf
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Marc: |
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245 $aEvidence confirms an anthropic origin of Amazonian Dark Earths.$h[electronic resource]
260 $c2022
300 $a6 p.
520 $aFirst described over 120 years ago in Brazil, Amazonian Dark Earths (ADEs) are expanses of dark soil that are exceptionally fertile and contain large quantities of archaeological artefacts. The elevated fertility of the dark and often deep A horizon of ADEs is widely regarded as an outcome of pre-Columbian human influence1. Archaeological research provides clear evidence that their widespread formation in lowland South America was concentrated in the Late Holocene, an outcome of sharp human population growth that peaked towards 1000 BP2,3,4. In their recent paper Silva et al.5 argue that the higher fertility of ADEs is principally a result of fluvial deposition and, as a corollary, that pre-Columbian peoples just made use of these locales, contributing little to their enhanced nutrient status. Soil formation is inherently complex and often difficult to interpret, requiring a combination of geochemical data, stratigraphy, and dating. Although Silva et al. use this combination of methods to make their case5, their hypothesis, based on the analysis of a single ADE site and its immediate surroundings (Caldeirão, see maps in Silva et al.5), is too limited to distinguish among the multiple possible mechanisms for ADE formation. Moreover, it disregards or misreads a wealth of evidence produced by archaeologists, soil scientists, geographers and anthropologists, showing that ADEs are anthropic soils formed on land surfaces enriched by inputs associated with pre-Columbian sedentary settlement6,7,8,9. To be accepted, and be pertinent at a regional level, Silva et al.’s hypothesis5 would need to be supported by solid evidence (from numerous ADE sites), which we demonstrate is lacking.
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773 $tNature Communications$gv. 13, n. 3444, 2022.
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Embrapa Florestas (CNPF) |
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