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| Registros recuperados : 19 | |
| 6. |  | BIRK, J. J.; STEINER, C.; TEIXEIRA, W. G.; ZECH, W.; GLASER, B. Microbial response to charcoal amendments and fertilization of a highly weathered tropical soil. In: WOODS, W. I.; TEIXEIRA, W. G.; LEHMANN, J.; STEINER, C.; WINKLERPRINS, A.; REBELLATO, L. (Ed.). Amazonian dark earths: Wim Sombroek's vision. Berlin: Springer, 2009. p. 309-324.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 9. | | LEHMANN, J.; SILVA JUNIOR, J. P. da; STEINER, C.; NEHLS, T.; ZECH, W.; GLASER, B. Nutrient availability and leaching in an archaeological Anthrosol and a Ferralsol of the Central Amazon basin: fertilizer, manure and charcoal amendments. Plant and Soil, v. 249, p. 343-357, 2003.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 10. | | KERN, J.; GIANI, L.; TEIXEIRA, W. G.; LANZA, G.; GLASER, B. What can we learn from ancient fertile anthropic soil (Amazonian Dark Earths, shell mounds, Plaggen soil) for soil carbon sequestration? Catena, v. 172, p. 104-112, Jan. 2019.| Biblioteca(s): Embrapa Solos. |
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| 11. | | ZECH, W.; CRAVO, M. da S.; LAABS, V.; PINTO, A.; LILIENFEIN, J.; GLASER, B.; TEIXEIRA, W.; LEHMANN, J. New approaches towards sustainability of land-use systems in Tropical Brazil. In: GERMAN-BRAZILIAN WORKSHOP ON NEOTROPICAL ECOSYSTEMS. ACHIEVEMENTS AND PROSPECTS OF COOPERATIVE RESEARCH, 2000, Hamburg. Proceedings... Hamburg: SHIFT: MADAM: WAVES, 2002. p. 118-119.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 12. | | ZECH, W.; CRAVO, M. da S.; LAABS, V.; PINTO, A.; LILIENFEIN, J.; GLASER, B.; WENCESLAU, T.; LEHMANN, J. New approaches towards sustainability of land-use systems in tropical Brazil. In: GERMAN-BRAZILIAN WORKSHOP ON NEOTROPICAL ECOSYSTEMS, 2000, Hamburg. Program and abstracts... Hamburg: University, 2000. p. 30| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 13. | | STEINER, C.; TEIXEIRA, W. G.; LEHMANN, J.; GLASER, B.; ARRUDA, M. R. de; ZECH, W.; BLUM, W. E. H. Slash and char as alternative to slash and burn - soil charcoal amendments maintain soil fertility and establish a carbon sink. In: INTERNATIONAL AGRICHAR INITIATIVE (IAI) 2007 CONFERENCE, 2007, Terrigal, Australia. [Abstracts]. Terrigal: IAI, 2007. p. 32-33.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 14. | | SOMBROEK, W.; KERN, D.; RODRIGUES, T. E.; CRAVO, M. da S.; CUNHA, T. J.; WOODS, W.; GLASER, B. Terra preta and terra mulata: pre-columbian Amazon Kitchen middens and agricultural fields, their sustainability and their replication. In: SYMPOSIUM ANTHROPOGENIC FACTORS OF SOIL FORMATION, 18.; WORLD CONGRESS OF SOIL SCIENCE, 17., 2002, Bangkok. Trabalho apresentado... Bangkok, 2002.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 15. | | SOMBROEK, W.; KERN, D. C.; RODRIGUES, T. E.; CRAVO, M. da S.; CUNHA, T. J. F.; WOODS, W.; GLASER, B. Terra Preta e Terra Mulata: suas potencialidade agrícolas, suas sustentabilidade e suas reproduções. In: TEIXEIRA, W. G.; KERN, D. C.; MADARI, B. E.; LIMA, H. N.; WOODS, I. W. (Ed.). As terras pretas de índio da Amazônia: sua caracterização e uso deste conhecimento na criação de novas áreas. Manaus: EDUA: Embrapa Amazônia Ocidental, 2010. p. 25-258.| Biblioteca(s): Embrapa Semiárido. |
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| 16. | | LEHMANN, J.; SILVA JUNIOR, J. P. da; RONDON, M.; CRAVO, M. D. S.; GREENWOOD, J.; NEHLS, T.; STEINER, C.; GLASER, B. Slash-and-char: a feasible alternative for soil fertility management in the Central Amazon? In: WORLD CONGRESS OF SOIL SCIENCE, 17., 2002, Bangkok, Thailand. Proceedings... [S.l.: s.n.], 2002. v. 2. p. 439. (WCSS. Symposium, 13). Paper n. 449.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 17. | | LEHMANN, J.; SILVA JUNIOR, J. P. da; RONDON, M.; CRAVO, M. da S.; GREENWOOD, J.; NEHLS, T.; STEINER, C.; GLASER, B. Slash-and-char: a feasible alternative for soil fertility management in the Central Amazon? In: WORLD CONGRESS OF SOIL SCIENCE, 17., 2002, Thailand. Proceedings... Bangkok: WCSS, 2002. p. 439. (WCSS. Symposium, 13). Paper n. 449.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 18. | | TAMMEORG, P.; BASTOS, A. C.; JEFFERY, S.; REES, F.; KERN, J.; GRABER, E. R.; VENTURA, M.; AMARO, A.; BUDAI, A.; CORDOVIL, C. M. D. S.; DOMENE, X.; GARDI, C.; GASCÓ, G.; HORÁK, J.; KAMMANN, C. I.; KONDRLOVA, E.; LAIRD, D.; LOUREIRO, S.; MARTINS, M. A. S.; PANZACCHI, P.; PRASAD, M.; PRODANA, M.; PUGA, A. P.; RUYSSCHAERT, G.; SAS PASZT, L.; SILVA, F. C.; TEIXEIRA, W. G.; TONON, G.; DELLE VEDOVE, G.; ZAVALLONI, C.; GLASER, B.; VERHEIJEN, F. G. A. Biochars in soils: towards the required level of scientific understanding. Journal of Environmental Engineering and Landscape Management, v. 25, n. 2, p. 192-207, 2017.| Biblioteca(s): Embrapa Solos. |
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| 19. | | 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. Evidence confirms an anthropic origin of Amazonian Dark Earths. Nature Communications, v. 13, n. 3444, 2022. 6 p.| Biblioteca(s): Embrapa Florestas; Embrapa Solos. |
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| Registros recuperados : 19 | |
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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]
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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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