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| Registros recuperados : 25 | |
| 6. |  | ANDRES, A. CONCENCO, G. MELO, P. T. B. S.; SCHMIDT, M.; RESENDE, R. G. Detecção da resistência de capim-arroz (Echinochloa sp.) ao herbicida quinclorac em regiões orizícolas do sul do Brasil. Planta daninha, Campinas, v. 25, n. 1, p. 221-226, 2007. Meta: 2008.| Biblioteca(s): Embrapa Clima Temperado. |
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| 7. | | FARIAS NETO, A. L. de; SCHMIDT, M.; HARTMAN, G. L.; LI, S.; DIERS, B. W. Inoculation methods under greenhouse conditions for evaluating soybean resistance to sudden death syndrome. Pesquisa Agropecuária Brasileira, Brasília, v. 43, n. 11, p. 1475-1482, nov. 2008.| Biblioteca(s): Embrapa Cerrados; Embrapa Unidades Centrais. |
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| 9. | | TEIXEIRA, W. G.; SCHMIDT, M.; SHINZATO, E.; MANSUR, K.; SCHAAN, D. P.; FONTANA, A.; CERNICCHIARO, G. Susceptibilidade magnética em amostras de solos de sitios arqueológicos do Brasil: potencialidades e limitações da avaliação do fenômeno da termoremanência. In: CONGRESSO DA ASSOCIAÇÃO BRASILEIRA DE ESTUDOS DO QUATERNÁRIO, 16., 2017, Bertioga. Mudanças climáticas no passado e no presente: conhecer para entender as consequências no futuro: anais. São Paulo: ABEQUA, 2017.| Biblioteca(s): Embrapa Solos. |
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| 10. | | HECKENBERGER, M. J.; KUIKURO, A.; KUIKURO, U. T.; RUSSELL, J. C.; SCHMIDT, M.; FAUSTO, C.; FRANCHETTO, B. Amazonia 1492: pristine forest or cultural parkland? Science, v. 301, p. 1710-1714, 2003.| Biblioteca(s): Embrapa Amazônia Ocidental. |
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| 11. | | BONAGAMBA, T. J.; COLNAGO, L. A.; TANNUS, A.; PEREIRA LEITE, V. B.; SCHMIDT, M. A.; PANEPUCCI, H. Desenvolvimento de um espectrômetro de alta resolução por ressonância magnética nuclear (RMN). In: REUNIÃO ANUAL DA SBPC, 39., 1987, Brasília, DF. Ciência e Cultura, São Paulo, v.39, n.7, p.283, jul. 1987. Suplemento. Resumos. ref.91-D.1.4.| Biblioteca(s): Embrapa Instrumentação. |
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| 12. | | BONAGAMBA, T. J.; COLNAGO, L. A.; TANNUS, A.; PEREIRA LEITE, V. B.; SCHMIDT, M. A.; PANEPUCCI, H. C. Desenvolvimento de um espectrômetro de (RMN) de alta resolução. In: ENCONTRO DE USUÁRIOS DE RESSONÂNCIA MAGNÉTICA NUCLEAR, 1., set. 1987, Angra dos Reis, RJ. Resumos... Rio de Janeiro: AUREMN, 1987. p.9.| Biblioteca(s): Embrapa Instrumentação. |
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| 13. | | SCHMIDT, M. C.; SUTTNER, R. J.; KLEIN, J. H.; GIBSON, P. T.; LIGHTFOOT, D. A.; MYERS JUNIOR, O. Registration of LS-G96 soybean germplasm resistant to soybean sudden death syndrome and soybean cyst nematode race 3. Crop Science, Madison, v. 39, p. 598, Mar/Apr. 1999.| Biblioteca(s): Embrapa Trigo. |
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| 14. | | FARIAS NETO, A. L. de; MOREIRA, C. T.; SOUZA, P. I. de M. de; DIANESE, A. de C.; SCHMIDT, M.; HARTMAN, G. L.; LI, S.; DIERS, B. W. Greenhouse evaluation of soybean germplasm for resistance to sudden death syndrome. In: SIMPÓSIO NACIONAL CERRADO, 9.; SIMPÓSIO INTERNACIONAL SAVANAS TROPICAIS, 2., 2008, Brasília, DF. Desafios e estratégias para o equilíbrio entre sociedade, agronegócio e recursos naturais: anais... Planaltina, DF: Embrapa Cerrados, 2008. 1 CD-ROM.| Biblioteca(s): Embrapa Cerrados. |
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| 15. | | FARIAS NETO, A. L. de; HASHMI, R.; SCHMIDT, M.; CARLSON, S. R.; HARTMAN, G. L.; LI, S.; NELSON, R. L.; DIERS, B. W. Mapping and confirmation of a new sudden death syndrome resistance QTL on linkage group D2 from the soybean genotypes PI 567374 and 'Ripley'. Molecular Breeding, v. 20, p. 53-62, 2007.| Biblioteca(s): Embrapa Cerrados. |
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| 17. | | SCHMIDT, M. E. P.; PIRES, F. B.; BRESSAN, L. P.; SILVA JUNIOR, F. V. da; LAMEIRA, O. A.; ROSA, M. B. da. Some triterpenic compounds in extracts of Cecropia and Bauhinia species for different sampling years. Revista Brasileira de Farmacognosia, v. 28, n. 1, p. 21-26, Jan./Feb. 2018.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 18. | | SCHMIDT, M. J.; GOLDBERG, S. L.; PERRON, J. T.; HECKENBERGER, M.; WATLING, J.; DORSHOW, W. B.; MORAES, B.; LIMA, H.; TEIXEIRA, W. G.; NEVES, E.; HOSLER, D.; WAURA, K.; KUIKURO, H.; KUIKURO, W.; KUIKURO, A.; FAUSTO, C.; FRANCHETTO, B. Estimating soil carbon in Southern Amazon late holocene anthropogenic landscapes containing archaeological 'Dark Earth' Anthrosols. In: AMERICAN GEOPHYSICAL UNION FALL MEETING, 2020. Abstracts [...]. Washington, DC: American Geophysical Union, 2020.| Biblioteca(s): Embrapa Solos. |
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| 19. | | SCHMIDT, M. J.; PY-DANIEL, A. R.; MORAES, C. de P.; VALLE, R. B. M.; CAROMANO, C. F.; TEIXEIRA, W. G.; BARBOSA, C. A.; FONSECA, J. A.; MAGALHÃES, M. P.; SANTOS, D. S. do C.; SILVA, R. da S. e; GUAPINDAIA, V. L.; MORAES, B.; LIMA, H. P.; NEVES, E. G.; HECKENBERGER, M. J. Dark earths and the human built landscape in Amazonia: a widespread pattern of anthrosol formation. Journal of Archaeological Science, v. 42, p. 152-165, Feb. 2014.| Biblioteca(s): Embrapa Solos. |
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| 20. | | SCHMIDT, M. J.; GOLDBERG, S. L.; HECKENBERGER, M.; FAUSTO, C.; FRANCHETTO, B.; WATLING, J.; LIMA, H.; MORAES, B.; DORSHOW, W. B.; TONEY, J.; KUIKURO, Y.; WAURA, K.; KUIKURO, H.; KUIKURO, T. W.; KUIKURO, T.; KUIKURI, Y.; KUIKURO, A.; TEIXEIRA, W. G.; ROCHA, B.; HONORATO, V.; TAVARES, H.; MAGALHÃES, M.; BARBOSA, C. A.; FONSECA, J. A. da; MENDES, K.; ALLEONI, L. R. F; CERRI, C. E. P.; ARROYO-KALIN, M.; NEVES, E.; PERRON, J. T. Intentional creation of carbon-rich dark earth soils in the Amazon. Science Advances, v. 9, n. 38, eadh8499, Sept. 2023.| Biblioteca(s): Embrapa Solos. |
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| Registros recuperados : 25 | |
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Registro Completo
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Biblioteca(s): |
Embrapa Solos. |
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Data corrente: |
27/10/2023 |
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Data da última atualização: |
06/11/2023 |
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Tipo da produção científica: |
Artigo em Anais de Congresso |
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Autoria: |
SCHMIDT, M. J.; GOLDBERG, S. L.; PERRON, J. T.; HECKENBERGER, M.; WATLING, J.; DORSHOW, W. B.; MORAES, B.; LIMA, H.; TEIXEIRA, W. G.; NEVES, E.; HOSLER, D.; WAURA, K.; KUIKURO, H.; KUIKURO, W.; KUIKURO, A.; FAUSTO, C.; FRANCHETTO, B. |
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Afiliação: |
MORGAN J. SCHMIDT, MASSACHUSETTS INSTITUTE OF TECHNOLOGY; SAMUEL LUKENS GOLDBERG, UNIVERSITY OF MIAMI; J. TAYLOR PERRON, MASSACHUSETTS INSTITUTE OF TECHNOLOGY; MICHAEL HECKENBERGER, UNIVERSITY OF FLORIDA; JENNIFER WATLING, UNIVERSIDADE DE SÃO PAULO; MUSEU DE ARQUEOLOGIA E ETNOLOGIA; WETHERBEE BRYAN DORSHOW, EARTH ANALYTIC, INC; PUENTE INSTITUTE; BRUNO MORAES, UNIVERSITY OF PITTSBURGH; MUSEU PARAENSE EMILIO GOELDI; HELENA LIMA, MUSEU PARAENSE EMILIO GOELDI; WENCESLAU GERALDES TEIXEIRA, CNPS; EDUARDO NEVES, UNIVERSIDADE DE SÃO PAULO; MUSEU DE ARQUEOLOGIA E ETNOLOGIA; DOROTHY HOSLER, MASSACHUSETTS INSTITUTE OF TECHNOLOGY; CENTER FOR MATERIALS RESEARCH IN ARCHAEOLOGY; KUMESSI WAURA, ASSOCIAÇÃO INDÍGENA KUIKURO DO ALTO XINGU; HULKE KUIKURO, ASSOCIAÇÃO INDÍGENA KUIKURO DO ALTO XINGU; WATE KUIKURO, ASSOCIAÇÃO INDÍGENA KUIKURO DO ALTO XINGU; AFUKAKA KUIKURO, ASSOCIAÇÃO INDÍGENA KUIKURO DO ALTO XINGU; CARLOS FAUSTO, UNIVERSIDADE FEDERAL DO RIO DE JANEIRO; BRUNA FRANCHETTO, UNIVERSIDADE FEDERAL DO RIO DE JANEIRO. |
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Título: |
Estimating soil carbon in Southern Amazon late holocene anthropogenic landscapes containing archaeological 'Dark Earth' Anthrosols. |
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Ano de publicação: |
2020 |
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Fonte/Imprenta: |
In: AMERICAN GEOPHYSICAL UNION FALL MEETING, 2020. Abstracts [...]. Washington, DC: American Geophysical Union, 2020. |
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Idioma: |
Inglês |
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Conteúdo: |
Amazonian dark earths (ADE) are anthropogenic soils with concentrated carbon and nutrients that formed mainly during the latter half of the Holocene, prior to the arrival of Europeans, but are still forming on a more limited scale up to the present in indigenous communities. ADE, a result of domestic, economic, and agricultural activities in and around human settlements, are noted for their extraordinary fertility and resilience and for the significant quantities of organic carbon, much in the form of charcoal. The deepest and most extensive areas of ADE are generally located on the bluffs of major rivers adjacent to floodplains, but significant areas of ADE have also been found in floodplains and in headwater and interfluvial areas. Our research aims to shed light on the distribution of modified soils in distinct regions of the Amazon in relation to landforms and the environment. Research on ADE has led to the development of a 'biochar' industry that promotes the incorporation of charcoal into the soil for the dual purpose of improving fertility and sequestering carbon, but the potential for large-scale carbon storage in anthropogenic soils is unclear, in part because the amount of carbon already stored in ADE is unknown as there is a notable lack of research attempting to quantify the carbon over the scale of a site or region. We undertook this challenge in the Upper Xingu region of southeastern Amazonia in partnership with the local Kuikuro indigenous community who have shared their valuable traditional knowledge on the creation and management of ADE. We used data from over 3500 soil samples from diverse contexts, both ancient and modern, that we collected and analyzed over the past two decades for organic carbon and a range of other chemical and physical properties that can serve as proxies for soil modification by humans. Dark earth samples from profiles down to 1 m depth in archaeological sites ranged from 20% to 150% more OC than unmodified forest soil and dark earth profiles in current and historic villages ranged from 20-90% more organic carbon. We used the results from soil sample transects to estimate the carbon in landuse zones within and surrounding modern, historic, and ancient settlement sites. In continuing work, we are attempting to use satellite remote sensing and AI to extrapolate our results across a larger region. MenosAmazonian dark earths (ADE) are anthropogenic soils with concentrated carbon and nutrients that formed mainly during the latter half of the Holocene, prior to the arrival of Europeans, but are still forming on a more limited scale up to the present in indigenous communities. ADE, a result of domestic, economic, and agricultural activities in and around human settlements, are noted for their extraordinary fertility and resilience and for the significant quantities of organic carbon, much in the form of charcoal. The deepest and most extensive areas of ADE are generally located on the bluffs of major rivers adjacent to floodplains, but significant areas of ADE have also been found in floodplains and in headwater and interfluvial areas. Our research aims to shed light on the distribution of modified soils in distinct regions of the Amazon in relation to landforms and the environment. Research on ADE has led to the development of a 'biochar' industry that promotes the incorporation of charcoal into the soil for the dual purpose of improving fertility and sequestering carbon, but the potential for large-scale carbon storage in anthropogenic soils is unclear, in part because the amount of carbon already stored in ADE is unknown as there is a notable lack of research attempting to quantify the carbon over the scale of a site or region. We undertook this challenge in the Upper Xingu region of southeastern Amazonia in partnership with the local Kuikuro indigenous community who have s... Mostrar Tudo |
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Thesaurus NAL: |
Anthrosols; Carbon cycle. |
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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/1157567/1/Estimating-soil-carbon-in-Southern-Amazon-late-holocene-anthropogenic-landscapes-2020.pdf
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Marc: |
LEADER 03365nam a2200325 a 4500
001 2157567
005 2023-11-06
008 2020 bl uuuu u00u1 u #d
100 1 $aSCHMIDT, M. J.
245 $aEstimating soil carbon in Southern Amazon late holocene anthropogenic landscapes containing archaeological 'Dark Earth' Anthrosols.$h[electronic resource]
260 $aIn: AMERICAN GEOPHYSICAL UNION FALL MEETING, 2020. Abstracts [...]. Washington, DC: American Geophysical Union$c2020
520 $aAmazonian dark earths (ADE) are anthropogenic soils with concentrated carbon and nutrients that formed mainly during the latter half of the Holocene, prior to the arrival of Europeans, but are still forming on a more limited scale up to the present in indigenous communities. ADE, a result of domestic, economic, and agricultural activities in and around human settlements, are noted for their extraordinary fertility and resilience and for the significant quantities of organic carbon, much in the form of charcoal. The deepest and most extensive areas of ADE are generally located on the bluffs of major rivers adjacent to floodplains, but significant areas of ADE have also been found in floodplains and in headwater and interfluvial areas. Our research aims to shed light on the distribution of modified soils in distinct regions of the Amazon in relation to landforms and the environment. Research on ADE has led to the development of a 'biochar' industry that promotes the incorporation of charcoal into the soil for the dual purpose of improving fertility and sequestering carbon, but the potential for large-scale carbon storage in anthropogenic soils is unclear, in part because the amount of carbon already stored in ADE is unknown as there is a notable lack of research attempting to quantify the carbon over the scale of a site or region. We undertook this challenge in the Upper Xingu region of southeastern Amazonia in partnership with the local Kuikuro indigenous community who have shared their valuable traditional knowledge on the creation and management of ADE. We used data from over 3500 soil samples from diverse contexts, both ancient and modern, that we collected and analyzed over the past two decades for organic carbon and a range of other chemical and physical properties that can serve as proxies for soil modification by humans. Dark earth samples from profiles down to 1 m depth in archaeological sites ranged from 20% to 150% more OC than unmodified forest soil and dark earth profiles in current and historic villages ranged from 20-90% more organic carbon. We used the results from soil sample transects to estimate the carbon in landuse zones within and surrounding modern, historic, and ancient settlement sites. In continuing work, we are attempting to use satellite remote sensing and AI to extrapolate our results across a larger region.
650 $aAnthrosols
650 $aCarbon cycle
700 1 $aGOLDBERG, S. L.
700 1 $aPERRON, J. T.
700 1 $aHECKENBERGER, M.
700 1 $aWATLING, J.
700 1 $aDORSHOW, W. B.
700 1 $aMORAES, B.
700 1 $aLIMA, H.
700 1 $aTEIXEIRA, W. G.
700 1 $aNEVES, E.
700 1 $aHOSLER, D.
700 1 $aWAURA, K.
700 1 $aKUIKURO, H.
700 1 $aKUIKURO, W.
700 1 $aKUIKURO, A.
700 1 $aFAUSTO, C.
700 1 $aFRANCHETTO, B.
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