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| 25. | | LAPOLA, D.; QUESADA, C. A. N.; NORBY, R. J.; ARAUJO, A. C.; DOMINGUES, T.; HARTLEY, I.; KRUIJT, B.; LEWIN, K.; MEIR, P.; RAMMIG, A.; WALKER, A.; OMETTO, J. The AmazonFACE research program: assessing the effects of increasing atmospheric CO2 on the ecology and resilience of the Amazon forest. In: INTERNATIONAL SCIENTIFIC CONFERENCE "OUR COMMON FUTURE UNDER CLIMATE CHANGE", 2015, Paris. Abstract book. [S.l.: s.n.], 2015. p. 264.| Biblioteca(s): Embrapa Amazônia Oriental. |
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| 30. | | MENDONÇA, H. V. de; MARTINS, C. E.; ROCHA, W. S. D. da; BORGES, C. A. V.; OMETTO, J. P. H. B.; OTENIO, M. H. Biofertilizer replace urea as a source of nitrogen for sugarcane production. Water, Air, & Soil Pollution, v. 229, n. 7, article 216, 2018. 7 p.| Biblioteca(s): Embrapa Gado de Leite. |
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| 33. | | REZENDE, L. F. C. de; ARENQUE, B.; OMETTO, J.; RANDOW, C. von; MOURA, M. S. B. de; AIDAR, S. de T.; SOUZA, L. S. B. de. Study of scenarios and answers from Caatinga vegetation in the face of increased concentration of CO2 in the atmosphere. In: INTERNATIONAL SYMPOSIUM ON CLIMATE CHANGE, IMPACTS AND VULNERABILITIES IN BRAZIL: PREPARING THE BRAZILIAN NORTHEAST FOR THE FUTURE, 2012, Natal. Abstracts... Natal: UFRN: IBD, 2012.| Biblioteca(s): Embrapa Semiárido. |
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| 40. | | MALHI, Y.; MELACK, J.; GATTI, L. V.; OMETTO, J.; KESSELMEIER, J.; WOLFF, S.; ARAGÃO, L. E. O.; COSTA, M.; SALESKA, S.; PANGALA, S. R.; BASSO, L. S.; RIZZO, L.; ARAUJO, A. C. de; RESTREPO-COUPE, N. Biogeochemical cycles of the Amazon. In: SCIENCE panel for the Amazon: Amazon assessment report 2021: part I: The Amazon as a regional entity of the Earth system. New York, NY: United Nations Sustainable Development Solutions Network, 2021. Cap. 6, pag. irregular.| Biblioteca(s): Embrapa Amazônia Oriental. |
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Registro Completo
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Biblioteca(s): |
Embrapa Amazônia Oriental. |
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Data corrente: |
27/02/2008 |
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Data da última atualização: |
23/11/2022 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Circulação/Nível: |
Internacional - A |
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Autoria: |
DAVIDSON, E. A.; CARVALHO, C. J. R. de; FIGUEIRA, A. M.; ISHIDA, F. Y.; OMETTO, J. P. H. B.; NARDOTO, G. B.; SABÁ, R. T.; HAYASHI, S. N.; LEAL, E. C.; VIEIRA, I. C. G.; MARTINELLI, L. A. |
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Afiliação: |
Eric A. Davidson, The Woods Hole Research Center; CLAUDIO JOSE REIS DE CARVALHO, CPATU; Adelaine Michela Figueira, CENA; Françoise Yoko Ishida, CENA; Jean Pierre H. B. Ometto, CENA; Gabriela B. Nardoto, CENA; Renata Tuma Sabá, bolsista CPATU; Sanae N. Hayashi, MPEG; Eliane C. Leal, MPEG; Ima Célia G. Vieira, MPEG; Luiz A. Martinelli, CENA. |
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Título: |
Recuperation of nitrogen cycling in Amazonian forests following agricultural abandonment. |
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Ano de publicação: |
2007 |
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Fonte/Imprenta: |
Nature, v. 447, n. 7147, p. 995-998, Jun. 2007. |
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DOI: |
10.1038/nature05900 |
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Idioma: |
Português |
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Notas: |
Disponível também on-line. |
|
Conteúdo: |
Phosphorus (P) is generally considered the most common limiting nutrient for productivity of mature tropical lowland forests growing on highly weathered soils1, 2, 3, 4, 5. It is often assumed that P limitation also applies to young tropical forests, but nitrogen (N) losses during land-use change may alter the stoichiometric balance of nutrient cycling processes. In the Amazon basin, about 16% of the original forest area has been cleared6, and about 30?50% of cleared land is estimated now to be in some stage of secondary forest succession following agricultural abandonment7. Here we use forest age chronosequences to demonstrate that young successional forests growing after agricultural abandonment on highly weathered lowland tropical soils exhibit conservative N-cycling properties much like those of N-limited forests on younger soils in temperate latitudes. As secondary succession progresses, N-cycling properties recover and the dominance of a conservative P cycle typical of mature lowland tropical forests re-emerges. These successional shifts in N:P cycling ratios with forest age provide a mechanistic explanation for initially lower and then gradually increasing soil emissions of the greenhouse gas nitrous oxide (N2O). The patterns of N and P cycling during secondary forest succession, demonstrated here over decadal timescales, are similar to N- and P-cycling patterns during primary succession as soils age over thousands and millions of years, thus revealing that N availability in terrestrial ecosystems is ephemeral and can be disrupted by either natural or anthropogenic disturbances at several timescales. MenosPhosphorus (P) is generally considered the most common limiting nutrient for productivity of mature tropical lowland forests growing on highly weathered soils1, 2, 3, 4, 5. It is often assumed that P limitation also applies to young tropical forests, but nitrogen (N) losses during land-use change may alter the stoichiometric balance of nutrient cycling processes. In the Amazon basin, about 16% of the original forest area has been cleared6, and about 30?50% of cleared land is estimated now to be in some stage of secondary forest succession following agricultural abandonment7. Here we use forest age chronosequences to demonstrate that young successional forests growing after agricultural abandonment on highly weathered lowland tropical soils exhibit conservative N-cycling properties much like those of N-limited forests on younger soils in temperate latitudes. As secondary succession progresses, N-cycling properties recover and the dominance of a conservative P cycle typical of mature lowland tropical forests re-emerges. These successional shifts in N:P cycling ratios with forest age provide a mechanistic explanation for initially lower and then gradually increasing soil emissions of the greenhouse gas nitrous oxide (N2O). The patterns of N and P cycling during secondary forest succession, demonstrated here over decadal timescales, are similar to N- and P-cycling patterns during primary succession as soils age over thousands and millions of years, thus revealing that N availabi... Mostrar Tudo |
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Palavras-Chave: |
Brasil. |
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Thesagro: |
Agricultura; Floresta; Nitrogênio. |
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Thesaurus NAL: |
Amazonia. |
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Categoria do assunto: |
-- |
|
Marc: |
LEADER 02556naa a2200325 a 4500
001 1409000
005 2022-11-23
008 2007 bl uuuu u00u1 u #d
024 7 $a10.1038/nature05900$2DOI
100 1 $aDAVIDSON, E. A.
245 $aRecuperation of nitrogen cycling in Amazonian forests following agricultural abandonment.$h[electronic resource]
260 $c2007
500 $aDisponível também on-line.
520 $aPhosphorus (P) is generally considered the most common limiting nutrient for productivity of mature tropical lowland forests growing on highly weathered soils1, 2, 3, 4, 5. It is often assumed that P limitation also applies to young tropical forests, but nitrogen (N) losses during land-use change may alter the stoichiometric balance of nutrient cycling processes. In the Amazon basin, about 16% of the original forest area has been cleared6, and about 30?50% of cleared land is estimated now to be in some stage of secondary forest succession following agricultural abandonment7. Here we use forest age chronosequences to demonstrate that young successional forests growing after agricultural abandonment on highly weathered lowland tropical soils exhibit conservative N-cycling properties much like those of N-limited forests on younger soils in temperate latitudes. As secondary succession progresses, N-cycling properties recover and the dominance of a conservative P cycle typical of mature lowland tropical forests re-emerges. These successional shifts in N:P cycling ratios with forest age provide a mechanistic explanation for initially lower and then gradually increasing soil emissions of the greenhouse gas nitrous oxide (N2O). The patterns of N and P cycling during secondary forest succession, demonstrated here over decadal timescales, are similar to N- and P-cycling patterns during primary succession as soils age over thousands and millions of years, thus revealing that N availability in terrestrial ecosystems is ephemeral and can be disrupted by either natural or anthropogenic disturbances at several timescales.
650 $aAmazonia
650 $aAgricultura
650 $aFloresta
650 $aNitrogênio
653 $aBrasil
700 1 $aCARVALHO, C. J. R. de
700 1 $aFIGUEIRA, A. M.
700 1 $aISHIDA, F. Y.
700 1 $aOMETTO, J. P. H. B.
700 1 $aNARDOTO, G. B.
700 1 $aSABÁ, R. T.
700 1 $aHAYASHI, S. N.
700 1 $aLEAL, E. C.
700 1 $aVIEIRA, I. C. G.
700 1 $aMARTINELLI, L. A.
773 $tNature$gv. 447, n. 7147, p. 995-998, Jun. 2007.
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