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Registro Completo |
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Biblioteca(s): |
Embrapa Agrobiologia; Embrapa Semiárido; Embrapa Solos. |
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Data corrente: |
08/02/2021 |
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Data da última atualização: |
03/11/2021 |
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Tipo da produção científica: |
Artigo em Periódico Indexado |
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Autoria: |
MENEZES, R. S. C.; SALES, A. T.; PRIMO, D. C.; ALBUQUERQUE, E. R. G. M. de; JESUS, K. N. de; PAREYN, F. G. C.; SANTANA, M. da S.; SANTOS, U. J. dos; MARTINS, J. C. R.; ALTHOFF, T. D.; NASCIMENTO, D. M. do; GOUVEIA, R. F.; FERNANDES, M. M.; LOUREIRO, D. C.; ARAUJO FILHO, J. C. de; GIONGO, V.; DUDA, G. P.; ALVES, B. J. R.; IVO, W. M. P. de M.; ANDRADE, E. M. de; PINTO, A. de S.; SAMPAIO, E. V. de S. B. |
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Afiliação: |
RÔMULO SIMÕES CEZAR MENEZES, UFPE; ALDO TORRES SALES, UFPE; DÁRIO COSTA PRIMO, UFPE; ELIZA ROSÁRIO GOMES MARINHO DE ALBUQUERQUE, ASSOCIAÇÃO PLANTAS DO NORDESTE; KENNEDY NASCIMENTO DE JESUS, FACULDADES DE ENFERMAGEM NOVA ESPERANÇA; FRANS GERMAIN CORNEEL PAREYN, ASSOCIAÇÃO PLANTAS DO NORDESTE; MÔNICA DA SILVA SANTANA, UFCE; UEMESON JOSÉ DOS SANTOS, UFPE; JÚLIO CÉSAR RODRIGUES MARTINS, FACULDADES DE ENFERMAGEM NOVA ESPERANÇA; TIAGO DINIZ ALTHOFF, UFPE; DIEGO MARCELINO DO NASCIMENTO, UFPE; RAFAEL FEITOSA GOUVEIA, UFS; MILTON MARQUES FERNANDES, UFS; DIEGO CAMPANA LOUREIRO, UFS; JOSE COELHO DE ARAUJO FILHO, CNPS; VANDERLISE GIONGO, CPATSA; GUSTAVO PEREIRA DUDA, UFAPE; BRUNO JOSE RODRIGUES ALVES, CNPAB; WALANE MARIA PEREIRA DE MELLO IVO, CPATC; EUNICE MAIA DE ANDRADE, UFERSA; ALEXANDRE DE SIQUEIRA PINTO, UFS; EVERARDO VALADARES DE SÁ BARRETTO SAMPAIO, UFPE. |
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Título: |
Soil and vegetation carbon stocks after land-use changes in a seasonally dry tropical forest. |
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Ano de publicação: |
2021 |
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Fonte/Imprenta: |
Geoderma, v. 390, 114943, May 2021. |
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DOI: |
https://doi.org/10.1016/j.geoderma.2021.114943 |
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Idioma: |
Inglês |
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Conteúdo: |
The lack of robust scientific data still hinders estimates of soil and plant carbon (C) losses due to land-use changes in most dry tropical ecosystems. The present study investigated the effects of land-use and cover changes on total ecosystem C stocks in NE Brazil, aiming to quantify C losses after the removal of the native forest, known as Caatinga. The sampling design included the four main land-use/cover types (Dense Caatinga, Open Caatinga, Pastures and Crop fields) and the seven main soil classes (Arenosols, Acrisols, Regosols, Ferrasols, Luvisols, Planosols, and Leptosols), a combination that represents over 90% of the region. This design resulted in 192 sampling points (48 in each land-use), distributed proportionally to the area of occurrence of each soil class. In each sampling point, we determined C stocks in soil organic matter (SOM) and roots (to a depth of 1 m or rock layer), aboveground vegetation biomass (trees and herbs, separately), deadwood, and surface litter. Areas covered by Dense Caatinga store, on average, nearly 125 Mg ha-1 of C. Most of this C is stored in the soil organic matter (72.1%), followed by aboveground biomass (15.9%), belowground biomass (7.3%), deadwood (2.9%), litter (1.3%), and herbaceous biomass (0.5%). The substitution of Dense Caatinga to plant pastures and crop fields caused losses of >50% of ecosystem C stocks, reaching almost 65 Mg ha-1 of C, with nearly equal losses from the SOM and vegetation biomass compartments. Open Caatinga store nearly 30% less C than Dense Caatinga. Contrary to what was expected, the overall differences in C stocks between soil classes were not significant, with a few exceptions. We expect that the findings of this study will contribute to a more robust inventory of GHG emissions/removals due to land-use changes in NE Brazil and other dry tropical regions of the globe. MenosThe lack of robust scientific data still hinders estimates of soil and plant carbon (C) losses due to land-use changes in most dry tropical ecosystems. The present study investigated the effects of land-use and cover changes on total ecosystem C stocks in NE Brazil, aiming to quantify C losses after the removal of the native forest, known as Caatinga. The sampling design included the four main land-use/cover types (Dense Caatinga, Open Caatinga, Pastures and Crop fields) and the seven main soil classes (Arenosols, Acrisols, Regosols, Ferrasols, Luvisols, Planosols, and Leptosols), a combination that represents over 90% of the region. This design resulted in 192 sampling points (48 in each land-use), distributed proportionally to the area of occurrence of each soil class. In each sampling point, we determined C stocks in soil organic matter (SOM) and roots (to a depth of 1 m or rock layer), aboveground vegetation biomass (trees and herbs, separately), deadwood, and surface litter. Areas covered by Dense Caatinga store, on average, nearly 125 Mg ha-1 of C. Most of this C is stored in the soil organic matter (72.1%), followed by aboveground biomass (15.9%), belowground biomass (7.3%), deadwood (2.9%), litter (1.3%), and herbaceous biomass (0.5%). The substitution of Dense Caatinga to plant pastures and crop fields caused losses of >50% of ecosystem C stocks, reaching almost 65 Mg ha-1 of C, with nearly equal losses from the SOM and vegetation biomass compartments. Open Caatinga... Mostrar Tudo |
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Palavras-Chave: |
Ecossistema Caatinga; Estoque do carbono; Estoques do ecossistema; Semiárido. |
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Thesagro: |
Caatinga; Desmatamento; Dióxido de Carbono; Floresta Tropical; Mudança Climática; Solo; Uso da Terra; Vegetação. |
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Thesaurus Nal: |
Carbon; Carbon dioxide; Deforestation; Land use; Land use change; Vegetation. |
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Categoria do assunto: |
P Recursos Naturais, Ciências Ambientais e da Terra |
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Marc: |
LEADER 03564naa a2200601 a 4500
001 2130671
005 2021-11-03
008 2021 bl uuuu u00u1 u #d
024 7 $ahttps://doi.org/10.1016/j.geoderma.2021.114943$2DOI
100 1 $aMENEZES, R. S. C.
245 $aSoil and vegetation carbon stocks after land-use changes in a seasonally dry tropical forest.$h[electronic resource]
260 $c2021
520 $aThe lack of robust scientific data still hinders estimates of soil and plant carbon (C) losses due to land-use changes in most dry tropical ecosystems. The present study investigated the effects of land-use and cover changes on total ecosystem C stocks in NE Brazil, aiming to quantify C losses after the removal of the native forest, known as Caatinga. The sampling design included the four main land-use/cover types (Dense Caatinga, Open Caatinga, Pastures and Crop fields) and the seven main soil classes (Arenosols, Acrisols, Regosols, Ferrasols, Luvisols, Planosols, and Leptosols), a combination that represents over 90% of the region. This design resulted in 192 sampling points (48 in each land-use), distributed proportionally to the area of occurrence of each soil class. In each sampling point, we determined C stocks in soil organic matter (SOM) and roots (to a depth of 1 m or rock layer), aboveground vegetation biomass (trees and herbs, separately), deadwood, and surface litter. Areas covered by Dense Caatinga store, on average, nearly 125 Mg ha-1 of C. Most of this C is stored in the soil organic matter (72.1%), followed by aboveground biomass (15.9%), belowground biomass (7.3%), deadwood (2.9%), litter (1.3%), and herbaceous biomass (0.5%). The substitution of Dense Caatinga to plant pastures and crop fields caused losses of >50% of ecosystem C stocks, reaching almost 65 Mg ha-1 of C, with nearly equal losses from the SOM and vegetation biomass compartments. Open Caatinga store nearly 30% less C than Dense Caatinga. Contrary to what was expected, the overall differences in C stocks between soil classes were not significant, with a few exceptions. We expect that the findings of this study will contribute to a more robust inventory of GHG emissions/removals due to land-use changes in NE Brazil and other dry tropical regions of the globe.
650 $aCarbon
650 $aCarbon dioxide
650 $aDeforestation
650 $aLand use
650 $aLand use change
650 $aVegetation
650 $aCaatinga
650 $aDesmatamento
650 $aDióxido de Carbono
650 $aFloresta Tropical
650 $aMudança Climática
650 $aSolo
650 $aUso da Terra
650 $aVegetação
653 $aEcossistema Caatinga
653 $aEstoque do carbono
653 $aEstoques do ecossistema
653 $aSemiárido
700 1 $aSALES, A. T.
700 1 $aPRIMO, D. C.
700 1 $aALBUQUERQUE, E. R. G. M. de
700 1 $aJESUS, K. N. de
700 1 $aPAREYN, F. G. C.
700 1 $aSANTANA, M. da S.
700 1 $aSANTOS, U. J. dos
700 1 $aMARTINS, J. C. R.
700 1 $aALTHOFF, T. D.
700 1 $aNASCIMENTO, D. M. do
700 1 $aGOUVEIA, R. F.
700 1 $aFERNANDES, M. M.
700 1 $aLOUREIRO, D. C.
700 1 $aARAUJO FILHO, J. C. de
700 1 $aGIONGO, V.
700 1 $aDUDA, G. P.
700 1 $aALVES, B. J. R.
700 1 $aIVO, W. M. P. de M.
700 1 $aANDRADE, E. M. de
700 1 $aPINTO, A. de S.
700 1 $aSAMPAIO, E. V. de S. B
773 $tGeoderma$gv. 390, 114943, May 2021.
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| 1. |  | DENG, J.; XIE, X.-L.; WANG, D.-F.; ZHAO, C.; LV, F.-H.; LI, X.; YANG, J.; YU, J.-L.; SHEN, M.; GAO, L.; YANG, J.-Q.; LIU, M.-J.; LI, W.-R.; WANG, Y.-T.; WANG, F.; LI, J.-Q.; HEHUA, E.; LIU, Y.-G.; SCHEN, Z.-Q.; REN, Y.-L.; LIU, G.-J.; CHEN, Z.-H.; GORKHALI, N. A.; RUSHDI, H. E.; SALEHIAN-DEHKORDI, H.; ESMAILIZADEH, A.; NOSRATI, M.; PAIVA, S. R.; CAETANO, A. R.; STEPÁNEK, O.; OLSAKER, I.; WEIMANN, C.; ERHARDT, G.; CURIK, I.; KANTANEN, J.; MWACHARO, J. M.; HANOTTE, O.; BRUFORD, M. W.; CIANI, E.; PERIASAMY, K.; AMILLS, M.; LENSTRA, J. A.; HAN, J.-L.; ZHANG, H.-P.; LI, L.; LI, M.-H. Paternal origins and migratory episodes of domestic sheep. Current Biology, v. 30, n. 20, p. 4085-4095, 2020.| Tipo: Artigo em Periódico Indexado | Circulação/Nível: A - 1 |
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