Use este identificador para citar ou linkar para este item: https://repositorio.inpa.gov.br/handle/1/13026
Registro completo de metadados
Campo DCValorIdioma
dc.contributor.authorBarros, Henrique Seixas-
dc.contributor.authorFearnside, Philip Martin-
dc.date.accessioned2020-04-17T20:50:12Z-
dc.date.available2020-04-17T20:50:12Z-
dc.date.issued2016-
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/13026-
dc.description.abstractAmazon forest stocks large quantities of carbon both in plant biomass and in soil. Deforestation has accelerated the process of forest fragmentation in the Brazilian Amazon, resulting in changes in carbon stocks in both biomass and soil. Logging, including that under legal forest management, can create edge-like conditions inside the forest. We investigated the relationship between changes in carbon stocks in the soil and the distance to the nearest edge in forest remnants after about 30 years of isolation. We assessed the effect of edges using geographically weighted regression (GWR), which considers the non-stationary character of soil carbon stocks and assigns relative weights to the observations according to the distance between them. Data from 265 georeferenced plots distributed over 28 ha of forest fragments in the Manaus region were included in these analyses. Soil-carbon stocks were estimated for areas before (1984–1986) and after (2012–2013) isolation of the fragments. The GWR model indicated an apparent relationship between change in carbon stocks and distance from the edge (R2 = 0.79). The largest changes occurred in plots located closest to the edges. In 202 plots ⩽100 m from an edge, soil-carbon stock increased significantly (p = 0.01) by a mean of 1.34 Mg ha−1 over the ∼30-year period. Such changes in soil carbon stocks appear to be associated with higher rates of tree mortality caused by microclimatic changes in these areas. Increased necromass inputs combined with changes in composition and structure of vegetation may result in increased rates of decomposition of organic matter, transferring carbon to the soil compartment and increasing soil carbon stocks. Considering both “hard” edges adjacent to deforestation and “soft” edges in logging areas, the soil-carbon increase we measured implies an absorption of 6 × 106 MgC in Brazilian Amazonia. In hard edges maintained for ∼30 years, the soil-carbon increase offsets 8.3% of the carbon losses from “biomass collapse” in the first 100 m from a clearing. Soil carbon did not change significantly in 63 forest-interior plots, suggesting that global climate change has not yet had a detectible effect on this forest carbon compartment. © 2016en
dc.language.isoenpt_BR
dc.relation.ispartofVolume 379, Pags. 30-36pt_BR
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Brazil*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/br/*
dc.subjectBiomassen
dc.subjectDeforestationen
dc.subjectGlobal Warmingen
dc.subjectGreenhouse Gasesen
dc.subjectSoilsen
dc.subjectAmazon Forestsen
dc.subjectEdge Effecten
dc.subjectForest Fragmentationsen
dc.subjectGHG emissionen
dc.subjectSoil Carbonen
dc.subjectCarbonen
dc.subjectBiomassen
dc.subjectCarbon Sequestrationen
dc.subjectDeforestationen
dc.subjectEdge Effecten
dc.subjectForest Edgeen
dc.subjectFragmentationen
dc.subjectGlobal Warmingen
dc.subjectGreenhouse Gasen
dc.subjectLogging (timber)en
dc.subjectMortalityen
dc.subjectRegression Analysisen
dc.subjectSoil Carbonen
dc.subjectSoil Organic Matteren
dc.subjectTreeen
dc.subjectVegetation Dynamicsen
dc.subjectAmazonasen
dc.subjectAmazoniaen
dc.subjectBrasilen
dc.subjectManausen
dc.titleSoil carbon stock changes due to edge effects in central Amazon forest fragmentsen
dc.typeArtigopt_BR
dc.identifier.doi10.1016/j.foreco.2016.08.002-
dc.publisher.journalForest Ecology and Managementpt_BR
Aparece nas coleções:Artigos

Arquivos associados a este item:
Arquivo Descrição TamanhoFormato 
artigo-inpa.pdf773,58 kBAdobe PDFThumbnail
Visualizar/Abrir


Este item está licenciada sob uma Licença Creative Commons Creative Commons