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Please use this identifier to cite or link to this item: https://repositorio.inpa.gov.br/handle/1/18810
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dc.contributor.authorRubinstein, Adriana-
dc.contributor.authorVasconcelos, Heraldo L.-
dc.date.accessioned2020-06-15T22:03:10Z-
dc.date.available2020-06-15T22:03:10Z-
dc.date.issued2005-
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/18810-
dc.description.abstractMost of the forests of the Amazon basin grow on nutrient-poor soils (Jordan 1982). Despite this, these forests remain productive through a variety of nutrient conservation mechanisms and a very effective system of organic matter decomposition and nutrient cycling (Jordan 1982). When an area of forest is fragmented however, the remaining patches experience modified microclimatic conditions (Camargo & Kapos 1995, Didham & Lawton 1999), and changes in floristic composition (Laurance et al. 1998), which can affect the decomposer community (Didham et al. 1996, Souza & Brown 1994) and consequently the decomposition process. Copyright © 2005 Cambridge University Press.en
dc.language.isoenpt_BR
dc.relation.ispartofVolume 21, Número 6, Pags. 699-702pt_BR
dc.rightsRestrito*
dc.subjectCommunity Structureen
dc.subjectDecompositionen
dc.subjectHabitat Fragmentationen
dc.subjectLeaf Litteren
dc.subjectNutrient Cyclingen
dc.subjectTurnoveren
dc.subjectAmazon Basinen
dc.subjectSouth Americaen
dc.subjectWestern Hemisphereen
dc.subjectWorlden
dc.titleLeaf-litter decomposition in Amazonian forest fragmentsen
dc.typeArtigopt_BR
dc.identifier.doi10.1017/S0266467405002762-
dc.publisher.journalJournal of Tropical Ecologypt_BR
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