Pasture damage by an Amazonian earthworm
Armand Chauvel (),
Michel Grimaldi,
Eleusa Barros,
Eric Blanchart,
Thierry Desjardins,
Max Sarrazin and
Patrick Lavelle
Additional contact information
Armand Chauvel: Laboratoire dEcologie des Sols Tropicaux, ORSTOM
Michel Grimaldi: ORSTOM/INRA, Science du Sol
Eleusa Barros: INPA/ORSTOM-Ecologia
Eric Blanchart: ORSTOM Martinique
Thierry Desjardins: Laboratoire dEcologie des Sols Tropicaux, ORSTOM
Max Sarrazin: INPA/ORSTOM-Ecologia
Patrick Lavelle: Laboratoire dEcologie des Sols Tropicaux, ORSTOM
Nature, 1999, vol. 398, issue 6722, 32-33
Abstract:
Abstract Almost all cultivated soils undergo some reduction in the porosity of the surface layers, and nowhere is this more evident than in tropical rainforests that have been converted to pastures. Following deforestation in an area of Costa Rica, soil bulk density has been shown to increase rapidly after conversion to pasture, leading to poor drainage and a reduced rate of gaseous diffusion1. These factors limit methane consumption and promote the anaerobic production of methane. A similar effect on methane flux has been found in upland soils in the Brazilian Amazonian basin after conversion from forest to pasture2,3. Increases in atmospheric methane are therefore not limited to emissions from flooded soils4, as forest-to-pasture conversion promotes the anaerobic mineralization of organic matter by changing the physical properties of soil.
Date: 1999
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Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:398:y:1999:i:6722:d:10.1038_17946
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DOI: 10.1038/17946
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