Institute of Ecology and Environmental Sciences, iEES Paris, Sorbonne Université, CNRS, IRD, INRA, UPEC, Univ Paris Diderot, 4 Place Jussieu, Paris 75005, France
Institute of Ecology and Environmental Sciences, iEES Paris, Sorbonne Université, CNRS, IRD, INRA, UPEC, Univ Paris Diderot, 4 Place Jussieu, Paris 75005, France
Renewable Materials Research Centre, Department of Wood and Forest Sciences, Université Laval, Québec, QC, Canada
Kevin Potard
Institute of Ecology and Environmental Sciences, iEES Paris, Sorbonne Université, CNRS, IRD, INRA, UPEC, Univ Paris Diderot, 4 Place Jussieu, Paris 75005, France
Célia R. Montes
IEE, LEST, Universidade de São Paulo, São Paulo 05508-010, Brazil
Patricia Merdy
Université de Toulon, Aix Marseille Univ, CNRS, IM2NP, Toulon, France
Adolpho J. Melfi
IEE, LEST, Universidade de São Paulo, São Paulo 05508-010, Brazil
Yves Lucas
Université de Toulon, Aix Marseille Univ, CNRS, IM2NP, Toulon, France
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Total article views: 5,596 (including HTML, PDF, and XML)
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The vulnerability to decomposition of organic C in Amazonian podzols as a result of predicted drier soil moisture regimes was tested: more than four times as much CO2 was released from soils under oxic conditions with the addition of N relative to soils under the prevailing anoxic conditions. An extrapolation of the data to the whole of the Amazonian podzols suggests that this increased C-CO2 flux to the atmosphere could be equivalent to 8 % of the current net global C flux to the atmosphere.
The vulnerability to decomposition of organic C in Amazonian podzols as a result of predicted...