Large fluxes and rapid turnover of mineral-associated carbon across topographic gradients in a humid tropical forest: insights from paired <sup>14</sup>C analysis

It has been proposed that the large soil carbon (C) stocks of humid tropical forests result predominantly from C stabilization by reactive minerals, whereas oxygen (O<sub>2</sub>) limitation of decomposition has received much less attention. We examined the importance of these factors in...

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Bibliographic Details
Main Authors: S. J Hall, G. McNicol, T. Natake, W. L. Silver
Format: Article
Language:English
Published: Copernicus Publications 2015-04-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/12/2471/2015/bg-12-2471-2015.pdf

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