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