Soil carbon loss with warming: New evidence from carbon‐degrading enzymes
Climate warming affects soil carbon (C) dynamics, with possible serious consequences for soil C stocks and atmospheric CO2 concentrations. However, the mechanisms underlying changes in soil C storage are not well understood, hampering long‐term predictions of climate C‐feedbacks. The activity of the...
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Published in | Global change biology Vol. 26; no. 4; pp. 1944 - 1952 |
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Main Authors | , , , , , , , , , , , |
Format | Journal Article |
Language | English |
Published |
England
Blackwell Publishing Ltd
01.04.2020
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Subjects | |
Online Access | Get full text |
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Summary: | Climate warming affects soil carbon (C) dynamics, with possible serious consequences for soil C stocks and atmospheric CO2 concentrations. However, the mechanisms underlying changes in soil C storage are not well understood, hampering long‐term predictions of climate C‐feedbacks. The activity of the extracellular enzymes ligninase and cellulase can be used to track changes in the predominant C sources of soil microbes and can thus provide mechanistic insights into soil C loss pathways. Here we show, using meta‐analysis, that reductions in soil C stocks with warming are associated with increased ratios of ligninase to cellulase activity. Furthermore, whereas long‐term (≥5 years) warming reduced the soil recalcitrant C pool by 14%, short‐term warming had no significant effect. Together, these results suggest that warming stimulates microbial utilization of recalcitrant C pools, possibly exacerbating long‐term climate‐C feedbacks.
Our results, for the first time, identify progressive shifts from cellulase to ligninase as key drivers of soil C storage to long‐term experimental warming. These results provide new insights to reconcile the highly debated topic of the effects of climate warming on soil C storage, particularly for long‐term climate warming. |
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ISSN: | 1354-1013 1365-2486 |
DOI: | 10.1111/gcb.14986 |