Alpine soil carbon is vulnerable to rapid microbial decomposition under climate cooling View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

2017-09

AUTHORS

Linwei Wu, Yunfeng Yang, Shiping Wang, Haowei Yue, Qiaoyan Lin, Yigang Hu, Zhili He, Joy D Van Nostrand, Lauren Hale, Xiangzhen Li, Jack A Gilbert, Jizhong Zhou

ABSTRACT

As climate cooling is increasingly regarded as important natural variability of long-term global warming trends, there is a resurging interest in understanding its impact on biodiversity and ecosystem functioning. Here, we report a soil transplant experiment from lower to higher elevations in a Tibetan alpine grassland to simulate the impact of cooling on ecosystem community structure and function. Three years of cooling resulted in reduced plant productivity and microbial functional potential (for example, carbon respiration and nutrient cycling). Microbial genetic markers associated with chemically recalcitrant carbon decomposition remained unchanged despite a decrease in genes associated with chemically labile carbon decomposition. As a consequence, cooling-associated changes correlated with a decrease in soil organic carbon (SOC). Extrapolation of these results suggests that for every 1 °C decrease in annual average air temperature, 0.1 Pg (0.3%) of SOC would be lost from the Tibetan plateau. These results demonstrate that microbial feedbacks to cooling have the potential to differentially impact chemically labile and recalcitrant carbon turnover, which could lead to strong, adverse consequences on soil C storage. Our findings are alarming, considering the frequency of short-term cooling and its scale to disrupt ecosystems and biogeochemical cycling. More... »

PAGES

2102-2111

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/ismej.2017.75

DOI

http://dx.doi.org/10.1038/ismej.2017.75

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1085560596

PUBMED

https://www.ncbi.nlm.nih.gov/pubmed/28534876


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