Microbial nitrogen and phosphorus co‐limitation across permafrost region

Abstract The status of plant and microbial nutrient limitation have profound impacts on ecosystem carbon cycle in permafrost areas, which store large amounts of carbon and experience pronounced climatic warming. Despite the long‐term standing paradigm assumes that cold ecosystems primarily have nitr...

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Bibliographic Details
Published in:Global Change Biology
Main Authors: Zhang, Dianye, Wang, Lu, Qin, Shuqi, Kou, Dan, Wang, Siyu, Zheng, Zhihu, Peñuelas, Josep, Yang, Yuanhe
Other Authors: National Basic Research Program of China, National Natural Science Foundation of China
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2023
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Online Access:http://dx.doi.org/10.1111/gcb.16743
https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.16743
Description
Summary:Abstract The status of plant and microbial nutrient limitation have profound impacts on ecosystem carbon cycle in permafrost areas, which store large amounts of carbon and experience pronounced climatic warming. Despite the long‐term standing paradigm assumes that cold ecosystems primarily have nitrogen deficiency, large‐scale empirical tests of microbial nutrient limitation are lacking. Here we assessed the potential microbial nutrient limitation across the Tibetan alpine permafrost region, using the combination of enzymatic and elemental stoichiometry, genes abundance and fertilization method. In contrast with the traditional view, the four independent approaches congruently detected widespread microbial nitrogen and phosphorus co‐limitation in both the surface soil and deep permafrost deposits, with stronger limitation in the topsoil. Further analysis revealed that soil resources stoichiometry and microbial community composition were the two best predictors of the magnitude of microbial nutrient limitation. High ratio of available soil carbon to nutrient and low fungal/bacterial ratio corresponded to strong microbial nutrient limitation. These findings suggest that warming‐induced enhancement in soil nutrient availability could stimulate microbial activity, and probably amplify soil carbon losses from permafrost areas.