Data from: Warming alters surface soil organic matter composition despite unchanged carbon stock in a Tibetan permafrost ecosystem ...

1. Climate warming can alter ecosystem carbon (C) balance and also the composition of soil organic matter (SOM), with important local and global implications. However, the extent to which rising temperature affects SOM composition in permafrost ecosystems remains poorly understood. 2. Here, we exper...

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Bibliographic Details
Main Authors: Li, Fei, Peng, Yunfeng, Chen, Leiyi, Yang, Guibiao, Abbott, Benjamin W, Zhang, Dianye, Fang, Kai, Wang, Guanqin, Wang, Jun, Yu, Jianchun, Liu, Li, Zhang, Qiwen, Chen, Kelong, Mohammat, Anwar, Yang, Yuanhe
Format: Dataset
Language:English
Published: Dryad 2019
Subjects:
permafrost
Online Access:https://dx.doi.org/10.5061/dryad.bcc2fqz7p
https://datadryad.org/stash/dataset/doi:10.5061/dryad.bcc2fqz7p
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Summary:1. Climate warming can alter ecosystem carbon (C) balance and also the composition of soil organic matter (SOM), with important local and global implications. However, the extent to which rising temperature affects SOM composition in permafrost ecosystems remains poorly understood. 2. Here, we experimentally warmed a permafrost ecosystem by open-top chambers (OTCs) on the Tibetan Plateau for four years to quantify the responses of C inputs via vegetation production, C losses via soil respiration, and soil organic carbon (SOC) stocks in the top 30 cm. We also characterized the molecular composition of SOM using 13C nuclear magnetic resonance (NMR) and biomarker analyses. 3. The results indicated that warming treatment significantly increased root biomass, soil respiration, heterotrophic respiration and its contribution to soil respiration by 16.7%, 49.0%, 63.2% and 9.5%, respectively. While we observed no change in SOC stocks, warming altered SOM composition in the 0-10 cm layer during the fourth experimental ...

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