Unexpected no significant soil carbon losses in the Tibetan grasslands due to rodent bioturbation

Author:

Huang Miao1,Gan Dezhao1,Li Zheng2,Wang Jinsong3ORCID,Niu Shuli34ORCID,Zuo Hongchao1,Long Ruijun2,Ma Lei1ORCID

Affiliation:

1. College of Atmospheric Sciences, Lanzhou University , No. 222 Tian-shui South Road, Cheng-guan District, Lanzhou 730000 , P.R. China

2. College of Ecology, Lanzhou University , No. 222 Tian-shui South Road, Cheng-guan District, Lanzhou 730000 , P.R. China

3. Key Laboratory of Ecosystem Network Observation and Simulation, Institute of Geographical Sciences and Natural Resources Research, Chinese Academy of Sciences , Beijing 100101 , P.R. China

4. School of Resources and Environment, University of Chinese Academy of Sciences , Beijing 100049 , P.R. China

Abstract

Abstract The Tibetan grasslands store 2.5% of the Earth’s soil organic carbon. Unsound management practices and climate change have resulted in widespread grassland degradation, providing open habitats for rodent activities. Rodent bioturbation loosens topsoil, reduces productivity, changes soil nutrient conditions, and consequently influences the soil organic carbon stocks of the Tibetan grasslands. However, these effects have not been quantified. Here, using meta-analysis and upscaling approaches, we found that rodent bioturbation impacts on the Tibetan grassland soil organic carbon contents were depth-dependent, with significant (P < 0.001) decreasing of 24.4% in the topsoil (0 to 10 cm) but significant (P < 0.05) increasing of 35.9% in the deeper soil layer (40 to 50 cm), and nonsignificant changes in other soil layers. The depth-dependent responses in soil organic carbon content were closely associated with rodent tunnel burrowing, foraging, excrement deposition, and mixing of the upper and deeper soil layers. Rodent bioturbation had shown nonsignificant impacts on soil bulk density, independent of soil layer. Tibetan grasslands totally lose −35.2 Tg C yr–1 (95% CI: −48.5 to −21.1 Tg C yr–1) and –32.9 Tg C yr–1 (−54.2 to −8.6 Tg C yr–1) due to rodent bioturbation in the 0 to 10 or 0 to 30 cm soil layer, while no significant net loss was found over the 0 to 90 cm layer. Our findings highlight the importance of considering depth-dependent factors to robustly quantify the net changes in the terrestrial soil organic carbon stocks resulting from disturbances such as rodent bioturbation.

Publisher

Oxford University Press (OUP)

Reference60 articles.

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