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

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 con...

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Autores principales: Huang, Miao, Gan, Dezhao, Li, Zheng, Wang, Jinsong, Niu, Shuli, Zuo, Hongchao, Long, Ruijun, Ma, Lei
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Oxford University Press 2022
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10042278/
https://www.ncbi.nlm.nih.gov/pubmed/36992818
http://dx.doi.org/10.1093/pnasnexus/pgac314
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author Huang, Miao
Gan, Dezhao
Li, Zheng
Wang, Jinsong
Niu, Shuli
Zuo, Hongchao
Long, Ruijun
Ma, Lei
author_facet Huang, Miao
Gan, Dezhao
Li, Zheng
Wang, Jinsong
Niu, Shuli
Zuo, Hongchao
Long, Ruijun
Ma, Lei
author_sort Huang, Miao
collection PubMed
description 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.
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spelling pubmed-100422782023-03-28 Unexpected no significant soil carbon losses in the Tibetan grasslands due to rodent bioturbation Huang, Miao Gan, Dezhao Li, Zheng Wang, Jinsong Niu, Shuli Zuo, Hongchao Long, Ruijun Ma, Lei PNAS Nexus Physical Sciences and Engineering 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. Oxford University Press 2022-12-30 /pmc/articles/PMC10042278/ /pubmed/36992818 http://dx.doi.org/10.1093/pnasnexus/pgac314 Text en © The Author(s) 2022. Published by Oxford University Press on behalf of National Academy of Sciences. https://creativecommons.org/licenses/by/4.0/This is an Open Access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly cited.
spellingShingle Physical Sciences and Engineering
Huang, Miao
Gan, Dezhao
Li, Zheng
Wang, Jinsong
Niu, Shuli
Zuo, Hongchao
Long, Ruijun
Ma, Lei
Unexpected no significant soil carbon losses in the Tibetan grasslands due to rodent bioturbation
title Unexpected no significant soil carbon losses in the Tibetan grasslands due to rodent bioturbation
title_full Unexpected no significant soil carbon losses in the Tibetan grasslands due to rodent bioturbation
title_fullStr Unexpected no significant soil carbon losses in the Tibetan grasslands due to rodent bioturbation
title_full_unstemmed Unexpected no significant soil carbon losses in the Tibetan grasslands due to rodent bioturbation
title_short Unexpected no significant soil carbon losses in the Tibetan grasslands due to rodent bioturbation
title_sort unexpected no significant soil carbon losses in the tibetan grasslands due to rodent bioturbation
topic Physical Sciences and Engineering
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10042278/
https://www.ncbi.nlm.nih.gov/pubmed/36992818
http://dx.doi.org/10.1093/pnasnexus/pgac314
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