Articles | Volume 8, issue 2
https://doi.org/10.5194/soil-8-687-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/soil-8-687-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Original research article
| 
28 Oct 2022
Original research article |
| 28 Oct 2022
| 28 Oct 2022
Biotic factors dominantly determine soil inorganic carbon stock across Tibetan alpine grasslands
Junxiao Pan
Key Laboratory of Ecosystem Network Observation and Modeling,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, People's Republic of China
Jinsong Wang
CORRESPONDING AUTHOR
Key Laboratory of Ecosystem Network Observation and Modeling,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, People's Republic of China
Dashuan Tian
Key Laboratory of Ecosystem Network Observation and Modeling,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, People's Republic of China
Ruiyang Zhang
Key Laboratory of Ecosystem Network Observation and Modeling,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, People's Republic of China
Yang Li
Key Laboratory of Ecosystem Network Observation and Modeling,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, People's Republic of China
Lei Song
Key Laboratory of Ecosystem Network Observation and Modeling,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, People's Republic of China
College of Resources and Environment, University of Chinese Academy
of Sciences, Beijing 100049, People's Republic of China
Jiaming Yang
Key Laboratory of Ecosystem Network Observation and Modeling,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, People's Republic of China
Chunxue Wei
Key Laboratory of Ecosystem Network Observation and Modeling,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, People's Republic of China
Key Laboratory of Ecosystem Network Observation and Modeling,
Institute of Geographic Sciences and Natural Resources Research, Chinese
Academy of Sciences, Beijing 100101, People's Republic of China
College of Resources and Environment, University of Chinese Academy
of Sciences, Beijing 100049, People's Republic of China
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Cited
9 citations as recorded by crossref.
- Soil texture and microorganisms dominantly determine the subsoil carbonate content in the permafrost-affected area of the Tibetan Plateau M. Shao et al. 10.3389/fmicb.2023.1125832
- Depth-dependent drivers of soil aggregate carbon across Tibetan alpine grasslands J. Pan et al. 10.1016/j.scitotenv.2023.161428
- Decadal soil total carbon loss in northern hinterland of Tibetan Plateau W. Wu et al. 10.1016/j.scitotenv.2024.171190
- Soil inorganic carbon stocks increase non-synergistically with soil organic carbon after ecological restoration practices in drylands E. Liu et al. 10.1016/j.jenvman.2023.119070
- The Contribution of Biotic Factors in Explaining the Global Distribution of Inorganic Carbon in Surface Soils X. Zeng et al. 10.1029/2023GB007957
- E-SCAN: Electrochemical Scanning of Carbonates, an In Situ Approach for Screening and Quantifying Inorganic Carbon in Soil V. Dhamu et al. 10.1021/acs.jafc.3c02948
- Natural and regenerated saltmarshes exhibit different bulk soil and aggregate-associated organic and inorganic carbon contents but similar total carbon contents Z. Ma et al. 10.1016/j.jenvman.2023.119451
- Effects of increasing soil moisture on Antarctic desert microbial ecosystems E. Zhang et al. 10.1111/cobi.14268
- Seasonal freeze–thaw processes regulate and buffer the distribution of microbial communities in soil horizons Y. Zhao & X. Hu 10.1016/j.catena.2023.107348
9 citations as recorded by crossref.
- Soil texture and microorganisms dominantly determine the subsoil carbonate content in the permafrost-affected area of the Tibetan Plateau M. Shao et al. 10.3389/fmicb.2023.1125832
- Depth-dependent drivers of soil aggregate carbon across Tibetan alpine grasslands J. Pan et al. 10.1016/j.scitotenv.2023.161428
- Decadal soil total carbon loss in northern hinterland of Tibetan Plateau W. Wu et al. 10.1016/j.scitotenv.2024.171190
- Soil inorganic carbon stocks increase non-synergistically with soil organic carbon after ecological restoration practices in drylands E. Liu et al. 10.1016/j.jenvman.2023.119070
- The Contribution of Biotic Factors in Explaining the Global Distribution of Inorganic Carbon in Surface Soils X. Zeng et al. 10.1029/2023GB007957
- E-SCAN: Electrochemical Scanning of Carbonates, an In Situ Approach for Screening and Quantifying Inorganic Carbon in Soil V. Dhamu et al. 10.1021/acs.jafc.3c02948
- Natural and regenerated saltmarshes exhibit different bulk soil and aggregate-associated organic and inorganic carbon contents but similar total carbon contents Z. Ma et al. 10.1016/j.jenvman.2023.119451
- Effects of increasing soil moisture on Antarctic desert microbial ecosystems E. Zhang et al. 10.1111/cobi.14268
- Seasonal freeze–thaw processes regulate and buffer the distribution of microbial communities in soil horizons Y. Zhao & X. Hu 10.1016/j.catena.2023.107348
Latest update: 29 Jun 2024
Short summary
We found that climatic, edaphic, plant and microbial variables jointly affect soil inorganic carbon (SIC) stock in Tibetan grasslands, and biotic factors have a larger contribution than abiotic factors to the variation in SIC stock. The effects of microbial and plant variables on SIC stock weakened with soil depth, while the effects of edaphic variables strengthened. The contrasting responses and drivers of SIC stock highlight differential mechanisms underlying SIC preservation with soil depth.
We found that climatic, edaphic, plant and microbial variables jointly affect soil inorganic...
