Articles | Volume 15, issue 4
https://doi.org/10.5194/bg-15-987-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-15-987-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Stable isotopic constraints on global soil organic carbon turnover
Chao Wang
CAS Key Laboratory of Forest Ecology and Management,
Institute of Applied Ecology, Chinese Academy of Sciences,
Shenyang, 110164, China
Benjamin Z. Houlton
Department of Land, Air and Water Resources,
University of California, Davis, CA, 95616, USA
Dongwei Liu
CAS Key Laboratory of Forest Ecology and Management,
Institute of Applied Ecology, Chinese Academy of Sciences,
Shenyang, 110164, China
Jianfeng Hou
CAS Key Laboratory of Forest Ecology and Management,
Institute of Applied Ecology, Chinese Academy of Sciences,
Shenyang, 110164, China
College of Resources and Environment, University of
Chinese Academy of Sciences, Beijing, 100049, China
Weixin Cheng
CAS Key Laboratory of Forest Ecology and Management,
Institute of Applied Ecology, Chinese Academy of Sciences,
Shenyang, 110164, China
Department of Environmental Studies, University of
California, Santa Cruz, 1156 High Street, Santa Cruz, CA,
95064, USA
CAS Key Laboratory of Forest Ecology and Management,
Institute of Applied Ecology, Chinese Academy of Sciences,
Shenyang, 110164, China
School of Geographical Sciences, Northeast Normal
University, Changchun, 130024, China
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- Variations in soil δ13C with alpine meadow degradation on the eastern Qinghai–Tibet Plateau Y. Zhao et al. 10.1016/j.geoderma.2018.12.005
- Soil Organic Carbon Turnover Response to Nitrogen and Phosphorus Additions in Eastern China: Evidence from Stable Carbon Isotopes L. Chen et al. 10.3390/f14071314
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- Reduced turnover rate of topsoil organic carbon in old-growth forests: a case study in subtropical China X. Xiong et al. 10.1186/s40663-021-00337-5
Latest update: 14 Dec 2024
Short summary
Soil contains a large amount of organic carbon and plays a crucial role in regulating Earth's C cycle and climate system. In this study, we collected soil-carbon isotope data within a 1 m depth globally and provided an isotope-based approach for understanding soil carbon decomposition rate. Compared with other methods, utilization of C isotope composition ratios in the soil profile provides an independent approach that does not rely on disruption of plant-soil-microbe interactions.
Soil contains a large amount of organic carbon and plays a crucial role in regulating Earth's C...
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