Articles | Volume 13, issue 17
https://doi.org/10.5194/bg-13-5057-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-13-5057-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
13 Sep 2016
Research article |
| 13 Sep 2016
Temperature exerts no influence on organic matter δ13C of surface soil along the 400 mm isopleth of mean annual precipitation in China
Yufu Jia
College of Resources and Environmental Sciences, China Agricultural
University, Beijing 100193, China
Guoan Wang
CORRESPONDING AUTHOR
College of Resources and Environmental Sciences, China Agricultural
University, Beijing 100193, China
Qiqi Tan
College of Resources and Environmental Sciences, China Agricultural
University, Beijing 100193, China
Zixun Chen
College of Resources and Environmental Sciences, China Agricultural
University, Beijing 100193, China
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Cited
13 citations as recorded by crossref.
- Variation of stable carbon and nitrogen isotopes ratio in Ficus tikoua and their linkage to its specific pollinator L. Tan et al. 10.1016/j.flora.2022.152073
- Temperature effect on abundance and distribution of leaf wax n-alkanes across a temperature gradient along the 400 mm isohyet in China J. Wang et al. 10.1016/j.orggeochem.2018.03.009
- Climatic significance of the stable carbon isotopic composition of surface soils in northern Iran and its application to an Early Pleistocene loess section Q. Wang et al. 10.1016/j.orggeochem.2018.11.011
- Temperature patterns of soil carbon: nitrogen: phosphorus stoichiometry along the 400 mm isohyet in China Q. Tan et al. 10.1016/j.catena.2021.105338
- Relationship between the stable carbon isotopic composition of modern plants and surface soils and climate: A global review Z. Rao et al. 10.1016/j.earscirev.2016.12.007
- Effects of long-term nitrogen addition on the δ15N and δ13C of Larix gmelinii and soil in a boreal forest G. Liu et al. 10.1186/s13717-022-00382-0
- Glacial-interglacial vegetation changes in northeast China inferred from isotopic composition of pyrogenic carbon from Lake Xingkai sediments W. Sun et al. 10.1016/j.orggeochem.2018.03.004
- Increased precipitation accelerates soil organic matter turnover associated with microbial community composition in topsoil of alpine grassland on the eastern Tibetan Plateau C. Han et al. 10.1139/cjm-2017-0157
- Effects of land use change from natural forest to plantation on C, N and natural abundance of 13C and 15N along a climate gradient in eastern China M. Ngaba et al. 10.1038/s41598-019-52959-z
- Clarifying the response of soil organic carbon storage to increasing temperature through minimizing the precipitation effect Q. Tan et al. 10.1016/j.geoderma.2020.114398
- Variation of δ13C and soil organic carbon under different precipitation gradients in alpine grassland on the Qinghai–Tibetan Plateau Y. Zhao et al. 10.1007/s11368-022-03223-x
- Carbon isotope composition of land snail shells as a proxy for precipitation amount in the East Asian Monsoon region: A case study from Hainan Island H. Tan et al. 10.1016/j.palaeo.2022.111309
- Stable Carbon Isotopes of Fossil Plant Lipids Support Moderately High pCO2 in the Early Paleogene T. Chapman et al. 10.1021/acsearthspacechem.9b00146
13 citations as recorded by crossref.
- Variation of stable carbon and nitrogen isotopes ratio in Ficus tikoua and their linkage to its specific pollinator L. Tan et al. 10.1016/j.flora.2022.152073
- Temperature effect on abundance and distribution of leaf wax n-alkanes across a temperature gradient along the 400 mm isohyet in China J. Wang et al. 10.1016/j.orggeochem.2018.03.009
- Climatic significance of the stable carbon isotopic composition of surface soils in northern Iran and its application to an Early Pleistocene loess section Q. Wang et al. 10.1016/j.orggeochem.2018.11.011
- Temperature patterns of soil carbon: nitrogen: phosphorus stoichiometry along the 400 mm isohyet in China Q. Tan et al. 10.1016/j.catena.2021.105338
- Relationship between the stable carbon isotopic composition of modern plants and surface soils and climate: A global review Z. Rao et al. 10.1016/j.earscirev.2016.12.007
- Effects of long-term nitrogen addition on the δ15N and δ13C of Larix gmelinii and soil in a boreal forest G. Liu et al. 10.1186/s13717-022-00382-0
- Glacial-interglacial vegetation changes in northeast China inferred from isotopic composition of pyrogenic carbon from Lake Xingkai sediments W. Sun et al. 10.1016/j.orggeochem.2018.03.004
- Increased precipitation accelerates soil organic matter turnover associated with microbial community composition in topsoil of alpine grassland on the eastern Tibetan Plateau C. Han et al. 10.1139/cjm-2017-0157
- Effects of land use change from natural forest to plantation on C, N and natural abundance of 13C and 15N along a climate gradient in eastern China M. Ngaba et al. 10.1038/s41598-019-52959-z
- Clarifying the response of soil organic carbon storage to increasing temperature through minimizing the precipitation effect Q. Tan et al. 10.1016/j.geoderma.2020.114398
- Variation of δ13C and soil organic carbon under different precipitation gradients in alpine grassland on the Qinghai–Tibetan Plateau Y. Zhao et al. 10.1007/s11368-022-03223-x
- Carbon isotope composition of land snail shells as a proxy for precipitation amount in the East Asian Monsoon region: A case study from Hainan Island H. Tan et al. 10.1016/j.palaeo.2022.111309
- Stable Carbon Isotopes of Fossil Plant Lipids Support Moderately High pCO2 in the Early Paleogene T. Chapman et al. 10.1021/acsearthspacechem.9b00146
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Latest update: 19 Apr 2024
Short summary
Soil organic carbon can be used for climate reconstruction and carbon cycle study. This work assessed the effect of temperature on surface soil δ13C by an investigation from 27 sites across a temperature gradient along an isohyet. This study shows that soil type and vegetation type had influences on soil δ13C, while temperature was not related to soil δ13C. This suggests that organic carbon isotopes in sediments cannot be used for the paleotemperature reconstruction.
Soil organic carbon can be used for climate reconstruction and carbon cycle study. This work...
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