| China Geological Survey Chinese Academy of Geological Sciences | Host |
| 科学出版社 | Publish |
| Citation: |
GENG Wenda, JI Wenbing, LIU Bingquan, YE Guiqi, MA Xudong, HOU Qingye, YU Tao, YANG Zhongfang. 2025. Research status and progress of carbon isotope in soil−vegetation−ecology−environment[J]. Geology in China, 52(3): 867-889. doi: 10.12029/gc20240604001
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Research status and progress of carbon isotope in soil−vegetation−ecology−environment
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Abstract
This paper is the result of environmental geological suvery engineering.
Objective In recent decades, the theory of stable carbon isotopes has been gradually perfected, and with the progress and development of testing techniques, carbon isotope analysis has become more accurate and efficient. As a powerful tool, carbon isotope tracer technology is widely used in soil−vegetation−ecology−environment research and plays an important role.
Methods In this paper, a large number of literatures on the application of carbon isotope technology are reviewed, and the latest research progress on the principle and practical application of stable carbon isotope technology at home and abroad is reviewed.
Results Using stable carbon isotope technology, the genetic source of natural organic matter such as coal, oil and natural gas can be effectively identified. Global climate change can be effectively retrieved through the changes of carbon isotope composition in different geological bodies such as cave stalagmites, loess sediments, lake sediments, tree rings, Marine foraminifera, Marine carbonate rocks and ice cores. In addition, carbon stable isotopes are also used to trace the geochemical cycle of soil organic carbon, and solve the problems of inorganic carbon sink transformation and carbon pool identification in arid and semi−arid areas.
Conclusions Stable carbon isotope technology has been widely used in the research of coal−oil−natural gas field, global climate change, organic carbon cycle in superorganism system and inorganic carbon sink source, and has achieved a lot of research results. In the future, with the continuous progress of equipment and testing technology, relevant theories and research methods will become increasingly mature and perfect, and carbon isotope tracer will play a greater role.
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References
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GENG Wenda, JI Wenbing, LIU Bingquan, YE Guiqi, MA Xudong, HOU Qingye, YU Tao, YANG Zhongfang. 2025. Research status and progress of carbon isotope in soil−vegetation−ecology−environment[J]. Geology in China, 52(3): 867-889. doi: 10.12029/gc20240604001
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Figure 1.
Carbon isotope composition of some important geological bodies (modified from Wei Juying et al., 1988)
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Figure 2.
Sofer map of marine oil in Early Cretaceous clastic rocks in the southern oil fields of the Mesopotamian Basin (after Al−Khafaji et al., 2021)
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Figure 3.
Carbon isotope type curve of immature oil in Gaosheng Leijia area of Western Depression (after Li Meijun et al., 2000)
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Figure 4.
Comparison of individual hydrocarbon isotopes between oil reservoirs and source rocks (after Yang Yizhuo et al., 2022)
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Figure 5.
C1-4 carbon isotope box plot of atmospheric fields in China (after Dai Jinxing et al., 2024)
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Figure 6.
Revised identification chart of natural gas genesis types
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Figure 7.
Cross section profile of Jurassic gas reservoir in the western Sichuan depression (after Ye Sujuan et al., 2017)
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Figure 8.
Natural gas migration in the 4th member of the Xujiahe Formation in the western Sichuan depression (after Shen Zhongmin et al., 2011)
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Figure 9.
Time series of carbon stable isotopes in stalagmites AB2 (orange) and AB3 (blue) from Anjohibe Cave, Madagascar (after Burns et al., 2016)
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Figure 10.
Comprehensive comparison of different carrier types of carbon isotopes in loess (after Xu Xiangchun et al., 2021)
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Figure 11.
Tree-ring δ13C sequence from the past 270 years and self calibrated Palmer Drought Severity Index (scPDSI) sequence from the past 130 years
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Figure 12.
Carbon and oxygen isotope of benthic foraminifera in the South China Sea
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Figure 13.
Changes in atmospheric CO2 concentration and its δ13C value over the past millennium reconstructed from CO2 in WAIS Divide ice cores (after Bauska et al., 2015)
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Figure 14.
Time series of (a) global methane concentration and (b) stable carbon isotope ratio of global methane