深部碳循环的锌同位素示踪研究进展

王照雪; 刘盛遨; 李孟伦; 李曙光

doi:10.3799/dqkx.2020.159

Volume 45 Issue 6

Jun. 2020

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Article Navigation > Earth Science > 2020 > 45(6): 1967-1976

Wang Zhaoxue, Liu Sheng'ao, Li Menglun, Li Shuguang, 2020. Advances on Application of Zinc Isotope as a Tracer for Deep Carbon Cycles. Earth Science, 45(6): 1967-1976. doi: 10.3799/dqkx.2020.159

Citation:

Wang Zhaoxue, Liu Sheng'ao, Li Menglun, Li Shuguang, 2020. Advances on Application of Zinc Isotope as a Tracer for Deep Carbon Cycles. Earth Science, 45(6): 1967-1976. doi: 10.3799/dqkx.2020.159

Wang Zhaoxue, Liu Sheng'ao, Li Menglun, Li Shuguang, 2020. Advances on Application of Zinc Isotope as a Tracer for Deep Carbon Cycles. Earth Science, 45(6): 1967-1976. doi: 10.3799/dqkx.2020.159

Citation:

Wang Zhaoxue, Liu Sheng'ao, Li Menglun, Li Shuguang, 2020. Advances on Application of Zinc Isotope as a Tracer for Deep Carbon Cycles. Earth Science, 45(6): 1967-1976. doi: 10.3799/dqkx.2020.159

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Advances on Application of Zinc Isotope as a Tracer for Deep Carbon Cycles

doi: 10.3799/dqkx.2020.159

State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

Received Date: 2020-01-15
Publish Date: 2020-06-15

Abstract

Abstract

The deep carbon cycle and surface's carbon cycle together constitute the global carbon cycle. Research on deep carbon cycles is of significance for understanding the long-term climate change of the Earth given that >90% of Earth's carbon is stored in the deep Earth. Research on deep carbon cycles involves many aspects, among which one of the most important scientific issues is how to accurately identify recycled surface carbon in the mantle. Zinc (Zn) is a lithophile element and widely distributed in igneous rocks, mantle and sedimentary carbonates. There is a large Zn isotope difference between marine carbonates and the terrestrial mantle. Also, subduction-related dehydration, partial melting and magmatic differentiation only result in limited Zn isotope fractionation. Thus, Zn isotope has the potential as a novel tracer for deep carbon cycles. In this paper, the principle and potentiality of Zn isotope utilized as a tracer for deep carbon cycle are reviewed and the advances of using Zn isotope to trace deep carbon cycles in previous studies are presented. In addition, the combination between Zn and magnesium (Mg) isotopes is expect to the essential aspect of the deep carbon cycles in the future.
- deep carbon cycle,
- Zn isotope,
- mantle,
- carbonate,
- geochemistry

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References(63)

References

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