How does Carbon Cycle in the Mid-Ocean Ridge Deep？
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图 1 地球内部碳循环模式及相态变化（a）（修改自Stagno et al., 2019）；洋中脊深部碳循环模式（b）
1.方解石相，文石相; 2.白云石相; 3.文石-后文石相; 4.白云石Ⅲ相; 5.含铁碳酸盐相; 6.后文石相-含SP3混合碳碳酸盐相; 7.菱镁矿-菱镁矿Ⅱ相
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Nakamura, K., Takai, K., 2014. Theoretical Constraints of Physical and Chemical Properties of Hydrothermal Fluids on Variations in Chemolithotrophic Microbial Communities in Seafloor Hydrothermal Systems. Progress in Earth and Planetary Science, 1, 5. https://doi-org.proxy.library.carleton.ca/10.1186/2197-4284-1-5 Stagno, V., Cerantola, V., Aulbach, S., et al., 2019. Carbon-Bearing Phases Throughout Earth's Interior. Deep Carbon. Cambridge University Press, Cambridge: 66-88. https://doi.org/10.1017/9781108677950.004 汪品先, 田军, 黄恩清, 2018. 地球系统与演变. 北京: 科学出版社. 朱日祥, 侯增谦, 郭正堂, 等, 2021. 宜居地球的过去、现在与未来: 地球科学发展战略概要. 科学通报, 66(35): 4485-4490. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB202135001.htm -
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