1. High atmospheric CO2 levels in the early Mesoproterozoic estimated from paired carbon isotopic records from carbonates from North China.
- Author
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Zhang, Tonggang, Li, Menghan, Chen, Xiaoyan, Wang, Tieguan, and Shen, Yanan
- Subjects
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CARBONATES , *ATMOSPHERIC carbon dioxide , *CARBON isotopes , *SURFACE of the earth , *EARTH temperature , *SEDIMENT sampling - Abstract
• High atmospheric p CO 2 levels, constrained by the paired C-isotopic compositions of carbonate and organic carbon from ∼1.6 Ga Gaoyuzhuang Formation, could have played an important role in compensating for the low solar luminosity and maintaining the temperature of the Mesoproterozoic Earth's surface. It is hypothesized that the Mesoproterozoic was characterized by a prevailing warm climate and a high atmospheric p CO 2 level. However, quantitative constraints on Mesoproterozoic atmospheric p CO 2 are scarce. Here, we report high-resolution organic and inorganic carbon isotope records from sediment samples aged ∼1.6 Ga, collected from Hebei Province in North China. The δ13C org values of these Mesoproterozoic samples vary from −28.4‰ to −34.3‰, and the δ13C carbonate values range from −2.1‰ to 0.4‰. The paired carbonate and organic carbon isotope records can be used as a proxy to quantify the atmospheric CO 2 concentration during the Mesoproterozoic. According to the calibration between the photosynthetic isotopic effect and atmospheric CO 2 , atmospheric CO 2 concentrations are estimated to be within the range of 910–18,800 ppmv, ∼2–50 times greater than the present atmospheric level. The results support the previous hypothesis which suggests that high levels of atmospheric CO 2 prevailed in the Early Mesoproterozoic. High atmospheric pCO 2 levels could have played an important role in compensating for the possible lower solar luminosity and maintaining the temperature of the Mesoproterozoic Earth's surface. [ABSTRACT FROM AUTHOR]
- Published
- 2022
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