1. Reverse weathering may amplify post-Snowball atmospheric carbon dioxide levels.
- Author
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Li, Fangbing, Penman, Donald, Planavsky, Noah, Knudsen, Andrew, Zhao, Mingyu, Wang, Xiangli, Isson, Terry, Huang, Kangjun, Wei, Guangyi, Zhang, Shuang, Shen, Jun, Zhu, Xiangkun, and Shen, Bing
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ATMOSPHERIC carbon dioxide , *CLIMATE in greenhouses , *ICE sheets , *WEATHERING , *ANALYTICAL geochemistry , *CARBON dioxide , *CARBON cycle , *RESERVOIR drawdown - Abstract
• Both mineralogical and geochemical analysis suggest a shift towards more extensive reverse weathering within the uppermost portion of the glaciogenic Nantuo Formation. • This reverse weathering was likely driven by a combination of rising temperatures and pH and high dissolved silica concentrations. • The carbon cycle modeling implies that widespread reverse weathering could have driven a protracted (millions of years) carbon dioxide drawdown following deglaciation. Snowball Earth glaciations are the most extreme climate perturbations recorded in Earth's history. It has been argued that the termination of these events was characterized by a single rapid transition from near-global ice coverage to an ice-free greenhouse climate state. Notably, this deviates with more extended transition periods of ice sheet waxing and waning typical of Phanerozoic glaciations. Using a coupled mineralogical and Mg and Li isotopic approach, we explore the role that authigenic clay formation within the seafloor may have played on Earth's climate during deglaciation of the Marinoan Snowball Earth event. Marine authigenic clay formation—a process referred to as reverse weathering—recycles carbon within the ocean–atmosphere system and acts to elevate atmospheric CO 2 levels. The results indicate a shift towards more extensive reverse weathering within the uppermost portion of the glaciogenic Nantuo Formation in South China. Carbon cycle modeling indicates that widespread reverse weathering could have driven a protracted (millions of years) carbon dioxide drawdown following high carbon dioxide levels expected during deglaciation. [ABSTRACT FROM AUTHOR]
- Published
- 2021
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