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September 23, 2025Open Access

Supplemental Material: Thermogenic methane release after Marinoan glaciation induced extremely ¹³C-depleted calcite precipitation in cap dolostones

Hongwei Ping et al.

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Key Points

Thermogenic methane release triggered calcite precipitation, leading to extreme 13C-depletion.
Analysis shows significant impact of Marinoan glaciation on geological processes in cap dolostones.
The study provides critical insights into methane's effects on carbon cycling post-glaciation.
Understanding these processes is vital for reconstructing historical climatic changes and their implications.

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Implication

Analysis demonstrates 13C-depleted calcite precipitation in cap dolostones after Marinoan glaciation, indicating thermogenic methane's role.

Abstract

Methods, Figures S1–S7, and Tables S1–S4.

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Cite This Study

Ping et al. (2025) studied this question.

synapsesocial.com/papers/68d4759931b076d99fa6daf2 https://doi.org/10.1130/geol.s.30190201.v1

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1Supplemental Material: Thermogenic methane release after Marinoan glaciation induced extremely <sup>13</sup>C-depleted calcite precipitation in cap dolostones2025
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