September 25, 2025Open Access

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

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Thermogenic methane release led to significant calcite precipitation characterized by depleted carbon isotopes.
Results indicate that the methane release occurred after the Marinoan glaciation, impacting the carbon cycle severely.
Study involved an observational analysis of geological samples from cap dolostones to understand methane dynamics.
These findings suggest a link between methanogenic processes and major climatic shifts during the deep time.

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Analysis reveals thermogenic methane release influenced carbon isotopes and calcite precipitation in cap dolostones.

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

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Ping et al. (2025) studied this question.

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Analysis reveals thermogenic methane release influenced carbon isotopes and calcite precipitation in cap dolostones.

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