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Rapid rise in atmospheric CO<sub>2</sub> marked the end of the Late Palaeozoic Ice Age.

Nat Geosci · 2025 · PMC11732749 · PMID 39822309

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a decreasing trendno p-value reported
Unlike the elevated CO 2 event, this gradual rebound is influenced by δ 11 B sw , which shows a decreasing trend throughout the Permian.

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