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Mercury isotopes in sedimentary rocks as a paleoenvironmental proxy

CHINESE SCIENCE BULLETIN-CHINESE (2023)

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Summary: This study investigates the mercury isotope composition and behavior of trace elements in K-Pg sediments from the Bidart section in southwest France. The findings suggest that the Deccan Traps volcanic activity may have contributed to the K-Pg mass extinction.

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Intensified continental chemical weathering and carbon-cycle perturbations linked to volcanism during the Triassic-Jurassic transition

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Mercury evidence for combustion of organic-rich sediments during the end-Triassic crisis

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Different controls on the Hg spikes linked the two pulses of the Late Ordovician mass extinction in South China

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Major volcanic eruptions linked to the Late Ordovician mass extinction: Evidence from mercury enrichment and Hg isotopes

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Summary: The Late Ordovician mass extinction was the second most severe Phanerozoic biodiversity crisis, with uncertain triggering and killing mechanisms. Studies have shown mercury enrichments in multiple regions globally during the Late Ordovician, indicating an increase in environmental mercury loading, possibly due to volcanic activity.

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Characteristics of Hg concentrations and isotopes in terrestrial and marine facies across the end-Permian mass extinction

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