Do mercury isotopes record the signature of massive volcanism in marine sedimentary records? | Zendy

Alyson M. Thibodeau | Zendy; Bridget A. Bergquist | Zendy

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Do mercury isotopes record the signature of massive volcanism in marine sedimentary records?

Author(s) -

Alyson M. Thibodeau,

Bridget A. Bergquist

Publication year - 2016

Publication title -

geology

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 2.609

H-Index - 215

eISSN - 1943-2682

pISSN - 0091-7613

DOI - 10.1130/focus012017.1

Subject(s) - volcanism , geology , phanerozoic , anoxic waters , sedimentary rock , extinction event , mercury (programming language) , isotopic signature , geologic record , large igneous province , paleontology , earth science , oceanography , geochemistry , isotope , magmatism , structural basin , cenozoic , tectonics , physics , quantum mechanics , computer science , programming language , biological dispersal , population , demography , sociology

Large Igneous Provinces (LIPs) are associated with a significant number of mass extinctions and ocean anoxic events (OAEs) during the Phanerozoic. However, the role of LIPs in triggering and sustaining biotic and environmental crises is controversial (e.g., [Bond and Wignall, 2014][1]). These

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