Tracing volcanic emissions from the Central Atlantic Magmatic Province in the sedimentary record

The end-Triassic mass extinction (ETME) is thought to have been caused by voluminous, pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last decades, various geochemical signals and proxy records, including δ13C, pCO2, iridium and other platinum-group elements, merc...

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Veröffentlicht in:	Earth-science reviews 2021-01, Vol.212, p.103444, Article 103444
Hauptverfasser:	Lindström, Sofie, Callegaro, Sara, Davies, Joshua, Tegner, Christian, van de Schootbrugge, Bas, Pedersen, Gunver K., Youbi, Nasrrddine, Sanei, Hamed, Marzoli, Andrea
Format:	Artikel
Sprache:	eng
Schlagworte:	C-isotope Iridium Mercury PAH Triassic–Jurassic boundary Volcanism
Online-Zugang:	Volltext
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