Volcanism and deep-ocean acidification across the end-Triassic extinction event
Volume: 440, Pages: 725 - 733
Published: Dec 1, 2015
Abstract
The end-Triassic extinction event marks one of the “big five” mass extinction events of the Phanerozoic. The ultimate cause of the extinction is considered to be volcanic activity at the Central Atlantic magmatic province (CAMP), yet the underlying nature of global environmental changes that accompanied the biotic turnover remains elusive. Here we present chemical and mineralogical studies across the end-Triassic extinction level of the deep-sea...
Paper Details
Title
Volcanism and deep-ocean acidification across the end-Triassic extinction event
Published Date
Dec 1, 2015
Volume
440
Pages
725 - 733
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