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Marcasite at the Permian‐Triassic Transition
Ocean anoxia and hydrosphere acidification (i.e., acid rain and/or ocean acidification) are likely consequences of a massive release of volatiles in a complex causeand-effect relationship between the Siberian Traps large igneous province (STLIP) and the end-Permian mass extinction (EPME), as reviewed in recent studies (Bonddoi:10.1002/9781119507444.ch16 fatcat:oszk2nznnbdxtjh5ma3lzkosfy