Comment Canfield oceans (Score 1) 760
at times in Earth history, notably the Late Ordovician, Late Devonian, and Late Permian, widespread shelf and cratonic-basinal anoxia, and, at least in the latter two cases, photic-zone euxinia, have accompanied mass extinction (Wilde & Berry 1984; Wignall & Hallam 1992; Wang et al. 1993, 1996; Bond et al. 2004). Could sulfide poisoning serve as the kill mechanism in these extinctions?
Biomarker evidence perhaps provides a more compelling link between euxinia and extinction for the Late Devonian and Late Permian (Grice et al. 2005). . . . But why would a collapse of marine productivity trigger terrestrial ecosystem disruption and extinction?
Sulfide release from the oceans serves as a link to terrestrial biotic crisis during the end-Permian. One-dimensional atmospheric modeling by Kump et al. (2005) predicted that toxic levels of H2S could rapidly accumulate in the well-mixed troposphere once reaction of sulfide with atmospheric hydroxyl radical reduced OH to very low levels. The abrupt rise in atmospheric H2S concentrations would be accompanied by rising atmospheric methane levels and destruction of the ozone layer. Not only would terrestrial organisms be unable to escape the toxic effects of H2S, but they also would be subject to high levels of UV radiation following the predicted collapse of the ozone layer.
This does sound very tentative. On the other hand, it corresponds with my tenuous understanding of the claims of Dyer and Ward. Can you shed any light? I don't want to be going around making false claims.