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- W4309468427 abstract "The timing and connections between global cooling, marine redox conditions, and biotic turnover are underconstrained for the Late Ordovician. The second most severe mass extinction occurred at the end of the Ordovician period, resulting in ~85% loss of marine species between two extinction pulses. As the only Big 5 extinction that occurred during icehouse conditions, this interval is an important modern analog to constrain environmental feedbacks. We present a previously unexplored thallium isotope records from two paleobasins that record global marine redox conditions and document two distinct and rapid excursions suggesting vacillating (de)oxygenation. The strong temporal link between these perturbations and extinctions highlights the possibility that dynamic marine oxygen fluctuations, rather than persistent, stable global anoxia, played a major role in driving the extinction. This evidence for rapid oxygen changes leading to mass extinction has important implications for modern deoxygenation and biodiversity declines." @default.
- W4309468427 created "2022-11-28" @default.
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- W4309468427 date "2022-11-16" @default.
- W4309468427 modified "2023-09-30" @default.
- W4309468427 title "Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction" @default.
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- W4309468427 doi "https://doi.org/10.1126/sciadv.abn8345" @default.
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