The ocean has been shielding the earth from the worst effects of rapid climate change by absorbing excess carbon dioxide from the atmosphere. This absorption of CO 2 is driving …
The temporal link between large igneous province (LIP) eruptions and at least half of the major extinctions of the Phanerozoic implies that large scale volcanism is the main driver of …
SD Burgess, S Bowring, S Shen - Proceedings of the …, 2014 - National Acad Sciences
The end-Permian mass extinction was the most severe loss of marine and terrestrial biota in the last 542 My. Understanding its cause and the controls on extinction/recovery dynamics …
Y Cui, M Li, EE Van Soelen, F Peterse… - Proceedings of the …, 2021 - National Acad Sciences
The end-Permian mass extinction event (∼ 252 Mya) is associated with one of the largest global carbon cycle perturbations in the Phanerozoic and is thought to be triggered by the …
The history of Earth's biodiversity is punctuated episodically by mass extinctions. These are characterized by major declines of taxon richness, but the accompanying ecological …
Understanding the interplay of climatic and biological events in deep time requires resolving the precise timing and pattern of paleotemperature changes and their temporal relationship …
Abstract The Meishan section, South China is the Global Stratotype Section and Point (GSSP) for the Permian–Triassic boundary (PTB), and is also well known for the best record …
Oceanic environments and biotas were in a state of near-continuous perturbation during the Early Triassic, the~ 5-million-year interval following the latest Permian mass extinction …