C Korte, HW Kozur - Journal of Asian Earth Sciences, 2010 - Elsevier
The Palaeozoic–Mesozoic transition is marked by distinct perturbations in the global carbon cycle resulting in a prominent negative carbon-isotope excursion at the Permian–Triassic (P …
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 …
MR Saltzman, E Thomas, FM Gradstein - The geologic time scale, 2012 - academia.edu
Variations in the 13C/12C value of total dissolved inorganic carbon (DIC) in the world's oceans through time have been documented through stratigraphic study of marine …
Strontium Isotope Stratigraphy | Application of Modern Stratigraphic TechniquesTheory and Case Histories | GeoScienceWorld Books | GeoScienceWorld Skip to Main Content …
Abstract The Permian/Triassic boundary approximately 251.9 million years ago marked the most severe environmental crisis identified in the geological record, which dictated the …
K Grice, C Cao, GD Love, ME Böttcher, RJ Twitchett… - Science, 2005 - science.org
Carbon and sulfur isotopic data, together with biomarker and iron speciation analyses of the Hovea-3 core that was drilled in the Perth Basin, Western Australia, indicate that euxinic …
Ocean acidification triggered by Siberian Trap volcanism was a possible kill mechanism for the Permo-Triassic Boundary mass extinction, but direct evidence for an acidification event …
C Cao, GD Love, LE Hays, W Wang, S Shen… - Earth and Planetary …, 2009 - Elsevier
The Permian–Triassic Boundary event at 252.2 Ma marks the largest extinction of marine fauna in the Phanerozoic and there is a wide consensus that the extinction coincided with an …
Controversy over the oxygen isotope composition of seawater began in the 1950's, since which time there has been no agreement over whether the oxygen isotope composition of …