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A new chronology for the end-Triassic mass extinction
Triassic–Jurassic organic carbon isotope stratigraphy of key sections in the western Tethys realm (Austria)
A candidate GSSP for the base of the Jurassic in the Northern Calcareous Alps (Kuhjoch section; Karwendel Mountains, Tyrol, Austria).
Atmospheric Carbon Injection Linked to End-Triassic Mass Extinction
- M. Ruhl, N. R. Bonis, G. Reichart, J. S. Sinninghe Damsté, Wolfram M Kürschner
- Environmental Science, GeographyScience
- 22 July 2011
The end-Triassic mass extinction coincided with a massive release of carbon to the atmosphere and rapid climate change. The end-Triassic mass extinction (~201.4 million years ago), marked by…
The global stratotype sections and point (GSSP) for the base of the jurassic system at kuhjoch (Karwendel Mountains, Northern Calcareous Alps, Tyrol, Austria)
The Global Stratotype Section and Point (GSSP) defining the base of the Jurassic System Lower Jurassic Epoch and Hettangian Stage is situated at the Kuhjoch pass, Karwendel Mountains, Northern…
Globally enhanced mercury deposition during the end-Pliensbachian extinction and Toarcian OAE: A link to the Karoo–Ferrar Large Igneous Province
Astronomical constraints on the duration of the early Jurassic Hettangian stage and recovery rates following the end-Triassic mass extinction (St Audrie's Bay/East Quantoxhead, UK)
The quest for chron E23r at Partridge Island, Bay of Fundy, Canada: CAMP emplacement postdates the end-Triassic extinction event at the North American craton
The Partridge Island stratigraphic section at the Bay of Fundy, Maritime Canada, reveals a continental sedimen- tary succession with the end-Triassic mass extinction level closely followed by basalts…
Jurassic climate mode governed by ocean gateway
A new large high-quality oxygen-isotope dataset is presented from an interval that includes previously suggested mode transitions, and it is hypothesized that northward oceanic heat transport was impeded by uplift, triggering Cool Mode conditions more widely.
Mercury evidence for pulsed volcanism during the end-Triassic mass extinction
- L. Percival, M. Ruhl, S. Hesselbo, H. Jenkyns, T. Mather, J. Whiteside
- Geography, Environmental ScienceProceedings of the National Academy of Sciences
- 19 June 2017
Pulsatory volcanism, and associated perturbations in the ocean–atmosphere system, likely had profound implications for the rate and magnitude of the end-Triassic mass extinction and subsequent biotic recovery.