Proxy evidence from the Gartnerkofel-1 core (Carnic Alps, Austria) for hypoxic conditions in the western Tethys during the end-Permian mass-extinction event

Author:

Rampino Michael R.ORCID,Baransky Eva,Rodriguez Sedelia

Funder

New York University

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference146 articles.

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2. Association of 34S-depleted pyrite layers with negative carbonate δ13C excursions at the Permian/Triassic boundary: evidence for upwelling of sulfidic deep-ocean water masses;Algeo;Geochem. Geophys. Geosyst.,2008

3. The Permian-Triassic of the Gartnerkofel-1 core (Carnic Alps, Austria): Geochemistry of common and trace elements II – INAA and RNAA;Attrep;Abhandlungen der Geologischen Bundesanstalt,1991

4. Baud, A., 2003. Geochemical changes at the Permian-Triassic transition in Southern Alps and adjacent area: a review. Annali dell'Universita degli Studi di Ferrara, Volume Speciale 2005, 5–11.

5. Isotopic signatures of mercury contamination in latest Permian oceans;Beauchamp;Geology,2016

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