Association of34S-depleted pyrite layers with negative carbonateδ13C excursions at the Permian-Triassic boundary: Evidence for upwelling of sulfidic deep-ocean water masses

Author:

Algeo Thomas1,Shen Yanan2,Zhang Tonggang2,Lyons Timothy3,Bates Steven3,Rowe Harry4,Nguyen T. K. T.5

Affiliation:

1. Department of Geology; University of Cincinnati; Cincinnati; Ohio; 45221-0013; USA

2. Centre de Recherche en Géochimie et en Géodynamique; Université du Quebec à Montréal; C.P. 8888, Succursale Centre-Ville,; Montreal, Quebec; Canada; H3C 3P8

3. Department of Earth Sciences; University of California; Riverside; California; 92521-0423; USA

4. Department of Geological Sciences; University of Kentucky; Lexington; Kentucky; 40506; USA

5. Institute of Geophysics; Vietnamese Academy of Science and Technology; Hanoi; Vietnam

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

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