Carbon isotope records reveal synchronicity between carbon cycle perturbation and the “Carnian Pluvial Event” in the Tethys realm (Late Triassic)

In the early Late Triassic a period of increased rainfall, named the Carnian Pluvial Event (CPE), is evidenced by major lithological changes in continental and marine successions worldwide. The environmental change seems to be closely associated with a negative carbon isotope excursion that was iden...

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Veröffentlicht in:	Global and planetary change 2015-04, Vol.127, p.79-90
Hauptverfasser:	Dal Corso, Jacopo, Gianolla, Piero, Newton, Robert J., Franceschi, Marco, Roghi, Guido, Caggiati, Marcello, Raucsik, Béla, Budai, Tamás, Haas, János, Preto, Nereo
Format:	Artikel
Sprache:	eng
Schlagworte:	Carbon cycle Carbon isotope Carbon isotopes Carbonate crisis Carbonates Carnian Pluvial Event Deposition Dolomite Late Triassic Marine Metazoa Oxygen depletion Petrography Rainfall
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