Widespread upper-ocean deoxygenation in the Alpine-Mediterranean Tethys during the Toarcian Oceanic Anoxic Event

Widespread upper-ocean deoxygenation in the Alpine-Mediterranean Tethys during the Toarcian Oceanic Anoxic Event

The early Toarcian (∼183 Ma) was characterized by pronounced climate warming associated with massive release of 13C-depleted carbon to the exogenic system, as evidenced by globally recognized negative carbon-isotope excursions (N-CIE) in biospheric carbon reservoirs. Global warming during this inter...

Podrobná bibliografie
Hlavní autoři:	Chen, W, Kemp, DB, Jenkyns, HC, Robinson, SA, Jiang, S, Pan, C, Li, C
Médium:	Journal article
Jazyk:	English
Vydáno:	Elsevier 2024

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