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...

詳細記述

書誌詳細
主要な著者: Chen, W, Kemp, DB, Jenkyns, HC, Robinson, SA, Jiang, S, Pan, C, Li, C
フォーマット: Journal article
言語:English
出版事項: Elsevier 2024