Primary v. carbonate production in the Toarcian, a case study from the Llanbedr (Mochras Farm) borehole, Wales

The leading hypothesis for the Toarcian oceanic anoxic event (T-OAE; c. 183 Ma) and the associated negative C-isotope excursion is the massive release of 12C favouring greenhouse conditions and continental weathering. The nutrient delivery to shallow basins supported productivity and, because of O2...

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Veröffentlicht in:	Carbon Cycle and Ecosystem Response to the Jenkyns Event in the Early Toarcian (Jurassic) 2021-01, Vol.514 (1), p.59-81
Hauptverfasser:	Menini, Alessandro, Mattioli, Emanuela, Hesselbo, Stephen P., Ruhl, Micha, Suan, Guillaume
Format:	Artikel
Sprache:	eng
Schlagworte:	Sciences of the Universe
Online-Zugang:	Volltext
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