Toarcian Oceanic Anoxic Event in the Pindos Ocean

Autor: Hugh C. Jenkyns, Emanuela Mattioli, N. Kafousia, Vasileios Karakitsios

Publikováno v: Geological Magazine
Geological Magazine, Cambridge University Press (CUP), 2011, 148 (4), pp.619-631. ⟨10.1017/S0016756811000082⟩
Geological Magazine, 2011, 148 (4), pp.619-631. ⟨10.1017/S0016756811000082⟩

The Early Toarcian (Early Jurassic, c. 183 Ma) was characterized by an Oceanic Anoxic Event (T-OAE), primarily identified by the presence of globally distributed approximately coeval black organic-rich shales. This event corresponded with relatively

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https://hal.archives-ouvertes.fr/hal-00661408