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

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0d85ae4f5edcc800d9cbfde2ff38b24a
https://hal.archives-ouvertes.fr/hal-00661408

Thermotectonic constraints on the geodynamic evolution of the Pindos fold‐and‐thrust‐belt by low‐temperature (U–Th)/He thermochronometry.

Autor: Athanassas, Constantin D., Papanikolaou, Dimitrios I., Falkowski, Sarah, Papanikolaou, Ioannis D., Ntokos, Dimitrios

Publikováno v: Geological Journal; Oct2021, Vol. 56 Issue 10, p5311-5328, 18p

PRELIMINARY DATA FROM THE FIRST RECORD OF THE EARLY TOARCIAN OCEANIC ANOXIC EVENT IN THE SEDIMENTS OF THE PINDOS ZONE (GREECE)

Autor: Kafousia N. Kafousia N., V. Karakitsios, H.C. Jenkyns

Publikováno v: Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Τόμ. 43 Αρ. 2 (2010): 12o Διεθνές Συνέδριο της Ελληνικής Γεωλογικής Εταιρίας; 627-633
Bulletin of the Geological Society of Greece; Vol. 43 No. 2 (2010): 12th International Conference of the G.S.G.; 627-633

The Early Toarcian Oceanic Anoxic Event (ca 183 Ma) coincides with high palaeotemperatures, regional anoxia to euxinia, marine transgression, mass extinction and high rates of organic-carbon burial in a global context. Most of the detailed studies of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::25118b4763efd906449881187e24fc7b
https://ejournals.epublishing.ekt.gr/index.php/geosociety/article/view/11225