The Late Hauterivian Faraoni ‘Oceanic Anoxic Event’: an update-Reference-Cited by-同舟云学术

The Late Hauterivian Faraoni ‘Oceanic Anoxic Event’: an update

Published:2014-06-01 Issue:6 Volume:185 Page:359-377
ISSN:1777-5817
Container-title:Bulletin de la Société Géologique de France
language:en
Short-container-title:

Author:

Baudin François¹,Riquier Laurent¹

Affiliation:

1. Sorbonne-Université, UPMC-Univ. Paris 06 et CNRS, UMR 7193 ISTeP, 4 place Jussieu, case 117, 75252 Paris cedex 05, France

Abstract

AbstractMost oceanic anoxic events (OAEs) took place during the middle part of the Cretaceous and the Late Hauterivian probably recorded the first anoxic event within this peculiar time interval. The so-called Faraoni event (~131 Ma) was initially defined as a short-lived anoxic event restricted to the Mediterranean domain. Since its recognition, numerous geochemical studies were conducted on the Faraoni event and new occurrences of this event were suggested outside the Tethyan domain. This paper presents an update on the Late Hauterivian Faraoni event and examines if this event agrees with the definition of OAEs.

Publisher

EDP Sciences

Subject

Geology

Link

https://pubs.geoscienceworld.org/sgf/bsgf/article-pdf/185/6/359/2969969/359.pdf

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