Turbidite‐induced re‐oxygenation episodes of the sediment‐water interface in a diverticulum of the Tethys Ocean during the Oceanic Anoxic Event 1a: The French Vocontian Basin

Turbidite‐induced re‐oxygenation episodes of the sediment‐water interface in a diverticulum of the Tethys Ocean during the Oceanic Anoxic Event 1a: The French Vocontian Basin

Abstract Widespread anoxic events affected the Tethys Ocean during the Mesozoic. The Ocean Anoxic Event 1a (Early Aptian), expressed as the Selli Level or Goguel Level (GL) in European basins. The GL was deposited in the French Vocontian Basin, a semi‐enclosed basin connected to the Tethys Ocean. Th...

Full description

Bibliographic Details
Main Authors: Alexis Caillaud, Melesio Quijada, Bastien Huet, Jean‐Yves Reynaud, Armelle Riboulleau, Viviane Bout‐Roumazeilles, François Baudin, Anthony Chappaz, Thierry Adatte, Jean‐Noël Ferry, Nicolas Tribovillard
Format: Article
Language:English
Published: Wiley 2020-06-01
Series:The Depositional Record
Subjects:
Clay minerals
Early Aptian
geochemistry
grain size
organic matter dilution
organic matter
Online Access:https://doi.org/10.1002/dep2.102

Internet

https://doi.org/10.1002/dep2.102

Similar Items