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European ammonoid diversity questions the spreading of anoxia as primary cause for the Cenomanian/Turonian (Late Cretaceous) mass extinction

Monnet, Claude ; Bucher, Hugo

In: Swiss Journal of Geosciences, 2007, vol. 100, no. 1, p. 137-144

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    Titre
    • European ammonoid diversity questions the spreading of anoxia as primary cause for the Cenomanian/Turonian (Late Cretaceous) mass extinction
    Auteur
    • Monnet, Claude. Paläontologisches Institut und Museum, Universität Zürich, Karl Schmid Strasse 4, CH-8006, Zürich, Switzerland
    • Bucher, Hugo. Paläontologisches Institut und Museum, Universität Zürich, Karl Schmid Strasse 4, CH-8006, Zürich, Switzerland
    Type de document
    • Postprint
    Langue
    • Anglais
    Publié dans
    • Swiss Journal of Geosciences, 2007, vol. 100, no. 1, p. 137-144. Birkhäuser-Verlag; www.birkhäuser.ch
    Autre version électronique
    Identifiant OAI-PMH
    • oai:doc.rero.ch:310596
    Summary
    Abstract.: Ammonoid diversity patterns show that the spreading of oceanic anoxia is not the initial and major kill mechanism for the Cenomanian/Turonian mass extinction as usually suggested. In the Anglo-Paris Basin and the Vocontian Basin, the drop of ammonoid species richness starts around the middle/late Cenomanian boundary, i.e. 0.75 myr before the occurrence of anoxic deepwater sediments. The stepwise extinction of first heteromorphs and then acanthoceratids is incompatible with the rise of the oxygen minimum zone. Moreover, shelf environments of these basins remained well oxygenated during the Cenomanian/Turonian boundary interval. Thus, we stress that other causative mechanisms initiated the ammonoid extinction even if anoxia subsequently participated in the demise of marine ecosystems