Carbon and oxygen isotope signals from the Callovian-Oxfordian in French sedimentary basins. - Archive ouverte HAL Accéder directement au contenu
Communication Dans Un Congrès Année : 2014

Carbon and oxygen isotope signals from the Callovian-Oxfordian in French sedimentary basins.

Résumé

High-resolution carbon and oxygen isotope data from the Paris Basin and the Subalpine Basin (France) are available in a precise biostratigraphic framework for the Callovian-Oxfordian stages. A biostratigraphically well-constrained δ13C curve, derived from bulk carbonates in the Paris Basin and the Subalpine Basin, is provided in order to document carbon-cycle evolution and to serve as a chemostratigraphic reference for the Callovian-Oxfordian in the Tethyan domain. Sea-temperature reconstructions, using diagenetically screened belemnite and oyster data, reveal major climate perturbations at the Middle-Late Jurassic transition.
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Dates et versions

hal-01016380 , version 1 (30-06-2014)

Identifiants

Citer

Pierre Pellenard, Romain Tramoy, Marine Cornuault, Emmanuelle Pucéat, Anna-Chiara Bartolini, et al.. Carbon and oxygen isotope signals from the Callovian-Oxfordian in French sedimentary basins.. 1st International Congress on Stratigraphy, Jul 2013, Lisbonne, Portugal. pp.865-867, ⟨10.1007/978-3-319-04364-7_163⟩. ⟨hal-01016380⟩
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