Carbon and Oxygen Isotope Signals from the Callovian-Oxfordian in French Sedimentary Basins

Affiliation auteurs!!!! Error affiliation !!!!
TitreCarbon and Oxygen Isotope Signals from the Callovian-Oxfordian in French Sedimentary Basins
Type de publicationConference Paper
Year of Publication2014
AuteursPellenard P, Tramoy R, Cornuault M, Puceat E, Bartolini A-C, Huret E, Martinez M, Fortwengler D, Marchand D, Thierry J
EditorRocha R, Pais J, Kullberg JC, Finney S
Conference NameSTRATI 2013
PublisherIUGS, Int Commiss Stratig; New Univ Lisbon, Fac Sci & Technol, Res Ctr Geol Sci & Engn; New Univ Lisbon, Fac Sci & Techno, Dept Earth Sci; GALP Energia SGPS S A; Partex Oil & Gas; Inst Francais Portugal; Centro Investigacao Ciencia & Engn Geologica; New U
Conference LocationGEWERBESTRASSE 11, CHAM, CH-6330, SWITZERLAND
ISBN Number978-3-319-04364-7; 978-3-319-04363-0
Mots-clésBelemnite, Bivalve, Callovian, Carbon cycle, Oxfordian, Palaeotemperatures
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 delta C-13 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.

DOI10.1007/978-3-319-04364-7_163