Search results for "Palaeotemperature"

showing 2 items of 2 documents

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

2013

3 pages; International audience; 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.

010506 paleontology[SDE.MCG]Environmental Sciences/Global ChangesCallovianBelemnitechemistry.chemical_elementStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesIsotopes of oxygenCarbon cycleOxfordianPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwater0105 earth and related environmental sciencesgeographygeography.geographical_feature_categoryδ13CBivalveCarbon cycleSedimentary basin[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryPalaeotemperatures[ SDE.MCG ] Environmental Sciences/Global Changeschemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyMontane ecologyCarbonGeology
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Isotopic seawater temperatures in the Albian Gault Clay of the Boulonnais (Paris Basin): Palaeoenvironmental implications

2016

13 pages; International audience; Oxygen isotopes were measured on several types of fossil hardparts from the Gault Clay Formation including benthic and planktonic foraminifera, belemnite guards, and fish small-teeth. Belemnites δ18O values indicate low temperatures (13.5–19.3 °C) with an increase from the Middle to Late Albian. Foraminifera provide variable δ18O values, some too low to be relevant in terms of temperature (until 42 °C). These low values probably result from a diagenetic alteration of the foraminiferal tests even though SEM observations revealed well-preserved microstructures. However, higher foraminiferal δ18O values recorded in some levels indicate temperatures in the rang…

010506 paleontologyδ18OGault Clay FormationForaminifera010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenForaminiferaPaleontologyPalaeotemperatureBelemnites guardsParis BasinFish teeth14. Life underwaterComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesbiologyfungiSelachian teethPaleontologyGeologyPelagic zoneAlbianbiology.organism_classificationDiagenesisSea surface temperature13. Climate actionBenthic zone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOxygen isotopes[ SDU.STU.HY ] Sciences of the Universe [physics]/Earth Sciences/HydrologyBelemnitesGeology
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