0000000000625726

AUTHOR

Fabienne Giraud

showing 2 related works from this author

The Mid-Cenomanian Event in southeastern France: evidence from palaeontological and clay mineralogical data.

2013

16 pages; International audience; Reconstruction of main palaeoenvironmental conditions across the Mid-Cenomanian Event (MCE I) in the hemipelagic Tethyan section of Blieux (Southeast France, Vocontian Basin) is proposed. Quantitative analyses of calcareous nannofossil, ammonoid and clay mineral assemblages have been made and compared with respect to sea level changes and the carbon cycle perturbations. The nannofossil primary productivity, as recorded by nannofossil fluxes and relative abundances of meso-eutrophic taxa, is low just below and during the MCE Ia, then slightly increases in the interval including the MCE Ib. The clay assemblages mainly consist of illite/smectite mixed-layers w…

010506 paleontology[SDE.MCG]Environmental Sciences/Global Changesengineering.material[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesClimatic conditionsPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySchloenbachiaCalcareous nannofossilsKaoliniteRelative species abundanceSea level[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesMiddle CenomanianbiologyAmmonoidsPaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrybiology.organism_classificationCretaceous[ SDE.MCG ] Environmental Sciences/Global ChangesVocontian Basin13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringPrimary productivityCenomanianClay minerals[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Palynofacies and calcareous nannofossils in the Upper Kimmeridgian, southeastern Paris basin (France)

2005

AbstractThe Upper Kimmeridgian Members “Calcaires blancs supérieurs” and the “Marnes à exogyres supérieures” of the southeastern Paris basin were investigated for their palynofacies and calcareous nannofossils. These members display alternating limestone-marl lithotypes and represent shallow marine palaeoenvironments. The lower carbonate member is interpreted as a proximal palaeoenvironment (palaeobathymetry = 5 to 10 m), where storm and swell deposits were prevalent and the salinity was occasionally weak. The relative richness of brown phytoclasts in this part is favoured by good preservation related to restricted conditions. These conditions would explain the dominance of the nannofoss…

010506 paleontologyPalaeoenvironments010502 geochemistry & geophysics01 natural sciencesPalynofaciesSedimentary depositional environmentCoccolithPaleontologychemistry.chemical_compoundMarlCalcareous nannofossilsDominance (ecology)14. Life underwaterCoquina0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyPalynologyUpper KimmeridgianMarine shallow-water dépositsGeologyParis basinPalynofacieschemistryCarbonate[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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