Search results for "paleoenvironmental change"

showing 3 items of 3 documents

Carbon cycle and sea-water palaeotemperature evolution at the Middle-Late Jurassic transition, eastern Paris Basin (France).

2014

14 pages; International audience; A very high-resolution carbon and oxygen stable isotope analysis (bulk-carbonate) of a biostratigraphically well-constrained Callovian-Oxfordian series is provided here for the first time. The homogeneity of the clayey series and the weak diagenetic alteration allow the isotopic signal variations to be considered as primary in origin. A prominent and brief negative excursion in the δ13C curve (−2‰), occurring at the start of the Middle Callovian (Jason Zone - Obductum Subzone) and correlated regionally, suggests a possible methane release. The increasing δ13C values thereafter up to the Early Oxfordian, concomitant with a warming episode, highlight the buri…

δ18OStratigraphy[SDE.MCG]Environmental Sciences/Global ChangesCallovianOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyIsotopes of oxygenCarbon cycleOxfordianPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterIsotope analysisδ13CbiologyCarbon isotopesGeologybiology.organism_classification[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistrySea-water paleotemperatures[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsPaleoenvironmental changes13. Climate actionIsotopes of carbon[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOxygen isotopesEconomic GeologyGlobal coolingBelemnitesGeology
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Paleoenvironmental and climatic changes during the last 25 ky along a W-E transect across the Mediterranean Sea.

2012

climatic changeplanktonic foraminiferastable isotopeMediterranean Seapaleoenvironmental change
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The late Messinian "Lago-Mare" event and the Zanclean Reflooding in the Mediterranean Sea: New insights from the Cuevas del Almanzora section (Vera B…

2020

Abstract The return to normal marine conditions in the Mediterranean Sea after the end of the Messinian Salinity Crisis (MSC), that led to the deposition of thick evaporitic succession followed by settlement of brackish to freshwater conditions of the “Lago-Mare”, is still subject to extensive debate between two opposite scenarios. One scenario implies an abrupt reflooding through the Gibraltar gateway of the Mediterranean Sea previously disconnected from the world ocean and partly desiccated. The second scenario postulates that the Mediterranean Sea kept a high-water level throughout the Messinian Salinity Crisis and was connected continuously to the Atlantic Ocean and to the Paratethys. T…

Planktonic foraminifera010504 meteorology & atmospheric sciences[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]010502 geochemistry & geophysics01 natural sciencesLago-Mare event Mediterranean Sea Messinian-Zanclean transition Ostracods Oxygen and carbon stable isotopes of planktonic foraminifera Paleoenvironmental changes Planktonic foraminifera Zanclean refloodingForaminiferaPaleontologyMediterranean seaOstracodMediterranean SeaLago-Mare eventOxygen and carbon stable isotopes of planktonic foraminifera14. Life underwaterChronostratigraphyMessinian-Zanclean transitionGlobigerinoidesComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesMilankovitch cyclesbiologyBrackish waterOstracodsGlobigerina bulloidesbiology.organism_classificationPaleoenvironmental changes13. Climate actionGeneral Earth and Planetary SciencesZanclean refloodingGeology
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