Search results for " paleotemperature"

showing 3 items of 3 documents

Venerid bivalve Venus verrucosa as a high-resolution archive of seawater temperature in the Mediterranean Sea

2021

Abstract High-resolution stable isotope data (δ18O, δ13C) were used to study growth strategies of the bivalve Venus verrucosa collected from three sites of the eastern coast of the Adriatic Sea. The principal objectives of this study were to identify the main growing season and to evaluate the potential applicability of δ18Oshell values to reconstruct the seasonal temperature variability. Calcium carbonate for oxygen and carbon isotope analyses was obtained by drilling the outer shell layer. Temporal and spatial variations in temperature and salinity values at the study sites were simulated using the 3D numerical ocean model ROMS. Annual periodicity of growth patterns was confirmed by δ18Os…

010506 paleontologyδ13Cδ18OStable isotope ratioTemperature salinity diagramsPaleontologyGrowing season010502 geochemistry & geophysicsOceanography01 natural sciencesOceanographyMediterranean seaSeawater14. Life underwaterBayStable isotopes ; Paleotemperature ; Adriatic Sea ; Growth rateEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Organic carbon composition and a new organic lipid paleotemperature proxy applied to the Messinian Tripoli Formation, Caltanissetta Basin, Sicily

2004

Settore GEO/01 - Paleontologia E PaleoecologiaMicroorganism paleotemperatureMessinian Tripoli FormationSettore GEO/08 - Geochimica E Vulcanologia
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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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