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- W2023872612 abstract "The evolution of the paleotemperatures of the Russian Platform over the Late Jurassic are inferred from stable isotope measurements on belemnite rostra. The δ 18O data indicate temperature variations ranging from 7 to 18 °C during the Oxfordian and a stable temperature cal 17 °C over Kimmeridgian and Volgian. The results are compared to data from the literature in the frame of the paleogeographic reconstruction of Europe for the Late Jurassic. Des analyses géochimiques effectuées sur des rostres de bélemnites provenant du bassin de la Volga permettent de reconstituer l'évolution des paléotempératures depuis le Callovien supérieur jusqu'au Volgien moyen. Le rapport isotopique de l'oxygène indique que la température des eaux est passée de 7 à 18 °C au cours de l'Oxfordien, puis est restée relativement stable, autour de 17 °C, au Kimméridgien et au Volgien. Ces résultats associés, aux données antérieures, permettent de caractériser l'évolution des climats au cours du Jurassique supérieur, dans le cadre paléogéographique européen." @default.
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- W2023872612 date "1998-02-01" @default.
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- W2023872612 title "Évolution de la paléotempérature des eaux de la plate-forme russe au cours du Jurassique supérieur" @default.
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- W2023872612 doi "https://doi.org/10.1016/s1251-8050(97)86813-9" @default.
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