SEA-SURFACE PALEOTEMPERATURE EVOLUTION OF THE RUSSIAN PLATFORM DURINGTHE UPPER JURASSIC

Authors
RIBOULLEAU A BAUDIN F DAUX V HANTZPERGUE P RENARD M ZAKHAROV V
Citation
A. Riboulleau et al., SEA-SURFACE PALEOTEMPERATURE EVOLUTION OF THE RUSSIAN PLATFORM DURINGTHE UPPER JURASSIC, Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 326(4), 1998, pp. 239-246
Citations number
41
Categorie Soggetti
Geosciences, Interdisciplinary
Journal title
Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes → ACNP
ISSN journal
12518050
Volume
326
Issue
4
Year of publication
1998
Pages
239 - 246
Database
ISI
SICI code
1251-8050(1998)326:4<239:SPEOTR>2.0.ZU;2-I
Abstract
The revolution of the paleotemperatures of the Russian Platform over t he Late Jurassic are inferred from stable isotope measurements on bele mnite rostra. The delta(18)O data indicate temperature variations rang ing from 7 to 18 degrees C during the Oxfordian and a stable temperatu re ca 17 degrees over Kimmeridgian and Volgian. The results are compar ed to data from the literature in the frame of the paleogeographic rec onstruction of Europe for the Late Jurassic. (C) Academie des sciences /Elsevier, Paris.