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• W1983124467 abstract "Research Article| February 01, 2007 Fish tooth δ18O revising Late Cretaceous meridional upper ocean water temperature gradients Emmanuelle Pucéat; Emmanuelle Pucéat 1UMR CNRS, 5561Biogéosciences, 6 Boulevard Gabriel, 21000 Dijon, France Search for other works by this author on: GSW Google Scholar Christophe Lécuyer; Christophe Lécuyer 2UMR CNRS, 5125 PaléoEnvironnement et PaléobioSphère, Université Claude Bernard Lyon 1, Bât. Géode, 27–43 Boulevard du 11 Novembre 1918, 69622 Villeurbanne Cedex, France Search for other works by this author on: GSW Google Scholar Yannick Donnadieu; Yannick Donnadieu 3UMR CEA/CNRS, 1572 Laboratoire des Sciences du Climat et de l'Environnement, CE Saclay, Orme des Merisiers, Bât. 701, 91191 Gif sur Yvette Cedex, France Search for other works by this author on: GSW Google Scholar Philippe Naveau; Philippe Naveau 3UMR CEA/CNRS, 1572 Laboratoire des Sciences du Climat et de l'Environnement, CE Saclay, Orme des Merisiers, Bât. 701, 91191 Gif sur Yvette Cedex, France Search for other works by this author on: GSW Google Scholar Henri Cappetta; Henri Cappetta 4UMR CNRS, 5554 Institut des Sciences de l'Evolution de Montpellier, Université de Montpellier II, Cc 064, Place Eugène Bataillon, 34095 Montpellier Cedex 5, France Search for other works by this author on: GSW Google Scholar Gilles Ramstein; Gilles Ramstein 5UMR CEA/CNRS, 1572 Laboratoire des Sciences du Climat et de l'Environnement, CE Saclay, Orme des Merisiers, Bat. 701, 91191 Gif sur Yvette Cedex, France Search for other works by this author on: GSW Google Scholar Brian T. Huber; Brian T. Huber 6Department of Paleobiology, National Museum of Natural History, P.O. Box 37012 NHB MRC 121, Washington, D.C. 20013-7012, USA Search for other works by this author on: GSW Google Scholar Juergen Kriwet Juergen Kriwet 7Museum of National History, Invalidenstrasse 43, 10115 Berlin, Germany Search for other works by this author on: GSW Google Scholar Geology (2007) 35 (2): 107–110. https://doi.org/10.1130/G23103A.1 Article history received: 16 Jun 2006 rev-recd: 08 Sep 2006 accepted: 15 Sep 2006 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Emmanuelle Pucéat, Christophe Lécuyer, Yannick Donnadieu, Philippe Naveau, Henri Cappetta, Gilles Ramstein, Brian T. Huber, Juergen Kriwet; Fish tooth δ18O revising Late Cretaceous meridional upper ocean water temperature gradients. Geology 2007;; 35 (2): 107–110. doi: https://doi.org/10.1130/G23103A.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The oxygen isotope composition of fossil fish teeth, a paleo–upper ocean temperature proxy exceptionally resistant to diagenetic alteration, provides new insight on the evolution of the low- to middle-latitude thermal gradient between the middle Cretaceous climatic optimum and the cooler latest Cretaceous period. The new middle Cretaceous low to middle latitude thermal gradient agrees with that previously inferred from planktonic foraminifera δ18O recovered from Deep Sea Drilling Project and Ocean Drilling Program drilling sites, although the isotopic temperatures derived from δ18O of fish teeth are uniformly higher by ∼3–4 °C. In contrast, our new latest Cretaceous thermal gradient is markedly steeper than those previously published for this period. Fish tooth δ18O data demonstrate that low- to middle-latitude thermal gradients of the middle Cretaceous climatic optimum and of the cooler latest Cretaceous are similar to the modern one, despite a cooling of 7 °C between the two periods. Our new results imply that no drastic changes in meridional heat transport are required to explain the Late Cretaceous climate. Based on climate models, such a cooling without any change in the low to mid- decrease dle latitude thermal gradient supports an atmospheric CO2 as the primary driver of the climatic evolution recorded during the Late Cretaceous. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W1983124467 date "2007-01-01" @default.
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• W1983124467 title "Fish tooth δ18O revising Late Cretaceous meridional upper ocean water temperature gradients" @default.
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