Deep circulation in the Late Cretaceous: Oxygen isotope paleotemperatures from Inoceramus remains in D.S.D.P. cores
Authors:
- E.S. SaltzmanESE.S. Saltzman
- E.J. BarronEBE.J. Barron
Open Access
- 1 November 1982
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 40 (1-3) , 167-181
Abstract
No abstract availableThis publication has 11 references indexed in Scilit:
- An Ice-Free Cretaceous? Results from Climate Model SimulationsScience, 1981
- On the Distribution of Climate Change Resulting from an Increase in CO2Content of the AtmosphereJournal of the Atmospheric Sciences, 1980
- Cenozoic and Late Mesozoic paleoceanographic and paleoglacial history recorded in circum-Antarctic deep-sea sedimentsMarine Geology, 1977
- Stratified waters as a key to the pastNature, 1976
- Oxygen isotope and cation composition of DSDP pore waters and the alteration of Layer II basaltsEarth and Planetary Science Letters, 1975
- Oxygen and Carbon Isotope Measurements of Late Cretaceous and Early Tertiary ForaminiferaMicropaleontology, 1974
- Distribution of Oxygen and Carbon Isotopes in Fossils of Late Cretaceous Age, Western Interior Region of North AmericaGeological Society of America Bulletin, 1969
- Isotopic standards for carbon and oxygen and correction factors for mass-spectrometric analysis of carbon dioxideGeochimica et Cosmochimica Acta, 1957
- Paleotemperatures of the Post-Aptian Cretaceous as Determined by the Oxygen Isotope MethodThe Journal of Geology, 1954
- Variation of O18 content of waters from natural sourcesGeochimica et Cosmochimica Acta, 1953