A reinterpretation of Mid‐Cretaceous shallow marine temperatures through model‐data comparison
- 1 December 1999
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 14 (6) , 679-697
- https://doi.org/10.1029/1999pa900034
Abstract
No abstract availableKeywords
This publication has 85 references indexed in Scilit:
- Evolution of early planktic foraminifersPublished by Elsevier ,2003
- Deep water formation and poleward ocean heat transport in the warm climate extreme of the Cretaceous (80 Ma)Geophysical Research Letters, 1998
- Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equationsPaleoceanography and Paleoclimatology, 1998
- Can increased poleward oceanic heat flux explain the warm Cretaceous climate?Paleoceanography and Paleoclimatology, 1996
- Experimental determination of stable isotope variability in Globigerina bulloides: implications for paleoceanographic reconstructionsMarine Micropaleontology, 1996
- A “simulation” of Mid‐Cretaceous climatePaleoceanography and Paleoclimatology, 1995
- Interspecies variation in stable isotopic signals of Maastrichtian planktonic foraminiferaPaleoceanography and Paleoclimatology, 1995
- Fractionation of carbon isotopes by phytoplankton and estimates of ancient CO2 levelsGlobal Biogeochemical Cycles, 1992
- Opening the carbon isotope “vital effect” black box 1. Seasonal temperatures in the euphotic zonePaleoceanography and Paleoclimatology, 1989
- Oxygen isotopic evidence for the depth stratification of tertiary and cretaceous planktic foraminiferaMarine Micropaleontology, 1978