Oxygen isotope ranking of late Eocene and Oligocene planktonic foraminifers: Implications for Oligocene sea-surface temperatures and global ice-volume
- 1 August 1984
- journal article
- research article
- Published by Elsevier in Marine Micropaleontology
- Vol. 9 (2) , 111-134
- https://doi.org/10.1016/0377-8398(84)90007-0
Abstract
No abstract availableThis publication has 22 references indexed in Scilit:
- Paleoclimatic analyses of middle Eocene through Oligocene planktic foraminiferal faunasPalaeogeography, Palaeoclimatology, Palaeoecology, 1983
- Vertical distribution and isotopic fractionation of living planktonic foraminifera from the Panama BasinNature, 1982
- Carbon and oxygen isotopic disequilibria of recent deep-sea benthic foraminiferaMarine Micropaleontology, 1981
- Core-top evaluation of benthic foraminiferal isotopic ratios for paleo-oceanographic interpretationsPalaeogeography, Palaeoclimatology, Palaeoecology, 1981
- Paleo-oceanographic utility of oxygen isotopic measurements on planktic foraminifera: Indian Ocean core-top evidencePalaeogeography, Palaeoclimatology, Palaeoecology, 1981
- Palaeoceanographic change in the Pacific at the Eocene–Oligocene boundaryNature, 1980
- Oxygen isotope palaeotemperatures from the Tertiary period in the North Sea areaNature, 1978
- Oxygen isotopic evidence for the depth stratification of tertiary and cretaceous planktic foraminiferaMarine Micropaleontology, 1978
- The genus Globigerinatheka BroennimannJournal of Foraminiferal Research, 1972
- Depth habitats of some species of pelagic Foraminifera as indicated by oxygen isotope ratiosAmerican Journal of Science, 1954