Ocean circulation in the Norwegian sea during the last deglaciation: Isotopic evidence
Authors:
- Eystein JansenEJEystein Jansen
- Helmut ErlenkeuserHEHelmut Erlenkeuser
- 1 April 1985
- journal article
- research article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 49 (3-4) , 189-206
Abstract
No abstract availableThis publication has 32 references indexed in Scilit:
- Oxygen and carbon isotope record of East Pacific core V19-30: implications for the formation of deep water in the late Pleistocene North AtlanticEarth and Planetary Science Letters, 1983
- Deglacial CO2 buildup: Constraints on the coral-reef modelPalaeogeography, Palaeoclimatology, Palaeoecology, 1982
- Carbon and oxygen isotopic disequilibria of recent deep-sea benthic foraminiferaMarine Micropaleontology, 1981
- Benthonic foraminifera in surface samples from the Norwegian continental margin between 62 degrees N and 65 degrees NJournal of Foraminiferal Research, 1981
- Core-top evaluation of benthic foraminiferal isotopic ratios for paleo-oceanographic interpretationsPalaeogeography, Palaeoclimatology, Palaeoecology, 1981
- Distribution and ecology of benthic foraminifera in the Norwegian-Greenland SeaMarine Micropaleontology, 1980
- Planktonic foraminiferal and oxygen isotopic stratigraphy and paleoclimatology of Norwegian Sea deep‐sea coresBoreas, 1978
- Abyssal benthonic foraminifera as hydrographic indicators in the western South Atlantic OceanJournal of Foraminiferal Research, 1978
- Laurentide Ice Sheet Meltwater Recorded in Gulf of Mexico Deep-Sea CoresScience, 1975
- Oxygen Isotope and Palaeomagnetic Stratigraphy of Equatorial Pacific Core V28-238: Oxygen Isotope Temperatures and Ice Volumes on a 105 Year and 106 Year ScaleQuaternary Research, 1973