A paleoclimatic evaluation of marine oxygen isotope stage 11 in the high-northern Atlantic (Nordic seas)
- 1 February 2000
- journal article
- Published by Elsevier in Global and Planetary Change
- Vol. 24 (1) , 27-39
- https://doi.org/10.1016/s0921-8181(99)00067-3
Abstract
No abstract availableKeywords
This publication has 44 references indexed in Scilit:
- Glacial-interglacial records of the reflectance of sediments from the Norwegian-Greenland-Iceland Sea (Nordic seas)International Journal of Earth Sciences, 1999
- Evidence for a steeper Eemian than Holocene sea surface temperature gradient between Arctic and sub-Arctic regionsPalaeogeography, Palaeoclimatology, Palaeoecology, 1999
- Surface water changes in the norwegian sea during last deglacial and holocene timesQuaternary Science Reviews, 1997
- Implications of Stratigraphic and Paleoclimatic Records of the Last Interglaciation from the Nordic SeasQuaternary Research, 1996
- Reflection of Scandinavian Ice Sheet Fluctuations in Norwegian Sea Sediments during the Past 150,000 YearsQuaternary Research, 1995
- Coarse fraction fluctuations in pelagic carbonate sediments from the tropical Indian Ocean: A 1500‐kyr record of carbonate dissolutionPaleoceanography and Paleoclimatology, 1994
- Chronology and correlation of Quaternary magnetostratigraphy and nannofossil biostratigraphy in Norwegian-Greenland Sea sedimentsInternational Journal of Earth Sciences, 1989
- Paleoproductivity: The benthic/planktonic ratio in foraminifera as a productivity indexMarine Geology, 1988
- Paleo‐oceanography of the Norwegian Sea during the past 130,000 years: coccolithophorid and foraminferal dataBoreas, 1982
- PLANKTONIC FORAMINIFERA: DIFFERENTIAL SETTLING, DISSOLUTION, AND REDEPOSITION1Limnology and Oceanography, 1972