Changes in surface salinity of the North Atlantic Ocean during the last deglaciation
- 1 August 1992
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 358 (6386) , 485-488
- https://doi.org/10.1038/358485a0
Abstract
No abstract availableKeywords
This publication has 24 references indexed in Scilit:
- U/Th and 14C ages of corals from Barbados and their use for calibrating the 14C time scale beyond 9000 years B.P.Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 1990
- A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulationNature, 1989
- Correction of accelerator mass spectrometry14C ages measured in planktonic foraminifera: Paleoceanographic implicationsPaleoceanography and Paleoclimatology, 1988
- The chronology of the last Deglaciation: Implications to the cause of the Younger Dryas EventPaleoceanography and Paleoclimatology, 1988
- Retreat velocity of the North Atlantic polar front during the last deglaciation determined by 14C accelerator mass spectrometryNature, 1987
- Does the ocean–atmosphere system have more than one stable mode of operation?Nature, 1985
- Late glacial climate history from ice coresPublished by Wiley ,1984
- The North Atlantic Ocean during the last deglaciationPalaeogeography, Palaeoclimatology, Palaeoecology, 1981
- Deglacial warming of the northeastern Atlantic ocean: correlation with the paleoclimatic evolution of the european continentPalaeogeography, Palaeoclimatology, Palaeoecology, 1981
- REVISED CARBONATE-WATER ISOTOPIC TEMPERATURE SCALEGSA Bulletin, 1953