Deep circulation change linked to HEINRICH Event 1 and Younger Dryas in a middepth North Atlantic Core
- 1 April 1994
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 9 (2), 185-194
- https://doi.org/10.1029/94pa00032
Abstract
No abstract availableKeywords
This publication has 21 references indexed in Scilit:
- Correlations between climate records from North Atlantic sediments and Greenland iceNature, 1993
- Patterns of Ice‐Rafted Detritus in the Glacial North Atlantic (40–55°N)Paleoceanography and Paleoclimatology, 1993
- Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial periodNature, 1992
- Changes in surface salinity of the North Atlantic Ocean during the last deglaciationNature, 1992
- Detrital carbonate-rich sediments, northwestern Labrador Sea: Implications for ice-sheet dynamics and iceberg rafting (Heinrich) events in the North AtlanticGeology, 1992
- North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperatureNature, 1987
- Retreat velocity of the North Atlantic polar front during the last deglaciation determined by 14C accelerator mass spectrometryNature, 1987
- High-latitude salinity effects and interhemispheric thermohaline circulationsNature, 1986
- Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years: changes in deep ocean circulation and chemical inventoriesEarth and Planetary Science Letters, 1985
- Deglacial warming of the northeastern Atlantic ocean: correlation with the paleoclimatic evolution of the european continentPalaeogeography, Palaeoclimatology, Palaeoecology, 1981