The chronology of the last Deglaciation: Implications to the cause of the Younger Dryas Event
- 1 February 1988
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 3 (1), 1-19
- https://doi.org/10.1029/pa003i001p00001
Abstract
No abstract availableThis publication has 40 references indexed in Scilit:
- 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
- Reconstruction of the last deglaciation: deconvolved records of ?18O profiles, micropaleontological variations and accelerator mass spectrometric14C datingClimate Dynamics, 1987
- 14C Dating of Plant Macrofossils in Lake SedimentRadiocarbon, 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
- Does the ocean–atmosphere system have more than one stable mode of operation?Nature, 1985
- Target preparation for milligram sized 14C samples and data evaluation for AMS measurementsNuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 1984
- Deglacial warming of the northeastern Atlantic ocean: correlation with the paleoclimatic evolution of the european continentPalaeogeography, Palaeoclimatology, Palaeoecology, 1981
- Radiocarbon in Annual Coral Rings of Belize and FloridaRadiocarbon, 1980
- Radiocarbon in annual coral rings of FloridaGeophysical Research Letters, 1978