A deep‐sea coral record of North Atlantic radiocarbon through the Younger Dryas: Evidence for intermediate water/deepwater reorganization
- 17 November 2006
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 21 (4)
- https://doi.org/10.1029/2005pa001192
Abstract
No abstract availableKeywords
This publication has 52 references indexed in Scilit:
- Evidence from the high‐latitude North Atlantic for variations in Antarctic Intermediate water flow during the last deglaciationGeochemistry, Geophysics, Geosystems, 2005
- Radiocarbon and stable isotope constraints on Last Glacial Maximum and Younger Dryas ventilation in the western North AtlanticPaleoceanography and Paleoclimatology, 2004
- Rapid transient changes in northeast Atlantic deep water ventilation age across Termination IPaleoceanography and Paleoclimatology, 2004
- Eastern North Atlantic deep-sea corals: tracing upper intermediate water Δ14C during the HoloceneEarth and Planetary Science Letters, 2004
- Deep-sea corals evidence periodic reduced ventilation in the North Atlantic during the LGM/Holocene transitionEarth and Planetary Science Letters, 2003
- Atlantic Ocean circulation during the Younger Dryas: Insights from a new Cd/Ca record from the western subtropical South AtlanticPaleoceanography and Paleoclimatology, 2003
- Uranium-series and radiocarbon geochronology of deep-sea corals: implications for Southern Ocean ventilation rates and the oceanic carbon cycleEarth and Planetary Science Letters, 2001
- Paleocean circulation during the Last Deglaciation: A bipolar seesaw?Paleoceanography and Paleoclimatology, 1998
- Rapid changes in ocean circulation and atmospheric radiocarbonPaleoceanography and Paleoclimatology, 1996
- A salt oscillator in the glacial Atlantic? 1. The conceptPaleoceanography and Paleoclimatology, 1990