Precession-driven changes in Iceland–Scotland Overflow Water penetration and bottom water circulation on Gardar Drift since ~ 200 ka
Citable URI
https://hdl.handle.net/1912/7770As published
https://doi.org/10.1016/j.palaeo.2015.09.042Abstract
Benthic foraminiferal stable isotopic records from a transect of sediment cores south
of the Iceland-Scotland Ridge reveal that the penetration depth of Iceland-Scotland Overflow
Water (ISOW) varied on orbital timescales with precessional pacing over the past ~ 200 kyr.
Similar, higher benthic foraminiferal δ13 C values (~ 1.0 ‰) were recorded at all transect sites
downstream of the Iceland-Scotland Ridge during interglacial periods (Marine Isotope
Chrons 5 and 1), indicating a deeply penetrating ISOW. During glacial periods (Marine
Isotope Chrons 6, 4, and 2), benthic foraminiferal δ13C values from the deeper (2700-3300
m), southern sites within this transect were significantly lower (~ 0.5 ‰) than values from the
northern (shallower) portion of the transect (~ 1.0 ‰), reflecting a shoaling of ISOW and
greater influence of glacial Southern Component Water (SCW) in the deep Northeast
Atlantic. Particularly during intermediate climate states, ISOW strength is driven by
precesional cycles, superimposed on the large-scale glacial-interglacial ISOW variability.
Millennial-scale variability in the penetration of ISOW, likely caused by high-frequency
Heinrich and Dansgaard-Oeschger Events, is most pronounced during intermediate climate
states.
Description
© The Author(s), 2015. This is the author's version of the work and is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Palaeogeography, Palaeoclimatology, Palaeoecology 440 (2015): 561-563, doi:10.1016/j.palaeo.2015.09.042.
Collections
Suggested Citation
Preprint: Elmore, Aurora C., Wright, James D., Chalk, Thomas B., "Precession-driven changes in Iceland–Scotland Overflow Water penetration and bottom water circulation on Gardar Drift since ~ 200 ka", 2015-09-21, https://doi.org/10.1016/j.palaeo.2015.09.042, https://hdl.handle.net/1912/7770The following license files are associated with this item:
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-NoDerivs 3.0 United States
Related items
Showing items related by title, author, creator and subject.
-
On the momentum transfer at the sea surface. I. On the frictional force between air and water and on the occurrence of a laminar boundary layer next to the surface of the sea. II. Measurements of vertical gradient of wind over water. III. Transport of surface water due to the wind system over the North Atlantic
(Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 1936-06)I. It is fairly generally assumed that the horizontal circulation of the ocean "troposphere" is maintained by the large scale permanent wind system of the atmosphere. Accurate knowledge of the tangential force exerted by ... -
Oxygen and hydrogen isotope fractionation in serpentine–water and talc–water systems from 250 to 450°C, 50 MPa
(2009-07-21)Oxygen and hydrogen isotope fractionation factors in the talc-water and serpentine-water systems have been determined by laboratory experiment from 250 to 450°C at 50 MPa using the partial exchange technique. Talc was ... -
Water column structure and statistics of denmark strait overflow water cyclones
(2013-10-30)Data from seven moorings deployed across the East Greenland shelfbreak and slope 280 km downstream of Denmark Strait are used to investigate the characteristics and dynamics of Denmark Strait Overflow Water (DSOW) cyclones. ...
