Skip to content
Home
About Us
Resources
Profiles Metrics
Authors Directory
Institutions Directory
Top Authors
Top Institutions
Top Sponsors
AI Digest
Contact Us
Menu
Home
About Us
Resources
Profiles Metrics
Authors Directory
Institutions Directory
Top Authors
Top Institutions
Top Sponsors
AI Digest
Contact Us
Home
About Us
Resources
Profiles Metrics
Authors Directory
Institutions Directory
Top Authors
Top Institutions
Top Sponsors
AI Digest
Contact Us
Menu
Home
About Us
Resources
Profiles Metrics
Authors Directory
Institutions Directory
Top Authors
Top Institutions
Top Sponsors
AI Digest
Contact Us
Publication Details
AFRICAN RESEARCH NEXUS
SHINING A SPOTLIGHT ON AFRICAN RESEARCH
agricultural and biological sciences
Changes in the vertical structure of the North Atlantic Ocean between glacial and modern times
Quaternary Science Reviews, Volume 11, No. 4, Year 1992
Notification
URL copied to clipboard!
Description
The distribution of planktic foraminiferal δ18O over the North Atlantic Ocean has been interpreted by Duplessy et al. (1991, 1992) in terms of the distribution of surface water salinity during the last glacial maximum (LGM) and the Younger Dryas (YD). We present here the implications of this surface salinity distribution for changes in deep convection during these periods. Temperature/salinity/density diagrams of the water column have been constructed using the plancktic and benthic foraminifera δ18O values together with sea surface temperature estimates obtained by using micropaleontological transfer functions. The precision of these reconstructions is limited by the remaining uncertainties in the two basic assumptions upon which the methods are based: - the sea surface temperature reconstruction by CLIMAP are valid within the statistical uncertainties; - the water salinity/δ18O relationship is well constrained for surface and intermediate ocean waters. A significant difference between the modern and the reconstructed glacial water structure is observed. During the LGM, the modern relatively warm and salty Norwegian Sea surface water and the North Atlantic Deep Water (NADW) were replaced by low salinity surface water in the northern Atlantic Ocean and the Norwegian Sea and cold deep water (0-1°C). However, surface water salinity in the central North Atlantic Ocean (52-54°N., 25-40°W.) was sufficiently high to permit deep water convection as a source of North Atlantic intermediate and deep waters. Open ocean convection at the northern limit of the subtropical surface waters (around 40°N.) may have contributed to the ventilation of the intermediate waters. The waters deeper than 2000 m were the result of mixing between poorly-oxygenated southern waters and well-ventilated North Atlantic deep waters. A similar reconstruction for the cold YD period indicates that the modern type of circulation, with warm and ventilated NADW, was largely in operation and that the hydrologic pattern was different from that prevailing during the LGM. © 1992.
Authors & Co-Authors
Labeyrie, Laurent D.
France, Paris
Cnrs Centre National de la Recherche Scientifique
Duplessy, Jean Claude
France, Paris
Cnrs Centre National de la Recherche Scientifique
Duprat, J.
France, Pessac
Environnements et Paléoenvironnements Océaniques et Continentaux
Juillet-Leclerc, Anne
France, Paris
Cnrs Centre National de la Recherche Scientifique
Moyes, Jean
France, Pessac
Environnements et Paléoenvironnements Océaniques et Continentaux
Michel, Elisabeth
France, Paris
Cnrs Centre National de la Recherche Scientifique
Kallel, Néjib
France, Paris
Cnrs Centre National de la Recherche Scientifique
Tunisia, Sfa
Now at Ecole D'ingénieurs
Shackleton, Nicholas John
United Kingdom, Cambridge
University of Cambridge
Statistics
Citations: 175
Authors: 8
Affiliations: 4
Identifiers
Doi:
10.1016/0277-3791(92)90022-Z
ISSN:
02773791
Research Areas
Environmental