Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

McManus, Jerry F; Francois, Roger; Gherardi, Jeanne-Marie; Keigwin, Lloyd D; Brown Leger, Susan (2004): (Table S1) Age determination of sediment core OCE326-GGC5 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.769839, Supplement to: McManus, JF et al. (2004): Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes. Nature, 428(6985), 834-837, https://doi.org/10.1038/nature02494

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
The Atlantic meridional overturning circulation is widely believed to affect climate. Changes in ocean circulation have been inferred from records of the deep water chemical composition derived from sedimentary nutrient proxies (Boyle and Keigwin, 1987, doi:10.1038/330035a0), but their impact on climate is difficult to assess because such reconstructions provide insufficient constraints on the rate of overturning (LeGrand and Wunsch, 1995, doi:10.1029/95PA01455). Here we report measurements of 231Pa/230Th, a kinematic proxy for the meridional overturning circulation, in a sediment core from the subtropical North Atlantic Ocean. We find that the meridional overturning was nearly, or completely, eliminated during the coldest deglacial interval in the North Atlantic region, beginning with the catastrophic iceberg discharge Heinrich event H1, 17,500 yr ago, and declined sharply but briefly into the Younger Dryas cold event, about 12,700 yr ago. Following these cold events, the 231Pa/230Th record indicates that rapid accelerations of the meridional overturning circulation were concurrent with the two strongest regional warming events during deglaciation. These results confirm the significance of variations in the rate of the Atlantic meridional overturning circulation for abrupt climate changes.
Coverage:
Latitude: 33.700000 * Longitude: -57.583300
Minimum DEPTH, sediment/rock: 0.65 m * Maximum DEPTH, sediment/rock: 4.07 m
Event(s):
OCE326-GGC5 (GGC5) * Latitude: 33.700000 * Longitude: -57.583300 * Elevation: -4550.0 m * Location: North Atlantic * Method/Device: Gravity corer (GC) * Comment: Oceanus 326, 1998
Size:
64 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML