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

Benway, Heather M; McManus, Jerry F; Oppo, Delia W; Cullen, James L (2010): (Table 1) Age determination of ODP Site 162-980 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.816307, Supplement to: Benway, HM et al. (2010): Hydrographic changes in the eastern subpolar North Atlantic during the last deglaciation. Quaternary Science Reviews, 29(23-24), 3336-3345, https://doi.org/10.1016/j.quascirev.2010.08.013

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

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
Millennial-scale climate fluctuations of the last deglaciation have been tied to abrupt changes in the Atlantic Meridional Overturning Circulation (MOC). A key to understanding mechanisms of MOC collapse and recovery is the documentation of upper ocean hydrographic changes in the vicinity of North Atlantic deep convection sites. Here we present new high-resolution ocean temperature and d18Osw records spanning the last deglaciation from an eastern subpolar North Atlantic site that lies along the flow path of the North Atlantic Current, approaching deep convection sites in the Labrador and Greenland-Iceland-Norwegian (GIN) Seas. High-resolution temperature and d18Osw records from subpolar Site 980 help track the movement of the subpolar/subtropical front associated with temperature and Atlantic MOC changes throughout the last deglaciation. Distinct d18Osw minima during Heinrich 1 (H1) and the Younger Dryas (YD) correspond with peaks in ice-rafted debris and periods of reduced Atlantic MOC, indicating the presence of melt water in this region that could have contributed to MOC reductions during these intervals. Increased tropical and subtropical d18Osw during these periods of apparent freshening in the subpolar North Atlantic suggest a buildup of salt at low latitudes that served as a negative feedback on reduced Atlantic MOC.
Further details:
Oppo, Delia W; McManus, Jerry F; Cullen, James L (2003): (Table S1) Age determination of ODP Hole 162-980B. PANGAEA, https://doi.org/10.1594/PANGAEA.816310
Oppo, Delia W; McManus, Jerry F; Cullen, James L (2003): Palaeo-oceanography: Deepwater variability in the Holocene epoch. Nature, 422(6929), 277-277, https://doi.org/10.1038/422277b
Project(s):
Coverage:
Latitude: 55.484933 * Longitude: -14.702267
Date/Time Start: 1995-07-10T00:00:00 * Date/Time End: 1995-07-11T00:00:00
Minimum DEPTH, sediment/rock: 0.005 m * Maximum DEPTH, sediment/rock: 4.920 m
Event(s):
162-980 * Latitude: 55.484933 * Longitude: -14.702267 * Date/Time Start: 1995-07-10T00:00:00 * Date/Time End: 1995-07-11T00:00:00 * Elevation: -2180.0 m * Penetration: 353.7 m * Recovery: 366.7 m * Location: South Atlantic Ocean * Campaign: Leg162 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 39 cores; 353.7 m cored; 0 m drilled; 103.7% recovery
Comment:
Sediment depth is given in mcd.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2Age, dated materialDated materialBenway, Heather M
3Age, datedAge datedkaBenway, Heather MAge, 14C AMS
4Age, dated standard deviationAge dated std dev±Benway, Heather MAge, 14C AMS
5Calendar ageCal ageka BPBenway, Heather MAge, 14C calibrated, CALIB 6.0 (Reimer et al., 2009)represent the maximum probability of the 2-sigma range
6Age, commentCommBenway, Heather M
Size:
155 data points

Download Data

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

View dataset as HTML