(Table 1) Age determination of ODP Site 162-980 ...

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 A...

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Bibliographic Details
Main Authors: Benway, Heather M, McManus, Jerry F, Oppo, Delia W, Cullen, James L
Format: Dataset
Language:English
Published: PANGAEA 2010
Subjects:
DEPTH, sediment/rock
Age, dated material
Age, dated
Age, dated standard deviation
Calendar age
Age, comment
Composite Core
Age, 14C AMS
Age, 14C calibrated, CALIB 6.0 Reimer et al., 2009
Leg162
Joides Resolution
Ocean Drilling Program ODP
Greenland
Iceland
north atlantic current
North Atlantic
Online Access:https://dx.doi.org/10.1594/pangaea.816307
https://doi.pangaea.de/10.1594/PANGAEA.816307
Description
Summary: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 ... : Sediment depth is given in mcd. ...

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