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Keigwin, Lloyd D; Boyle, Edward A (2008): (Table 1) Age determination of sediment cores HU89038_8 and OCE326-GGC5 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.832421, Supplement to: Keigwin, LD; Boyle, EA (2008): Did North Atlantic overturning halt 17,000 years ago? Paleoceanography, 23(1), PA1101, https://doi.org/10.1029/2007PA001500

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Abstract:
Models indicate that a complete shutdown of deep and intermediate water production is a possible consequence of extreme climate conditions in the northern North Atlantic, and the high ratio of 231Pa to 230Th on Bermuda Rise is evidence that this might have happened ∼17 ka during Heinrich event 1 (H1). However, new radiocarbon data from bivalves that lived at ∼4.6 km on the Bermuda Rise during H1 lead to a different conclusion. The bivalve data do indeed indicate ventilation of the deep western North Atlantic was suppressed during H1 but not as much as it was during the last glacial maximum. We propose that high diatom flux to the Bermuda Rise during H1 is at least in part responsible for increased 231Pa/230Th at that time. Although we cannot say for sure why opal production was so high in a gyre center location at that time, increased leakage of silica rich waters from the Southern Ocean to the North Atlantic is one possibility.
Further details:
McManus, Jerry F; Francois, Roger; Gherardi, Jeanne-Marie; Keigwin, Lloyd D; Brown Leger, Susan (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
Coverage:
Median Latitude: 33.695000 * Median Longitude: -57.579150 * South-bound Latitude: 33.690000 * West-bound Longitude: -57.583300 * North-bound Latitude: 33.700000 * East-bound Longitude: -57.575000
Minimum DEPTH, sediment/rock: 2.21 m * Maximum DEPTH, sediment/rock: 5.75 m
Event(s):
HU89038_8 * Latitude: 33.690000 * Longitude: -57.575000 * Elevation: -4500.0 m * Location: Bermuda Rise * Method/Device: Piston corer (PC)
OCE326-GGC5 (GGC5) * Latitude: 33.700000 * Longitude: -57.583300 * Elevation: -4550.0 m * Location: North Atlantic Ocean * Method/Device: Gravity corer (GC) * Comment: Oceanus 326, 1998
Comment:
Sample OCE326-GGGC5 2.21 m depth, G. inflata reported on previously by McManus et al. (2004).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Age, dated materialDated materialKeigwin, Lloyd D
3DEPTH, sediment/rockDepth sedmGeocode
4Age, datedAge datedkaKeigwin, Lloyd DAge, 14C AMS
5Age, dated standard deviationAge dated std dev±Keigwin, Lloyd DAge, 14C AMS
6Laboratory code/labelLab labelKeigwin, Lloyd D
7Calendar ageCal ageka BPKeigwin, Lloyd DAge, 14C calibrated
8Calendar age, standard deviationCal age std dev±Keigwin, Lloyd DAge, 14C calibrated
Size:
30 data points

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