Citation:

PANGAEA.134241

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Related to:

Sarnthein, Michael; Winn, Kyaw; Jung, Simon J A; Duplessy, Jean-Claude; Labeyrie, Laurent D; Erlenkeuser, Helmut; Ganssen, Gerald M (1994): Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions. Paleoceanography, 9(2), 209-267, https://doi.org/10.1029/93PA03301

Project(s):

Institute for Geosciences, Christian Albrechts University, Kiel (GIK/IfG)

Coverage:

Latitude: 5.670000 * Longitude: -19.851667

Date/Time Start: 1979-03-01T00:00:00 * Date/Time End: 1979-03-01T00:00:00

Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 10.500 m

Event(s):

GIK13519-1 * Latitude: 5.670000 * Longitude: -19.851667 * Date/Time: 1979-03-01T00:00:00 * Elevation: -2862.0 m * Recovery: 10.7 m * Location: Atlantic Ocean * Campaign: (FGGE-Equator 79 - First GARP Global Experiment) * Basis: Meteor (1964) * Method/Device: Gravity corer (Kiel type) (SL)

Parameter(s):

#	Name	Short Name	Unit	Principal Investigator	Comment
1	DEPTH, sediment/rock	Depth sed	m		Geocode
2	Age model	Age model	ka	Sarnthein, Michael
3	Age, comment	Comm		Sarnthein, Michael

License:

Creative Commons Attribution 3.0 Unported (CC-BY-3.0)

Size:

56 data points

Data

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

1 Depth sed [m]	2 Age model [ka]	3 Comm
0.000	0.00	assumption of no sediment loss
0.135	9.80	deduced from C14 analog age of 9.1 ka; after Bard et al. (1990)
0.248	18.30	deduced from C14 analog age of 14.8 ka; after Bard et al. (1990)
0.535	29.50	deduced from C14 analog age of 26 ka; after Bard et al. (1990)
0.835	55.45	d18O;event 3.31; after Martinson et al. (1987)
0.945	71.12	d18O;event 4.24; after Martinson et al. (1987)
1.125	79.25	d18O;event 5.1; after Martinson et al. (1987)
1.240	90.95	d18O;event 5.2; after Martinson et al. (1987)
1.475	110.79	d18O;event 5.4; after Martinson et al. (1987)
1.665	122.19	d18O;event 5.5; after Martinson et al. (1987)
1.812	129.84	d18O;event 6.0; after Martinson et al. (1987)
1.915	135.34	d18O;event 6.2; after Martinson et al. (1987)
2.770	189.61	d18O event 7; after Martinson et al. (1987)
3.700	244.18	d18Oevent 8; after Martinson et al. (1987)
4.160	303.00	d18O event 9; after Imbrie et al. (1984)
5.060	339.00	d18O event 10; after Imbrie et al. (1984)
5.580	362.00	d18O event 11; after Imbrie et al. (1984)
6.220	423.00	d18O event 12; after Imbrie et al. (1984)
6.850	478.00	d18Oevent 13; after Imbrie et al. (1984)
7.440	524.00	d18O event 14; after Imbrie et al. (1984)
7.580	565.00	d18Oevent 15; after Imbrie et al. (1984)
8.290	620.00	d18O event 16; after Imbrie et al. (1984)
8.840	659.00	d18O event 17; after Imbrie et al. (1984)
9.160	689.00	d18O event 18; after Imbrie et al. (1984)
9.680	726.00	d18O event 19; after Imbrie et al. (1984)
9.870	730.00	Brunhes;Matuyama
9.960	736.00	d18O event 20; after Imbrie et al. (1984)
10.500	774.00	d18O event 20; after Imbrie et al. (1984)