Citation:

PANGAEA.134735

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

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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: -25.490000 * Longitude: 11.307000

Date/Time Start: 1970-10-10T00:00:00 * Date/Time End: 1970-10-10T00:00:00

Minimum DEPTH, sediment/rock: 0.020 m * Maximum DEPTH, sediment/rock: 1.000 m

Event(s):

RC13-229 * Latitude: -25.490000 * Longitude: 11.307000 * Date/Time: 1970-10-10T00:00:00 * Elevation: -4191.0 m * Recovery: 16.37 m * Campaign: * Basis: Robert Conrad * Method/Device: Piston corer (PC)

Parameter(s):

#	Name	Short Name	Unit	Principal Investigator	Method/Device	Comment
1	DEPTH, sediment/rock	Depth sed	m			Geocode
2	Sedimentation rate	SR	cm/ka	Curry, William B	Calculated

License:

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

Size:

76 data points

Data

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

1 Depth sed [m]	2 SR [cm/ka]
0.020	3.30
0.020	3.30
0.020	3.30
0.020	3.30
0.025	3.30
0.025	3.30
0.045	3.30
0.065	3.30
0.085	3.30
0.100	3.30
0.100	3.30
0.100	3.30
0.100	3.30
0.100	3.30
0.145	3.30
0.200	3.59
0.200	3.59
0.200	3.59
0.200	3.59
0.200	3.59
0.250	3.59
0.250	3.59
0.300	3.59
0.300	3.59
0.300	3.59
0.300	3.59
0.300	3.59
0.310	3.59
0.310	3.59
0.350	3.59
0.350	3.59
0.400	3.59
0.400	3.59
0.400	3.59
0.400	3.59
0.410	3.59
0.450	3.59
0.450	3.59
0.450	3.59
0.500	4.02
0.500	4.02
0.500	4.02
0.500	4.02
0.500	4.02
0.550	4.02
0.550	4.02
0.600	4.02
0.600	4.02
0.600	4.02
0.600	4.02
0.600	4.02
0.600	4.02
0.600	4.02
0.650	4.02
0.700	4.02
0.700	4.02
0.700	4.02
0.710	4.02
0.710	4.02
0.750	4.02
0.750	4.02
0.800	4.02
0.800	4.02
0.800	4.02
0.800	4.02
0.800	4.02
0.900	4.02
0.900	4.02
0.900	4.02
0.900	4.02
0.900	4.02
1.000	4.02
1.000	4.02
1.000	4.02
1.000	4.02
1.000	4.02