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

Weinelt, Mara; Sarnthein, Michael (2003): Age model of sediment core GIK23259-2. PANGAEA, https://doi.org/10.1594/PANGAEA.97129

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

RIS CitationBibTeX CitationShow MapGoogle Earth

Related to:
Weinelt, Mara (1993): Veränderungen der Oberflächenzirkulation im Europäischen Nordmeer während der letzten 60.000 Jahre - Hinweise aus stabilen Isotopen. Berichte aus dem Sonderforschungsbereich 313, Christian-Albrechts-Universität, Kiel, 41, 106 pp, https://doi.org/10.2312/reports-sfb313.1993.41
Coverage:
Latitude: 72.030000 * Longitude: 9.265000
Date/Time Start: 1988-07-21T00:00:00 * Date/Time End: 1988-07-21T00:00:00
Minimum DEPTH, sediment/rock: 0.20 m * Maximum DEPTH, sediment/rock: 6.00 m
Event(s):
GIK23259-2 * Latitude: 72.030000 * Longitude: 9.265000 * Date/Time: 1988-07-21T00:00:00 * Elevation: -2518.0 m * Penetration: 14.75 m * Recovery: 7.51 m * Location: Arctic Ocean * Campaign: M7/2 * Basis: Meteor (1986) * Method/Device: Piston corer (Kiel type) (KOL)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Age modelAge modelkaSarnthein, Michaelsee age model comment
CommentCommentSarnthein, Michael
Size:
50 data points

Data

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


Depth sed [m]

Age model [ka]

Comment
0.203.30deduced from mesured C14 age of 3.42 ka; after Bard et al. (1990)
0.305.92deduced from mesured C14 age of 5.56 ka; after Bard et al. (1990)
0.559.00deduced from mesured C14 age of 8.46 ka; after Bard et al. (1990)
0.6412.40deduced from C14 analog age of 10.4 ka; after Bard et al. (1990)
0.9913.45deduced from mesured C14 age of 11.92 ka; after Bard et al. (1990)
1.2014.95deduced from mesured C14 age of 13.11 ka; after Bard et al. (1990)
1.2517.10deduced from C14 analog age of 13.6 ka; after Bard et al. (1990)
1.3515.67deduced from mesured C14 age of 13.55 ka; after Bard et al. (1990)
1.4018.30deduced from C14 analog age of 14.8 ka; after Bard et al. (1990)
1.7021.22deduced from mesured C14 age of 17.72 ka; after Bard et al. (1990)
1.9021.89deduced from mesured C14 age of 18.39 ka; after Bard et al. (1990)
2.4028.09deduced from mesured C14 age of 24.59 ka; after Bard et al. (1990)
2.5329.50deduced from C14 analog age of 26.0 ka; after Bard et al. (1990)
2.7033.22deduced from mesured C14 age of 29.72 ka; after Bard et al. (1990)
2.9036.37deduced from mesured C14 age of 32.87 ka; after Bard et al. (1990)
3.0036.69deduced from mesured C14 age of 33.19 ka; after Bard et al. (1990)
3.1043.10deduced from mesured C14 age of 39.6 ka; after Bard et al. (1990)
3.8555.45d18O event 3.3; after Martinson et al. (1987)
4.0565.22d18O event 4.22; after Martinson et al. (1987)
4.3079.46d18O event 5.1; after Martinson et al. (1987)
4.70103.55d18O event 5.3; after Martinson et al. (1987)
4.80110.79d18O event 5.4; after Martinson et al. (1987)
5.20125.00d18O event 5.5; after Martinson et al. (1987)
5.80135.10d18O event 6.2; after Martinson et al. (1987)
6.00141.00d18O event 6.3; after Martinson et al. (1987)