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Bühring, Christian (2001): Age model and sedimentation rates of sediment core GIK17940-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.113007, In supplement to: Bühring, C (2001): East Asian Monsoon variability on orbital- and millennial-to-sub-decadal time scales. PhD Thesis, Mathematisch-Naturwissenschaftliche Fakultät der Christian-Albrechts-Universität zu Kiel, Germany, 164 pp, urn:nbn:de:gbv:8-diss-5231

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Coverage:
Latitude: 20.116667 * Longitude: 117.383333
Date/Time Start: 1994-05-05T00:00:00 * Date/Time End: 1994-05-05T00:00:00
Minimum Elevation: -1727.0 m * Maximum Elevation: -1727.0 m
Event(s):
GIK17940-2 * Latitude: 20.116667 * Longitude: 117.383333 * Date/Time: 1994-05-05T00:00:00 * Elevation: -1727.0 m * Location: South China Sea * Campaign: SO95 (MONITOR MONSUN) * Basis: Sonne * Method/Device: Gravity corer (Kiel type) (SL)
Comment:
14C ages (Wang et al. 1999a) recal see comment; Different from Wang et al. (1999a): ignored avrg of multiple AMS-14C dat., but considers younger ages; in some cases model relies on ages with a min sum 1 error
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
Depth, compositeDepth compmcdSarnthein, MichaelIntercore correlation
Age modelAge modelkaSarnthein, MichaelAge model, lithological correlationusing CALIB 4.1 program with assumed general reservoir age of 402 yrs (Stuiver et al., 1998)
Age, errorAge e±Sarnthein, Michaelcal age BP with 1 error
Sedimentation rateSRcm/kaSarnthein, MichaelCalculated, see reference(s)
Size:
204 data points

Data

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


Depth comp [mcd]

Age model [ka]

Age e [±]

SR [cm/ka]
0.0000.0000.00548
0.4750.9470.04048
0.4750.9470.04050
1.0152.0300.11350
1.0152.0300.11350
1.1452.2910.06250
1.1452.2910.06260
1.5853.0220.11160
1.5853.0220.11138
1.7453.4400.06738
1.7453.4400.06752
2.3254.5520.18152
2.3254.5520.18158
2.6055.0350.08758
2.6055.0350.08750
3.3456.5220.13550
3.3456.5220.13552
4.3058.3610.07752
4.3058.3610.07761
5.0659.6090.37761
5.0659.6090.37785
6.21510.9670.23885
6.21510.9670.23876
6.50511.3480.51976
6.50511.3480.51924
6.56511.6000.05024
6.56511.6000.05039
7.22513.2800.11039
7.22513.2800.11039
7.92515.0900.14039
7.92515.0900.14021
8.42517.4600.15421
8.42517.4600.15450
8.52517.6600.16150
8.52517.6600.16130
8.92519.0100.19030
8.92519.0100.19020
9.12519.9900.22020
9.12519.9900.22013
9.22520.7600.22013
9.22520.7600.22013
9.32521.5500.14013
9.32521.5500.14015
10.32528.0100.59015
10.32528.0100.59035
11.02530.0000.59035
11.02530.0000.59026
12.12534.3001.10026
12.12534.3001.10013
12.72539.0002.40013
12.72539.0002.40033