Bauch, Henning A (2002): Sedimentation rate of sediment core GIK23059-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.82388
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Related to:
Bauch, Henning A (1993): Planktische Foraminiferen im Europäischen Nordmeer - ihre Bedeutung fuer die paläoozeanograpische Interpretation waehrend der letzten 600.000 Jahre. Berichte aus dem Sonderforschungsbereich 313, Christian-Albrechts-Universität, Kiel, 40, 108 pp, https://doi.org/10.2312/reports-sfb313.1993.40
Project(s):
Coverage:
Latitude: 70.305000 * Longitude: -3.121667
Date/Time Start: 1986-07-06T00:00:00 * Date/Time End: 1986-07-06T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.70 m
Event(s):
GIK23059-2 * Latitude: 70.305000 * Longitude: -3.121667 * Date/Time: 1986-07-06T00:00:00 * Elevation: -2283.0 m * Location: Norwegian Sea * Campaign: M2/2 * Basis: Meteor (1986) * Method/Device: Giant box corer (GKG)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | AGE | Age | ka BP | Geocode | ||
| 3 | Depth, composite | Depth comp | mcd | Bauch, Henning A | Intercore correlation | |
| 4 | Sedimentation rate | SR | cm/ka | Bauch, Henning A | Calculated, see reference(s) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
46 data points
Data
| 1 Depth sed [m] | 2 Age [ka BP] | 3 Depth comp [mcd] | 4 SR [cm/ka] |
|---|---|---|---|
| 0.01 | 2.869 | 0.01 | 2.55 |
| 0.02 | 3.261 | 0.02 | 2.55 |
| 0.03 | 3.654 | 0.03 | 2.55 |
| 0.04 | 4.046 | 0.04 | 2.55 |
| 0.05 | 4.438 | 0.05 | 2.55 |
| 0.06 | 4.831 | 0.06 | 2.55 |
| 0.08 | 5.615 | 0.08 | 2.55 |
| 0.10 | 0.640 | 0.10 | 1.47 |
| 0.12 | 7.760 | 0.12 | 1.47 |
| 0.14 | 9.120 | 0.14 | 7.43 |
| 0.16 | 9.389 | 0.16 | 7.43 |
| 0.18 | 9.658 | 0.18 | 7.43 |
| 0.20 | 9.927 | 0.20 | 7.43 |
| 0.22 | 10.196 | 0.22 | 7.43 |
| 0.24 | 10.465 | 0.24 | 7.43 |
| 0.25 | 10.600 | 0.25 | 1.00 |
| 0.26 | 11.600 | 0.26 | 1.00 |
| 0.28 | 13.600 | 0.28 | 3.08 |
| 0.30 | 14.250 | 0.30 | 3.08 |
| 0.32 | 14.900 | 0.32 | 3.14 |
| 0.34 | 15.537 | 0.34 | 3.14 |
| 0.35 | 15.855 | 0.35 | 3.14 |
| 0.70 | 27.000 | 0.70 | 3.14 |