Schulz, Hartmut (1995): Age model of sediment core SO90-93KL [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.58692, In supplement to: Schulz, H (1995): Meeresoberflächentemperaturen vor 10.000 Jahren - Auswirkungen des frühholozänen Insolationsmaximums = Sea-surface temperatures 10,000 years B.P. - consequences of the early Holocene insolation maximum. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 73, 156 pp, https://doi.org/10.2312/reports-gpi.1995.73
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Schulz, Hartmut; von Rad, Ulrich; Erlenkeuser, Helmut (1998): Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years. Nature, 393(6680), 54-57, https://doi.org/10.1038/31750
Coverage:
Latitude: 23.588000 * Longitude: 64.216000
Date/Time Start: 1993-09-16T00:00:00 * Date/Time End: 1993-09-16T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 7.48 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Age model | Age model | ka | Schulz, Hartmut | Age model, SPECMAP chronology, Imbrie et al. (1984) | calendar kyr |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
50 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 1.00 |
| 0.58 | 9.70 |
| 0.70 | 11.45 |
| 0.76 | 12.60 |
| 0.82 | 12.90 |
| 0.98 | 14.50 |
| 1.24 | 16.10 |
| 1.38 | 17.20 |
| 1.59 | 19.20 |
| 2.21 | 23.30 |
| 2.33 | 24.00 |
| 2.41 | 24.70 |
| 2.51 | 25.50 |
| 2.77 | 27.70 |
| 2.89 | 28.90 |
| 3.03 | 30.10 |
| 3.11 | 30.69 |
| 3.29 | 32.10 |
| 3.37 | 33.50 |
| 3.51 | 35.10 |
| 3.68 | 38.20 |
| 3.82 | 39.30 |
| 3.94 | 40.10 |
| 4.02 | 41.10 |
| 4.16 | 42.50 |
| 4.30 | 43.30 |
| 4.36 | 45.30 |
| 4.52 | 45.90 |
| 4.61 | 46.90 |
| 4.79 | 51.60 |
| 4.97 | 53.50 |
| 5.11 | 56.20 |
| 5.23 | 57.50 |
| 5.33 | 60.80 |
| 5.39 | 61.90 |
| 5.73 | 65.70 |
| 5.87 | 66.00 |
| 6.15 | 68.40 |
| 6.21 | 69.40 |
| 6.31 | 72.80 |
| 6.37 | 73.60 |
| 6.45 | 75.60 |
| 6.59 | 83.60 |
| 6.72 | 86.50 |
| 6.90 | 89.20 |
| 7.02 | 92.00 |
| 7.18 | 100.30 |
| 7.30 | 102.80 |
| 7.36 | 105.20 |
| 7.48 | 109.00 |