McIntyre, Andrew (2000): Age model for sediment core V25-56 (specmap.028) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.56374
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Imbrie, John D; McIntyre, Andrew; Mix, Alan C (1989): Oceanic response to orbital forcing in the late Quaternary: observational and experimental strategies. In: Berger, A; Schneider, S H & Duplessy, J C (eds.), Climate and Geosciences, A Challenge for Science and Society in the 21th Century. Boston (Kluwer Academic), 121-164, https://doi.org/10.1007/978-94-009-2446-8_7
McIntyre, Andrew; Ruddiman, William F; Karlin, K; Mix, Alan C (1989): Surface water response of the Equatorial Atlantic Ocean to orbital forcing. Paleoceanography, 4(1), 19-55, https://doi.org/10.1029/PA004i001p00019
Further details:
Duffy, A; Imbrie, John D (1989): Summary of Specmap archive No. 1. Spectral Mapping Project (Mapping Species Variability in Global Climate) (SPECMAP), hdl:10013/epic.32169.d001
Project(s):
Coverage:
Latitude: -3.550000 * Longitude: -35.230000
Date/Time Start: 1968-02-24T00:00:00 * Date/Time End: 1968-02-24T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 7.300 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 | SPECMAP |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
30 data points
Data
1 Depth sed [m] | 2 Age model [ka] |
---|---|
0.000 | 0.00 |
0.015 | 2.75 |
0.270 | 8.45 |
0.475 | 11.54 |
0.635 | 14.33 |
0.700 | 19.00 |
1.470 | 24.00 |
1.600 | 28.00 |
2.100 | 37.00 |
2.550 | 53.00 |
2.610 | 59.00 |
2.650 | 65.00 |
3.150 | 71.00 |
3.350 | 80.00 |
3.700 | 87.00 |
4.450 | 107.00 |
4.950 | 122.00 |
5.225 | 128.00 |
5.300 | 135.00 |
5.600 | 146.00 |
5.750 | 151.00 |
6.350 | 183.00 |
6.500 | 187.30 |
6.575 | 194.00 |
6.650 | 205.00 |
6.775 | 216.00 |
6.875 | 228.00 |
7.050 | 238.00 |
7.200 | 249.00 |
7.300 | 256.30 |