Imbrie, John D; McIntyre, Andrew; Mix, Alan C (1999): Age model for sediment core V30-97 (specmap.033) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.55771
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: 41.000000 * Longitude: -32.930000
Date/Time Start: 1973-05-28T00:00:00 * Date/Time End: 1973-05-28T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 9.100 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:
25 data points
Data
1 Depth sed [m] | 2 Age model [ka] |
---|---|
0.000 | 0.000 |
0.620 | 11.000 |
1.200 | 20.000 |
1.900 | 28.000 |
2.350 | 37.000 |
2.950 | 46.000 |
3.450 | 58.000 |
3.850 | 69.000 |
4.050 | 72.000 |
4.500 | 88.000 |
5.000 | 102.000 |
5.385 | 109.000 |
5.580 | 115.000 |
5.820 | 124.000 |
5.900 | 128.000 |
6.450 | 134.800 |
6.550 | 139.900 |
6.700 | 147.825 |
7.200 | 165.335 |
7.650 | 185.200 |
8.150 | 192.533 |
8.233 | 194.000 |
8.475 | 216.000 |
8.750 | 228.000 |
9.100 | 241.000 |