McClymont, Erin L; Rosell-Melé, V; Giraudeau, Jacques; Pierre, Catherine; Lloyd, Jerry M (2005): (Table 2) Age-control points used for the age extrapolation at ODP Site 175-1087 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.738372, In supplement to: McClymont, EL et al. (2005): Alkenone and coccolith records of the mid-Pleistocene in the south-east Atlantic: implications for the Uk37' index and South African climate. Quaternary Science Reviews, 24(14-15), 1559-1572, https://doi.org/10.1016/j.quascirev.2004.06.024
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -31.465083 * Longitude: 15.310889
Date/Time Start: 1997-10-03T00:00:00 * Date/Time End: 1997-10-03T00:00:00
Minimum DEPTH, sediment/rock: 12.03 m * Maximum DEPTH, sediment/rock: 50.80 m
Event(s):
175-1087 * Latitude: -31.465083 * Longitude: 15.310889 * Date/Time: 1997-10-03T00:00:00 * Elevation: -1371.6 m * Penetration: 1020.9 m * Recovery: 936.4 m * Location: Benguela Current, South Atlantic Ocean * Campaign: Leg175 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 102 cores; 948.4 m cored; 72.5 m drilled; 98.7% recovery
Comment:
Depth, sediment (m) is composite depth (mcd)
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 | McClymont, Erin L | ||
3 | Isotopic event | Isotopic event | McClymont, Erin L |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
54 data points
Data
1 Depth sed [m] | 2 Age model [ka] | 3 Isotopic event |
---|---|---|
12.03 | 406 | 11.3 |
13.00 | 423 | 12.0 |
13.90 | 478 | 13.0 |
15.25 | 528 | 14.0 |
16.20 | 615 | 15.5 |
16.52 | 628 | 16.2 |
19.28 | 718 | 18.2 |
20.25 | 754 | 18.4 |
23.08 | 793 | 20.2 |
28.18 | 871 | 22.2 |
29.33 | 919 | 24 |
31.02 | 965 | 26 |
32.43 | 1005 | 28 |
33.73 | 1044 | 30 |
35.30 | 1095 | 32 |
36.52 | 1127 | 34 |
37.25 | 1162 | 35 |
38.45 | 1203 | 36 |
38.80 | 1220 | 37 |
39.30 | 1246 | 38 |
42.90 | 1334 | 41 |
43.30 | 1346 | 42 |
44.60 | 1383 | 44 |
46.30 | 1416 | 46 |
48.00 | 1462 | 48 |
49.40 | 1505 | 50 |
50.80 | 1543 | 52 |