Medina-Elizalde, Martín; Lea, David W (2005): (Table S1) Age model of ODP Hole 130-806B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.772013, In supplement to: Medina-Elizalde, M; Lea, DW (2005): The Mid-Pleistocene Transition in the Tropical Pacific. Science, 310(5750), 1009-1012, https://doi.org/10.1126/science.1115933
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 0.318500 * Longitude: 159.361000
Date/Time Start: 1990-02-18T21:00:00 * Date/Time End: 1990-02-23T01:30:00
Minimum DEPTH, sediment/rock: 9.52 m * Maximum DEPTH, sediment/rock: 27.77 m
Event(s):
130-806B * Latitude: 0.318500 * Longitude: 159.361000 * Date/Time Start: 1990-02-18T21:00:00 * Date/Time End: 1990-02-23T01:30:00 * Elevation: -2519.9 m * Penetration: 743.1 m * Recovery: 666.36 m * Location: North Pacific Ocean * Campaign: Leg130 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 78 cores; 743.1 m cored; 0 m drilled; 89.7 % recovery
Comment:
Sediment depth is the official ODP depth (mbsf). Coring gaps between 16.17 and 16.02 mbsf, and between 25.72 and 25.52 mbsf. Based on visual alignment to the ODP Hole 677 benthic foraminiferal d18O (Shackleton et al., 1990). Coring gaps refer to losses due to sediment expansion (Berger et al., 1993, doi:10.2973/odp.proc.sr.130.023.1993) and sampling gaps refer to gaps in sections due to sample collection for organic geochemistry, interstitial water or smear slide analyses.
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Depth, reconstructed | Reconstr depth | m | Medina-Elizalde, Martín | adjusted meters below seafloor | |
| 3 | Age model | Age model | ka | Medina-Elizalde, Martín | Age model, stable isotope stratigraphy |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
36 data points
Data
| 1 Depth sed [m] | 2 Reconstr depth [m] | 3 Age model [ka] |
|---|---|---|
| 9.52 | 9.21 | 452.00 |
| 10.57 | 10.16 | 512.00 |
| 13.77 | 13.04 | 632.00 |
| 16.17 | 15.20 | 749.50 |
| 16.02 | 16.11 | 784.50 |
| 16.62 | 16.66 | 809.02 |
| 17.77 | 17.71 | 866.95 |
| 18.87 | 18.71 | 921.95 |
| 19.02 | 18.84 | 926.15 |
| 20.32 | 20.03 | 978.15 |
| 20.52 | 20.21 | 984.15 |
| 21.67 | 21.25 | 1031.25 |
| 22.02 | 21.57 | 1044.10 |
| 22.82 | 22.30 | 1076.90 |
| 25.12 | 24.39 | 1202.80 |
| 25.72 | 24.94 | 1235.20 |
| 25.52 | 25.51 | 1258.00 |
| 27.77 | 27.56 | 1348.00 |