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Medina-Elizalde, Martín; Lea, David W (2005): (Table S1) Age model of ODP Hole 130-806B. 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):
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 * 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):
#NameShort NameUnitPrincipal InvestigatorMethodComment
1DEPTH, sediment/rockDepthmGeocode
2Depth, reconstructedReconstr depthmMedina-Elizalde, Martínadjusted meters below seafloor
3Age modelAge modelkaMedina-Elizalde, MartínAge model, stable isotope stratigraphy
Size:
36 data points

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