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Shackleton, Nicholas J; Opdyke, Neil D (1997): Age model of sediment core V28-239. PANGAEA, https://doi.org/10.1594/PANGAEA.52019, In supplement to: Shackleton, NJ; Opdyke, ND (1976): Oxygen-isotope and paleomagnetic stratigraphy of Pacific core V28-239, late Plicene to latest Pleistocene. In: Cline, R M & Hays, J D (eds.), Investigations of late Quaternary paleogeography and paleoclimatology. (Geological Society of American Mem.), 145, 449-464, hdl:10013/epic.43488.d001

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Coverage:
Latitude: 3.250000 * Longitude: 159.180000
Date/Time Start: 1971-05-09T00:00:00 * Date/Time End: 1971-05-09T00:00:00
Minimum DEPTH, sediment/rock: 0.250 m * Maximum DEPTH, sediment/rock: 7.150 m
Event(s):
V28-239 * Latitude: 3.250000 * Longitude: 159.180000 * Date/Time: 1971-05-09T00:00:00 * Elevation: -3490.0 m * Recovery: 21.39 m * Campaign: V28 * Basis: Vema * Method/Device: Piston corer (PC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepthmGeocode
2Age modelAge modelkaShackleton, Nicholas JDepth in core determined by correlation with core V28-238. Ages are those estimated by Shackleton & Odyke (1973) by linear interpolation in core V28-238 using a rate of 1.7 cm/kyr. Terminations from Broecker & van Donk (1969). They defined terminatins on the basis of their interpretation of the saw-toothed character of the oxygen-isotope record. Owing to a possible hiatus in core V12-122, it appears that the event labeled termination VI by them is the stage 16-15 boundary.
Size:
18 data points

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