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McIntyre, Andrew; Imbrie, John D (1997): Stable isotopes of sediment core V22-174 (specmap.006) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52121

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Related to:
Imbrie, John D; Hays, James D; Martinson, Douglas G; McIntyre, Andrew; Mix, Alan C; Morley, Joseph J; Pisias, Nicklas G; Prell, Warren L; Shackleton, Nicholas J (1984): The orbital theory of Pleistocene climate: support from a revised chronology of the marine d18O record. In: Berger, A L, et al. (eds.), Milankovitch and Climate. 1: Dordrecht (D. Reidel Publishing Company), 269-305, hdl:10013/epic.48655.d001
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
Coverage:
Latitude: -10.070000 * Longitude: -12.820000
Date/Time Start: 1966-05-13T00:00:00 * Date/Time End: 1966-05-13T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 15.50 m
Event(s):
V22-174 * Latitude: -10.070000 * Longitude: -12.820000 * Date/Time: 1966-05-13T00:00:00 * Elevation: -2630.0 m * Recovery: 15.66 m * Campaign: V22 * Basis: Vema * Method/Device: Piston corer (PC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2Globigerinoides sacculifer, δ18OG. sacculifer δ18O‰ PDBImbrie, John DIsotope ratio mass spectrometry
Size:
164 data points

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