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Shackleton, Nicholas J; Hall, Michael A (1990): Stable carbon and oxygen isotope record of planktonic foraminifera of ODP Hole 115-709C [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.755884, Supplement to: Shackleton, NJ; Hall, MA (1990): Pliocene oxygen isotope stratigraphy of Hole 709C. In: Duncan, RA; Backmann, J; Peterson, LC; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 115, 529-538, https://doi.org/10.2973/odp.proc.sr.115.174.1990

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Abstract:
A closely spaced (5-cm interval) oxygen isotope stratigraphy of planktonic foraminifers from Hole 709C was completed for most of the Pliocene and lowermost Pleistocene (around 4.6-1.4 Ma). This will contribute data to the future testing of the Matthews and Poore model of 1980, in which it was assumed that low-latitude sea-surface temperature has remained virtually constant as global climate evolved.
Spectral analyses of the record by means of biostratigraphic time controls show a distinct peak at a period near 40 ka that is probably associated with the orbital obliquity cycle. Visual inspection of the record shows that intervals containing distinct 40-ka cycles are present in both lower and upper parts of the Pliocene even though a regular cycle cannot be followed throughout the entire 4-m.y. investigated.
Project(s):
Coverage:
Latitude: -3.915000 * Longitude: 60.551670
Date/Time Start: 1987-05-07T04:00:00 * Date/Time End: 1987-06-08T17:00:00
Event(s):
115-709C * Latitude: -3.915000 * Longitude: 60.551670 * Date/Time Start: 1987-05-07T04:00:00 * Date/Time End: 1987-06-08T17:00:00 * Elevation: -3039.0 m * Penetration: 353.7 m * Recovery: 330.03 m * Location: South Indian Ridge, South Indian Ocean * Campaign: Leg115 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 37 cores; 353.7 m cored; 0 m drilled; 93.3 % recovery
Size:
2 datasets

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