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Resig, Johanna M; Kroopnick, Peter M (1983): Stable isotope ratios of benthic and planktonic foraminifera from Miocene to Pliocene sediments of DSDP Hole 7-62A on the Eauripik Rise, Pacific Ocean (Table 1) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.682292, Supplement to: Resig, JM; Kroopnick, PM (1983): Isotopic and distributional evidence of a planktonic habitat for the foraminiferal genus Streptochilus Brönnimann and Resig, 1971. Marine Micropaleontology, 8(3), 235-248, https://doi.org/10.1016/0377-8398(83)90026-9

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Abstract:
Oxygen and carbon isotope analyses show that the biserial forarniniferal genus Streptochilus, which was originally described from pelagic sediments on the Eauripik Rise and Ontong Java Plateau, lived deep in the upper water column within the oxygen minimum layer. The species of Streptochilus average from 4 to 19% of the foraminiferal assemblages in which benthic forms compose less than 1 or 2%. Specimens of Streptochilus are selectively dissolved when in contact with the bottom water mass. Their rapid evolutionary turnover of less than a few million years and their wide areal distribution in the equatorial Indo-Pacific are indicative of planktonic foraminifera. Aside from usefulness of the species of Streptochilus as stratigraphic indices, these Neogene biserial planktonic foraminifera are potential indices of paleoceanographic stratification.
Project(s):
Coverage:
Latitude: 1.870000 * Longitude: 141.938300
Date/Time Start: 1969-08-15T00:00:00 * Date/Time End: 1969-08-15T00:00:00
Minimum DEPTH, sediment/rock: 102.1 m * Maximum DEPTH, sediment/rock: 264.1 m
Event(s):
7-62A * Latitude: 1.870000 * Longitude: 141.938300 * Date/Time: 1969-08-15T00:00:00 * Elevation: -2607.0 m * Penetration: 364 m * Recovery: 303.3 m * Location: North Pacific/RIDGE * Campaign: Leg7 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 38 cores; 337 m cored; 0 m drilled; 90 % recovery
Comment:
Ages are approximated, Temperature calculation: T (∞C) = 16.5-4.3 * (deltaO18 O3) + 1.4 * (deltaO18 O3)**2, based on the revised paleotemperature equation of Epstein et al. (1953)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmGeocode
2AGEAgeka BPGeocode
3Sample code/labelSample labelResig, Johanna MDSDP/ODP/IODP sample designation
4EpochEpochResig, Johanna M
5Planktic foraminifera zonePlank foram zoneResig, Johanna M
6Globigerinoides sacculifer, δ13CG. sacculifer δ13C‰ PDBResig, Johanna MIsotope ratio mass spectrometry
7Globigerinoides sacculifer, δ18OG. sacculifer δ18O‰ PDBResig, Johanna MIsotope ratio mass spectrometry
8Temperature, calculatedT cal°CResig, Johanna MCalculated from stable oxygen isotopesIsotopic T, Globigerinoides sacculifer
9Globorotalia tumida, δ13CG. tumida δ13C‰ PDBResig, Johanna MIsotope ratio mass spectrometry
10Globorotalia tumida, δ18OG. tumida δ18O‰ PDBResig, Johanna MIsotope ratio mass spectrometry
11Temperature, calculatedT cal°CResig, Johanna MCalculated from stable oxygen isotopesIsotopic T, Globorotalia tumida
12Streptochilus globulosum, δ13CS. globulosum δ13C‰ PDBResig, Johanna MIsotope ratio mass spectrometry
13Streptochilus globulosum, δ18OS. globulosum δ18O‰ PDBResig, Johanna MIsotope ratio mass spectrometry
14Temperature, calculatedT cal°CResig, Johanna MCalculated from stable oxygen isotopesIsotopic T, Streptochilus globulosum
15Foraminifera, benthic δ13CForam benth δ13C‰ PDBResig, Johanna MIsotope ratio mass spectrometry
16Foraminifera, benthic δ18OForam benth δ18O‰ PDBResig, Johanna MIsotope ratio mass spectrometry
17Temperature, calculatedT cal°CResig, Johanna MCalculated from stable oxygen isotopesIsotopic T, benthic foraminifera
18Siphouvigerina sp., δ13CSiphouvigerina sp. δ13C‰ PDBResig, Johanna MIsotope ratio mass spectrometry
19Siphouvigerina sp., δ18OSiphouvigerina sp. δ18O‰ PDBResig, Johanna MIsotope ratio mass spectrometry
20Temperature, calculatedT cal°CResig, Johanna MCalculated from stable oxygen isotopesIsotopic T, Siphouvigerina sp.
21Uvigerina spp., δ13CUvigerina spp. δ13C‰ PDBResig, Johanna MIsotope ratio mass spectrometry
22Uvigerina spp., δ18OUvigerina spp. δ18O‰ PDBResig, Johanna MIsotope ratio mass spectrometry
23Temperature, calculatedT cal°CResig, Johanna MCalculated from stable oxygen isotopesIsotopic T, Uvigerina spp.
Size:
39 data points

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