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Saltzman, Eric S; Barron, E J (1982): Stable oxygen and carbon isotope ratios and paleotemperature reconstructions from Inoceramus in Cretaceous sediments of DSDP Sites [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.701741, Supplement to: Saltzman, ES; Barron, EJ (1982): Deep circulation in the Late Cretaceous: oxygen isotope paleotemperatures from Inoceramus remains in D.S.D.P. cores. Palaeogeography, Palaeoclimatology, Palaeoecology, 40(1-3), 167-181, https://doi.org/10.1016/0031-0182(82)90088-8

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Abstract:
Inoceramus is an epibenthic bivalve which lived in a wide variety of paleoenvironments encompassing a broad range of paleodepths. A survey of all Cretaceous sediments from Deep Sea Drilling Project legs 1-69 and 75 revealed over 500 Inoceramus specimens at twenty sites. Of these, 47 well-preserved Late Cretaceous specimens from the South Atlantic, Pacific and Indian Oceans were analyzed for oxygen and carbon isotopes. The specimens exhibit small internal isotopic variability and oxygen isotopic paleotemperatures that are consistent with a deep-sea habitat. Paleotemperatures ranging from 5 to 16°C show that Late Cretaceous oceans were significantly warmer than the present oceans. The data suggest that deep water was formed both by cooling at high latitudes and by evaporation in the subtropics.
Project(s):
Coverage:
Median Latitude: -8.175980 * Median Longitude: 35.993210 * South-bound Latitude: -29.949800 * West-bound Longitude: -30.600500 * North-bound Latitude: 33.820500 * East-bound Longitude: 178.919000
Date/Time Start: 1969-01-15T00:00:00 * Date/Time End: 1980-07-29T00:00:00
Event(s):
3-21 * Latitude: -28.585000 * Longitude: -30.597500 * Date/Time: 1969-01-15T00:00:00 * Elevation: -2113.0 m * Penetration: 130.6 m * Recovery: 72.6 m * Location: South Atlantic/CONT RISE * Campaign: Leg3 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 9 cores; 70.4 m cored; 0 m drilled; 103.1 % recovery
6-48B * Latitude: 32.408300 * Longitude: 158.021700 * Date/Time: 1969-06-30T00:00:00 * Elevation: -2619.0 m * Penetration: 72.9 m * Recovery: 210.7 m * Location: North Pacific/PLATEAU * Campaign: Leg6 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 3 cores; 21 m cored; 0 m drilled; 98.6 % recovery
22-217 * Latitude: 8.926200 * Longitude: 90.538800 * Date/Time: 1972-02-24T00:00:00 * Elevation: -3010.0 m * Penetration: 614.5 m * Recovery: 181.6 m * Location: Indian Ocean//RIDGE * Campaign: Leg22 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 35 cores; 326.5 m cored; 9.5 m drilled; 55.6 % recovery
Size:
10 datasets

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Datasets listed in this publication series

  1. Saltzman, ES; Barron, EJ (1982): (Table 1) Multiple stable isotope analyses of single Inoceramus specimens of DSDP Hole 3-21 in the South Atlantic Ocean. https://doi.org/10.1594/PANGAEA.701697
  2. Saltzman, ES; Barron, EJ (1982): (Table 2) Stable oxygen and carbon isotope ratios of Inoceramus and paleotemperture reconstruction from DSDP Hole 3-21 in the South Atlantic Ocean. https://doi.org/10.1594/PANGAEA.701709
  3. Saltzman, ES; Barron, EJ (1982): (Table 2) Stable oxygen and carbon isotope ratios of Inoceramus and paleotemperture reconstruction from DSDP Hole 6-48B in the Pacific Ocean. https://doi.org/10.1594/PANGAEA.701710
  4. Saltzman, ES; Barron, EJ (1982): (Table 2) Stable oxygen and carbon isotope ratios of Inoceramus and paleotemperture reconstruction from DSDP Hole 22-217 in the Indian Ocean. https://doi.org/10.1594/PANGAEA.701711
  5. Saltzman, ES; Barron, EJ (1982): (Table 2) Stable oxygen and carbon isotope ratios of Inoceramus and paleotemperture reconstruction from DSDP Hole 25-249 in the Indian Ocean. https://doi.org/10.1594/PANGAEA.701727
  6. Saltzman, ES; Barron, EJ (1982): (Table 1) Multiple stable isotope analyses of single Inoceramus specimens of DSDP Hole 39-355 in the South Atlantic Ocean. https://doi.org/10.1594/PANGAEA.701698
  7. Saltzman, ES; Barron, EJ (1982): (Table 2) Stable oxygen and carbon isotope ratios of Inoceramus and paleotemperture reconstruction from DSDP Hole 39-3551 in the South Atlantic Ocean. https://doi.org/10.1594/PANGAEA.701712
  8. Saltzman, ES; Barron, EJ (1982): (Table 2) Stable oxygen and carbon isotope ratios of Inoceramus and paleotemperture reconstruction from DSDP Hole 62-465A in the Pacific Ocean. https://doi.org/10.1594/PANGAEA.701713
  9. Saltzman, ES; Barron, EJ (1982): (Table 1) Multiple stable isotope analyses of single Inoceramus specimens of DSDP Hole 75-530A in the South Atlantic Ocean. https://doi.org/10.1594/PANGAEA.701699
  10. Saltzman, ES; Barron, EJ (1982): (Table 2) Stable oxygen and carbon isotope ratios of Inoceramus and paleotemperture reconstruction from DSDP Hole 75-530A in the South Atlantic Ocean. https://doi.org/10.1594/PANGAEA.701714