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  • 113-689B; 113-690C; DRILL; Drilling/drill rig; Joides Resolution; Leg113; Ocean Drilling Program; ODP; South Atlantic Ocean  (1)
  • 119-744A; AGE; Chiloguembelina cubensis, δ13C; Chiloguembelina cubensis, δ18O; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Globigerinita juvenilis, δ13C; Globigerinita juvenilis, δ18O; Globorotaloides suteri, δ13C; Globorotaloides suteri, δ18O; Indian Ocean; Joides Resolution; Leg119; Mass spectrometer VG Micromass 602; Nannofossil zone; Ocean Drilling Program; ODP; Planktic foraminifera zone; Sample code/label; Stilostomella subspinosa, δ13C; Stilostomella subspinosa, δ18O  (1)
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  • 1
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    PANGAEA
    In:  Supplement to: Barrera, Enriqueta C; Huber, Brian T (1990): Evolution of Antarctic waters during the Maestrichtian: foraminifer oxygen and carbon isotope ratios, Leg 113. In: Barker, PF; Kennett, JP; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 113, 813-827, https://doi.org/10.2973/odp.proc.sr.113.137.1990
    Publication Date: 2024-01-09
    Description: Oxygen and carbon isotopic ratios were measured from Maestrichtian benthic and planktonic foraminifer species and bulk carbonate samples from ODP Sites 689 and 690, drilled on the Maud Rise during Leg 113. Careful scanning electron microscope observations reveal that test calcite in some intervals was diagenetically altered, although Sr/Ca and isotopic ratios of these tests do not appear to have been modified significantly. Foraminifer d18O values at both sites document a cooling trend during early Maestrichtian time, a rapid drop in water temperatures at the time of the first appearance of Abathomphalus mayaroensis in the high southern latitude regions (about 69.9 Ma), and lower water temperatures during late Maestrichtian time. d13C values record a depletion in 13C in the latest early Maestrichtian time beginning at about 72.2 Ma, just prior to the sharp late Maestrichtian increase in d18O values. These trends are similar to those previously reported for well-preserved benthic foraminifer species from Seymour Island, in the Antarctic Peninsula. Paleotemperature estimates are also comparable to those at Seymour Island and suggest temperate climatic conditions in Antarctica and that bottom waters in the southern South Atlantic region were of Antarctic origin. Benthic and planktonic foraminifer 613C values fluctuate sympathetically and are higher in upper Maestrichtian sediments than in the lower Maestrichtian sequence.
    Keywords: 113-689B; 113-690C; DRILL; Drilling/drill rig; Joides Resolution; Leg113; Ocean Drilling Program; ODP; South Atlantic Ocean
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2024-01-09
    Keywords: 119-744A; AGE; Chiloguembelina cubensis, δ13C; Chiloguembelina cubensis, δ18O; Cibicidoides spp., δ13C; Cibicidoides spp., δ18O; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Globigerinita juvenilis, δ13C; Globigerinita juvenilis, δ18O; Globorotaloides suteri, δ13C; Globorotaloides suteri, δ18O; Indian Ocean; Joides Resolution; Leg119; Mass spectrometer VG Micromass 602; Nannofossil zone; Ocean Drilling Program; ODP; Planktic foraminifera zone; Sample code/label; Stilostomella subspinosa, δ13C; Stilostomella subspinosa, δ18O
    Type: Dataset
    Format: text/tab-separated-values, 687 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
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