Quilty, Patrick G (2002): Foraminifer, epifauna and infauna abundance of ODP Hole 183-1138A and core ELT54.007-PC, Kerguelen Plateau [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.785103, Supplement to: Quilty, PG (2002): Paleoenvironmental significance of Late Cretaceous foraminifers from ODP Site 1138 samples, a dredge and Eltanin core E54-7, Kerguelen Plateau, Indian Ocean. In: Frey, FA; Coffin, MF; Wallace, PJ; Quilty, PG (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 183, 1-28, https://doi.org/10.2973/odp.proc.sr.183.003.2002
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Published: 2002 (exact date unknown) • DOI registered: 2012-07-25
Abstract:
Late Campanian and Maastrichtian benthic foraminifers are recorded from 12 samples from Ocean Drilling Program (ODP) Leg 183, Cores 183-1138A-52R through 63R (487.3-602.4 meters below seafloor), Kerguelen Plateau, Indian Ocean, and Danian benthics from one sample in the same section. The entire late Maastrichtian foraminifer fauna is noted from a dredge sample 220 km to the north. The structure of the fauna is compared with the Cenomanian-Turonian of the nearby Eltanin core E54-7. Faunas are reviewed in terms of planktonic percentage, composition, epifaunal/infaunal ratios, and dominance/diversity indices. The region was in the cool Austral Faunal Province through the Campanian-Maastrichtian and was probably warmer in the Cenomanian-Turonian. The ODP section is now 1600 meters below sea level and has subsided several hundred meters since deposition. Its fauna is dominated by epifaunal species suggesting little influence of upwelling. The dredge location has subsided little. Its fauna has a high infaunal content consistent with significant influence of upwelling near the plateau edge. The dominant benthic species remain constant through the ODP Cretaceous section, but subdominance changes, and the section is divided into three informal zones based on dominance/subdominance characteristics of the benthic fauna. Brief taxonomic comments are made on several species and some are figured.
Project(s):
Coverage:
Median Latitude: -53.617807 * Median Longitude: 77.556071 * South-bound Latitude: -55.880000 * West-bound Longitude: 75.575333 * North-bound Latitude: -51.421670 * East-bound Longitude: 81.118000
Date/Time Start: 1972-01-01T00:00:00 * Date/Time End: 1999-01-31T06:15:00
Event(s):
183-1138A * Latitude: -53.551750 * Longitude: 75.974880 * Date/Time Start: 1999-01-07T23:30:00 * Date/Time End: 1999-01-31T06:15:00 * Elevation: -1141.4 m * Penetration: 842.7 m * Recovery: 411.98 m * Location: Indian Ocean * Campaign: Leg183 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 89 cores; 842.7 m cored; 0 m drilled; 48.9 % recovery
ELT54.007-PC * Latitude: -55.880000 * Longitude: 81.118000 * Date/Time: 1972-01-01T00:00:00 * Elevation: -4142.0 m * Recovery: 5.27 m * Campaign: ELT54 * Basis: Eltanin * Method/Device: Piston corer (PC)
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
3 datasets
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Datasets listed in this publication series
- Quilty, PG (2002): (Table T2) Abundance of epifauna, infauna and cylindrical specimens of ODP Hole 183-1138A. https://doi.org/10.1594/PANGAEA.785100
- Quilty, PG (2002): (Table T1) Planktonic and benthic foraminifer abundance of ODP Hole 183-1138A. https://doi.org/10.1594/PANGAEA.785099
- Quilty, PG (2002): (Table T3) Abundance of epifauna and infauna and number of species in core ELT54.007-PC obtained during Eltanin cruise 54. https://doi.org/10.1594/PANGAEA.785102