Stant, S. Audra et al. (2004): Quaternary nannofossil biostratigraphy from Ocean Drilling Program Leg 189, Tasmanian Gateway

Leg/Site/Hole:
ODP 189
Identifier:
2005-011452
georefid

10.2973/odp.proc.sr.189.109.2004
doi

Creator:
Stant, S. Audra
Florida State University, Department of Geological Sciences, Tallahassee, FL, United States
author

Lara, Jonathan
University of California at Santa Barbara, United States
author

Roessig, Kristeen L. McGonigal
Ocean Drilling Program, United States
author

Ladner, Bryan C.
Utrecht University, Netherlands
author

Identification:
Quaternary nannofossil biostratigraphy from Ocean Drilling Program Leg 189, Tasmanian Gateway
2004
In: Exon, Neville F., Kennett, James P., Malone, Mitchell J., Brinkhuis, Henk, Chaproniere, George C. H., Ennyu, Atsuhito, Fothergill, Patrick, Fuller, Michael D., Grauert, Marianne, Hill, Peter J., Janecek, Thomas R., Kelly, Daniel C., Latimer, Jennifer C., Nees, Stefan, Ninnemann, Ulysses S., Nuernberg, Dirk, Pekar, Stephen F., Pellaton, Caroline C., Pfuhl, Helen A., Robert, Christian M., Roessig, Kristeen L. McGonigal, Roehl, Ursula, Schellenberg, Stephen A., Shevenell, Amelia E., Stickley, Catherine E., Suzuki, Noritoshi, Touchard, Yannick, Wei, Wuchang, White, Timothy S., Proceedings of the Ocean Drilling Program; scientific results; the Tasmanian gateway; Cenozoic climatic and oceanographic development; covering Leg 189 of the cruises of the drilling vessel JOIDES Resolution; Hobart, Tasmania, to Sydney, Australia; Sites 1168-1172; 11 March-6 May 2000
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
189
Quaternary sediments were recovered at all five sites drilled during Ocean Drilling Program (ODP) Leg 189 in the Tasmanian Gateway. Two of these sites lie north of the present-day Subtropical Front (STF), and three sites lie south of the STF. Quaternary sediments recovered at Sites 1168, 1170, 1171, and 1172 were studied in detail to determine the calcareous nannofossil biostratigraphy and construct an age model for these sediments. The Pliocene/Pleistocene boundary was identified by the last occurrence (LO) of Discoaster brouweri at Site 1172 and approximated by the LO of Calcidiscus macintyrei at the other sites because of a lack of discoasterids. A hiatus encompassing the entire Helicosphaera sellii Zone was tentatively identified at Sites 1168 and 1172 by the coincident LOs of C. macintyrei and H. sellii. Similar hiatuses have been noted at ODP Site 1127 on the Great Australian Bight, Deep Sea Drilling Project Site 282 off the Tasman subcontinent, and ODP Site 1165 in Prydz Bay, Antarctica.
English
Coverage:Geographic coordinates:
North:-42.3000
West:144.0000East: 150.0000
South:-48.3000

Quaternary geology; algae; biostratigraphy; biozones; Cenozoic; cores; correlation; gateways; Indian Ocean; Leg 189; marine environment; microfossils; models; nannofossils; Ocean Drilling Program; Pacific Ocean; paleo-oceanography; paleoecology; paleoenvironment; Plantae; Pleistocene; Quaternary; sedimentation; sedimentation rates; South Pacific; Southwest Pacific; species diversity; Tasman Sea; West Pacific;

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