Collins, Eric S. et al. (1996): Tithonian benthic foraminifers from Hole 901A

Leg/Site/Hole:
ODP 149
ODP 149 901
Identifier:
2007-088088
georefid

10.2973/odp.proc.sr.149.253.1996
doi

Creator:
Collins, Eric S.
Dalhousie University, Centre for Marine Geology, Halifax, NS, Canada
author

Kuhnt, Wolfgang
Rice University, United States
author

Scott, David B.
Ocean Drilling Program, United States
author

Identification:
Tithonian benthic foraminifers from Hole 901A
1996
In: Whitmarsh, Robert B., Sawyer, Dale S., Klaus, Adam, Beslier, Marie-Odile, Collins, Eric S., Comas, Maria Carmen, Cornen, Guy, de Kaenel, Eric, Pinheiro, Luis de Menezes, Gervais, Elisabeth, Gibson, Ian L., Harry, Dennis L., Hobart, Michael A., Kanamatsu, Toshiya, Krawcyzk, Charlotte M., Liu, Li, Lofts, Jeremy C., Marsaglia, Kathleen M., Meyers, Philip A., Milkert, Doris, Milliken, Kitty L., Morgan, Julia K., Ramirez, Pedro, Seifert, Karl E., Shaw, Timothy J., Wilson, Chris, Yin, Chuan, Zhao, Xixi, Proceedings of the Ocean Drilling Program; scientific results, Iberia abyssal plain; covering Leg 149 of the cruises of the Drilling Vessel JOIDES Resolution; Balboa Harbor, Panama, to Lisbon, Portugal; sites 897-901, 10 March-25 May 1993
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
149
193-201
Dark gray laminated silty claystones (Unit II) drilled at Site 901 contain Tithonian benthic foraminifer assemblages that indicate a neritic depositional environment and probably dysaerobic bottom-water conditions. Three benthic foraminifer zones are distinguished within Unit II. The upper part of the unit is dominated by Spirillina polygyrata, contains Globospirillina spp. (Samples 149-901A-3R-1, 10-12 cm, to 149-901A-3R-1, 75-77 cm) and is interpreted as late Tithonian. Samples 149-901A-3R-1, 87-89 cm, to 149-901A-6R-1, 74-76 cm, contain Epistomina uhligi and Lingulina franconica and are probably early Tithonian. The early Tithonian Neobulimina atlantica Zone is characterized by the occurrence of the zonal marker and Epistomina uhligi and reaches from Sample 149-901A-6R-1, 128-130 cm, to the base of the drilled-sequence. The sediments and benthic foraminiferal assemblage characteristics of the Tithonian-aged sequence in Hole 901A are unknown elsewhere in the Atlantic and may represent deposition in a marginal shelf basin with increased terrigenous and organic flux.
Coverage:Geographic coordinates:
North:40.4029
West:-11.0335East: -11.0335
South:40.4029

Stratigraphy; assemblages; Atlantic Ocean; benthic taxa; biostratigraphy; clastic rocks; Europe; Foraminifera; Iberian abyssal plain; Iberian Peninsula; Invertebrata; Jurassic; Leg 149; lithofacies; Mesozoic; microfossils; North Atlantic; Northeast Atlantic; Ocean Drilling Program; ODP Site 901; Portlandian; Protista; sedimentary rocks; siltstone; Southern Europe; Tithonian; Upper Jurassic;

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