Iwai, Masao et al. (2002): Calcareous nannofossils, pollen, and spores from Leg 178 Sites 1095, 1097, 1100, and 1103, western Antarctic Peninsula; age constraints and environmental implications

Leg/Site/Hole:
ODP 178
ODP 178 1095
ODP 178 1097
ODP 178 1100
ODP 178 1103
Identifier:
2003-022423
georefid

10.2973/odp.proc.sr.178.227.2001
doi

Creator:
Iwai, Masao
Kochi University, Department of Geology, Kochi, Japan
author

Kameo, K.
Istituto Nazionale di Oceanografia e di Geofisica Sperimentale, Italy
author

Miyake, N.
Ocean Drilling Program, United States
author

Identification:
Calcareous nannofossils, pollen, and spores from Leg 178 Sites 1095, 1097, 1100, and 1103, western Antarctic Peninsula; age constraints and environmental implications
2002
In: Baker, Peter F. (editor), Camerlenghi, Angelo (editor), Acton, Gary D. (editor), Brachfeld, Stefanie A., Cowan, Ellen A., Daniels, James, Domack, Eugene W., Escutia, Carlota, Evans, Andrew J., Eyles, Nicholas, Guyodo, Yohan J. B., Hatfield, Kate L., Iorio, Marina, Iwai, Masao, Kyte, Frank T., Lauer, Christine, Maldonado, Andres, Moerz, Tobias, Osterman, Lisa E., Pudsey, Carol J., Schuffert, Jeffrey D., Sjunneskog, Charlotte M., Weinheimer, Amy L., Williams, Trevor, Winter, Diane M., Wolf-Welling, Thomas C. W., Ramsay, Anthony T. S. (editor), Proceedings of the Ocean Drilling Program, scientific results, Antarctic glacial history and sea-level change; covering Leg 178 of the cruises of the drilling vessel JOIDES Resolution; Punta Arenas, Chile, to Cape Town, South Africa; sites 1095-1103; 5 February-9 April 1998
Texas A&M University, Ocean Drilling Program, College Station, TX, United States
178
Calcareous nannofossils, pollen, and spores were examined on samples from Ocean Drilling Program Leg 178 Site 1095 on the continental rise and Sites 1097, 1100, and 1103 on the outer continental shelf of the western Antarctic Peninsula. Stratigraphically useful specimens of calcareous nannofossils occur in Site 1095 sediments assigned to Zones CN15, CN13b, and CN11. Calcareous nannofossils are rare but occur throughout the sedimentary sequences from seismic Units S1 to S3 on the continental shelf. Most of the calcareous nannofossils in Units S1 and S2 are composed of Cretaceous specimens that have been recycled by glacial processes. The occurrence of Dictyococcites in samples within Unit S3 upper Miocene sediments without any reworked specimens suggests those sediments are deposited in an open-ocean environment. These results are consistent with those from foraminifer and radiolarian studies. Pollen and spores including Nothofagidites, the genus for fossil pollen referred to as Nothofagus, are also observed in Unit S3 sediments. The sparse occurrence of pollen and spores, however, makes it difficult to assess the nature of the Antarctic terrestrial vegetation.
Coverage:Geographic coordinates:
North:-63.2300
West:-78.2916East: -65.2755
South:-66.5900

Stratigraphy; algae; Angiospermae; Antarctic Ocean; Antarctic Peninsula; Antarctica; biostratigraphy; continental rise; continental shelf; cores; Cretaceous; Dicotyledoneae; Dictyocha; Invertebrata; Leg 178; Mesozoic; microfossils; miospores; nannofossils; Nothofagus; Ocean Drilling Program; ocean floors; ODP Site 1095; ODP Site 1097; ODP Site 1100; ODP Site 1103; paleoenvironment; palynomorphs; Plantae; pollen; Protista; Silicoflagellata; species diversity; Spermatophyta;

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