Hostname: page-component-cd9895bd7-dzt6s Total loading time: 0 Render date: 2024-12-25T19:20:31.633Z Has data issue: false hasContentIssue false
  • English
  • Français

Manumiella seymourensis new species, a stratigraphically significant dinoflagellate cyst from the Maastrichtian of Seymour Island, Antarctica

Published online by Cambridge University Press:  20 May 2016

Rosemary A. Askin
Rosemary A. Askin*
Affiliation:
Byrd Polar Research Center, The Ohio State University, 1090 Carmack Road, Columbus, Ohio, 43210,
Get access Rights & Permissions [Opens in a new window]

Abstract

The peridiniacean dinoflagellate cyst Manumiella seymourensis new species described herein characterizes Maastrichtian shallow marine sediments cropping out on Seymour Island, northeastern Antarctic Peninsula. It dominates palynological assemblages throughout the lower Maastrichtian (and possibly uppermost Campanian) to lower upper Maastrichtian part of the López de Bertodano Formation. Despite its superficial similarity to some other southern mid to high paleolatitude Campanian-Maastrichtian species, M. seymourensis represents a discrete, biostratigraphically useful population of peridiniacean cysts. Its morphology and size parameters remain consistent throughout almost all of its stratigraphic range, equated with relatively stable environmental conditions throughout much of the Maastrichtian in the James Ross Basin. Morphological variations, equated with environmental change, are apparent in specimens in the lowermost and uppermost parts of its range.

Type
Research Article
Information
Journal of Paleontology , Volume 73 , Issue 3 , May 1999 , pp. 373 - 379
Copyright
Copyright © The Paleontological Society 

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Askin, R. A. 1988a. Campanian to Paleocene palynological succession of Seymour and adjacent islands, northeastern Antarctic Peninsula, p. 131–153. In Feldmann, R. M. and Woodburne, M. O. (eds.), Geology and Paleontology of Seymour Island, Antarctic Peninsula. Geological Society of America Memoir, 169.Google Scholar
Askin, R. A. 1988b. The palynological record across the Cretaceous/Tertiary transition on Seymour Island, Antarctica, p. 155–162. In Feldmann, R. M. and Woodburne, M. O. (eds.), Geology and Paleontology of Seymour Island, Antarctic Peninsula. Geological Society of America Memoir, 169.Google Scholar
Askin, R. A. 1990a. Cryptogam spores from the upper Campanian and Maastrichtian of Seymour Island, Antarctica. Micropaleontology, 36:141–156.Google Scholar
Askin, R. A. 1990b. Campanian to Paleocene spore and pollen assemblages of Seymour Island, Antarctica. Review of Palaeobotany and Palynology, 65:105–113.Google Scholar
Askin, R. A. 1994. Monosulcate angiosperm pollen from the López de Bertodano Formation (upper Campanian-Maastrichtian-Danian) of Seymour Island, Antarctica. Review of Palaeobotany and Palynology, 81:151–164.Google Scholar
Askin, R. A., and Jacobson, S. R. 1996. Palynological change over the Cretaceous-Tertiary boundary on Seymour Island, Antarctica: environmental and depositional factors, p. 7–25. In MacLeod, N. and Keller, G. (eds.), Cretaceous-Tertiary Mass Extinctions: Biotic and Environmental Changes. W.W. Norton & Co., New York.Google Scholar
Askin, R. A., Elliot, D. H., Stilwell, J. D., and Zinsmeister, W. J. 1991. Stratigraphy and paleontology of Campanian and Eocene sediments, Cockburn Island, Antarctic Peninsula. South American Journal of Earth Sciences, 4:99–117.Google Scholar
Baldoni, A. M., and Barreda, V. 1986. Estudio palinológico de las formaciónes López de Bertodano y Sobral, Isla Vicecomodoro Marambio, Antártida. Boletim IG-USP, Serie Científica, Universidade de Sao Paulo, 17:89–98.Google Scholar
Barnes, R. P., and Riding, J. B. 1994. Angular unconformity between the López de Bertodano and La Meseta Formations (Campanian-Maastrichtian and Eocene), Cockburn Island, northern Antarctic Peninsula. South American Journal of Earth Sciences, 7:35–44.CrossRefGoogle Scholar
Barrera, E., and Huber, B. T. 1990. Evolution of Antarctic waters during the Maastrichtian: foraminifer oxygen and carbon isotope ratios, ODP Leg 113. Proceedings of the Ocean Drilling Program, Scientific Results, 113:813–827.Google Scholar
Barrera, E., Huber, B. T., Savin, S. M., and Webb, P. N. 1987. Antarctic marine temperatures: Late Campanian through early Paleocene. Paleoceanography, 2:21–47.Google Scholar
Bujak, J. P., and Davies, E. H. 1983. Modern and fossil Peridiniineae. American Association of Stratigraphic Palynologists Contributions Series, 13, 203 p.Google Scholar
Del Valle, R. A., Elliot, D. H., and McDonald, D. I. M. 1992. Sedimentary basins on the east flank of the Antarctic Peninsula: proposed nomenclature. Antarctic Science, 4:477–478.Google Scholar
Dettmann, M. E., and Thomson, M. R. A. 1987. Cretaceous palynomorphs from the James Ross Island area, Antarctica—a pilot study. British Antarctic Survey Bulletin, 77:13–59.Google Scholar
Downie, C., Hussain, M. A., and Williams, G. L. 1971. Dinoflagellate cysts and acritarch associations in the Paleogene of southeast England. Geosciences and Man, 3:29–35.Google Scholar
Elliot, D. H. 1988. Tectonic setting and evolution of the James Ross basin, northern Antarctic Peninsula, p. 541–555. In Feldmann, R. M. and Woodburne, M. O. (eds.), Geology and Paleontology of Seymour Island, Antarctic Peninsula. Geological Society of America Memoir, 169.Google Scholar
Elliot, D. H., Hoffman, S. M., and Rieske, D. E. 1992. Provenance of Paleocene strata, Seymour Island, p. 347–355. In Yoshida, Y. et al. (eds.), Recent Progress in Antarctic Earth Science. TERRAPUB, Tokyo.Google Scholar
Elliot, D. H., Askin, R. A., Kyte, F. T., and Zinsmeister, W. J. 1994. Iridium and dinocysts at the Cretaceous-Tertiary boundary on Seymour Island: implications for the K-T event. Geology, 22:675–678.Google Scholar
Francis, J. E. 1986. Growth rings in Cretaceous and Tertiary wood from Antarctica and their palaeoclimatic implications. Palaeontology, 29:665–684.Google Scholar
Francis, J. E. 1991. Palaeoclimatic significance of Cretaceous-early Tertiary fossil forests of the Antarctic Peninsula, p. 623–627. In Thomson, M. R. A., Crame, J. A., and Thomson, J. W., (eds.), Geological Evolution of Antarctica. Cambridge University Press, Cambridge.Google Scholar
Goodman, D. K. 1979. Dinoflagellate “communities” from the lower Eocene Nanjemoy Formation of Maryland, U.S.A. Palynology, 3:169–190.Google Scholar
Grande, L., and Chatterjee, S. 1987. New Cretaceous fish fossils from Seymour Island, Antarctic Peninsula. Palaeontology, 30:829–837.Google Scholar
Harland, R. 1973. Dinoflagellate cysts and acritarchs from the Bearpaw Formation (upper Campanian) of southern Alberta, Canada. Palaeontology, 16:665–706.Google Scholar
Harwood, D. M. 1988. Upper Cretaceous and lower Paleocene diatom and silicoflagellate biostratigraphy of Seymour Island, eastern Antarctic Peninsula, p. 55–129. In Feldmann, R. M. and Woodburne, M. O. (eds.), Geology and Paleontology of Seymour Island, Antarctic Peninsula. Geological Society of America Memoir, 169.Google Scholar
Huber, B. T. 1988. Upper Campanian-Paleocene foraminifera from the James Ross Island region, Antarctic Peninsula, p. 163–252. In Feldmann, R. M. and Woodburne, M. O. (eds.), Geology and Paleontology of Seymour Island, Antarctic Peninsula. Geological Society of America Memoir, 169.Google Scholar
Huber, B. T., and Watkins, D. K. 1992. Biogeography of Campanian-Maastrichtian calcareous plankton in the region of the Southern Ocean: Paleogeographic and Paleoclimatic implications, p. 31–60. In Kennett, J. P. and Warnke, D. A. (eds.), The Antarctic Paleoenvironment: a perspective on global change. American Geophysical Union, Antarctic Research Series, 56.Google Scholar
Huber, B. T., Harwood, D. M., and Webb, P. N. 1983. Upper Cretaceous microfossil biostratigraphy of Seymour Island, Antarctic Peninsula. Antarctic Journal of the United States, 18:72–74.Google Scholar
Keating, J. M. 1992. Palynology of the Lachman Crags Member, Santa Marta Formation (Upper Cretaceous) of north-west James Ross Island. Antarctic Science, 4:293–304.CrossRefGoogle Scholar
Kirsch, K-H. 1991. Dinoflagellatenzsten aus der Oberkreide des Helvetikums und Nordultrahelvetikums von Oberbayern. Münchner Geowissenschaftliche Abhandlungen, Geologie und Paläontologie, 22A,: 1-306.Google Scholar
Lawver, L. A., Gahagan, L. M., and Coffin, M. F. 1992. The development of paleoseaways around Antarctica, p. 7–30. In Kennett, J. P. and Warnke, D. A. (eds.), The Antarctic Paleoenvironment: a perspective on global change. American Geophysical Union, Antarctic Research Series, 56.Google Scholar
Lentin, J. K., and Manum, S. B. 1986. A new peridinioid dinoflagellate from Campanian sediments recovered from DSDP Leg 22, Site 217, Indian Ocean. Palynology, 10:111–116.Google Scholar
Macellari, C. E. 1984. Late Cretaceous stratigraphy, sedimentology, and macropaleontology of Seymour Island, Antarctic Peninsula. Unpublished Ph.D dissertation, The Ohio State University, Columbus, Ohio, 599 p.Google Scholar
Macellari, C. E. 1986. Late Campanian-Maastrichtrian ammonite fauna from Seymour Island (Antarctic Peninsula). Journal of Paleontology Memoir, 18, 55 p.Google Scholar
Macellari, C. E. 1988. Stratigraphy, sedimentology, and paleoecology of Upper Cretaceous/Paleocene shelf-deltaic sediments of Seymour Island, Antarctic Peninsula, p. 25–53. In Feldmann, R. M. and Woodburne, M. O. (eds.), Geology and Paleontology of Seymour Island, Antarctic Peninsula. Geological Society of America Memoir, 169.Google Scholar
Mao, S., and Mohr, B. A. M. 1992. Late Cretaceous dinoflagellate cysts (?Santonian-Maestrichtian) from the Southern Indian Ocean (Hole 748C), p. 307–341. In Wise, S. W. Jr., Schlich, R. et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, 120.Google Scholar
Marshall, N. G. 1990. Campanian dinoflagellates from southeastern Australia. Alcheringa, 14:1–38.Google Scholar
Palamarczuk, S., Ambrosini, G., Medina, F. A., Martinez Macchiavello, J. C., and Rinaldi, C. A. 1984. Las formaciones López de Bertodano y Sobral en la isla Vicecomodoro Marambio, Antártida. 9th Congreso Geológico Argentino Actas, 1:399–419.Google Scholar
Pirrie, D., Crame, J. A., and Riding, J. B. 1991. Late Cretaceous stratigraphy and sedimentology of Cape Lamb, Vega Island, Antarctica. Cretaceous Research, 12:227–258.Google Scholar
Pirrie, D., Crame, J. A., Riding, J. B.Lomas, S. A., and Riding, J. B. 1997. Late Cretaceous stratigraphy of the Admiralty Sound region, James Ross Basin, Antarctica. Cretaceous Research, 18:109–137.CrossRefGoogle Scholar
Rinaldi, C. A. 1982. The Upper Cretaceous in the James Ross Island Group, p. 281–286. In Craddock, C. (ed.), Antarctic Geoscience. University of Wisconsin Press, Madison.Google Scholar
Rinaldi, C. A., Massabie, A., Morelli, J., Rosenman, H. L., and Del Valle, R. 1978. Geologia de la Isla Vicecomodoro Marambio. Contribución del Instituto Antártico Argentino, 217:37 p.Google Scholar
Smith, S. W. 1992. Microplankton from the Cape Lamb Member, López de Bertodano Formation (Upper Cretaceous), Cape Lamb, Vega Island. Antarctic Science, 4:337–353.CrossRefGoogle Scholar
Stott, D. L., and Kennett, J. P. 1990. The paleoceanographic and paleoclimatic signature of the Cretaceous/Paleogene boundary in the Antarctic: stable isotope results from ODP Leg 113. Proceedings of the Ocean Drilling Program, Scientific Results, 113:829–848.Google Scholar
Tshudy, D. M., and Feldmann, R. M. 1988. Macruran decapods, and their epibionts, from the López de Bertodano Formation (Upper Cretaceous), Seymour Island, Antarctica, p. 291–302. In Feldmann, R. M. and Woodburne, M. O. (eds.), Geology and Paleontology of Seymour Island, Antarctic Peninsula. Geological Society of America Memoir, 169.Google Scholar
Wall, D. 1965. Microplankton, pollen, and spores from the Lower Jurassic in Britain. Micropaleontology, 11:151–190.Google Scholar
Wilson, G. J. 1984. Some new dinoflagellate species from the New Zealand Haumurian and Piripauan Stages (Santonian-Maastrichtian, Late Cretaceous). New Zealand Journal of Botany, 22:549–556.CrossRefGoogle Scholar
Zinsmeister, W. J., and Macellari, C. E. 1988. Bivalvia (Mollusca) from Seymour Island, Antarctic Peninsula. p. 253–284. In Feldmann, R. M. and Woodburne, M. O. (eds.), Geology and Paleontology of Seymour Island, Antarctic Peninsula. Geological Society of America Memoir, 169.Google Scholar