Hostname: page-component-78c5997874-g7gxr Total loading time: 0 Render date: 2024-11-10T20:48:03.115Z Has data issue: false hasContentIssue false
  • English
  • Français

Glacial–interglacial records from sediments in Powell Basin, Antarctica

Published online by Cambridge University Press:  19 November 2018

Young-Suk Bak ,
Kyu-Cheul Yoo ,
Jae Il Lee  and
Ho Il Yoon
Young-Suk Bak*
Affiliation:
The Earth and Environmental System Research Center, Chonbuk National University, Jeonju 54896, Korea
Kyu-Cheul Yoo
Affiliation:
Korea Polar Research Institute, 26 Songdomirae-ro, Yeonsu-gu, Incheon 21990, Korea
Jae Il Lee
Affiliation:
Korea Polar Research Institute, 26 Songdomirae-ro, Yeonsu-gu, Incheon 21990, Korea
Ho Il Yoon
Affiliation:
Korea Polar Research Institute, 26 Songdomirae-ro, Yeonsu-gu, Incheon 21990, Korea
*
sydin@jbnu.ac.kr
Get access Rights & Permissions [Opens in a new window]

Abstract

Palaeoenvironmental history is reconstructed from diatoms in two sediment cores, GC01-PW02 and GC03-PW02, recovered from Powell Basin, Antarctica. A total of 43 species belonging to 21 genera are identified from GC01-PW02. A total of 61 species belonging to 27 genera are identified from GC03-PW02. The number of diatom valves g-1 of dry sediment ranges from 0.1–48.3 × 106 valves g-1. Based on diatom abundance, six assemblage zones were identified from GC01-PW02, and five diatom zones were identified from GC03-PW02. Barren intervals represent glacial periods, while intervals with higher diatom abundances were deposited during interglacial periods and reduced sea ice cover. The occurrence of Rouxia leventerae only within the deepest zone of each of the cores indicates that the core sediments were deposited since marine isotope stage (MIS) 6.

Keywords

diatom zonesGC01-PW02GC03-PW02MIS 6
Type
Physical Sciences
Information
Antarctic Science , Volume 30 , Issue 6 , December 2018 , pp. 371 - 378
Copyright
© Antarctic Science Ltd 2018 

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

Abelmann, A. & Gersonde, R. 1991. Biosiliceous particle flux in the Southern Ocean. Marine Chemistry, 35, 503–536.Google Scholar
Armand, L.K., Crosta, X., Romero, O. & Pichon, J.-J. 2005. The biogeography of major diatom taxa in Southern Ocean sediments: 1. Sea-ice related species. Palaeogeography, Palaeoclimatology, Palaeoecology, 223, 93–126.Google Scholar
Barbara, L., Crosta, X., Masse, G. & Ther, O. 2010. Deglacial environments in eastern Prydz Bay, East Antarctica. Quaternary Science Reviews, 29, 2731–2740.Google Scholar
Bak, Y.S. & Lee, Y.U. 2017. Late Quaternary Paleoclimatic change in the Ulleung Basin, East Sea, Korea. Acta Geologica Sinica, 91, 263–269.Google Scholar
Bart, P.J., Sjunneskog, C. & Chow, J.M. 2011. Piston-core based biostratigraphic constrains on Pleistocene oscillations of the West Antarctic Ice Sheet in western Ross Sea between North Basin and AND-1B drill site. Marine Geology, 289, 86–99.Google Scholar
Carstens, J. & Wefer, G. 1992. Recent distribution of planktonic foraminifera in the Nansen Basin Arctic Ocean. Deep-Sea Research A - Oceanographic Research Papers, 39, 507–524.Google Scholar
Cody, R.D., Levy, R.H., Harwood, D.M. & Sadler, P.M. 2008. Thinking outside the zone: high-resolution quantitative biochronology for the Antarctic Neogene. Palaeogeography Palaeoclimatology Palaeoecology, 260, 92–121.Google Scholar
Crosta, X., Romero, O., Armand, L.K. & Pichon, J.-J. 2005. The biogeography of major diatom taxa in Southern Ocean sediments: 2. Open-ocean related species. Palaeogeography, Palaeoclimatology, Palaeoecology, 223, 66–92.Google Scholar
Dinniman, M.S. & Klinck, J.M. 2004. A model study of circulation and cross-shelf exchange on the west Antarctic Peninsula continental shelf. Deep-Sea Research II, 51, 2003–2022.Google Scholar
Dinniman, M.S., Klinck, J.M. & Smith, W.O. Jr. 2011. A model study of Circumpolar Deep Water on the west Antarctic peninsula and Ross Sea continental shelves. Deep-Sea Research II, 58, 1508–1523.Google Scholar
Garrison, D.L. 1991. Antarctic sea ice biota. American Zoologist, 31, 17–33.Google Scholar
Gersonde, R. 1984. Siliceous microorganisms in sea ice and their record in sediments in the southern Weddell Sea (Antarctica). In Ricard, M., ed. Proceedings of the 8th diatom symposium. Koenigstein: Koeltz Scientific Books, 549–566.Google Scholar
Gersonde, R. & Zielinski, U. 2000. The reconstruction of late Quaternary Antarctic sea-ice distribution - the use of diatoms as a proxy for sea ice. Palaeogeography, Palaeoclimatology, Palaeoecology, 162, 263–286.Google Scholar
Horner, R. 1985. Sea ice biota. Boca Raton, FL: CRC Press, 215 pp.Google Scholar
King, E.C. & Barker, P.F. 1988. The margins of the South Orkney microcontinent. Journal of Geological Society of London, 145, 317–331.Google Scholar
Leventer, A. & Dunbar, R. 1996. Factors influencing the distribution of diatoms and other algae in the Ross Sea. Journal of Geophysical Research - Oceans, 101, 18 489–18 500.Google Scholar
Maddison, E.J., Pike, J. & Leventer, A. 2006. Post-glacial seasonal diatom record of the Mertz Glacier Polynya, East Antarctica. Marine Micropaleontology, 60, 66–88.Google Scholar
Maddison, E.J., Pike, J., Leventer, A. & Domack, E.W. 2005. Deglacial seasonal and sub-seasonal diatom record from Palmer Deep, Antarctica. Journal of Quaternary Science, 20, 435–446.Google Scholar
Naval Oceanography Command Detachment. 1985. Sea ice climatic atlas. Vol. 1: Antarctic. NSTL MS 39529-500, NAVAIR 50-1C-540, ADA-168716. Asheville, NC: Naval Oceanography Command Detachment, 131 pp.Google Scholar
Ninnemann, U.S. & Charles, C.D. 2002. Changes in the mode of Southern Ocean circulation over the last glacial cycle revealed by foraminiferal stable isotopic variability. Earth and Planetary Science Letters, 6260, 1–14.Google Scholar
Prézelin, B.B., Hofmann, E.E., Mengelt, C. & Klinck, J.M. 2000. The linkage between Upper Circumpolar Deep Water (UCDW) and phytoplankton assemblages on the west Antarctic Peninsula continental shelf. Journal of Marine Research, 58, 165–202.Google Scholar
Pudsey, C.J. 1992. Late Quaternary changes in Antarctic Bottom Water velocity inferred from sediment grain size in the northern Weddell Sea. Marine Geology, 107, 9–33.Google Scholar
Rodriguez-Fernandez, J., Balanya, J.C., Galindo-Zaldivar, J. & Maldonado, A. 1997. Tectonic evolution of a restricted ocean basin: the Powell Basin (northeastern Antarctic Peninsula). Geodinamica Acta, 10, 159–174.Google Scholar
Scherer, R.P. 1994. A new method for the determination of absolute abundance of diatoms and other silt-sized sedimentary particles. Journal of Paleolimnology, 12, 171–179.Google Scholar
Scott, P., McMinn, A. & Hosie, G. 1994. Physical parameters influencing diatom community structure in eastern Antarctic sea ice. Polar Biology, 14, 507–517.Google Scholar
Spindler, M. & Dieckmann, G. 1986. Distribution and abundance of the planktic foraminifer Neogloboquadrina pachyderma in sea ice of the Weddell Sea (Antarctica). Polar Biology, 5, 185–191.Google Scholar
Stickley, C.E., Pike, J., Leventer, A., Dunbar, R., Domack, E.W., et al. 2005. Deglacial ocean and climate seasonality in laminated diatom sediments, Mac.Robertson Shelf, Antarctica. Palaeoceanography, Palaeoclimatology, Palaeoecology, 227, 290–310.Google Scholar
Tanimura, Y., Fukuchi, M., Watanabe, K. & Moriwaki, K. 1990. Diatoms in water column and sea ice in Lutzow-Holm Bay, Antarctica, and their preservation in the underlying sediments. Bulletin of the National Science Museum, Tokyo, Series C, 18, 15–39.Google Scholar
Taylor, F. & McMinn, A. 2002. Late Quaternary diatom assemblages from Prydz Bay, eastern Antarctica. Quaternary Research, 57, 151–161.Google Scholar
Taylor, F. & Leventer, A. 2003. Late Quaternary palaeoenvironments in Prydz Bay, East Antarctica: interpretations from marine diatoms. Antarctic Science, 15, 512–521.Google Scholar
Tolotti, R., Salvi, C., Salvi, G. & Bonci, M.C. 2013. Late Quaternary climate variability as recorded by micropaleontological diatom data and geochemical data in the western Ross Sea, Antarctica. Antarctic Science, 25, 804–820.Google Scholar
Zielinski, U., Bianchi, C., Gersonde, R. & Kunz-Pirrung, M. 2002. Last occurrence datums of the diatoms Rouxia leventerae and Rouxia constricta: indicators for marine isotope stages 6 and 8 in Southern Ocean sediments. Marine Micropaleontology, 46, 127–137.Google Scholar