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Comparison of Radiolarian/Planktonic Foraminiferal Paleoceanography of the Subantarctic Indian Ocean

Published online by Cambridge University Press:  20 January 2017

Douglas F. Williams
Affiliation:
Graduate School of Oceanography, University of Rhode Island, Kingston, Rhode Island 02881 USA
John Keany
Affiliation:
Graduate School of Oceanography, University of Rhode Island, Kingston, Rhode Island 02881 USA

Abstract

A detailed paleoceanographic history of the Subantarctic region for the last million years was determined using paleomagnetic stratigraphy, radiolarian and planktonic foraminiferal biostratigraphy, and the oxygen isotope record from stages 1 to 13 (0.5 MY) in a deep-sea core (E45-74) from the southern Indian Ocean. Changes in the abundances of Antarctissa strelkovi and Neogloboquadrina pachyderma record 12 glacial/interglacial cycles. The paleoceanographic events based on the combined results of these siliceous and calcareous indexes agree with changes in the global ice-volume record. Calcium carbonate dissolution selectively alters the planktonic foraminiferal fauna and causes test fragmentation and increased numbers of benthic foraminifera and radiolarians. Intense periods of calcium carbonate dissolution are associated principally with glacial episodes and are probably related to increased Antarctic bottom-water activity as well as changes in surface-water mass positions.

Type
Original Articles
Copyright
University of Washington

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References

Arrhenius, G., 1952. Sediment cores from the East Pacific. Reports of the Swedish Deep-Sea Expedition 1947–1948. 5, 1 227.Google Scholar
, A.W.H., 1969. Planktonic foraminifera. Distribution of Selected Groups of Marine Invertebrates in Waters South of 35°S Latitude. Antarctic Map Folio Series. American Geographical Society, 9 12 Folio II.Google Scholar
, A.W.H., Duplessy, J.C., é and Duplessy, 1976. Subtropical convergence fluctuations and Quaternary climates in the middle latitudes of the Indian Ocean. Science. 194, 419 422.Google Scholar
, A.W.H., Tolderland, D.S., é and Tolderland, 1971. Distribution and ecology of living planktonic foraminifera in surface waters of the Atlantic and Indian Oceans. Funnell, B.M., Riedel, W.R., The Micropaleontology of the Oceans. Cambridge University Press, Cambridge, 105 149.Google Scholar
Berger, W., 1968. Planktonic foraminifera: Selective solution and paleoclimatic interpretation. Deep-Sea Research. 15, 31 43.Google Scholar
Berger, W.H., 1973. Deep-sea carbonates: Pleistocene dissolution cycles. Journal of Foraminiferal Research. 3, 187 195.Google Scholar
Damuth, J.D., 1975. Quaternary climate change as revealed by calcium carbonate fluctuations in western Equatorial Atlantic Sediments. Deep-Sea Research. 22, 725 743.Google Scholar
Dansgaard, W., Tauber, H., 1969. Glacier oxygen-18 content and Pleistocene ocean temperatures. Science. 166, 499 502.Google Scholar
Dow, R.L., 1976. Radiolarian distribution and the late Pleistocene history of the Southeast Indian Ocean. Unpublished M. S. Thesis. University of Rhode Island, Kingston, R. I. Google Scholar
Echols, R.J., Kennett, J.P., 1973. Distribution of foraminifera in the surface sediment. Marine Sediments of the Southern Oceans. Antarctic Map Folio Series. American Geographical Society, 13 17 Folio.Google Scholar
Emiliani, C., 1955. Pleistocene paleotemperatures. Journal of Geology. 63, 538 578.Google Scholar
Emiliani, C., 1966. Paleotemperature analysis of Caribbean cores P6394-8 and P6304-9 and a generalized temperature curve for the past 425,000 years. Journal of Geology. 74, 109 126.Google Scholar
Fillon, R.H., 1972. Evidence from the Ross Sea for widespread submarine erosion. Nature Physical Science. 238, 40 42.Google Scholar
Gardner, J.88., 1975. Late Pleistocene carbonate dissolution cycles in the eastern equatorial Atlantic. Sliter, W.89., , A.W.H., Berger, W.H., Dissolution of Deep-Sea Carbonates. Cushman Foundation for Foraminiferal Research Special Publication. 13, 129 141.Google Scholar
Goodell, H.G., 1973. The sediments. Marine Sediments of the Southern Oceans. American Geographical Society, Antarctic Map Folio Series. Folio 17.Google Scholar
Gordon, A.L., 1971. Antarctic polar front zone. Reid, J.L., Antarctic Oceanology I. Antarctic Research Series. Vol. 19, Americal Geophysical Union, Washington, D.C, 205 221.Google Scholar
Gordon, A.L., 1972. Introduction: Physical oceanography of the Southeast Indian Ocean. Hayes, D.E., Antarctic Oceanology II. Antarctic Research Series. Vol. 19, American Geophysical Union, Washington, D.C, 3 9.Google Scholar
Hays, J.D., 1965. Radiolaria and late Tertiary and Quaternary history of Antarctic Seas. Biology of the Antarctic Sea II: Antarctic Research Series. Vol. 5, American Geophysical Union, Washington, D.C, 125 184.Google Scholar
Hays, J.D., Lozano, J.A., Shackleton, N.J., Irving, G., 1976a. An 18,000 B.P. reconstruction of the Atlantic and Western Indian sectors of the Antarctic Ocean. Cline, R.M., Hays, J.D., Investigations of Late Quaternary Paleoceanography and Paleoclimatology. Geological Society of America, Memoir. 145, 337 372.Google Scholar
Hays, J.D., Imbrie, J., Shackleton, N.J., 1976b. Variations in the Earth's orbit: Pacemaker of the Ice Ages. Science. 194, 1121 1132.Google Scholar
Hays, J.D., Opdyke, N.D., 1967. Antarctic radiolaria, magnetic reversals and climate change. Science. 158, 1001 1011.Google Scholar
Hays, J.D., Saito, T., Opdyke, N.D., Burckle, L.H., 1969. Pliocene-Pleistocene sediments of the equatorial Pacific: Their paleomagnetic, biostratigraphic and climatic record. Geological Society of America, Bulletin. 80, 1481 1514.Google Scholar
Hays, J.D., Shackleton, N.J., 1976. Globally synchronous extinctions of the radiolarian Stylatractus universus . Geology. 4, 649 652.Google Scholar
Keany, J., 1973. New Radiolarian paleoclimatic index in the Plio-Pleistocene of the Southern Ocean. Nature (London). 246, 139 141.Google Scholar
Kennett, J.P., 1966. Foraminiferal evidence of a shallow calcium carbonate solution boundary, Ross Sea, Antarctica. Science. 153, 191 193.Google Scholar
Kennett, J.P., 1969. Distribution of planktonic foraminifera in surface sediments to the southeast of New Zealand. Bronniman, P., Renz, H.H., Proceedings of the First International Conference on Planktonic Microfossils, Geneva 1967. Vol. 2, Edizioni Technoscienza, Roma, 307 322.Google Scholar
Kennett, J.P., 1970. Pleistocene paleoclimates and foraminiferal biostratigraphy in subantarctic deep-sea cores. Deep-Sea Research. 17, 305 318.Google Scholar
Kennett, J.P., Watkins, N.D., 1976. Regional deep-sea dynamic processes recorded by Late Cenozoic sediments of the southeastern Indian Ocean. Geological Society of America, Bulletin. 87, 321 339.Google Scholar
Kowsman, R.O., 1973. Coarse components in surface sediments of the Panama basin. Journal of Geology. 81, 473 494.Google Scholar
Lozano, J.A., Hays, J.D., 1976. Relationship of radiolarian assemblages to sediment types and physical oceanography in Atlantic and Western Indian Ocean sectors of the Antarctic Ocean. Cline, R.M., Hays, J.D., Investigations of Late Quaternary Paleoceanography and Paleoclimatology. Geological Society of America, Memoir. 145, 303 336.Google Scholar
Luz, B., 1973. Stratigraphic and paleoclimatic analysis of late Pleistocene tropical southeast Pacific cores. Quaternary Research. 3, 56 72.Google Scholar
Luz, B., Shackleton, N.J., 1975. CaCO3 solution in the tropical east Pacific during the past 130,000 years. Sliter, W.90., , A.W.H., Berger, W.H., Dissolution of Deep-Sea Carbonates. Cushman Foundation for Foraminiferal Research Special Publication. 13, 142 150.Google Scholar
Miyajima, M.H., 1976. Subantarctic region, southeast Indian Ocean: Absolute chronology of upper Pleistocene calcareous nannofossil zones and paleoclimatic history determined from silicoflagellate, coccolith and carbonate analyses. Tallahassee, Florida State University Sedimentology Research Laboratory Contribution. No. 42.Google Scholar
Ninkovitch, D., Shackleton, N.J., 1975. Distribution, stratigraphic position and age of ash layer “L” in the Panama basin region. Earth and Planetary Science Letters. 27, 20 34.Google Scholar
Peters, C.S., 1976. Oxygen isotopic analysis of two cores from the Vema Channel, southwestern Atlantic Ocean: An evaluation of the method and results. Woods Hole Oceanographic Institution Techological Report 76-10. (unpublished manuscript).Google Scholar
Petrushevskaya, M.G., 1967. Radiolaria of the orders Spumellaria and Nassellaria of the Antarctic region. Collection: Investigations of the Fauna of the Seas, IV (XII). Rezultaty biologicheskikh issledovanii Sovetskoi Antarkticheskoi ekspeditsii (1955–1958). M.-L. izd-vo Nauka, [In Russian].Google Scholar
Sanders, H.L., 1968. Marine benthic diversity: A comparative study. American Naturalist. 102, 243 282.Google Scholar
Shackleton, N.J., 1967. Oxygen isotope analyses and Pleistocene temperatures re-assessed. Nature (London). 215, 15 17.Google Scholar
Shackleton, N.J., Opdyke, N.D., 1973. Oxygen isotope and paleomagnetic stratigraphy of Equatorial Pacific core oxygen isotope temperatures on a 105 year and 106 year scale. Quaternary Research. 3, 39 55.Google Scholar
Thiede, J., 1973. Planktonic foraminifera in hemipelagic sediments: Shell preservation off Portugal and Morocco. Geological Society of America, Bulletin. 84, 2749 2754.Google Scholar
Thompson, P.R., Saito, T., 1975. Pacific Pleistocene sediments: Planktonic foraminiferal dissolution cycles and geochronology. Geology. 2, 333 335.Google Scholar
Thunell, R.C., 1976. Calcium carbonate dissolution history in Late Quaternary deep-sea sediments, Western Gulf of Mexico. Quaternary Research. 6, 281 297.Google Scholar
Vella, P., Ellwood, B.B., Watkins, N.D., 1975. Surface-water temperature changes in the Southern Ocean southwest of Australia during the last one million years. Special Bulletin, Royal Society of New Zealand presented at IX INQUA Congress. Christchurch, New Zealand, 1973 .Google Scholar
Vella, P., Watkins, N.D., 1975 Middle and Late Quaternary Paleomagnetics and Biostratigraphy of Four Subantarctic Deep-Sea Cores from Southwest of Australia: O. L. Bandy Memorial Volume. University Southern California Press, Los Angeles, Calif. Google Scholar
Watkins, N.D., Keany, J., Ledbetter, M.T., Huang, T.C., 1974. Antarctic glacial history from analyses of ice-rafted deposits in marine sediments: New model and initial tests. Science. 186, 533 536.Google Scholar
Williams, D.F., 1975. Magnitude and timing of major water-mass movements in the southern Indian Ocean during the Late Quaternary. EOS, Transactions, American Geophysical, Union. 56, 384.Google Scholar
Williams, D.F., 1976a. Planktonic Foraminiferal Paleoecology in Deep-Sea Sediments of the Indian Ocean. Unpublished Ph.D. dissertation. University of Rhode Island, Kingston, R.I. Google Scholar
Williams, D.F., 1976b. Late Quaternary migrations of the Subtropical Convergence and Polar Front in the southeast Indian Ocean. Marine Micropaleontology. 1, 363 375.Google Scholar
Williams, D.F., Johnson, W., 1975. Diversity of Recent planktonic foraminifera in the southern Indian Ocean and late Pleistocene paleotemperatures. Quaternary Research. 5, 237 250.Google Scholar
Yamashiro, C., 1975. Differentiating dissolution and transport effects in foraminiferal sediments from the Panama Basin. Sliter, W.91., , A.W.H., Berger, W.H., Dissolution of Deep-Sea Carbonates. Cushman Foundation of Foraminiferal Research Special Publication. 13, 151 159.Google Scholar