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Late Pleistocene Climate Record in the Eustis Loess Section, Nebraska, Based on Land Snail Assemblages and Magnetic Susceptibility

Published online by Cambridge University Press:  20 January 2017

Denis-Didier Rousseau  and
George Kukla
Denis-Didier Rousseau
Affiliation:
URA CNRS 327, Institut des Sciences de l'Evolution, Université Montpellier II, Place Eugéne Bataillon. 34095 Montpellier cedex 5, France; and Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964
George Kukla
Affiliation:
Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964
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Abstract

Based on multivariate analysis of mollusk assemblages and magnetic susceptibility of the Eustis section in western Nebraska, the climate of the Peoria loess steppe was relatively mild and, in terms of annual precipitation, relatively moist during the advance stages of Woodfordian ice. It was cold and dry during ice retreat. The diversity and composition of mollusk species indicates that the extreme cold and dry climate was reached during the late phase of Peoria time, in mollusk zone MZ3. Although soil moisture during the growing season at that time was high, the growing season was short and annual precipitation totals were low. Low values of magnetic susceptibility imply relatively rapid dust deposition during this interval, Judging from the current ecological tolerance of the species, no closed forest existed in the area. Only scattered shrubs or isolated tree stands may have been present. The late Peoria MZ3 assemblage compares favorably with the Columella fauna of Europe. In contrast, the early Peoria mollusk assemblages MZ1 and MZ2 compare well with the European pleniglacial Pupilla associations. Based on available 14 C dates from the studied region and on assumed relation of magnetic susceptibility to sedimentation rates, the estimated age of the MZ1 and MZ2 zones is 24,000 to 16,000 yr, whereas that of MZ3 is 16,000 to 12,000 yr.

Type
Research Article
Information
Quaternary Research , Volume 42 , Issue 2 , September 1994 , pp. 176 - 187
Copyright
University of Washington

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References

An, Z. S. Kukla, G. J. Porter, S. C., and Xiao, J, (1991). Magnetic susceptibility evidence of monsoon variation on the loess plateau of central China during the last 130,000 years. Quaternary Research 36, 29–36.CrossRefGoogle Scholar
Andrews, J. T. (1987). The Late Wisconsin glaciation and deglaciation of the Laurentide ice sheet. In “The Geology of North America. Vol. K-3. North America and adjacent Oceans during the Last Deglaciation” (Ruddiman, W. F. and Wright, H. E., Eds.), pp. 13–37. The Geological Society of America, Boulder, CO.Google Scholar
Beg6t, I. Edwards, M. Hopkins, D. Keskinen, M., and Kukla, G. (1991). Old Crow tephra at the Palisades of the Yukon, Alaska. Quaternary Research 35, 291–297.CrossRefGoogle Scholar
Benzecri, J. P., and Benzecri, F. (1980). “Pratique de l’analyse des donn6es.” Dunod, Paris.Google Scholar
Boellstorff, J. D., and Te Punga, M. T. (1977). Fission-track ages and correlation of middle and lower Pleistocene from Nebraska and New Zealand. New Zealand Journal of Geology and Geophysics 20, 47–58.Google Scholar
Frankel, L. (1956). “Pleistocene Geology and Paleoecology of Parts of Nebraska and adjacent Areas.” Unpublished Ph.D. thesis, Department of Geology, University of Nebraska, Lincoln.Google Scholar
Frye, J. C. Leonard, A. B. Willman, H. B. Glass, H. D., and Follmer, L. R. (1974). The late Woodfordian Jules Soil and associated molluscan faunas. Illinois State Geological Survey Circular 486, 1–11.Google Scholar
Goodfriend, G. A. (1987). Radiocarbon age anomalies in shell carbonate of land snails from semi-arid areas. Radiocarbon 29, 159–167.Google Scholar
Heller, F., and Liu, T. S. (1984). Magnetism of Chinese loess deposits. Geophysical Journal 11, 125–141.Google Scholar
Hovan, S. A., and Rea, D. K. (1991). Late Pleistocene continental climate and oceanic variability recorded in northwest Pacific sediments. Paleoceanography 6, 349–370.Google Scholar
Hovan, S. A. Rea, D. K. Pisias, N. G., and Shackleton, N. J. (1989). A direct link between the China loess and marine t)l80 records: Aeolian flux to the north Pacific. Nature 340, 296–298.Google Scholar
Hughes, T. (1987). Ice dynamics and deglaciation models. In “The Geology of North America. Vol. K-3. North America and adjacent Oceans during the Last Deglaciation” (Ruddiman, W. F. and Wright, H. E., Eds.), pp. 183–220. The Geological Society of America, Boulder, CO.Google Scholar
Johnson, G. H. (1965). The Stratigraphy, Paleontology, and Paleoecology of the Peoria Loess (Upper Pleistocene) of Southwestern Indiana.” Unpublished Ph.D. thesis, Department of Geology, Indiana University.Google Scholar
Johnson, W, C. May, D, W., and Souders, V. J. (1990). Age and distribution of the Gilman Canyon formation of Nebraska and Kansas. Geological Society of America 22(7), A87. [Abstracts with programs] Google Scholar
Klima, B. Kukla, J. Lozek, V., and de Vries, H. (1962). Stratigraphie des Pleistozans und Alter des palaeolithischen Rastplatzes in der Ziegelei von Dolni Vestonice (Unter-Wistemitz). Anthropozoikum 11, 93–145.Google Scholar
Kukla, G. J. (1978). The classical European glacial stages: Correlations with deep-sea sediments. Transactions Nebraska Academy of Sciences 6, 57–93.Google Scholar
Kukla, G. J. (1987). Loess stratigraphy in central China. Quaternary Science Reviews 6, 191–219.Google Scholar
Kukla, G. J., and An, Z. S. (1989). Loess stratigraphy in central China. Palaeogeography, Palaeoclimatology, Palaeoecology 72, 203–225.Google Scholar
Kukla, G. Heller, F. Liu, X. M. Xu, T. C. Liu, T. C., and An, Z. S. (1988). Pleistocene climates in China dated by magnetic susceptibility. Geology 16, 811–814.Google Scholar
Kukla, G. An, Z. S. Melice, J. L. Gavin, J., and Xiao, J. L. (1990). Magnetic susceptibility record of Chinese loess. Royal Society of Edinburgh Transactions, Earth Sciences 81, 263–288.Google Scholar
Leonard, A. B. (1952). Illinoian and Wisconsinan molluscan faunas in Kansas. University of Kansas Paleontological Contributions 4, 1–38.Google Scholar
Leonard, A. B. (1959). Handbook of Gastropods in Kansas. University of Kansas, Museum Natural History Publication 20, 1–224.Google Scholar
Limondin, N., and Rousseau, D. D. (1991). Holocene climates reflected by malacological sequence at Verri£res, Seine Valley, France. Boreas 20, 207–229.Google Scholar
Lozek, V. (1964). Quartarmollusken der Tschechoslowakei. Rozpravy Ustredniho Ustavu Geologickeho 31, 1–374.Google Scholar
Maher, B. A., and Taylor, R. H. (1988). Formation of ultrafme-grained magnetite in soils. Nature 336, 368–370.CrossRefGoogle Scholar
Maher, B. A., and Thompson, R. (1991). Mineral magnetic record of the Chinese loess and paleosols. Geology 19, 3–6.Google Scholar
May, D. W., and Holen, S. R. (1993). Radiocarbon ages of soils and charcoal in late Wisconsinan loess, South-central Nebraska. Quaternary Research 39, 55–58.Google Scholar
Naeser, C. W. Izett, G. A., and Wilcox, R. E. (1971). Zircon fissiontrack ages of Pearlette-like volcanic ash beds in the Great Plains. Geological Society America Memoir 3, 657.Google Scholar
Puiss6gur, J. J. (1976). Mollusques continentaux quatemaires de Bourgogne. Significations stratigraphiques et climatiques. Rapports avec d’autres faunes bordales de France. Me moires geologiques Universite Dijon 3, 1–241.Google Scholar
Rousseau, D. D. (1986). Application de la mdthode d’analyse factorielle des correspondances aux malacofaunes de Tourville (Saalien). Bulletin Centre Geomorphologie Caen 31, 5–20.Google Scholar
Rousseau, D. D. (1987). Palaeoclimatology of the Achenheim series (middle and upper Pleistocene, Alsace, France). A malacological analysis. Palaeogeography, Palaeociimatology, Palaeoecology 59, 293–314.Google Scholar
Rousseau, D. D. (1991). Climatic transfer function from Quaternary molluscs in European loess deposits. Quaternary Research 35, 195–209.CrossRefGoogle Scholar
Rousseau, D. D., and Puiss6gur, J. J. (1989). Analyse de la malacofaune continentale. In LLe gisement pal£olithique de Biache-St-Vaast (Pas-de-Calais)” (Tuffreau, A. and Sommd, J., Eds.), M6moire special Societe prihistorique fran?aise 21, pp. 89–102.Google Scholar
Rousseau, D. D., and Puiss6gur, J. J. (1990). A 350,000 years climatic record from the loess sequence of Achenheim, Alsace, France. Boreas 19, 203–216.Google Scholar
Rousseau, D. D. Limondin, N., and Puiss6gur, J. J. (1993). Holocene environmental signals from mollusc assemblages in Burgundy (France). Quaternary Research 40, 237–253.Google Scholar
Schultz, C. B., and Stout, T. M. (1961). Field conference on the Tertiary and Pleistocene of western Nebraska. University Nebraska State Museum Special Publication 2, 1–55.Google Scholar
Schultz, C. B. Stout, T. M., and Tanner, L. G. (1965). The Medicine Creek artifact sites. In “Central Great Plains” (Schultz, C. B. and Smith, H. T. U., Eds.), pp. 84–92. Vllth INQUA Congress. Guidebook for field conference D.Google Scholar
Souders, V. L. Elder, J. A., and Dreeszen, V. H. (1971). Guidebook to selected Pleistocene Paleosols in Eastern Nebraska. University Ne-braska Conservation and Survey Division, Lincoln, NE, 1–17.Google Scholar
Verosub, K. L. Fine, P. Singer, M. J., andTenPas, J. (1993). Pedogenesis and paleoclimate: Interpretation of the magnetic susceptibility record of Chinese loess-paleosol sequences. Geology 21, 1011–1014.2.3.CO;2>CrossRefGoogle Scholar
Wayne, W. J. Aber, J. S. Agard, S. S. Bergantino, R. N. Bluemle, J. P. Coates, D. A. Cooley, M. E. Madole, R. F. Martin, J. E. Mears, B. Morrison, R. B., and Sutherland, W. M. (1991). Quaternary geology of the Northern Great Plains. In “The Geology of North America. Vol. K-2. Quaternary Nonglacial Geology; Conterminous US” (Morrison, R. B., Ed.), pp. 441–476. The Geological Society of America, Boulder, CO.Google Scholar
Wells, P. V., and Stewart, J. D. (1987). Spruce charcoal, conifer macrofossils, and landsnail and small-vertebrate faunas in Wisconsinan sediments on the High Plains of Kansas. In “Quaternary Environments of Kansas” (Johnson, W. C., Ed.), pp. 129–140. Kansas Geological Survey Guidebook series 5, Lawrence, KS.Google Scholar
Welch, J. E., and Hale, J. M. (1987). Pleistocene loess in Kansas— Status, present problems, and future considerations. In “Quaternary Environments of Kansas” (Johnson, W. C., Ed.), pp. 67–84. Kansas Geological Survey Guidebook series 5, Lawrence, KS.Google Scholar
Zhou, L. P. Oldfield, F. Wintle, A. G. Robinson, S. G., and Wang, J. T. (1990). Partly pedogenetic origin of magnetic variations in Chinese loess. Nature 346, 737–739.Google Scholar