Hostname: page-component-7dd5485656-tbj44 Total loading time: 0 Render date: 2025-10-31T03:18:06.117Z Has data issue: false hasContentIssue false
  • English
  • Français

Glacial Meltwater in Lake Huron during Early Postglacial Time as Inferred from Single-Valve Analysis of Oxygen Isotopes in Ostracodes

Published online by Cambridge University Press:  20 January 2017

David L. Dettman ,
Alison J. Smith ,
David K. Rea ,
Theodore C. Moore Jr.  and
Kyger C. Lohmann
David L. Dettman
Affiliation:
Department of Geological Sciences, University of Michigan, 1006 C.C. Little Building, Ann Arbor, Michigan, 48109-1063
Alison J. Smith
Affiliation:
Department of Geology, Kent State University, 221 McGilvrey Hall, Kent, Ohio 44242
David K. Rea
Affiliation:
Department of Geological Sciences and Center for Great Lakes and Aquatic Sciences, University of Michigan, 1006 C.C. Little Building, Ann Arbor, Michigan 48109-1063
Theodore C. Moore Jr.
Affiliation:
Department of Geological Sciences and Center for Great Lakes and Aquatic Sciences, University of Michigan, 1006 C.C. Little Building, Ann Arbor, Michigan 48109-1063
Kyger C. Lohmann
Affiliation:
Department of Geological Sciences, University of Michigan, 1006 C.C. Little Building, Ann Arbor, Michigan 48109-1063
Get access Rights & Permissions [Opens in a new window]

Abstract

δ18O measurements of benthic ostracodes are used to reconstruct the δ18O history of Lake Huron and Georgian Bay water between 10,600 and 7600 14C yr B.P. This δ18O record was calibrated using a comparison of the δ18O values of modern ostracodes and Lake Huron water, where a fractionation of 1.0358 was measured between the oxygen isotope ratios of the most isotopically positive ostracode Candona subtriangulata and lake water. The most positive shell δ18O value was used because it is precipitated in the cold (0° to 2°C) water common to both deep and shallow environments. The δ18O of Lake Huron water reflects a large glacial meltwater component for much of its history before 7600 14C yr B.P. Times of low lake level correlate with the highest ratio of glacial meltwater to local precipitation in the basin (most negative δ18O values). Georgian Bay water was more negative in δ18O than Lake Huron water of the same age; this reflects a higher proportion of glacial meltwater in Georgian Bay and its separation from Lake Huron during times of low lake level.

Information

Type
Research Article
Information
Quaternary Research , Volume 43 , Issue 3 , May 1995 , pp. 297 - 310
Copyright
University of Washington

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.)

Article purchase

Temporarily unavailable

References

Ayers, J. C. Anderson, D. V. Chandler, D. C., and Lauff, G. H. (1956). “Currents and water masses of Lake Huron (1954 Synoptic Surveys)” Great Lakes Research Institute Technical Paper No. I. Great Lakes Research Institute, Ann Arbor, Michigan.Google Scholar
Beeton, A. M. Smith, S. H., and Hooper, F. H, (1967). “Physical limnology of Saginaw Bay, Lake Huron,” Great Lakes Fishery Commission Technical Report No. 12. Great Lakes Fishery Commission, Ann Arbor, Michigan.Google Scholar
Broecker, W. S. Kennett, J. P. Flower, B. P. Teller, J. T. Trumbore, S. Bonani, G., and Wolfli, W. (1989). Routing of meltwater from the Laurentide Ice Sheet during the Younger Dryas cold episode. Science 341, 318–321.Google Scholar
Chivas, A. R. DeDekker, P. Cali, J. A. Chapman, A. Kiss, E., and Shelley, J. M. G. (1993). Coupled stable-isotope and trace-element measurements of lacustrine carbonates as paleoclimate indicators. In“Climate Change in Continental Isotopic Records” (Swart, P. K. Lohmann, K. C. McKenzie, J., and Savin, S., Eds.), AGU Geophysical Monograph 78, pp. 113–121. Am. Geophys. Union, Washington, DC.Google Scholar
Chivas, A. R. DeDekker, P., and Shelley, J. M. G. (1986). Magnesium content of non-marine ostracode shells: a new palaeosalinometer and palaeothermometer, Palaeogeography, Palaeoclimatology, Palaeoecoiogy 54, 43–61.Google Scholar
Cohen, A. C., and Morin, J. G. (1990). Patterns of reproduction in ostracodes: a review. Journal of Crustacean Biology 10, 184–211.CrossRefGoogle Scholar
Colman, S. M. Jones, G. A. Forester, R. M., and Foster, D. S. (1990). Holocene paleocfimatic evidence and sedimentation rates from a core in southwestern Lake Michigan. Journal of Paleolimnology 4, 269–284.CrossRefGoogle Scholar
Colman, S. M. Keigwin, L. D., and Forester, R. M. (1994). Two episodes of meltwater influx from glacial Lake Agassiz into the Lake Michigan basin and their climatic contrasts. Geology 22, 547–550.Google Scholar
DeDekker, P., and Forester, R. M. (1988). The use of ostracodes to reconstruct continental palaeoenvironmental records. In “Ostracoda in the Earth Sciences” (DeDekker, P. Colin, J. P., and Peypouquet, J. P., Eds.), pp. 175–200. Elsevier, Amsterdam.Google Scholar
Delorme, L. D. (1978). Distribution of freshwater ostracodes in Lake Erie. Journal of Great Lakes Research 4, 216-220,Google Scholar
Friedman, I., and O’Neil, J. R. (1977). “Compilation of stable isotope fractionation factors of geochemical interest.” Geological Survey Professional Paper 440-KK.Google Scholar
Heard, W.H. (1965). Comparative life histories of the North American pill clams (Spheriidae: Pisidium). Malacologia 2, 381–411.Google Scholar
Hut, G. (1987). “Consultant’s group meeting on stable isotope reference samples for geochemical and hydrological investigations.” International Atomic Energy Agency Internal Report.Google Scholar
Klassen, R. W. (1983). Lake Agassiz and the late glacial history of northern Manitoba. In “Glacial Lake Agassiz” (Teller, J. T. and Clayton, L., Eds.), Geological Association of Canada Special Paper 26, pp. 97–116. Geological Association of Canada, St. John’s, Newfoundland.Google Scholar
Lewis, C. F. M., and Anderson, T. W. (1989). Oscillations of lake levels and cool phases of the Laurentian Great Lakes caused by inflows from glacial Lakes Agassiz and Barlow-Ojibway. Journal of Paleolimnology 2, 99–146.CrossRefGoogle Scholar
Lewis, C. F. M., and Anderson, T. W. (1992). Stable isotope (O and C) and pollen trends in eastern Lake Erie, evidence for a locally-induced climatic reversal of Younger Dryas age in the Great Lakes basin. Climate Dynamics 6, 241–250.Google Scholar
McKenzie, J. A. (1985). Carbon isotopes and productivity in the lacustrine and marine environment. In “Chemical Processes in Lakes” (Stumm, W., Ed.), pp. 99–118. Wiley, New York.Google Scholar
Moore, T. C. Jr. Rea, D. K. Lewis, C. F. M. Mayer, L. A., and Dobson, D. M. (1994). Seismic stratigraphy of Lake Huron -Georgian Bay and post-glacial lake level history. Canadian Journal of Earth Sciences 31, 1606–1617.Google Scholar
Rea, D. K., and Colman, S. M. (in press). Radiocarbon ages of prebomb clams and the hard-water effect in Lakes Michigan and Huron. Journal of Paleolimnology. Google Scholar
Rea, D. K. Moore, T. C. Jr. Lewis, C. F. M. Mayer, L. A. Dettman, D. L., and Smith, A. J. (1994). Stratigraphy and paleolimnologic record of early Holocene sediments in northern Lake Huron and Georgian Bay. Canadian Journal of Earth Sciences 31, 1586–1605.CrossRefGoogle Scholar
Rea, D. K. Owen, R. M., and Meyers, P. A. (1981). Sedimentary processes in the Great Lakes. Reviews of Geophysics and Space Physics 19, 635–648.CrossRefGoogle Scholar
Romanek, C. S. Grossman, E. L., and Morse, J. W. (1992). Carbon isotopic fractionation in synthetic aragonite and calcite: effects of temperature and precipitation rate. Geochimica et Cosmochimica Acta 56, 419–430.Google Scholar
Rooth, C. (1982), Hydrology and ocean circulation. Progress in Oceanography 11, 131–149.CrossRefGoogle Scholar
Salomons, W., and Mook, W. G. (1986). Isotope geochemistry of carbonates in the weathering zone. In “Handbook of Environmental Isotope Geochemistry, Vol. 2, The Terrestrial Environment, B” (Fritz, P., and Fontes, J. Ch., Eds.), pp. 239–270. Elsevier, Amsterdam.Google Scholar
Tanaka, N. Monaghan, M. C., and Rye, D. M. (1986). Contribution of metabolic carbon to mollusc and barnacle shell carbonate. Nature 320, 520–523.Google Scholar
Teller, J. T. (1987). Proglacial lakes and the southern margin of the Laurentian Ice Sheet. In “North America and Adjacent Oceans during the Last Deglaciation” (Ruddiman, W. F., and Wright, H. E. J., Eds.), pp. 39–69. Geol. Soc. Am., Boulder, CO.Google Scholar
Teller, J. T. (1990). Volume and routing of late-glacial runoff from the southern Laurentide ice sheet. Quaternary Research 34, 12–23.Google Scholar
TUrpen, J., and Angell, R. (1971). Aspects of molting and calcification in the ostracode heterocypris. Biological Bulletin 140, 331–338.Google Scholar
Upper Lakes Reference Group (1977). “The waters of Lake Huron and Lake Superior, Volume II (Part B) Lake Huron, Georgian Bay, and the North Channel.” (Bratzel, M. P. Jr. Thompson, M. E., and Bowden, R.J., Eds.). Report to the International Joint Commission, Windsor, Ontario, Canada.Google Scholar
Way, C. M. (1988). Seasonal allocation of energy to respiration, growth, and reproduction in the freshwater clams, Pisidium variable and P. compressum (Bivalvia: Pisidiidae). Freshwater Biology 19, 321–332.Google Scholar
Webb, T. III Bartlein, P. J., and Kutzbach, J. E. (1987). Climatic change in eastern North America during the past 18,000 years; Comparisons of pollen data with model results, In “North America and Adjacent Oceans during the Last Deglaciation” (Ruddiman, W. F., and Wright, H, E. J., Eds.), pp. 447–462. Geol. Soc. Am., Boulder, CO.Google Scholar