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Stratigraphy, Paleontology, and Age of Lake Algonquin Sediments in Southwestern Ontario, Canada

Published online by Cambridge University Press:  20 January 2017

P.F. Karrow ,
T.W. Anderson ,
A.H. Clarke ,
L.D. Delorme  and
M.R. Sreenivasa
P.F. Karrow
Affiliation:
Department of Earth Sciences, University of Waterloo, Waterloo, Ontario, Canada
T.W. Anderson
Affiliation:
Geological Survey of Canada, Canada Centre for Inland Waters, Burlington, Ontario, Canada
A.H. Clarke
Affiliation:
National Museum of Natural Science, Ottawa, Ontario, Canada
L.D. Delorme
Affiliation:
Environment Canada, Water Resources Branch, Canada Centre for Inland Waters, Burlington, Ontario, Canada
M.R. Sreenivasa
Affiliation:
Department of Biology, Scarborough College, West Hill, Ontario, Canada
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Abstract

Molluscs, ostracodes, diatoms, pollen, plant macrofossils, peat, and wood have been found in glacial Lake Algonquin sediments, and estuarine-alluvial sediments of the same age, in southern Ontario. Molluscs and ostracodes are particularly abundant and widespread. Pollen analysis of Lake Algonquin sediments, bogs on the Algonquin terrace, and upland bogs above the Algonquin terrace, indicate that Lake Algonquin was still in existence at the time of the spruce-pine pollen transition, previously dated at an average of 10,600 yr BP at a number of sites in Michigan, Ohio, and southern Ontario. Wood in estuarine-alluvial sediments graded to the Algonquin level is of similar radiocarbon age. Evidence from several sites in the eastern Great Lakes area suggests the presence of a preceding low-water stage (Kirkfield outlet stage); drowned and alluviated valleys and fining-upward sediment sequences have been identified in this study as further supporting evidence. Lake Algonquin drained from the southern sites by isostatic tilting and eventual opening of the “North Bay outlet” some time shortly after 10,400 yr BP.

Our radiocarbon dates suggest the low-water stage has an age of about 11,000 yr BP, and that Lake Algonquin drained 10,000–15,000 y. a. Dates previously published for the Lake Michigan basin are generally too young in comparison with ours, and dates on the Champlain Sea are generally too old. More critical evaluation of all dating results is desirable.

From fossil remains we suggest a rapidly expanding fauna in the waters of Lake Algonquin. The spruce pollen period was a time of rapid faunal and floral migration, when the ice front was retreating from Kirkfield to North Bay, Ontario. Diversity of some species and fossil numbers increased substantially at the transition from spruce to pine just before Lake Algonquin drained.

Type
Research Article
Information
Quaternary Research , Volume 5 , Issue 1 , March 1975 , pp. 49 - 87
Copyright
University of Washington

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References

Anderson, T.W., (1971). Postglacial Vegetative Changes in the Lake Huron-Lake Simcoe District, Ontario, with Special Reference to Glacial Lake Algonquin. Ph.D. Thesis University of Waterloo, Waterloo, Ontario 246.Google Scholar
Antevs, E., (1925). Retreat of the last ice sheet in eastern Canada. Geological Survey Canada Memoir 146, 142.Google Scholar
Baker, F.C., (1920). The Life of the Pleistocene or Glacial Period. Illinois University Bulletin 17, 476.Google Scholar
Baker, F.C., (1928). The fresh water Mollusca of Wisconsin. Part 1, Gastropoda. Wisconsin Geological and Natural History Survey Bull. 70, 507.Google Scholar
Benninghoff, W.S., (1962). Calculation of pollen and spore density in sediments by addition of exotic pollen in known quantities (abstract). Pollen et Spores 4, 332 333.Google Scholar
Boye Petersen, J., (1928). The aerial algae of Iceland. The Botany of Iceland 2, 325 447.Google Scholar
Boye Petersen, J., (1943). Some halobian spectra (Diatoms). Det Kongelige Danske Videnskabernes Selskab Biologiske Meddelelser 17, 1 93.Google Scholar
Broecker, W.S., Farrand, W.R., (1963). Radiocarbon age of the Two Creeks forest bed, Wisconsin. Geological Society of American Bulletin 74, 795 802.CrossRefGoogle Scholar
Calkin, P.E., (1970). Strand lines and chronology of the glacial Great Lakes in northwestern New York. Ohio Journal of Science 70, 78 96.Google Scholar
Chapman, E.J., (1861a). Some notes on the drift deposits of western Canada, and on the ancient extension of the lake area of that region. Canadian Journal n.s. 6, 221 229.Google Scholar
Chapman, E.J., (1861b). Additional note on the occurrence of fresh-water shells in the upper drift deposits of western Canada. Canadian Journal n.s. 6, 497 498.Google Scholar
Chapman, L.J., (1954). An outlet of Lake Algonquin at Fossmill, Ontario. Proceedings of the Geological Association of Canada 6, 61 68.Google Scholar
Clarke, A.H., (1973). The freshwater molluscs of the Canadian Interior Basin. Malacologia 13, 1 509.Google Scholar
Cleve-Euler, A., (1953). Die Diatomeen von Schweden und Finnland. Kgl. Svenska Vetenskapsakad. Handl NS 4, 1 254.Google Scholar
Davis, M.B., (1969). Climatic changes in southern Connecticut recorded by pollen deposition at Rogers Lake. Ecology 50, 409 422.Google Scholar
Deane, R.E., (1950). The Pleistocene geology of the Lake Simcoe district, Ontario. Geological Survey Canada Memoir 256, 108.Google Scholar
Delorme, L.D., (1971). Paleoecological determinations using Pleistocene freshwater ostracodes. Bulletin Centre Recherche Pau SNPA 5, 341 347.Google Scholar
Evenson, E.B., (1973). Late Pleistocene shorelines and stratigraphic relations in the Lake Michigan basin. Geological Society of America Bulletin 84, 2281 2298.Google Scholar
Faegri, K., Iversen, J., (1964). Textbook of Modern Pollen Analysis. Scandinavian Univ. Books, Copenhagen, Denmark 237.Google Scholar
Farrand, W.R., (1962). Postglacial uplift in North America. American Journal of Science 260, 181 199.CrossRefGoogle Scholar
Farrand, W.R., (1970). Revision of the Valders drift border of the Lake Michigan lobe. Geological Society of America Abstract 2, 387(Abstracts with program, North Central Section).Google Scholar
Farrand, W.R., Miller, B.B., (1968). Radiocarbon dates on and depositional environment of the Wasaga Beach (Ontario) marl deposit. Ohio Journal of Science 68, 235 239.Google Scholar
Farrand, W.R., Zahner, R., Benninghoff, W.S., (1969). Cary-Port Huron Interstade: Evidence from a buried bryophyte bed, Cheboygan County, Michigan. Geological Society of America Special Paper 123, 249 262.CrossRefGoogle Scholar
Fernald, M.L., (1950). Gray's Manual of Botany. 8th edition American Book Co, New York 1632.Google Scholar
Flint, R.F., (1955). Rates of advance and retreat of the margin of the late-Wisconsin ice sheet. American Journal of Science 253, 249 255.Google Scholar
Florin, M.B., (1970). Late-glacial diatoms of Kirchner Marsh, south-eastern Minnesota. Nova Hedwigia, Beihefte 31, 667 746.Google Scholar
Foged, N., (1953). Diatoms from West Greenland. Medd. Om. Groenland 147, 1 86.Google Scholar
Foged, N., (1959). Diatoms from Afghanistan. Biol. Skr. Dan. Vid. Selsk. 2, 1 95.Google Scholar
Foged, N., (1964). Freshwater diatoms from Spitzbergen. Tramsö Museums Skrifter 11, 1 204.Google Scholar
Gilliam, J.A., Kapp, R.O., Bogue, R.D., (1967). A post-Wisconsin pollen sequence from Vestaburg Bog, Montcalm County, Michigan. Papers Michigan Academy of Science, Arts, and Letters 52, 3 17.Google Scholar
Goldthwait, J.W., (1910). An instrumental survey of the shorelines of extinct Lakes Algonquin and Nipissing in southwestern Ontario. Geological Survey Canada Memoir 10, 57.Google Scholar
Gravenor, C.P., (1957). Surficial geology of the Lindsay-Peterborough area, Ontario, Victoria, Peterborough, Durham, and Northumberland Counties, Ontario. Geological Survey Canada Memoir 288, 60.Google Scholar
Handley, C.O. Jr., (1953). Marine mammals in Michigan Pleistocene beaches. Journal of Mammology 34, 252 253.Google Scholar
Harrison, J.E., (1970). Deglaciation and proglacial drainage evolution: North Bay-Mattawa region, Ontario. Proceedings of the 13th Conference, Great Lakes Research 756 767.Google Scholar
Harrison, J.E., (1972). Quaternary geology of the North Bay-Mattawa region. Geological Survey of Canada Paper 26–71, 37.Google Scholar
Havinga, A.J., (1967). Palynology and pollen preservation. Rev. Palaeobot. Palynol. 2, 81 98.Google Scholar
Harrison, J.E., (1971). An experimental investigation into the decay of pollen and spores in various soil types. In Sporopollenin. Brooks, J., Grant, P.R., Muir, M.D., van Gijzel, P., Shaw, G., Academic Press, London and New York 446 479.Google Scholar
Heard, W.H., (1962). The Sphaeriidae (Mollusca: Pelecypoda) of the North American Great Lakes. American Midland Naturalist 67, 194 198.CrossRefGoogle Scholar
Herrington, H.B., (1962). A revision of the Sphaeriidae of North America, (Mollusca: Pelecypoda). Michigan University Museum of Zoology Miscellaneous Publication 118, 74.Google Scholar
Hough, J.L., (1958). Geology of the Great Lakes. Univ. Ill. Press, Urbana 310.Google Scholar
Hough, J.L., (1963). The prehistoric Great Lakes of North America. American Scientist 51, 84 109.Google Scholar
Hough, J.L., (1966). Correlation of glacial lake stages in the Huron-Erie and Michigan basins. Journal of Geology 74, 62 77.Google Scholar
Hultén, E., (1968). Flora of Alaska and Neighbouring Territories. Stanford Univ. Press, Calif 1008.Google Scholar
Hunter, A.F., (1903). The Algonquin shoreline in Simcoe County, Ontario. Geological Survey of Canada Summary Report 1902, A281 A304.Google Scholar
Hustedt, F., (1930). Bacillariophyta. Pascher, A., Die Süsswasser Flora Mitteuropas Vol. 10, G. Fisher, Jena.Google Scholar
Hustedt, F., (1962). Die Kieselalgen Deutschlands, Osterreichs und der Schweiz. (of Robenhorst, F. L.). Kryptogamenflora Akadamische Verlagsgesellschaft 7, 815.Google Scholar
Johnson, W.A., (1916). The Trent Valley outlet of Lake Algonquin and the deformation of the Algonquin water-plane in the Lake Simcoe district, Ontario. Geological Survey of Canada Museum Bulletin 23, 27.Google Scholar
Jorgensen, E.G., (1948). Diatom communities in some Danish lakes and ponds. Det Kongelige Danske Videnskabernes Selskab Biologiske Skrifter 5, 1 140.Google Scholar
Kapp, R.O., Gooding, A.M., (1964). A radiocarbon-dated pollen profile from Sunbeam Prairie Bog, Drake Co., Ohio. American Journal of Science 262, 259 266.Google Scholar
Karrow, P.F., Anderson, T.W., (1971). Paleontology and radiocarbon dating of Lake Algonquin sediments in southwestern Ontario. Geological Society of America Abstracts with program (North Central Section) 3, 269.Google Scholar
Karrow, P.F., Clark, J.R., Terasmae, J., (1961). The age of Lake Iroquois and Lake Ontario. Journal of Geology 69, 659 667.Google Scholar
Karrow, P.F., Clarke, A.H., Herrington, H.B., (1972). Pleistocene molluscs from Lake Iroquois deposits in Ontario. Canadian Journal of Earth Sciences 9, 589 595.Google Scholar
Kolbe, R.W., (1927). Zur Oekologie, Morphologie und Systematic der Brackwasser-Diatomeen. Die Kieselalgen des Sperenberger Salzgebietes: Pflanzenf 7, 146.Google Scholar
Lasca, N.P., (1970). Pleistocene geology from Milwaukee to the Kettle Interlobate Moraine. Pleistocene geology of southern Wisconsin. Geological Society of America Meeting University of Wisconsin, Milwaukee, Wisc C1 C14(Field trip guidebook).Google Scholar
Leverett, F., Taylor, F.B., (1915). The Pleistocene of Indiana and Michigan and the history of the Great Lakes. U.S. Geological Survey Monograph 53, 529.Google Scholar
Lewis, C.F.M., (1969). Late Quaternary history of lake levels in the Huron and Erie basins. Proceedings of the 12th Conference, Great Lakes Research 250 270.Google Scholar
Lowdon, J.A., Robertson, I.M., Blake, W. Jr., (1971). Geological Survey of Canada Radiocarbon dates XI. Radiocarbon 13, 255 324.Google Scholar
Mangerud, J., (1972). Radiocarbon dating of marine shells, including a discussion of apparent age of the Recent shells from Norway. Boreas 1, 143 172.Google Scholar
Mott, R.J., (1968). A radiocarbon-dated marine algal bed of the Champlain Sea episode near Ottawa, Ontario. Canadian Journal of Earth Sciences 5, 319 324.CrossRefGoogle Scholar
Ogden, J.G. III, (1966). Forest history of Ohio I. Radiocarbon dates and pollen stratigraphy of Silver Lake, Logan County, Ohio. Ohio Journal of Science 66, 387 400.Google Scholar
Ogden, J.G. III, (1967). Radiocarbon and pollen evidence for a sudden change in climate in the Great Lakes region approximately 10,000 years ago. Cushing, E.J., Wright, H.E. Jr., Quaternary Paleocology Yale University Press, New Haven 117 127.Google Scholar
Ogden, J.G. III, Hay, R.J., (1964). Ohio Wesleyan University natural radiocarbon measurements I. Radiocarbon 6, 340 348.Google Scholar
Patrick, R., (1943). The diatoms of Linsley Pond, Connecticut. Academy of Natural Science, Philadelphia Proceedings 95, 53 110.Google Scholar
Patrick, R., Reimer, C.W., (1966). The diatoms of the United States. Monograph Academy of Natural Science, Philadelphia 13, .Google Scholar
Pennington, W., (1943). Lake sediments. The bottom deposits of the North basin of Windermere with special reference to the diatom succession. New phytol 42, 1 27.Google Scholar
Peterson, R.L., (1965). A well-preserved grizzly bear skull recovered from a Late Glacial deposit near Lake Simcoe, Ontario. Nature (London) 208, 1233 1234.CrossRefGoogle Scholar
Prest, V.K., (1970). Quaternary geology of Canada. Geology and Economic Minerals of Canada. Geologic Survey of Canada Economic Geology Series 1, 677 764.Google Scholar
Rawson, D.S., (1930). The bottom fauna of Lake Simcoe and its role in the ecology of the lake. University of Toronto Studies Publication of the Ontario Fisheries and Research Laboratory 40, 183.Google Scholar
Robins, S.G., Hohn, M.H., (1972). Effects of postglacial lakes on Fox Lake, Beaver Island, Michigan, based on the analysis of the fossil diatom flora. Michigan Academician 4, 349 358.Google Scholar
Round, E.F., (1957). The Late-Glacial and post-Glacial diatom succession in the Kentmere Valley deposit. New Phytol 56, 98 126.Google Scholar
Round, E.F., (1966). The diatoms of a core from Esthwaite water. New Phytol. 60, 43 59.Google Scholar
Rowe, J.C., (1959). Forest regions of Canada. Canada Department of Northern Affairs National Research Forestry Branch Bulletin 123, 71.Google Scholar
Rubin, M., Alexander, C., (1960). U. S. Geological Survey radiocarbon dates V. American Journal of Science Radiocarbon Supplement 2, 129 185.Google Scholar
Schneider, A.F., (1970). Age and correlation of the Glenwood stage of Lake Chicago. Geological Society of American Abstracts with program (North Central Section) 2, 404.Google Scholar
Spencer, J.W., (1891). Deformation of the Algonquin beach and birth of Lake Huron. American Journal of Science Third Series 41, 12 21.Google Scholar
Spurr, S.H., Zumberge, J.H., (1956). Late Pleistocene features of Cheboygan and Emmet counties, Michigan. American Journal of Science 254, 96 109.Google Scholar
Sreenivasa, B.A., (1968). A Late-Glacial and Postglacial Pollen Diagram from the Waterloo Moraine Waterloo County, Ontario. M.Sc. thesis Univ. of Waterloo 87.Google Scholar
Sreenivasa, M.R., (1970). Recent and Extant Diatom Assemblages in Southern Ontario. Ph.D. thesis Univ. Waterloo 360.Google Scholar
Sreenivasa, M.R., Duthie, H.C., (1973). Diatoms in the Grand River, Southern Ontario. Hydrobiologia 42, 161 224.Google Scholar
Stanley, G.M., (1936). Lower Algonquin beaches of Penetanguishene Peninsula. Geological Society of America Bulletin 47, 1933 1960.CrossRefGoogle Scholar
Stanley, G.M., (1937). Lower Algonquin beaches of Cape Rich, Georgian Bay. Geological Society of America Bulletin 48, 1665 1686.Google Scholar
Stanley, G.M., (1938). Impounded Early Algonquin beaches at Sucker Creek, Grey County, Ontario. Papers Michigan Academy of Science, Arts, and Letters 23, 477 495.Google Scholar
Taylor, F.B., (1913). The moraine systems of southwestern Ontario. Transactions of the Royal Canadian Institute 10, 57 79.Google Scholar
Terasmae, J., (1959). Notes on the Champlain Sea episode in the St. Lawrence lowland, Quebec. Science 130, 334 336.Google Scholar
Terasmae, J., (1968). A discussion of deglaciation and the boreal forest history in the northern Great Lakes region. Proceedings of the Entomological Society of Ontario 99, 31 43.Google Scholar
Terasmae, J., Hughes, O.L., (1960). Glacial retreat in the North Bay area, Ontario. Science 131, 1444 1446.Google Scholar
Thornthwaite, C.W., (1948). An approach toward a rational classification of climate. Geographical Review 38, 55 94.Google Scholar
Tovell, W.M., Deane, R.E., (1966). Grizzly bear skull: site of a find near Lake Simcoe. Science 154, 158.Google Scholar
Watts, W.A., Bright, R.C., (1968). Pollen, seed, and mollusk analysis of a sediment core from Pickerel Lake, northeastern South Dakota. Geological Society of America Bulletin 79, 855 876.Google Scholar
Watts, W.A., Winter, T.C., (1966). Plant macrofossils from Kirchner Marsh, Minnesota—a paleoecological study. Geological Society of America Bulletin 77, 1339 1360.Google Scholar
Wood, R.D., (1967). Charophytes of North America. Stella's Printing, West Kingston, Rhode Island 72.Google Scholar
Wright, H.E. Jr., (1971). Retreat of the Laurentide ice sheet from 14,000 to 9,000 years ago. Quaternary Research 1, 316 330.Google Scholar
Zumberge, J.H., Potzger, J.E., (1956). Late Wisconsin chronology of the Lake Michigan basin correlated with pollen studies. Geological Society of America Bulletin 67, 271 288.Google Scholar