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Paleoenvironmental records of water level and climatic changes from the middle to late holocene at a Lake Erie coastal wetland, Ontario, Canada

Published online by Cambridge University Press:  20 January 2017

Sarah A. Finkelstein  and
Anthony M. Davis
Sarah A. Finkelstein*
Affiliation:
Department of Geography, University of Toronto, 100 St. George Street, Toronto, Ontario, Canada M5S 3G3
Anthony M. Davis
Affiliation:
Department of Geography, University of Toronto, 100 St. George Street, Toronto, Ontario, Canada M5S 3G3
*
*Corresponding author. Tel.: +1 416 978 3375; fax: +1 416 9463886. E-mail address:[email protected](S.A. Finkelstein).
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Abstract

Pollen and diatom assemblages, and peat stratigraphies, from a coastal wetland on the northern shore of Lake Erie were used to analyze water level and climatic changes since the middle Holocene and their effects on wetland plant communities. Peat deposition began 4700 cal yr B.P. during the Nipissing II transgression, which was driven by isostatic rebound. At that time, a diatom-rich wild rice marsh existed at the site. Water level dropped at the end of the Nipissing rise at least 2 m within 200 yr, leading to the development of shallower-water plant communities and an environment too dry for most diatoms to persist. The sharp decline in water level was probably driven primarily by outlet incision, but climate likely played some role. The paleoecological records provide evidence for post-Nipissing century-scale transgressions occurring around 2300, 1160, 700 and 450 cal yr B.P. The chronology for these transgressions correlates with other studies from the region and implies climatic forcing. Peat inception in shallow sloughs across part of the study area around 700 cal yr B.P. coincides with the Little Ice Age. These records, considered alongside others from the region, suggest that the Little Ice Age may have resulted in a wetter climate across the eastern Great Lakes region.

Keywords

PollenDiatomsPeat stratigraphyGreat Lakes water levelsNipissing riseLittle Ice AgeCoastal wetlandsLake ErieLate HoloceneOntario
Type
Original Articles
Information
Quaternary Research , Volume 65 , Issue 1 , January 2006 , pp. 33 - 43
Copyright
University of Washington

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References

Baedke, S.J., and Thompson, T.A. (2000). A 4,700 year record of lake level and isostasy for Lake Michigan. Journal of Great Lakes Research 26, 416–426.CrossRefGoogle Scholar
Baker, R.G., Maher, L.J., Chumbley, C.A., and Van Zant, K.A. (1992). Patterns of Holocene environmental change in the Midwest. Quaternary Research 37, 379–389.CrossRefGoogle Scholar
Battarbee, R.W., Jones, V.J., Flower, R.J., Cameron, N.G., Bennion, H., Carvalho, L., and Juggins, S. (2001). Diatoms In: Smol, J.P., Birks, H.J.B., and Last, W.M. Tracking Environmental Change Using Lake Sediments. Terrestrial, Algal, and Siliceous Indicators vol. 3, Kluwer, Dordrecht, The Netherlands., pp. 155–202.Google Scholar
Bennett, K.D., and Willis, K.J. (2001). Pollen. In: Smol, J.P., Birks, H.J.B., Last, W.M. Tracking Environmental Change Using Lake Sediments. Terrestrial, Algal, and Siliceous Indicators vol. 3, Kluwer, Dordrecht, The Netherlands. 5–32.Google Scholar
Booth, R.K., and Jackson, S.T. (2003). A high-resolution record of late-Holocene moisture variability from a Michigan raised bog, USA. The Holocene 13, 863–876.CrossRefGoogle Scholar
Booth, R.K., Jackson, S.T., and Thompson, T.A. (2002). Paleoecology of a northern Michigan lake and the relationships among climate, vegetation and Great Lakes water levels. Quaternary Research 57, 120–130.Google Scholar
Boyle, J. (2001). Inorganic geochemical methods in paleolimnology. In: Last, W.M., Smol, J.P. Tracking Environmental Change Using Lake Sediments. Physical and Geochemical Methods vol. 2, Kluwer, Dordrecht, The Netherlands.83–141.Google Scholar
Bunting, M.J., Duthie, H.C., Campbell, D.R., Warner, B.G., and Turner, L.J. (1997). A paleoecological record of recent environmental change at Big Creek Marsh, Long Point, Lake Erie. Journal of Great Lakes Research 23, 349–368.Google Scholar
Bunting, M.J., Morgan, C.R., van Bakel, M., and Warner, B.G. (1998). Pre-European settlement conditions and human disturbance of a coniferous swamp in southern Ontario. Canadian Journal of Botany 76, 1770–1779.Google Scholar
Campbell, I.D., and McAndrews, J.H. (1991). Cluster analysis of late Holocene pollen trends in Ontario. Canadian Journal of Botany 69, 1719–1730.CrossRefGoogle Scholar
Clark, J.S., and Royall, P.D. (1995). Transformation of a northern hardwood forest by aboriginal (Iroquois) fire: charcoal evidence from Crawford Lake, Ontario, Canada. The Holocene 5, 1–9.Google Scholar
Coakley, J.P. (1989). The origin and evolution of a complex cuspate foreland: Pointe-aux-Pins, Lake Erie, Ontario. Geographie Physique Et Quaternaire 43, 65–76.CrossRefGoogle Scholar
Coakley, J.P., and Lewis, C.F.M. (1985). Postglacial lake levels in the Erie basin. In: Karrow, P.F., Calkin, P. Quaternary Evolution of the Great Lakes. Special Paper vol. 30, Geological Association of Canada, Ottawa.195–212.Google Scholar
Crow, G.E., and Hellquist, C.B. (2000). Aquatic and Wetland Plants. University of Wisconsin Press, Madison.Google Scholar
Cwynar, L.C., Burden, E., and McAndrews, J.H. (1979). Inexpensive sieving method for concentrating pollen and spores from fine-grained sediments. Canadian Journal of Earth Sciences 16, 1115–1120.CrossRefGoogle Scholar
Davis, M.B., Douglas, C., Calcote, R., Cole, K.L., Winkler, M.G., and Flakne, R. (2000). Holocene climate in the western Great Lakes National Parks and Lakeshores: implications for future climatic changes. Conservation Biology 14, 968–983.Google Scholar
Earle, J.C., and Duthie, H.C. (1984). A multivariate statistical approach for interpreting marshland diatom succession. In: Ricard, M. Proceedings of the 8th Diatom Symposium, Paris. Koeltz Scientific Books, Koenigstein, Germany.441–458.Google Scholar
Fægri, K., and Iversen, J. (1989). Textbook of Pollen Analysis. 4th ed.John Wiley and Sons, Chichester.Google Scholar
Finkelstein, S.A. (2003). Identifying pollen grains of Typha latifolia, Typha angustifolia and Typha xglauca . Canadian Journal of Botany 81, 985–990.CrossRefGoogle Scholar
Finkelstein, S.A., and Davis, A.M. (2005). Modern pollen rain and diatom assemblages in a Lake Erie coastal marsh. Wetlands 25, 551–563.CrossRefGoogle Scholar
Finkelstein, S.A., Peros, M.C., and Davis, A.M. (2005). Late Holocene paleoenvironmental change in a Great Lakes coastal wetland: integrating pollen and diatom datasets. Journal of Paleolimnology 33, 1–12.Google Scholar
Fraser, G.S., Larsen, C.E., and Hester, N.C. (1990). Climate control of lake levels in the Lake Michigan and Lake Huron basins. In: Schneider, A.F., and Fraser, G.S. Late Quaternary History of the Lake Michigan Basin. Special Paper vol. 251, Geological Society of America, Boulder, CO.75–89.Google Scholar
Gajewski, K. (1988). Late Holocene climate changes in Eastern North-America estimated from pollen data. Quaternary Research 29, 255–262.Google Scholar
Gajewski, K., Winkler, M.G., and Swain, A.M. (1985). Vegetation and fire history from three lakes with varved sediments in northwestern Wisconsin (USA). Review of Palaeobotany and Palynology 44, 277–292.CrossRefGoogle Scholar
Grimm, E.C. (1987). CONISS: a Fortran-77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Computers and Geosciences 13, 13–35.Google Scholar
Haas, J.N., and McAndrews, J.H. (1999). The summer drought related hemlock (Tsuga canadensis) decline in Eastern North America 5700 to 5100 years ago. In: McManus, K.A., Shields, K.S., and Souto, D.R. Symposium on Sustainable Management of Hemlock Ecosystems in Eastern North America. General Technical Report NE-267. US Department of Agriculture, Forest Service, Northeastern Research Station, Durham, NH. 81–88.Google Scholar
Hansel, A.K., Mickelson, D.M., Schneider, A.F., and Larson, C.E. (1985). Late Wisconsinan and Holocene history of the Lake Michigan basin. In: Karrow, P.F., and Calkin, P.E. Quaternary Evolution of the Great Lakes. Special paper vol. 30, Geological Association of Canada, Ottawa.39–53.Google Scholar
Jackson, S.T., and Booth, R.K. (2002). The role of late Holocene climate variability in the expansion of yellow birch in the western Great Lakes region. Diversity and Distributions 8, 275–284.Google Scholar
Janssen, C.R. (1966). Recent pollen spectra from the deciduous and coniferous forests of northeastern Minnesota: a study in pollen dispersal. Ecology 47, 804–825.Google Scholar
Kapp, R.O., Davis, O.K., King, J.E., and Ronald, O. (2000). Kapp's Pollen and Spores. 2nd ed. American Association of Stratigraphic Palynologists Foundation Publication, College Station, TX, USA.Google Scholar
Krammer, K., and Lange-Bertalot, H. (1986–1991). Bacillariophyceae. Susswasser-flora von Mitteleuropa 2(1–4). Gustav Fischer, Stuttgart, Germany.Google Scholar
Larsen, C.E. (1985). A stratigraphic study of beach features on the southeastern shore of Lake Michigan: new evidence for Holocene lake level fluctuations. Environmental Geology Notes vol. 112, Illinois State Geological Survey, Champaign, IL.Google Scholar
Lee, G.-A., Davis, A.M., Smith, D.G., and McAndrews, J.H. (2004). Identifying fossil wild rice (Zizania) pollen from Cootes Paradise, Ontario. Journal of Archaeological Science 31, 411–421.Google Scholar
Maycock, P.F. (1963). The phytosociology of the deciduous forest of extreme southern Ontario. Canadian Journal of Botany 41, 379–438.CrossRefGoogle Scholar
McAndrews, J.H. (1981). Late Quaternary climate of Ontario: temperature trends from the fossil record. In: Mahaney, W.C. Quaternary Paleoclimate. GeoAbstracts, Norwich.319–355.Google Scholar
McAndrews, J.H., and Boyko-Diakonow, M. (1989). Pollen analysis of varved sediment at Crawford Lake, Ontario: evidence of Indian and European farming. In: Fulton, R.J. Quaternary Geology of Canada and Greenland. Geology of Canada vol. 1, Geological Survey of Canada, Ottawa.528–530.Google Scholar
McAndrews, J.H., Berti, A.A., and Norris, G. (1973). Key to the Quaternary Pollen and Spores of the Great Lakes Region. Royal Ontario Museum, Toronto.CrossRefGoogle Scholar
McCarthy, F.M.G., and McAndrews, J.H. (1988). Water levels in Lake Ontario 4230–2000 years BP: evidence from Grenadier Pond, Toronto, Canada. Journal of Paleolimnology 1, 99–113.CrossRefGoogle Scholar
Monaghan, G.W. (2002). Geoarchaeology of the Marquette Viaduct relocation project sites 20BY28 and 20BY387, Bay City, Michigan. In: Lovis, W.A. A Bridge to the Past. MSU Museum and Department of Anthropology, East Lansing, MI.2–1–2–38.Google Scholar
Pengelly, J.W., Tinkler, K.J., Parkins, W.G., and McCarthy, F.M.G. (1997). 12,600 years of lake level changes, changing sills, ephemeral lakes and Niagara Gorge erosion in the Niagara Peninsula and eastern Lake Erie basin. Journal of Paleolimnology 17, 377–402.CrossRefGoogle Scholar
Rodionov, S.N. (1994). Association between winter precipitation and water level fluctuations in the Great Lakes and atmospheric circulation patterns. Journal of Climate 7, 1693–1706.Google Scholar
Smith, I.R. (2002). Diatom-based Holocene paleoenvironmental records from continental sites on northeastern Ellesmere Island, high Arctic, Canada. Journal of Paleolimnology 27, 9–28.Google Scholar
Stockmarr, J. (1971). Tablets with spores used in absolute pollen analysis. Pollen et Spores 13, 615–621.Google Scholar
Stuiver, M., and Reimer, P.J. (1993). Extended 14-C database and revised CALIB 3.0 14-C age calibration program. Radiocarbon 35, 215–230.Google Scholar
Stuiver, M., Reimer, P.J., Bard, E., Beck, J.W., Burr, G.S., Hughen, K.A., Kromer, B., McCormac, G., van der Plicht, J., and Spurk, M. (1998). INTCAL98 Radiocarbon Age Calibration, 24000-0 cal BP. Radiocarbon 40, 1041–1083.Google Scholar
Szeicz, J.M., and MacDonald, G.M. (1991). Postglacial vegetation history of oak savanna in southern Ontario. Canadian Journal of Botany 69, 1507–1519.Google Scholar
Telford, R.J., Heegaard, E., Birks, H.J.B. (2004). The intercept is a poor estimate of a calibrated radiocarbon age. The Holocene 14, 296–298.CrossRefGoogle Scholar
Yang, J.R., and Duthie, H.C. (1994). Diatom paleoecology of East Lake, Ontario: a 5400 year record of limnological change. In: Marino, D., Montresor, M. Proceedings of the 13th International Diatom Symposium. Biopress Limited, Bristol, UK.555–571.Google Scholar
Yang, J.R., and Duthie, H.C. Regression and weighted averaging models relating surficial sedimentary diatom assemblages to water depth in Lake Ontario. (1995). Journal of Great Lakes Research 21, 84–94.CrossRefGoogle Scholar