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Deglaciation, basin formation and post-glacial climate change from a regional network of sediment core sites in Ohio and eastern Indiana

Published online by Cambridge University Press:  20 January 2017

Katherine C. Glover ,
Thomas V. Lowell ,
Gregory C. Wiles ,
Donald Pair ,
Patrick Applegate  and
Irena Hajdas
Katherine C. Glover*
Affiliation:
Department of Geology, University of Cincinnati, Cincinnati, OH 45221-0013, USA
Thomas V. Lowell
Affiliation:
Department of Geology, University of Cincinnati, Cincinnati, OH 45221-0013, USA
Gregory C. Wiles
Affiliation:
Department of Geology, The College of Wooster, Wooster, OH 44691, USA
Donald Pair
Affiliation:
Department of Geology, University of Dayton, Dayton, OH 45469-2364, USA
Patrick Applegate
Affiliation:
Department of Physical Geography and Quaternary Geology, Stockholm University, S-106 91 Stockholm, Sweden
Irena Hajdas
Affiliation:
PSI/ETH Laboratory for Ion Beam Physics, Schafmattstr. 20 HPK H27, CH-8093 Zurich, Switzerland
*
⁎Corresponding author at: Department of Geography, UCLA, Los Angeles, CA 90095-1524. E-mail address:kcglover@ucla.edu (K. C. Glover).
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Abstract

Many paleoclimate and landscape change studies in the American Midwest have focused on the Late Glacial and early Holocene time periods (~ 16–11 ka), but little work has addressed landscape change in this area between the Last Glacial Maximum and the Late Glacial (~ 22–16 ka). Sediment cores were collected from 29 new lake and bog sites in Ohio and Indiana to address this gap. The basal radiocarbon dates from these cores show that initial ice retreat from the maximal last-glacial ice extent occurred by 22 ka, and numerous sites that are ~ 100 km inside this limit were exposed by 18.9 ka. Post-glacial environmental changes were identified as stratigraphic or biologic changes in select cores. The strongest signal occurs between 18.5 and 14.6 ka. These Midwestern events correspond with evidence to the northeast, suggesting that initial deglaciation of the ice sheet, and ensuing environmental changes, were episodic and rapid. Significantly, these changes predate the onset of the Bølling postglacial warming (14.8 ka) as recorded by the Greenland ice cores. Thus, deglaciation and landscape change around the southern margins of the Laurentide Ice Sheet happened ~ 7 ka before postglacial changes were felt in central Greenland.

Keywords

Last Glacial MaximumTermination 1OhioIndianaMidwestRadiocarbon datingPost-glacialLacustrine depositGreenlandDeglaciation
Type
Research Article
Information
Quaternary Research , Volume 76 , Issue 3 , November 2011 , pp. 401 - 410
Copyright
University of Washington

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References

Andersen, K.K., Svensson, A., Johnsen, S.J., Rasmussen, S.O., Bigler, M., Röthlisberger, R., Ruth, U., Siggaard-Andersen, M.L., Steffensen, J.P., Dahl-Jensen, D., Vinther, B.M., and Clausen, H.B. The Greenland ice core chronology, 15–42 kyr. Part 1: constructing the time scale. Quaternary Science Reviews 25, (2006). 3246–3257.Google Scholar
Anderson, R.F., Ali, S., Bradtmiller, L.I., Nielson, S.H.H., Fleisher, M.Q., Anderson, B.E., and Burckle, L.H. Wind-driven upwelling in the Southern Ocean and the deglacial rise in atmospheric CO2 . Science 323, (2009). 1443–1448.Google Scholar
Bailey, R.E., (1972). Late- and postglacial environmental changes in northwestern Indiana. Dissertation. Indiana University, Bloomington, Indiana, USA.Google Scholar
Balco, G., and Schaefer, J.M. Cosmogenic-nuclide and varve chronologies for the deglaciation of southern New England. Quaternary Geochronology 1, (2006). 15–28.Google Scholar
Balco, G., Stone, J.O.H., Porter, S.C., and Caffee, M.W. Cosmogenic-nuclide ages for New England coastal moraines, Martha's Vineyard and Cape Cod, Massachusetts, USA. Quaternary Science Reviews 21, (2002). 2127–2135.Google Scholar
Balco, G., Briner, J., Finkel, R.C., Rayburn, J.A., Ridge, J.C., and Schaefer, J.M. Regional beryllium-10 production rate calibration for late-glacial northeastern North America. Quaternary Geochronology 4, (2009). 93–107.Google Scholar
Bard, E., Rostek, F., Turon, J., and Gendreau, S. Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic. Science 289, (2000). 1321–1324.Google Scholar
Barker, S., Diz, P., Vautravers, M.J., Pike, J., Knorr, G., Hall, I.R., and Broecker, W.S. Interhemispheric Atlantic seesaw response during the last deglaciation. Nature 457, (2009). 1097–1101.Google Scholar
Berger, A., and Loutre, M.F. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10, 4 (1991). 297–317.Google Scholar
Bevington, P., and Robinson, D.K. Data Reduction and Analysis for the Physical Sciences. (2003). McGraw Hill, St. Louis.Google Scholar
Cheng, H., Edwards, L., Broecker, W.S., Denton, G.H., Kong, X., Wang, Y., Zhang, R., and Wang, X. Ice Age Terminations. Science 326, (2009). 248–252.CrossRefGoogle ScholarPubMed
Clark, P.U., Dyke, A.S., Shakun, J.D., Carlson, A.E., Clark, J., Wohlfarth, B., Mitrovica, J.X., Hostetler, S.W., and McCabe, A.M. The last glacial maximum. Science 325, 5941 (2009). 710–771.Google Scholar
Clayton, L., and Moran, S.R. Chronology of late Wisconsinan Glaciation in Middle North America. Quaternary Science Reviews 1, (1983). 55–82.Google Scholar
Dean, W.E. Determination of carbonate and organic matter in calcareous sediments and sedimentary rocks by loss on ignition: comparison with other methods. Journal of Sedimentary Petrology 44, 1 (1974). 242–248.Google Scholar
Denton, G.H., Heusser, C.J., Lowell, T.V., Moreno, P.I., Andersen, B.G., Heusser, L.E., Schluchter, C., and Marchant, D.R. Interhemispheric linkage of paleoclimate during the last glaciation. Geografiska Annaler, Series A: Physical Geography 81, (1999). 107–153.CrossRefGoogle Scholar
Denton, G.H., Broecker, W.S., and Alley, R.B. The mystery interval 17.5 to 14.5 kyrs ago. PAGES News 14, (2006). 14–16.Google Scholar
Denton, G.H., Anderson, R.F., Toggweiler, J.R., Edwards, R.L., Schaefer, J.M., and Putnam, A.E. The last glacial termination. Science 328, (2010). 1652–1656.Google Scholar
Ellis, K.G., Mullins, H.T., and Patterson, W.P. Deglacial to middle Holocene (16,600 to 6000 calendar years BP) climate change in the northeastern United States inferred from multi-proxy stable isotope data, Seneca Lake, New York. Journal of Paleolimnology 31, (2004). 343–361.Google Scholar
Glover, K.C., (2004). Paleoenvironmental Evidence for the Last Termination in two bog sequences and a Regional Network of sites from Ohio and Eastern Indiana. Master's Thesis. University of Cincinnati, Cincinnati, Ohio, USA.Google Scholar
Hemming, S.R. Heinrich events: massive Late Pleistocene detritus layers of the North Atlantic and their global imprint. Reviews of Geophysics 42, (2004). 1–43.Google Scholar
Heusser, L., Maenza-Gmelch, T., Lowell, T., and Hinnefeld, R. Late Wisconsin periglacial environments of the southern margin of the Laurentide Ice Sheet reconstructed from pollen analyses. Journal of Quaternary Science 17, (2002). 773–780.Google Scholar
Hinnefeld, R., (1996). The eolian component of last glacial maximum lacustrine sediment; the Bunnel Road site in Southwest Ohio. Master's Thesis. University of Cincinnati, Cincinnati, Ohio, USA.Google Scholar
LeGrande, A.N., and Schmidt, G.A. Sources of Holocene variability of oxygen isotopes in paleoclimate archives. Climate of the Past 5, (2009). 441–455.Google Scholar
Lowe, J.J., Rasmussen, S.O., Björck, S., Hoek, W.Z., Steffensen, J.P., Walker, M.J.C., Yu, Z.C. the INTIMATE group Synchronisation of paleoenvironmental events in the North Atlantic region during the Last Termination: a revised protocol recommended by the INTIMATE group. Quaternary Science Reviews 27, (2008). 6–17.Google Scholar
Lowell, T.V. The application of radiocarbon age estimates to the dating of glacial sequences: an example from the Miami sublobe, Ohio, U.S.A. Quaternary Science Reviews 14, (1995). 85–99.Google Scholar
Lowell, T.V., Savage, J.M., Brockman, C.S., and Stuckenrath, R. Radiocarbon Analyses from Cincinnati, Ohio and Their Implications for Glacial Stratigraphic Interpretations. Quaternary Research 34, (1990). 1–11.Google Scholar
Lowell, T.V., Heusser, C.J., Andersen, B.G., Moreno, P.I., Hauser, A., Heusser, L.E., Schluchter, C., Marchant, D.R., and Denton, G.H. Interhemispheric correlation of late pleistocene glacial events. Science 269, (1995). 1541–1549.Google Scholar
Ogden, J.G. Forest History of Ohio. I. Radiocarbon Dates and Pollen Stratigraphy of Silver Lake, Logan County, Ohio. Ohio Journal of Science 66, (1966). 387–400.Google Scholar
Overpeck, J.T., Webb, T. III, and Prentice, I.C. Quantitative interpretation of fossil pollen spectra: dissimilarity coefficients and the method of modern analogs. Quaternary Research 23, 1 (1985). 87–108.Google Scholar
Parrenin, F., Loulergue, L., and Wolff, E. EPICA Dome C Ice Core Timescales EDC3. IGBP PAGES/World Data Center for Paleoclimatology Data Contribution Series # 2007–083. (2007). NOAA/NCDC Paleoclimatology Program, Boulder CO, USA.Google Scholar
Porter, S.C., and Carson, R.J. Problems of interpreting radiocarbon dates from dead-ice terrain, with an example from the Puget Lowland of Washington. Quaternary Research 1, (1971). 410–414.CrossRefGoogle Scholar
Pritchard, K.L., (2006). Relationships and patterns of channel formation during deglaciation of the Miami Lobe, near Piqua, Ohio. Master's Thesis. University of Cincinnati, Cincinnati, Ohio, USA.Google Scholar
Rasmussen, S.O., Andersen, K.K., Svensson, A.M., Steffensen, J.P., Vinther, B.M., Clausen, H.B., Siggaard-Andersen, M.L., Johnsen, S.J., Larsen, L.B., Dahl-Jensen, D., Bigler, M., Röthlisberger, R., Fischer, H., Goto-Azuma, K., Hansson, M.E., and Ruth, U. A new Greenland ice core chronology for the last glacial termination. Journal of Geophysical Research 111, (2006). D06102 Google Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Bronk Ramsey, C., Buck, C.E., Burr, G., Edwards, R.L., Friedrich, M., Grootes, P.M., Guilderson, T.P., Hajdas, I., Heaton, T.J., Hogg, A.G., Hughen, K.A., Kaiser, K.F., Kromer, B., McCormac, F.G., Manning, S.W., Reimer, R.W., Richards, D.A., Southon, J., Turney, C.S.M., van der Plicht, J., and Weyhenmeyer, C. IntCal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP. Radiocarbon 51, (2009). 1111–1150.Google Scholar
Schaefer, J.M., Denton, G.H., Barrell, D.J.A., Ivy-Ochs, S., Kubik, P.W., Andersen, B.G., Phillips, F.M., Lowell, T.V., and Schlüchter, C. Near-synchronous interhemispheric termination of the last glacial maximum in mid-latitudes. Science 312, 5779 (2006). 1510–1513.Google Scholar
Shane, L.C.K. Palynology and radiocarbon chronology of Battaglia Bog, Portage County, Ohio. Ohio Journal of Science 72, 2 (1975). 96–102.Google Scholar
Shane, L.C.K. Late-glacial vegetational and climatic history of the Allegheny Plateau and the Till Plains of Ohio and Indiana, U.S.A. Boreas 16, (1987). 1–20.Google Scholar
Shane, L.C.K. Changing palynological methods and their role in three successive interpretations of the late-glacial environments at Bucyrus Bog, Ohio, USA. Boreas 18, (1989). 297–309.Google Scholar
Shane, L.C.K., and Anderson, K.H. Intensity, gradients, and reversals in late glacial environmental change in east-central North America. Quaternary Science Reviews 12, (1993). 307–320.Google Scholar
Singer, D.K., Jackson, S.T., Madsen, B.A., and Wilcox, D.A. Differentiating climatic and successional influences on long-term development of a marsh. Ecology 77, (1996). 1765–1778.Google Scholar
Stuiver, M., and Reimer, P.J. Calib 6.0. Belfast, Northern Ireland: calib.org. Retrieved from calib.qub.ac.uk/calib/calib.html (2010). Google Scholar
Svensson, A., Andersen, K.K., Bligler, H.B., Dahl-Jensen, D., Davies, S.M., Johnsen, S.J., Muscheler, R., Parrenin, F., Rasmussen, S.O., Röthlisberger, R., Seierstad, I., Steffensen, J.P., and Vinther, B.M. A 60 000 year Greenland stratigraphic ice core chronology. Climate of the Past 4, (2008). 47–57.CrossRefGoogle Scholar
van der Veen, C.J. Polar ice sheets and global sea level: how well can we predict the future?. Global and Planetary Change 32, (2002). 165–194.Google Scholar
Whitehead, D.R., Jackson, S.T., Sheehan, M.C., and Leyden, B.W. Late-Glacial vegetation associated with caribou and mastodon in central Indiana. Quaternary Research 17, (1982). 241–257.Google Scholar
Williams, A.S. Late-glacial–postglacial vegetational history of the Pretty Lake region, northeastern Indiana. U.S. Geological Survey Professional Paper 686-B. (1974). U.S. Government Printing Office, Washington, D.C., USA.Google Scholar