Hostname: page-component-586b7cd67f-r5fsc Total loading time: 0 Render date: 2024-11-22T18:56:56.807Z Has data issue: false hasContentIssue false
  • English
  • Français

The 8.2-ka abrupt climate change event in Brown's Lake, northeast Ohio

Published online by Cambridge University Press:  20 January 2017

Brian Lutz ,
Gregory Wiles ,
Thomas Lowell  and
Joshua Michaels
Brian Lutz*
Affiliation:
Department of Geology, The College of Wooster, 1189 Beall Ave., Wooster, OH 44691, USA
Gregory Wiles
Affiliation:
Department of Geology, The College of Wooster, 1189 Beall Ave., Wooster, OH 44691, USA
Thomas Lowell
Affiliation:
Department of Geology, University of Cincinnati, P.O. Box 0013, Cincinnati, OH 45221, USA
Joshua Michaels
Affiliation:
Department of Geology, University of Cincinnati, P.O. Box 0013, Cincinnati, OH 45221, USA
*
⁎Corresponding author. E-mail address:[email protected] (B. Lutz).
Get access Rights & Permissions [Opens in a new window]

Abstract

Many Northern Hemisphere paleoclimatic records, including ice cores, speleothems, lake sediments, ocean cores and glacier chronologies, indicate an abrupt cooling event about 8200 cal yr BP. A new well-dated series of sediment cores taken from Brown's Lake, a kettle in Northeast Ohio, shows two closely spaced intervals of loess deposition during this time period. The source of loess is uncertain; however, it is likely from an abandoned drainage and former glacial lake basin located to the north of the stagnant ice topography that gave rise to the kettle lake. Strong visual stratigraphy, loss on ignition data and sediment grain size analyses dated with 3 AMS radiocarbon dates place the two intervals of loess deposition between 8950 and 8005 cal yr BP. The possibility of a two-phase abrupt climate change at this time is a finding that has been suggested in other research. This record adds detail to the spatial extent and timing as well as possible structure of the 8.2-ka abrupt climate change event.

Keywords

Abrupt climate change8.2-ka eventLoessLakesHolocene climate change
Type
Short Paper
Information
Quaternary Research , Volume 67 , Issue 2 , March 2007 , pp. 292 - 296
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.)

References

Alley, R.B., and Ágústsdóttir, A.M. The 8k event: Cause and consequences of major Holocene abrupt climate change. Quaternary Science Reviews 24, (2005). 1123–1149.CrossRefGoogle Scholar
Alley, R.B., Mayewski, P.A., Sowers, T., Stuiver, M., Taylor, K.C., and Clark, P.U. Holocene climatic instability: A prominent, widespread event 8200 years ago. Geology 25, (1997). 483–486.2.3.CO;2>CrossRefGoogle Scholar
Alley, R.B., Marotzke, J., Nordhaus, W.D., Overpeck, J.T., Peteet, D.M., Pielke, R.A. Jr., Pierrehumbert, R.T., Rhines, B., Stocker, T.F., Talley, L.D., and Wallace, J.M. Abrupt climate change. Science 299, (2003). 2005–2010.CrossRefGoogle ScholarPubMed
Bailey, C., (2003). Reconstruction of the late-glacial environmental history of Brown's Lake Bog, Northeast Ohio.. Unpublished undergraduate thesis. The College of Wooster.Google Scholar
Baldini, J.U.L., McDermott, F., and Fairchild, I.J. Structure of the 8200-year cold event revealed by a speleothem trace element record. Science 296, (2002). 2203–2206.CrossRefGoogle ScholarPubMed
Clarke, G.K.C., Leverington, D.W., Teller, J.T., and Dyke, A.S. Paleohydraulics of the last outburst flood from glacial Lake Agassiz and the 8200 BP cold event. Quaternary Science Reviews 23, (2004). 389–407.CrossRefGoogle Scholar
Denton, G.H., and Karlén, W. Holocene climatic variations—Their pattern and possible cause. Quaternary Research 3, (1973). 155–205.CrossRefGoogle Scholar
Garnett, E.R., Andrews, J.E., Preece, R.C., and Dennis, P.F. Climatic change recorded by stable isotopes and trace elements in a British Holocene tufa. Journal of Quaternary Science 19, (2004). 251–262.CrossRefGoogle Scholar
Hayward, R.K., and Lowell, T.V. Variations in the loess accumulation rates in the mid-continent, United States, as reflected by magnetic susceptibility. Geology 21, (1993). 821–824.2.3.CO;2>CrossRefGoogle Scholar
Heiri, O., Lemcke, G., and Lotter, A.F. Loss on ignition as a method for estimating organic and carbonate content in sediments: Reproducibility and comparability of results. Journal of Paleolimnology 25, (2001). 101–110.CrossRefGoogle Scholar
Hu, R.S., Slawinski, D., Wright, H.E. Jr., Ito, E., Johnson, R.B., Kelts, K.R., McEwan, R.F., and Boedigheimer, A. Abrupt changes in North American climate during the early Holocene times. Nature 400, (1999). 437–440.CrossRefGoogle Scholar
Hubbard, G.D. Ancient finger lakes of Ohio. American Journal of Science 25, (1908). 239–243.CrossRefGoogle Scholar
Keigwin, L.D., Sachs, J.P., Rosenthal, Y., and Boyle, E.A. The 8200 year B.P. event in the slope water system, western subpolar North Atlantic. Paleoceanography 20, 2 (2005). A2003 CrossRefGoogle Scholar
Kurek, J., Cwynar, L.C., and Spear, R.W. The 8200 cal yr BP cooling event in eastern North America and the utility of midge analysis for Holocene temperature reconstructions. Quaternary Science Reviews 23, (2004). 627–639.CrossRefGoogle Scholar
Leuenberger, M.C., Lang, C., and Schwander, J. Delta (super 15) N measurements as a calibration tool for the paleothermometer and gas–ice age differences: A case study for the 8200 B.P. event on GRIP ice. Journal of Geophysical Research 104D, (1994). 22163–22170.Google Scholar
Mayewski, P.A., Rohling, E.E., Stager, J.C., Karlén, W., Maasch, K.A., Meeker, L.D., Meyerson, E.A., Gasse, F., van Kreveld, S., Holmgren, K., Lee-Thorp, J., Rosqvist, G., Rack, F., Staubwasser, M., Schneiderk, R.R., and Steig, E.J. Holocene climate variability. Quaternary Research 62, (2004). 243–255.CrossRefGoogle Scholar
Schmidt, G.A., and LeGrande, A.N. The Goldilocks abrupt climate change event. Quaternary Science Reviews 24, (2005). 1109–1110.CrossRefGoogle 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.CrossRefGoogle Scholar
Shuman, B., Bartlein, P., Logar, N., Newby, P., Webb, T. III Parallel climate and vegetation responses to the early Holocene collapse of the Laurentide Ice Sheet. Quaternary Science Reviews 21, 1793, (2002). 1805 Google Scholar
Thompson, L.G., Mosley-Thompson, E., Davis, M.E., Henderson, K.A., Brecher, H.H., Zagorodnov, V.S., Mashiotta, T.A., Lin, P.N., Mikhalenko, V.N., Hardy, D.R., and Beer, J. Kilimanjaro ice core records: Evidence of Holocene climate change in tropical Africa. Science 298, (2002). 589–593.CrossRefGoogle ScholarPubMed
Tinner, W., and Lotter, A.F. Central European vegetation response to abrupt climate change at 8.2 ka. Geology 29, (2001). 551–554.2.0.CO;2>CrossRefGoogle Scholar
Yu, Z.C., and Eicher, U. Abrupt climate oscillations during the last deglaciation in central North America. Science 282, (1998). 2235–2238.CrossRefGoogle ScholarPubMed