Hostname: page-component-cd9895bd7-p9bg8 Total loading time: 0 Render date: 2024-12-28T15:33:13.742Z Has data issue: false hasContentIssue false
  • English
  • Français

Fingerprinting of glacial silt in lake sediments yields continuous records of alpine glaciation (35–15 ka), western USA

Published online by Cambridge University Press:  11 July 2012

Joseph G. Rosenbaum ,
Richard L. Reynolds  and
Steven M. Colman
Joseph G. Rosenbaum*
Affiliation:
U.S. Geological Survey, MS 980 Federal Center, Denver, CO 80225, USA
Richard L. Reynolds
Affiliation:
U.S. Geological Survey, MS 980 Federal Center, Denver, CO 80225, USA
Steven M. Colman
Affiliation:
Large Lake Observatory, University of Minnesota, Duluth, MN 55812, USA Department of Geological Sciences, University of Minnesota, Duluth, MN 55812, USA
*
⁎Corresponding author at: USGS MS980 DFC, Box 25046, Denver, CO 80225, USA. Fax: + 1 303 236 5349. Email Address:jrosenbaum@usgs.gov
Get access Rights & Permissions [Opens in a new window]

Abstract

Fingerprinting glacial silt in last glacial-age sediments from Upper Klamath Lake (UKL) and Bear Lake (BL) provides continuous radiocarbon-dated records of glaciation for the southeastern Cascade Range and northwestern Uinta Mountains, respectively. Comparing of these records to cosmogenic exposure ages from moraines suggests that variations in glacial flour largely reflect glacial extent. The two areas are at similar latitudes and yield similar records of glacial growth and recession, even though UKL lies less than 200 km from the ocean and BL is in the continental interior. As sea level began to fall prior to the global Last Glacial Maximum (LGM), existing glaciers in the UKL area expanded. Near the beginning of the global LGM (26.5 ka), the BL record indicates onset of glaciation and UKL-area glaciers underwent further expansion. Both records indicate that local glaciers reached their maximum extents near the end of the global LGM, remained near their maxima for ~ 1000 yr, and underwent two stages of retreat separated by a short period of expansion.

Keywords

Bear LakeCascade RangeGlacial siltLake sedimentLast glacial intervalMagnetic propertiesUinta MountainsUpper Klamath Lake
Type
Articles
Information
Quaternary Research , Volume 78 , Issue 2 , September 2012 , pp. 333 - 340
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

Ashby, J.M., Geissman, J.W., and Weil, A.B. Paleomagnetic and fault kinematic assessment of Laramide-age deformation in the eastern Uinta Mountains or, has the eastern end of the Uinta Mountains been bent?. Dehler, C.M., Pederson, J.L., Sprinkel, D.A., Kowallis, B.J. Uinta Mountain Geology 33, (2005). Utah Geological Association Publication, 285–320.Google Scholar
Bakke, J., Lie, Ø., Nesje, A., Dahl, S.O., and Paasche, Ø. Utilizing physical sediment variability in glacier-fed lakes for continuous glacier reconstructions during the Holocene, northern Folgefonna, western Norway. The Holocene 15, (2005). 161–176.Google Scholar
Bakke, J., Dahl, S.O., Paasche, Ø., Simonsen, J.R., Kvisvik, B., Bakke, K., and Nesje, A. A complete record of Holocene glacier variability at Austre Okstindbreen, northern Norway: an integrated approach. Quaternary Science Reviews 29, (2010). 1246–1262.Google Scholar
Balco, G., Stone, J.O., Lifton, N.A., and Dunai, T.J. A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements. Quaternary Geochronology 3, (2008). 174–195.Google Scholar
Benson, L.V., May, H.M., Antweiler, R.C., Brinton, T.I., Kashgarian, M., Smoot, J.P., and Lund, S.P. Continuous lake-sediment records of glaciation in the Sierra Nevada between 52,600 and 12,500 14CyrBP. Quaternary Research 50, (1998). 113–127.Google Scholar
Benson, L., Madole, R., Landis, G., and Gosse, J. New data for Late Pleistocene Pinedale alpine glaciation in southwestern Colorado. Quaternary Science Reviews 24, (2005). 49–60.Google Scholar
Bischoff, J.L., and Cummins, K. Wisconsin glaciation of the Sierra Nevada (79,000–15,000 yr BP) as recorded by rock flour in sediments of Owens Lake, California. Quaternary Research 55, (2001). 14–24.Google Scholar
Bradbury, J.P., Colman, S.M., and Dean, W.E. Limnological and climatic environments at Upper Klamath Lake, Oregon, during the past 45,000 yr. Journal of Paleolimnology 31, (2004). 167–188. (Upper Klamath Lake, Oregon, USA) CrossRefGoogle Scholar
Bryant, B., (1992). Geologic and structure maps of the Salt Lake City 1 × 2 quadrangle, Utah and Wyoming. U.S. Geological Survey Miscellaneous Investigation Series Map I-1997, 1:250,000.Google Scholar
Carver, G.A., (1972). Glacial Geology of the Mountain Lakes Wilderness and Adjacent Parts of the Cascade Range. PhD Dissertation. University of Washington Oregon, Seattle., 76 pp.Google Scholar
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, (2009). 710–714.Google Scholar
Colman, S.M., Bradbury, J.P., McGeehin, J.P., Holmes, C.W., Edginton, D., and Sarna-Wojcicki, A.M. Chronology of sediment deposition in Upper Klamath Lake, Oregon. Journal of Paleolimnology 31, (2004). 139–149. (Upper Klamath Lake, Oregon, USA) Google Scholar
Colman, S.M., Rosenbaum, J.G., Kaufman, D.S., Dean, W.E., and McGeehin, J.P. Radiocarbon ages and age models for the past 30,000 yr in Bear Lake, Utah and Idaho. Rosenbaum, J.G., and Kaufman, D.S. Paleoenvironments of Bear Lake, Utah and Idaho, and Its Catchment. Geological Society of America Special Paper 450, (2009). 133–144.Google Scholar
Dahl, S.O., Bakke, J., Lie, O., and Nesje, A. Reconstruction of former glacier equilibrium-line altitudes based on proglacial sites: an evaluation of approaches and selection of sites. Quaternary Science Reviews 22, (2003). 275–287.Google Scholar
Dunlop, D.J., and Özdemir, Ö. Rock Magnetism: Fundamentals and Frontiers. (1997). Cambridge University Press, New York, NY. 573 pp.Google Scholar
Gibbons, A.B., Megeath, J.D., and Pierce, K.L. Probability of moraine survival in a succession of glacial advances. Geology 12, (1984). 327–330.2.0.CO;2>CrossRefGoogle Scholar
Hallet, D.J., Hills, L.U., and Clague, J.J. New accelerator mass spectrometer radiocarbon ages for the Mazama tephra layer from Kootenay National Park, British Columbia, Canada. Canadian Journal of Earth Science 34, (1997). 1202–1209.Google Scholar
Heil, C.W., King, J.W., Rosenbaum, J.G., Reynolds, R.L., and Colman, S.M. Paleomagnetism and environmental magnetism of GLAD800 sediment cores from Bear Lake, Utah and Idaho. Rosenbaum, J.G., and Kaufman, D.S. Paleoenvironments of Bear Lake, Utah and Idaho, and Its Catchment. Geological Society of America Special Paper 450, (2009). 291–310.Google Scholar
Karlén, W. Lacustrine sediments and tree-limit variations as evidence of Holocene climatic fluctuations in Lappland, northern Sweden. Geografiska Annaler 58A, (1976). 1–34.Google Scholar
Kaufman, D.S., Bright, J., Dean, W.E., Rosenbaum, J.G., Moser, K., Anderson, R.S., Colman, S.M., Heil, C.W., Jiménez-Moreno, G., Reheis, M.C., and Simmons, K.R. A quarter-million years of paleoenvironmental change at Bear Lake, Utah and Idaho. Rosenbaum, J.G., and Kaufman, D.S. Paleoenvironments of Bear Lake, Utah and Idaho, and Its Catchment. Geological Society of America Special Paper 450, (2009). 311–351.Google Scholar
King, J.W., and Channel, J.E.T. Sedimentary magnetism, environmental magnetism, and magnetostratigraphy. Reviews of Geophysics 29, (1991). 358–370.Google Scholar
Laabs, B.J.C., Munroe, J.S., Rosenbaum, J.G., Refsnider, K.A., Mickelson, D.M., Singer, B.S., and Caffee, M.W. Chronology of the last glacial maximum in the upper Bear River basin, Utah. Arctic, Antarctic, and Alpine Research 39, (2007). 537–548.Google Scholar
Laabs, B.J.C., Refsnider, K.A., Munroe, J.S., Mickelson, D.M., Applegate, P.J., Singer, B.S., and Caffee, M.W. Latest Pleistocene glacial chronology of the Uinta Mountains: support for moisture-driven asynchrony of the last deglaciation. Quaternary Science Reviews 28, (2009). 1171–1187.Google Scholar
Laabs, B.J.C., Marchetti, D.W., Munroe, J.S., Refsnider, K.A., Gosse, J.C., Lips, E.W., Becker, R.A., Mickelson, D.M., and Singer, B.S. Chronology of latest Pleistocene mountain glaciation in the western Wasatch Mountains, Utah, U.S.A. Quaternary Research (2011). http://dx.doi.org/10.1016/j.yqres.2011.06.016 Google Scholar
Leemann, A., and Niessen, F. Holocene glacial activity and climatic variations in the Swiss Alps: reconstructing a continuous record from proglacial lake sediments. The Holocene 4, (1994). 259–268.Google Scholar
Leonard, E.M. Use of lacustrine sedimentary sequences as indicators of Holocene glacial history, Banff National Park, Alberta, Canada. Quaternary Research 26, (1986). 218–231.Google Scholar
Leonard, E.M. The relationship between glacial activity and sediment production: evidence from a 4450-yr varve record of neoglacial sedimentation in Hector Lake, Alberta, Canada. Journal of Paleolimnology 17, (1997). 319–330.Google Scholar
Leonard, E.M. A continuous Holocene, glacial record inferred from proglacial lake sediments in Banff National Park, Alberta, Canada. Quaternary Research 51, (1999). 1–13.Google Scholar
Licciardi, J.M., and Pierce, K.L. Cosmogenic exposure-age chronologies of Pinedale and Bull Lake glaciations in greater Yellowstone and the Teton Range, USA. Quaternary Science Reviews 27, (2008). 814–831.Google Scholar
Licciardi, J.M., Clark, P.U., Brook, E.J., Pierce, K.L., Kurz, M.D., Elmore, D., and Sharma, P. Cosmogenic 3He and 10Be chronologies of the late Pinedale northern Yellowstone ice cap, Montana, USA. Geology 29, (2001). 1095–1098.Google Scholar
Licciardi, J.M., Clark, P.U., Brook, E.J., Elmore, D., and Sharma, P. Variable response of western glaciers during the last glaciation. Geology 32, (2004). 81–84.Google Scholar
Munroe, J.S., Laabs, B.J.C., Shakun, J.D., Singer, B.S., Mickelson, D.M., Refsnider, K.A., and Caffee, M.W. Latest Pleistocene advance of alpine glaciers in the southwestern Uinta Mountains, northeastern Utah, USA: evidence for the influence of local moisture sources. Geology 4, (2006). 841–844.Google Scholar
Nesje, A., Dahl, S.O., Andersson, C., and Matthhews, J.A. The lacustrine sedimentary sequence in Sygneskardvatnet, western Norway: a continuous, high-resolution record of the Jostedalsbreen ice cap during the Holocene. Quaternary Science Reviews 19, (2000). 1047–1065.Google Scholar
Noon, P.E., Birks, H.J.B., Jones, V.J., and Ellis-Evans, J.C. Quantitative models for reconstructing catchment ice-extent using physical–chemical characteristics of lake sediments. Journal of Paleolimnology 25, (2001). 375–392.CrossRefGoogle Scholar
Phillips, F.M., Zreda, M.G., Gosse, J.C., Klein, J., Evenson, E.B., Hall, R.D., Chadwick, O.A., and Sharma, P. Cosmogenic 36Cl and 10Be ages of Quaternary glacial and fluvial deposits of the Wind River Range, Wyoming. Geological Society of America Bulletin 109, (1997). 1453–1463.Google Scholar
Refsnider, K.A., Laabs, B.J.C., Plummer, M.A., Mickelson, D.M., Singer, B.S., and Caffee, M.W. Last glacial maximum climate inferences from cosmogenic dating and glacier modeling of the western Uinta ice field, Uinta Mountains, Utah. Quaternary Research 69, (2008). 130–144.Google Scholar
Reheis, M.C., Laabs, B.J.C., and Kaufman, D.S. Geology and geomorphology of Bear Lake Valley and upper Bear River, Utah and Idaho. Rosenbaum, J.G., and Kaufman, D.S. Paleoenvironments of Bear Lake, Utah and Idaho, and Its Catchment. Geological Society of America Special Paper 450, (2009). 15–48.Google Scholar
Reynolds, R.L., Rosenbaum, J.G., Rapp, J., Kerwin, M.W., Bradbury, J.P., Colman, S.C., and Adam, D. Record of Late Pleistocene glaciation and deglaciation in the southern Cascade Range: I. Petrologic evidence from lacustrine sediment in Upper Klamath Lake, southern Oregon. Journal of Paleolimnology 31, (2004). 217–233. (Upper Klamath Lake, Oregon, USA) Google Scholar
Rodbell, D.T., Seltzer, G.O., Mark, B.G., Smith, J.A., and Abbott, M.B. Clastic sediment flux to tropical Andean lakes: records of glaciation and soil erosion. Quaternary Science Reviews 27, (2008). 1612–1626.Google Scholar
Rosenbaum, J.G., and Reynolds, R.L. Record of Late Pleistocene glaciation and deglaciation in the southern Cascade Range: II. Flux of glacial flour in a sediment core from Upper Klamath Lake, Oregon. Journal of Paleolimnology 31, (2004). 235–252. (Upper Klamath Lake, Oregon. USA) Google Scholar
Rosenbaum, J.G., and Reynolds, R.L. Basis for paleoenvironmental interpretation of magnetic properties of sediment from Upper Klamath Lake (Oregon): effects of weathering and mineralogical sorting. Journal of Paleolimnology 31, (2004). 253–265. (Upper Klamath Lake, Oregon. USA) Google Scholar
Rosenbaum, J.G., Heil, C.W. Jr. The glacial/deglacial history of sedimentation in Bear Lake, Utah and Idaho. Rosenbaum, J.G., and Kaufman, D.S. Paleoenvironments of Bear Lake, Utah and Idaho, and Its Catchment. Geological Society of America Special Paper 450, (2009). 247–261.Google Scholar
Rosenbaum, J.G., Dean, W.E., Reynolds, R.L., and Reheis, M.C. Allogenic sedimentary components of Bear Lake, Utah and Idaho. Rosenbaum, J.G., and Kaufman, D.S. Paleoenvironments of Bear Lake, Utah and Idaho, and Its Catchment. Geological Society of America Special Paper 450, (2009). 145–168.Google Scholar
Thomas, E.K., Szymanski, J., and Briner, J.P. Holocene alpine glaciation inferred from lacustrine sediments on northeastern Baffin Island, Arctic Canada. Journal of Quaternary Science 25, (2010). 146–161.Google Scholar
Vasskog, K., Paasche, Ø., Nesje, A., Boyle, J.F., and Birks, H.J.B. A new approach for reconstructing glacier variability based on lake sediments recording input from more than one glacier. Quaternary Research 77, (2012). 192–204.Google Scholar