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Luminescence chronology of late Pleistocene loess-paleosol and tephra sequences near Fairbanks, Alaska

Published online by Cambridge University Press:  20 January 2017

Glenn W. Berger
Glenn W. Berger*
Affiliation:
Desert Research Institute, 2215 Raggio Parkway, Reno, NV 89512-1095, USA
*
* Fax: +1-775-673-7397. E-mail address: [email protected]
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Abstract

Thermoluminescence (TL) and infrared-stimulated luminescence (IRSL) sediment-dating methods have been applied to paleosol- and tephra-bearing loess sequences younger than marine oxygen isotope stage (MIS) 7 at three important sites. TL ages indicate the development of significant paleosols ∼75,000 and ∼30,000 yr ago in the loess sequence at the Gold Hill site. Relatively minor soil development occurred ∼70,000 and ∼48,000 yr ago. Like the ∼75,000-yr-old soil, the 30,000-yr-old soil is apparently of global extent, and consistent in timing with inferred warm intervals elsewhere (e.g., Greenland, Europe, western and central China). At Birch Hill, replicate TL dating of primary loess combined with two earlier TL results from the same site, and with an earlier mean fission-track-glass-shard age of 140,000 ± 10,000 yr for the associated Old Crow tephra, yield a more precise numeric age of 142,300 ± 6600 yr for this Alaska/Yukon chronostratigraphic marker ash bed. Three of the TL ages at the Halfway House site are difficult to interpret, but combined with other evidence, they indicate: (1) the upper 5–6 m of loess from Halfway House is not part of the Gold Hill Loess (equivalent to pre-MIS 5 age) as long thought by T.L. Péwé, but rather is much younger; (2) the regionally significant variegated tephra, found in the Fairbanks and Klondike areas and previously thought to be older than MIS 5, has an age of 77,800 ± 4100 yr (late MIS 5).

Keywords

Luminescence datingLoessAlaskaLoess-paleosolTephraLate Pleistocene
Type
Research Article
Information
Quaternary Research , Volume 60 , Issue 1 , July 2003 , pp. 70 - 83
Copyright
University of Washington

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References

Adamiec, G., and Aitken, M.J., (1998). Dose-rate conversion factors. update. Ancient TL 16, 37–50.Google Scholar
Aitken, M.J., (1985). Thermoluminescence Dating. Academic Press, San Diego.Google Scholar
Aitken, M.J., (1998). Introduction to Optical Dating. Oxford University Press, Oxford, UK.Google Scholar
Allen, J.R.M., and Huntley, B., (2000). Weischelian palynological records from southern Europe. correlation and chronology. Quaternary International 73–74, 111–125.Google Scholar
An, Z., (2000). The history and variability of the East Asian paleomonsoon climate. Quaternary Science Reviews 19, 171–187.Google Scholar
Anderson, P.M., and Lozhkin, A.V., (2001). The Stage 3 interstadial complex (Karginskii/middle Wisconsinan interval) of Beringia. variations in paleoenvironments and implications for paleoclimatic interpretations. Quaternary Science Reviews 20, 93–125.Google Scholar
Bard, E., Arnold, M., Fairbanks, R.G., and Hamelin, B., (1993). Comparison of 14C and uranium series ages on corals. Radiocarbon 35, 191–199.Google Scholar
Begét, J.E., (1990). Mid-Wisconsinan climate fluctuations recorded in central Alaskan loess. Géographie Physique et Quaternaire 544, 3–13.Google Scholar
Begét, J.E., and Hawkins, D.B., (1989). Influence of orbital parameters on Pleistocene loess deposition in central Alaska. Nature 337, 151–153.Google Scholar
Begét, J.E., Stone, D.B., and Hawkins, D.B., (1990). Paleoclimatic forcing of magnetic susceptibility variations in Alaskan loess during the late Quaternary. Geology 18, 40–43.Google Scholar
Berger, G.W., (1988). Dating Quaternary events by luminescence. Easterbrook, D.J. Dating Quaternary Sediments, Geological Society of America Special Paper 227, Boulder, Colorado. 13–50.Google Scholar
Berger, G.W., (1990). Regression and error analysis for a saturating-exponential-plus-linear model. Ancient TL 8, 23–25.Google Scholar
Berger, G.W., (1990). Effectiveness of natural zeroing of the thermoluminescence in sediments. Journal of Geophysical Research 95, 12375–12397.Google Scholar
Berger, G.W., (1994). Thermoluminescence dating of sediments older than ∼100 ka. Quaternary Science Reviews 13, 445–455.CrossRefGoogle Scholar
Berger, G.W., (1995). Progress in luminescence dating methods for Quaternary sediments. in: Rutter, N.W., Catto, N. (Eds.), Dating methods for Quaternary Deposits GEOtext no. 2, Geological Association of Canada, pp. 81–103.Google Scholar
Berger, G.W., and Anderson, P.M., (2000). Extending the geochronometry of Arctic lake cores beyond the radiocarbon limit by using thermoluminescence. Journal of Geophysical Research 105, D12 15439–15455.Google Scholar
Berger, G.W., and Busacca, A.J., (1995). Thermoluminescence dating of late Pleistocene loess and tephra from eastern Washington and southern Oregon and implications for the eruptive history of Mount St. Helens. Journal of Geophysical Research 100, B11 22361–22374.Google Scholar
Berger, G.W., and Doran, P., (2001). Luminescence-dating zeroing tests in Lake Hoare, Taylor Valley, Antarctica. Journal of Paleolimnology 25, 519–529.Google Scholar
Berger, G.W., and Nielsen, E., (1991). Evidence from thermoluminescence dating for Middle Wisconsinan deglaciation in the Hudson Bay Lowland of Manitoba. Canadian Journal of Earth Science 28, 240–249.Google Scholar
Berger, G.W., Péwé, T.L., (1994). Chronology of interior Alaskan loess-paleosol deposits by thermoluminescence. in: Lanphere, M.A., Dalrymple, G.B., Turrin, B.D. (Eds.), Abstracts of the Eighth International Conference on Geochronology, Cosmochronology and Isotope Geology, U.S. Geological Survey, Circular 1107, pp. 28 Google Scholar
Berger, G.W., and Péwé, T.L., (2001). Last-Interglacial age of the Eva Forest Bed, central Alaska, from thermoluminescence dating of bracketing loess. Quaternary Science Reviews 20, 485–498.Google Scholar
Berger, G.W., Pillans, B.J., and Palmer, A.S., (1994). Test of thermoluminescence dating of loess from New Zealand and Alaska. Quaternary Science Reviews 13, 309–333.Google Scholar
Berger, G.W., Péwé, T.L., Westgate, J.A., and Preece, S., (1996). Age of Sheep Creek tephra (Pleistocene) in central Alaska from thermoluminescence dating of bracketing loess. Quaternary Research 45, 263–270.Google Scholar
Berger, G.W., Boardman, P.C., Brubaker, L., and Anderson, P.M., (2000). Mineralogical controls on luminescence ages for a core from Ahaliorak Lake, northern Alaska. Geological Society of America, Abstracts with Programs 32, 7 A324 Google Scholar
Berger, G.W., Almond, P., and Pillans, B.J., (2001). Luminescence dating and glacial stratigraphy in Westland, New Zealand. New Zealand Journal of Geology and Geophysics 44, 25–35.CrossRefGoogle Scholar
Berger, G.W., Pillans, B.J., and Tonkin, P.J., (2001). Luminescence chronology of loess-paleosol sequences from Canterbury region, South Island, New Zealand. New Zealand Journal of Geology and Geophysics 44, 501–516.Google Scholar
Bischoff, J.L., and Cummins, K., (2001). Wisconsin glaciation of the Sierra Nevada (79,000-15,000 yr B.P.) As recorded by rock flour in sediments of Owens Lake, California. Quaternary Research 55, 14–24.Google Scholar
Carignano, C., (1999). Late Pleistocene to recent climate change in Córdoba Province, Argentina. geomorphical evidence. Quaternary International 57/58, 117–134.CrossRefGoogle Scholar
Chen, F.H., Bloemendal, , Wang, J.M., Li, J.J., and Oldfield, F., (1997). High-resolution multi-proxy climate records from Chinese loess: evidence for rapid climatic changes over the last 75 kyr. Palaeogeography, Palaeoclimatology, Palaeoecology 130, 323–335.Google Scholar
Denton, G.H., and Stuiver, M., (1967). Late Pleistocene glacial stratigraphy and chronology, northwestern St. Elias Mountains, Yukon Territory, Canada. Geological Society of America Bulletin 78, 485–510.CrossRefGoogle Scholar
Fang, X.-M., Ono, Y., Fukusawa, H., Bao-Tian, P., Li, J.-J., Dong-Hong, G., Oi, K., Tsukamoto, S., Torii, M., and Mishima, T., (1999). Asian summer monsoon instability during the past 60,000 years. magnetic susceptibility and pedogenic evidence from the western Chinese Loess Plateau. Earth and Planetary Science Letters 168, 219–232.CrossRefGoogle Scholar
Frechen, M., (1999). Luminescence dating of loessic sediments from the Loess Plateau, China. Geologische Rundschau 87, 675–684.Google Scholar
Hamilton, T.D., (2001). Quaternary glacial, lacustrine, and fluvial interactions in the western Noatak basin, Northwest Alaska. Quaternary Science Reviews 20, 371–391.Google Scholar
Hamilton, T.D., and Brigham-Grette, J., (1991). The last interglaciation in Alaska. stratigraphy and paleoecology of potential sites. Quaternary International 10–12, 49–71.Google Scholar
Hamilton, T.D., and Ashley, G.M., (1993). Epiguruk. a late Quaternary environmental record from northwestern Alaska. Geological Society of America Bulletin 105, 583–602.Google Scholar
Hamilton, T.D., Craig, J.L., and Sellmann, P.V., (1988). The Fox permafrost tunnel. a late Quaternary geological record in central Alaska. Geological Society of America Bulletin 100, 948–969.Google Scholar
Hamilton, T.D., Ashley, G.M., Reed, K.M., and Schweger, C.E., (1993). Late Pleistocene vertebrates and other fossils from Epiguruk, northwestern Alaska. Quaternary Research 39, 381–389.Google Scholar
Huijzer, B., and Vandenberghe, J., (1998). Climatic reconstruction of the Weischelian Pleniglacial in northwestern and central Europe. Journal of Quaternary Science 15, 391–417.Google Scholar
Huntley, D.J., and Lamothe, M., (2001). Ubiquity of anomalous fading in K-feldspars and correction for it in optical dating. Canadian Journal Earth Sciences 38, 1093–1106.Google Scholar
Huntley, D.J., and Prescott, J.R., (2001). Improved methodology and new thermoluminescence ages for the dune sequence in south-east South Australia. Quaternary Science Reviews (Quaternary Geochronology) 20, 687–699.Google Scholar
Kirby, M.E., and Andrews, J.T., (1999). Mid-Wisconsin Laurentide Ice Sheet growth and decay. implications for Heinrich events 3 and 4. Paleoceanography 14, 211–223.Google Scholar
Krbetschek, M.R., Götze, J., Dietrich, A., and Trautmann, T., (1997). Spectral information from minerals relevant for luminescence dating. Radiation Measurements 27, 695–748.Google Scholar
Lambeck, K., Esat, T.M., and Potter, E.-K., (2002). Links between climate and sea levels for the past three million years. Nature 419, 199–206.Google Scholar
Lian, O.B., and Shane, P.A., (2000). Optical dating of paleosols bracketing the widespread Rotoehu tephra, North Island, New Zealand. Quaternary Science Reviews 19, 1649–1662.CrossRefGoogle Scholar
Liu, X.M., Hesse, P., Rolph, T., and Begét, J.E., (1999). Properties of mineralogy of Alaskan loess. evidence for pedogenesis. Quaternary International 62, 93–102.CrossRefGoogle Scholar
Martinson, D.G., Oisias, N.G., Hays, J.D., Imbrie, J., Moore, T.C. Jr., and Shackleton, N.J., (1987). Age dating and the orbital theory of the ice ages. development of a high-resolution 0 to 300,000-year chronostratigraphy. Quaternary Research 27, 1–29.CrossRefGoogle Scholar
Matthews, J.V. Jr., Schweger, C.E., Hughes, O.L., (1989). Climatic change in eastern Beringia during oxygen isotope stages 2 and 3: proposed thermal events. in: Carter, L.D., Hamilton, T.D., Galloway, J.P. (Eds.), Late Cenozoic History of the Interior Basins of Alaska and the Yukon, U.S. Geological Survey Circular 1026, pp. 34–38.Google Scholar
Muhs, D.R., Ager, T.A., and Begét, J.E., (2001). Vegetation and paleoclimate of the last interglacial period, central Alaska. Quaternary Science Reviews 20, 40–61.CrossRefGoogle Scholar
Muhs, D.R., Swinehart, J.B., Loope, D.B., Aleinikoff, J.N., and Been, J., (1999). 200,000 years of climate change recorded in eolian sediments of the High Plains of eastern Colorado and western Nebraska. Lageoson, D.R., Trudgill, B.D. Colorado and Adjacent Areas, Geological Society of America Field Guide 1, Boulder, Colorado. 71–91.Google Scholar
Muhs, D.R., Ager, T., Stafford, T.W. Jr., Pavich, M., Begét, J.E., McGeehin, J.P., (1997). The last interglacial-glacial cycle in late Quaternary loess, central interior, Alaska. in: Elias, S., Brigham-Grette, J. (Eds.), Program and Abstracts, Beringian Paleoenvironments Workshop, Florissant, Colorado., pp. 109–112.Google Scholar
Oches, E.A., Banerjee, S.K., Solheid, P.A., Frechen, M., (1998). High-resolution proxies of climate variability in the Alaskan loess record. in: Busacca, A.J. (Eds.), Dust, Aerosols, Loess Soils & Global Change: Conference Proceedings, Washington State University, College of Agriculture and Home Economics Miscellaneous Publication No. MISC0190, pp. 167–170.Google Scholar
Ollerhead, J., Huntley, D.J., and Berger, G.W., (1994). Luminescence dating of the Buctouche Spit, New Brunswick. Canadian Journal of Earth Sciences 31, 523–531.Google Scholar
Owen, L.A., Finkel, R.C., Caffee, M.W., and Gualtieri, L., (2002). Timing of multiple late Quaternary glaciations in the Hunza Valley, Karakoram Mountains, northern Pakistan. defined by cosmogenic radionuclide dating of moraines. Geological Society of America Bulletin 114, 593–604.Google Scholar
Paepe, R., Mariolakos, I., Van Overloop, E., and Keppens, E., (1990). Last Interglacial-Glacial north-south geosoil traverse (from stratotypes in the North Sea Basin and in the eastern Mediterranean). Quaternary International 5, 57–70.Google Scholar
Péwé, T.L., (1955). Origin of the upland silt near Fairbanks, Alaska. Bulletin of the Geological Society of America 67, 699–724.Google Scholar
Péwé, T.L., (1965). Fairbanks area. Péwé, T.L. Guidebook to the Quaternary Geology. Central and Southcentral Alaska. Department of Natural Resources, Alaska. 6–36.Google Scholar
Péwé, T.L., (1975). Quaternary stratigraphic nomenclature in central Alaska. U.S. Geological Survey Professional Paper 862, 32 p Google Scholar
Péwé, T.L., (1975). Quaternary geology of Alaska. U.S. Geological Survey Professional Paper 835, 145 p (Third printing, 1983) Google Scholar
Péwé, T.L., (1989). Quaternary stratigraphy of the Fairbanks area, Alaska. in: Carter, L.D., Hamilton, T.D., Galloway, J.P. (Eds.), Late Cenozoic History of the Interior Basins of Alaska and the Yukon. U.S. Geological Survey Circular 1026, 72–77.Google Scholar
Péwé, T.L., Berger, G.W., Westgate, J.A., Brown, P.M., and Leavitt, S.W., (1997). Eva Interglacial Forest Bed, unglaciated east-central Alaska. global warming 125,000 years ago. Geological Society of America Special Paper 319, 54 p Google Scholar
Porter, S.C., and An, Z., (1995). Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, 305–308.Google Scholar
Preece, S.J., (1991). Tephrostratigraphy of the late Cenozoic Gold Hill Loess, Fairbanks area, Alaska. Unpublished M.Sc. dissertation, University of Toronto, Google Scholar
Preece, S.J., Westgate, J.A., Stemper, B.A., and Péwé, T.L., (1999). Tephrochronology of the Late Cenozoic loess at Fairbanks, central Alaska. Geological Society of America Bulletin 111, 71–90.Google Scholar
Propopenko, A.A., Karabanov, E.B., Williams, D.F., Kuzmin, M.I., Khursevich, G.K., and Gvozdhov, A.A., (2001). The detailed record of climatic events during the past 75,000 yrs BP from the Lake Baikal drill core BDP-93-2. Quaternary International 80–81, 59–68.Google Scholar
Rahmstorf, S., (2002). Ocean circulation and climate during the past 120,000 years. Nature 419, 207–214.Google Scholar
Sandhu, A.S., Westgate, J.A., Preece, S.J., Froese, D.G., (2001). Glass-fission-track ages of Late Cenozoic distal tephra beds in the Klondike district, Yukon Territory. in: Emond, D.S., Weston, L.H. (Eds.), Yukon Exploration and Geology 2000, Exploration and Geological Services Division, Yukon., Indian and Northern Affairs Canada, pp. 247–256.Google Scholar
Servant, J., (2001). The 100 kyr cycle of deglaciation during the last 450 kyr. a new interpretation of oceanic and ice core data. Global and Planetary Change 29, 121–133.Google Scholar
Shi, Y., (2002). Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia. Quaternary International 97–98, 79–91.Google Scholar
Shi, Y., Liu, X., Li, B., and Yao, T., (1999). A very strong summer monsoon event during 30–40 ka BP in the Qinghai-Xizang (Tibet) Plateau and its relation to precessional cycle. Chinese Science Bulletin 44, 1851–1858.Google Scholar
Shi, Y., Yu, G., Liu, X., Li, B., and Yao, T., (2001). Reconstruction of the 30–40 ka BP enhanced Indian monsoon climate based on geological records from the Tibetan Plateau. Palaeogeography, Palaeoclimatology, Palaeoecology 169, 69–83.Google Scholar
Thompson, L.G., Yao, T., Davis, M.E., Henderson, K.A., Mosley-Thompson, E., Lin, P.-N., Beer, J., Synal, H.-A., Cole-Dai, J., and Bolzan, J.F., (1997). Tropical climate instability. the last glacial cycle from a Qinghai-Tibetan ice core. Science 276, 1821–1825.Google Scholar
Ukkonen, P., Lunkka, J.P., Jungner, H., and Donner, J., (1999). New radiocarbon dates from Finnish mammoths indicating large ice-free areas in Fennoscandia during the Middle Weischelian. Journal of Quaternary Science 14, 711–714.Google Scholar
van Andel, T.H., and Tzedakis, P.C., (1996). Palaeolithic landscapes of Europe and environs, 150,000-25,000 years ago. an overview. Quaternary Science Reviews 15, 481–500.Google Scholar
Westgate, J.A., Stemper, B.A., and Péwé, T.L., (1990). A 3 m.y. record of Pliocene-Pleistocene loess in interior Alaska. Geology 18, 858–861.Google Scholar
Westgate, J.A., Preece, S.J., and Sandhu, A. (2001). Tephra power: Providing a secure chronologic framework for Late Cenozoic geologic/paleoenvironmental studies in eastern Beringia. in: Storer, J.E. (Ed.), Canadian Quaternary Association Program and Abstracts, Heritage Branch, Government of Yukon, Whitehorse, Occasional Papers in Earth Science 1, 67–68.Google Scholar
Wintle, A.G., and Westgate, J.A., (1986). Thermoluminescence age of the Old Crow tephra in Alaska. Geology 14, 594–597.Google Scholar