Hostname: page-component-8448b6f56d-tj2md Total loading time: 0 Render date: 2024-04-19T14:40:59.258Z Has data issue: false hasContentIssue false

Evidence for Millennial-Scale Climate Change During Marine Isotope Stages 2 and 3 at Little Lake, Western Oregon, U.S.A.

Published online by Cambridge University Press:  20 January 2017

Laurie D. Grigg
Affiliation:
Department of Geography, University of Oregon, Eugene, Oregon, 97403
Cathy Whitlock
Affiliation:
Department of Geography, University of Oregon, Eugene, Oregon, 97403
Walter E. Dean
Affiliation:
U.S. Geological Survey, MS 980 Federal Center, Denver, Colorado, 80225

Abstract

Pollen and geochemical data from Little Lake, western Oregon, suggest several patterns of millennial-scale environmental change during marine isotope stage (MIS) 2 (14,100–27,600 cal yr B.P.) and the latter part of MIS 3 (27,600–42,500 cal yr B.P.). During MIS 3, a series of transitions between warm- and cold-adapted taxa indicate that temperatures oscillated by ca. 2°–4°C every 1000–3000 yr. Highs and lows in summer insolation during MIS 3 are generally associated with the warmest and coldest intervals. Warm periods at Little Lake correlate with warm sea-surface temperatures in the Santa Barbara Basin. Changes in the strength of the subtropical high and the jet stream may account for synchronous changes at the two sites. During MIS 2, shifts between mesic and xeric subalpine forests suggest changes in precipitation every 1000–3000 yr. Increases in Tsuga heterophylla pollen at 25,000 and 22,000 cal yr B.P. imply brief warmings. Minimum summer insolation and maximum global ice-volumes during MIS 2 correspond to cold and dry conditions. Fluctuations in precipitation at Little Lake do not correlate with changes in the Santa Barbara Basin and may be explained by variations in the strength of the glacial anticyclone and the position of the jet stream.

Type
Research Article
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, N.F. (1979). Middle Wisconsin stratigraphy and climatic reconstruction, southern Vancouver Island, British Columbia. Quaternary Research 11, 213237.CrossRefGoogle Scholar
Alley, R.B. (1998). Icing the North Atlantic. Nature 392, 335337.CrossRefGoogle Scholar
Anderson, P.M., Bartlein, P.J., Brubaker, L.B., Gajewski, K., and Ritchie, J.C. (1989). Modern analogues of late-Quaternary pollen spectra from the Western Interior of North America. Journal of Biogeography 161, 573596.CrossRefGoogle Scholar
Bard, E., Arnold, M., Hamelin, B., Tisnerat-Laborde, N., and Cabioch, G. (1998). Radiocarbon calibration by means of mass spectrometric 230Th/234U and 14C ages of corals: An updated database including samples from Barbados, Mururoa and Tahiti. Radiocarbon 40, 10851092.CrossRefGoogle Scholar
Barnosky, C.W. (1981). A record of late Quaternary vegetation from Davis Lake, southern Puget Lowland Washington. Quaternary Research 16, 221239.CrossRefGoogle Scholar
Barnosky, C.W. (1985). Late Quaternary vegetation near Battle Ground Lake, southern Puget Trough, Washington. Geological Society of America Bulletin 96, 263271.2.0.CO;2>CrossRefGoogle Scholar
Bartlein, P.J., Anderson, K.H., Anderson, P.M., Edwards, M.E., Mock, C.J., Thompson, R.S., Webb, R.S., Webb, T. III, and Whitlock, C. (1998). Paleoclimate simulations for North America over the past 21,000 years: Features of the simulated climate and comparisons with paleoenviornmental data. Quaternary Science Reviews 17, 549585.CrossRefGoogle Scholar
Behl, R.J., and Kennett, J.P. (1996). Brief interstadial events in the Santa Barbara Basin, NE Pacific, during the past 60 kyr. Nature 379, 243246.Google Scholar
Benson, L. Records of millennial-scale climate change from the Great Basin of the western United States. Clark, P.U., Webb, R.S., and Keigwin, L.D. (1999). Mechansims of Global Climate Change at Millennial Time Scales. American Geophys. Union, Washington. 203225.Google Scholar
Berger, A. (1978). Long-term variations of caloric insolation resulting from Earth's orbital elements. Quaternary Research 9, 139167.CrossRefGoogle Scholar
Bond, G.C., and Lotti, R. (1995). Iceberg discharges into the North Atlantic on millennial time scales during the last glaciation. Science 267, 10051009.Google Scholar
Bond, G.C., Showers, W., Cheseby, M., Lotti, R., Almasi, P., deMenocal, P., Priore, P., Cullen, H., Hajdas, I., and Bonani, G. (1997). A pervasive millennial-scale cycle in the North Atlantic Holocene and glacial climates. Science 278, 12571266.Google Scholar
Clark, P.U., and Bartlein, P.J. (1995). Correlation of late Pleistocene glaciation in the Western United States with North Atlantic Heinrich events. Geology 23, 483486.Google Scholar
Cwynar, L.C., Burden, E.B., and McAndrews, J.H. (1979). An inexpensive method for concentrating pollen and spores from fine grained sediments. Canadian Journal of Earth Sciences 16, 11151120.Google Scholar
Engleman, E.E., Jackson, L.L., Norton, D.R., and Fischer, A.G. (1985). Determination of carbonate carbon in geologic materials by coulometric titration. Chemical Geology 35, 125128.Google Scholar
Faegri, K., Kaland, P.E., and Krzywinski, K. (1989). Textbook of Pollen Analysis. Wiley, London.Google Scholar
Franklin, J.F., and Dyrness, C.T. (1988). Natural Vegetation of Oregon and Washington. Oregon State Univ. Press, Corvallis.Google Scholar
Gardner, J.V., Dean, W.E., and Dartnell, P. (1997). Biogenic sedimentation beneath the California current system for the past 30 kyr and its paleoceanographic significance. Paleoceanography 12, 207225.Google Scholar
Grigg, L.D., and Whitlock, C. (1998). Late-glacial vegetation and climate changes in western Oregon. Quaternary Research 49, 287298.CrossRefGoogle Scholar
Grimm, E.C. Data analysis and display. Huntley, B. (1988). Vegetation History. Kluwer Academic, Dordrecht. 4376.Google Scholar
Hendy, I.L., and Kennett, J.P. (1999). Latest Quaternary North Pacific surface-water responses imply atmosphere-driven climate instability. Geology 27, 291294.Google Scholar
Heusser, C.J., Heusser, L.E., and Peteet, D.M. (1999). Humptulips revisted: A revised interpretation of Quaternary vegetation and climate of western Washington, USA. Palaeogeography, Palaeoclimatology, Palaeoecology 150, 191221.Google Scholar
Hicock, S.R., Lian, O.B., and Mathewes, R.W. (1999). `Bond cycles' recorded in terrestrial Pleistocene sediments of southwestern British Columbia, Canada. Journal of Quaternary Science 14, 443449.3.0.CO;2-6>CrossRefGoogle Scholar
Hostetler, S.W., and Bartlein, P.J. (1986). Simulation of the potential responses of regional climate and surface processes in western North America to a canonical Heinrich event. Clark, P.U., Webb, R.S., and Keigwin, L.D. (1999). Mechanisms of Global Climate Change at Millennial Timescales. American Geophys. Union, Washington. 313327.Google Scholar
Heusser, C.J. (1972). Palynology and phytogeographical significance of a late-pleistocene refugium near Kalaloch, Washington. Quaternary Research 2, 189201.Google Scholar
Imbrie, J., Hays, J.D., Martinson, D.G., McIntyre, A., Mix, A.C., Morley, J.J., Pisias, N.G., Prell, W.L., and Shackleton, N.J. (1987). The orbital theory of Pleistocene climate: Support from a revised chronology of the marine δ18O record. Berger, A., Imbrie, J., Hays, J., Kukla, G., and Saltzman, B. (1984). Milankovitch and Climate. Reidel, Dordrecht. 269305.Google Scholar
Kitagawa, H., and van der Plicht, J. (1998). Atmospheric radiocarbon calibration to 45,000 yr B.P.: Late Glacial fluctuations and cosmogenic istope production. Science 279, 11871190.CrossRefGoogle Scholar
Lin, J.O., Broecker, W.S., Hemming, S.R., Hajdas, I., Anderson, R.F., Smith, G.I., Kelley, M., and Bonani, G. (1998). A reassessment of U-Th and 14C ages for late-glacial high-frequency hydrological events at Searles Lake, California. Quaternary Research 49, 1123.Google Scholar
Litchie, F. E., Golightly, D. W., and Lamothe, P. J. Inductively coupled plasma-atomic emission spectrometry. in Methods for Geochemical Analysis. Baedecker, P. A., Ed., USGS Bulletin 1770, B1B10.Google Scholar
Long, C.J., Whitlock, C., Bartlein, P.J., and Millspaugh, S.H. (1998). A 9000-year fire history from the Oregon Coast Range, based on a high-resolution charcoal study. Canadian Journal of Forest Research 28, 774787.CrossRefGoogle Scholar
Lund, D.C., and Mix, A.C. (1998). Millennial-scale deep water oscillations: Reflections of the North Atlantic in the deep Pacific from 10 to 60 ka. Paleoceanography 13, 1019.CrossRefGoogle Scholar
Mathewes, R.W. (1991). Climatic conditions in the western and northern Cordillera during the last glaciation: Paleoecologcial evidence. Géographie Physique et Quaternaire 45, 333339.CrossRefGoogle Scholar
Mazaud, A., Laj, C., Bard, E., Arnold, M., and Tric, E. (1991). Geomagnetic field control of 14C production over the last 80ky: Implications for the radiocarbon time-scale. Geophysical Research Letters 18, 18851888.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.Google Scholar
Meidinger, D., and Pojar, J. (1991). Ecosystems of British Columbia. British Columbia Ministry of Forests, Victoria.Google Scholar
Meyers, P.A., and Ishiwatari, R. (1993). Lacustrine organic geochemistry—An overview of indicators of organic matter sources and diagenesis in lake sediments. Organic Geochemistry 20, 867900.Google Scholar
Mikolajewicz, U., Crowley, T.J., Schiller, A., and Voss, R. (1997). Modeling teleconnections between the North Atlantic and Pacific during the Younger Dryas. Nature 387, 384387.CrossRefGoogle Scholar
Minckley, T.A., and Whitlock, C. (2000). Spatial variation of modern pollen rain in Oregon and southern Washington, USA. Review of Palaeobotany and Palynology 112, 97123.Google Scholar
Mock, C.J. (1996). Climatic controls and spatial variations of precipitation in the western United States. Jounal of Climate 9, 11111125.Google Scholar
Moore, P.D., and Webb, J.A. (1978). An Illustrated Guide to Pollen Analysis. Wiley, New York.Google Scholar
Overpeck, J.T., Webb, T. III, and Prentice, I.C. (1985). Quantitative interpretation of fossil pollen spectra: Dissimilarity coefficients and the method of modern analogs. Quaternary Research 23, 87108.Google Scholar
Pellat, M.G., Mathewes, R.W., and Walker, I.R. (1997). Pollen analysis and ordination of lake sediment-surface samples from coastal British Columbia, Canada. Canadian Journal of Botany 75, 799814.CrossRefGoogle Scholar
Peteet, D., Del Genio, A., and Lo, K. (1997). Sensitivity of northern hemisphere air temperatures and snow expansion to North Pacific sea surface temperatures in the Goddard Institute for Space Studies general circulation model. Journal of Geophysical Research 102, 781791.Google Scholar
Raymo, M.E., Ganley, K., Carter, S., Oppo, D.W., and McManus, J. (1998). Millennial-scale climate instability during the early Pleistocene epoch. Nature 392, 699702.CrossRefGoogle Scholar
Stuiver, M., and Reimer, P.J. (1993). Extended 14C data base and revised CALIB 3.0 14C age calibration program. Radiocarbon 35, 215230.Google Scholar
Thompson, R, and Oldfield, F. Environmental Magnetism. Allen & Unwin, London.Google Scholar
Thompson, R.S., Whitlock, C., Bartlein, P.J., Harrison, S.P., and Spaulding, W.G. Climatic changes in the western United States since 18,000 yr B.P. Wright, H.E., Kutzbach, J.E., Ruddiman, W.F., Street-Perrott, F.A., Webb, T. III, and Bartlein, P.J. (1993). Global Climates since the Last Glacial Maximum. University of Minn. Press, Minneapolis. 468513.Google Scholar
Thompson, R.S., Anderson, K.H., and Bartlein, P.J. (1999). Atlas of relations between climatic parameters and distributions of important trees and shrubs in North America; introduction and conifers. U.S. Geological Survey, Reston.Google Scholar
Warner, B.G., Clague, J.J., and Mathewes, R.W. (1984). Geology and paleoecology of a Mid-Wisconsin peat from the Queen Charlotte Islands, British Columbia, Canada. Quaternary Research 21, 337350.Google Scholar
Whitlock, C., and Bartlein, P.J. (1997). Vegetation and climate change in northwest America during the past 125 kyr. Nature 388, 5761.Google Scholar
Whitlock, C., and Grigg, L.D. (1999). Paleoecological evidence of Milankovitch and Sub-Milankovitch climate variations in the western U.S. during the late Quaternary. Webb, R.S., Clark, P.U., and Keigwin, L.D. Mechanisms of Global Climate Change at Millennial Time Scales. American Geophys. Union, Washington. 227241.Google Scholar
Worona, M.A., and Whitlock, C. (1995). Late-Quaternary vegetation and climate history near Little Lake, central Coast Range, Oregon. Geological Society of America Bulletin 107, 867876.Google Scholar
Wright, H.E.J., Mann, D.H., and Glaser, P.H. (1983). Piston cores for peat and lake sediments. Ecology 65, 657659.Google Scholar