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Late Quaternary Vegetation and Climatic History of the Long Valley Area, West-Central Idaho, U.S.A.

Published online by Cambridge University Press:  20 January 2017

James P. Doerner  and
Paul E. Carrara
James P. Doerner
Affiliation:
Department of Geography, University of Northern Colorado, Greeley, Colorado, 80639
Paul E. Carrara
Affiliation:
U.S. Geological Survey, Mail Stop 913, Denver Federal Center, Denver, Colorado, 80225
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Abstract

Paleoenvironmental data, including pollen and sediment analyses, radiocarbon ages, and tephra identifications of a core recovered from a fen, provide a ca. 16,500 14C yr B.P. record of late Quaternary vegetation and climate change in the Long Valley area of west-central Idaho. The fen was deglaciated prior to ca. 16,500 14C yr B.P., after which the pollen rain was dominated by Artemisia, suggesting that a cold, dry climate prevailed until ca. 12,200 14C yr B.P. From ca. 12,200 to 9750 14C yr B.P. temperatures gradually increased and a cool, moist climate similar to the present prevailed. During this period a closed spruce–pine forest surrounded the fen. This cool, moist climate was briefly interrupted by a dry and/or cold interval between ca. 10,800 and 10,400 14C yr B.P. that may be related to the Younger Dryas climatic oscillation. From ca. 9750 to 3200 14C yr B.P. the regional climate was significantly warmer and drier than at present and an open pine forest dominated the area around the fen. Maximum aridity occurred after the deposition of the Mazama tephra (ca. 6730 14C yr B.P.). After 3200 14C yr B.P. regional cooling brought cool, moist conditions to the area; the establishment of the modern montane forest around the fen and present-day cool and moist climate began at ca. 2000 14C yr B.P.

Keywords

Idahopollen analysisdeglaciationlate-Quaternary
Type
Research Article
Information
Quaternary Research , Volume 56 , Issue 1 , July 2001 , pp. 103 - 111
Copyright
University of Washington

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References

Baker, R.G. Holocene vegetational history of the Western United States. Wright, H.E. Jr. (1983). Late-Quaternary Environments of the United States. Vol. 2, The Holocene. Univ. of Minnesota Press, Minneapolis. 109–127.Google Scholar
Barry, R.G., and Chorley, R.J. (1976). Atmosphere, weather, and climate. Methuen, London.Google Scholar
Beiswenger, J.M. (1991). Late Quaternary vegetational history of Grays Lake, Idaho. Ecological Monographs 61, 165–182.Google Scholar
Benson, J.B., Lund, S., Kashgarian, M., and Mensing, S. (1997). Nearly synchronous climate change in the Northern Hemisphere during the last glacial termination. Nature 388, 263–265.CrossRefGoogle Scholar
Bright, R.C. (1966). Pollen and seed stratigraphy of Swan Lake, southeastern Idaho: Its relation to regional vegetational history and to Lake Bonneville history. Tebiwa 9, 1–47.Google Scholar
Bright, R.C., and Davis, O.K. (1982). Quaternary paleoecology of the Idaho national engineering laboratory, Snake River Plain, Idaho. American Midland Naturalist 108, 21–33.CrossRefGoogle Scholar
Busacca, A.J., and McDonald, E.V. (1994). Regional sedimentation of late Quaternary loess on the Columbia Plateau: Sediment source areas and loess distribution patterns. Washington Division of Geology and Earth Resources Bulletin 80, 181–190.Google Scholar
Colman, S.M., and Pierce, K.L. (1986). Glacial sequence near McCall, Idaho: Weathering rinds, soil development, morphology, and other relative-age criteria. Quaternary Research 25, 25–42.Google Scholar
Cooper, D.J. (1986). Community structure and classification of Rocky Mountain wetland ecosystems. U.S. Fish and Wildlife Service Biological Report 86, 66–147.Google Scholar
Davis, O.K., Sheppard, J.C., and Robertson, S. (1986). Contrasting climatic histories for the Snake River Plain, Idaho, resulting from multiple thermal maxima. Quaternary Research 26, 321–339.Google Scholar
Dean, W.E. Jr. (1974). 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, 249–253.Google Scholar
Doerner, J.P., and Carrara, P.E. (1999). Deglaciation and postglacial vegetation history of the West Mountains, west-central Idaho, U.S.A. Arctic, Antarctic, and Alpine Research 31, 303–311.Google Scholar
Faegri, K., Iverson, J., and Krywinski, K. (1989). Textbook of Pollen Analysis. Wiley, New York.Google Scholar
Foit, F.F. Jr., Mehringer, P.J. Jr., and Sheppard, J.C. (1993). Age, distribution, and stratigraphy of Glacier Peak tephra in eastern Washington and western Montana, United States. Canadian Journal of Earth Science 30, 535–552.Google Scholar
Grimm, E.C. (1985). Data analysis and display. Huntley, B., Webb, T. III (1988). Vegetation History. Kluwer Academic, Dordrecht. 43–76.Google Scholar
Hall, S. A. Quaternary pollen analysis and vegetational history of the southwest. in Pollen Records of Late-Quaternary North American Sediments Bryant, V. M. Jr., and Holloway, R. G., Eds., pp. 95–123. Am. Assoc. of Stratigraphic Palynologist Foundation, Dallas.Google Scholar
Hallet, D.J., Hills, L.V., and Clague, J.J. (1997). New accelerator mass spectometry radiocarbon ages for the Mazama tephra layer from Kootenay National Park, British Columbia, Canada. Canadian Journal of Earth Sciences 34, 1202–1209.CrossRefGoogle Scholar
Kapp, R.O. (1969). How to Know Pollen and Spores. Brown, Dubuque.Google Scholar
Legg, T.W., and Baker, R.G. (1980). Palynology of Pinedale sediments, Devlins Park, Boulder County, Colorado. Arctic and Alpine Research 12, 319–333.Google Scholar
MacDonald, G.M. (1989). Postglacial paleoecology of the subalpine forest—Grassland ecotone of southwestern Alberta: New insights on vegetation and climate change in the Canadian Rocky Mountains and adjacent foothills. Paleogeography, Paleoclimatology, Paleoecology 73, 155–173.Google Scholar
Mack, R.N., Rutter, N.W., Bryant, V.M. Jr., and Valstro, S. (1978). Reexamination of postglacial vegetation history in northern Idaho: Hager Pond, Bonner Co. Quaternary Research 10, 241–255.Google Scholar
Mack, R.N., Rutter, N.W., and Valstro, S. (1983). Holocene vegetational history of the Kootenai River Valley, Montana. Quaternary Research 20, 177–193.Google Scholar
Maher, L.J. Jr. (1963). Pollen analysis of surface materials from southern SanJuan Mountains, Colorado. Geological Society of America Bulletin 74, 1485–1504.Google Scholar
Mehringer, P.J. Jr. (1987). Late-Quaternary pollen records from the interior Pacific Northwest and northern Great Basin of the United States. Bryant, V.M. Jr., and Holloway, R.G. (1985). Pollen Records of Late-Quaternary North American Sediments. Am. Assoc. of Stratigraphic Palynologist Foundation, Dallas. 167–189.Google Scholar
Mehringer, P.J. Jr., Arno, S.F., and Petersen, K.L. (1977). Postglacial history of Lost Trail Pass Bog, Bitterroot Mountains, Montana. Arctic and Alpine Research 9, 345–368.CrossRefGoogle Scholar
Mehringer, P.J. Jr., Sheppard, J.C., Foit, F.F. Jr. (1984). The age of the Glacier Peak tephra in west-central Montana. Quaternary Research 21, 36–41.Google Scholar
Moore, P.D., Webb, J.A., and Collinson, M.E. (1991). Pollen Analysis. Blackwell Sci, London.Google Scholar
Mullineaux, D.R. (1986). Summary of pre-1980 tephra-fall deposits erupted from Mount St. Helens, Washington State, U.S.A. Bulletin of Volcanology 48, 17–26.Google Scholar
Othberg, K. L. Landforms and surface deposits of Long Valley, Valley County, Idaho. Idaho Geological Survey Map 5, scale approximately 1:62,500.Google Scholar
Schmidt, D.L., and Mackin, J.H. (1970). Quaternary geology of Long and Bear Valleys, west-central Idaho. U.S. Geological Survey Bulletin 22 Google Scholar
Stuiver, M., and Reimer, P.J. (1993). Extended 14C data base and revised CALIB 3.0 14C age calibration program. Radiocarbon 35, 215–230.CrossRefGoogle Scholar
Thompson, R.S., Whitlock, C., Bartlein, P.J., and Spaulding, W.G. (1992). Climatic changes in the western United States since 18,000 yr B.P. Wright, H.E. Jr., Kutzbach, J.E., Ruddiman, W.F., Street-Perrott, F.A., Webb, T. III (1993). Global climates since the last glacial maximum. Univ. of Minnesota Press, Minneapolis. 468–513.Google Scholar
Whitlock, C. (1993). Postglacial vegetation and climate of Grand Teton and southern Yellowstone National Parks. Ecological Monographs 63, 173–198.Google Scholar
Whitlock, C., and Bartlein, P.J. (1993). Spatial variations of Holocene climatic change in the Yellowstone region. Quaternary Research 39, 231–238.Google Scholar
Whitlock, C., Bartlein, P.J., and Van Norman, K.J. (1995). Stability of Holocene climate regimes in the Yellowstone region. Quaternary Research 43, 433–436.CrossRefGoogle Scholar
Wright, H.E. Jr., Bent, A.M., Hansen, B.S., Maher, L.J. Jr. (1973). Present and past vegetation of the Chuska Mountains, northwestern New Mexico. Geological Society of America Bulletin 84, 1155–1180.2.0.CO;2>CrossRefGoogle Scholar
Monthly station normals of temperature, precipiation, and heating and cooling degrees days 1961–90, Idaho. Climatology of the United States, Google Scholar