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Postglacial fire, vegetation, and climate history in the Clearwater Range, Northern Idaho, USA

Published online by Cambridge University Press:  20 January 2017

Andrea Brunelle
Affiliation:
University of Oregon, Department of Geography, 1251 University of Oregon, Eugene, OR 97403, USA
Cathy Whitlock
Affiliation:
University of Oregon, Department of Geography, 1251 University of Oregon, Eugene, OR 97403, USA

Abstract

The environmental history of the Northern Rocky Mountains was reconstructed using lake sediments from Burnt Knob Lake, Idaho, and comparing the results with those from other previously published sites in the region to understand how vegetation and fire regimes responded to large-scale climate changes during the Holocene. Vegetation reconstructions indicate parkland or alpine meadow at the end of the glacial period indicating cold-dry conditions. From 14,000 to 12,000 cal yr B.P., abundant Pinus pollen suggests warmer, moister conditions than the previous period. Most sites record the development of a forest with Pseudotsuga ca. 9500 cal yr B.P. indicating warm dry climate coincident with the summer insolation maximum. As the amplification of the seasonal cycle of insolation waned during the middle Holocene, Pseudotsuga was replaced by Pinus and Abies suggesting cool, moist conditions. The fire reconstructions show less synchroneity. In general, the sites west of the continental divide display a fire-frequency maximum around 12,000–8000 cal yr B.P., which coincides with the interval of high summer insolation and stronger-than-present subtropical high. The sites on the east side of the continental divide have the highest fire frequency ca. 6000–3500 cal yr B.P. and may be responding to a decrease in summer precipitation as monsoonal circulation weakened in the middle and late Holocene. This study demonstrated that the fire frequency of the last two decades does not exceed the historical range of variability in that periods of even higher-than-present fire frequency occurred in the past.

Type
Research Article
Copyright
University of Washington

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References

Agee, J.K, (1993). Fire Ecology of Pacific Northwest Forests. Island Press, Washington, D.C.Google Scholar
Arno, S., (1976). The Historical Role of Fire on the Bitterroot National Forest. Research Paper INT-187. USDA Forest Service, Google Scholar
Arno, S, (1980). Forest fire history in the northern Rockies. Journal of Forestry 78, 460465.Google Scholar
Baker, R.G, (1983). Holocene vegetational history of the western United States. Wright, H.E Jr. Late Quaternary Environments of the United States. The Holocene Vol. 2, University of Minnesota Press, Minneapolis. 109126.Google Scholar
Barnosky, C.W, Anderson, P.M, and Bartlein, P.J, (1987). The northwestern U.S. during deglaciation; Vegetational history and paleoclimatic implications. Ruddiman, W.F, Wright, H.E Jr. North America and Adjacent Oceans During the Last Deglaciation, Geology of North America Vol. K-3, Geological Survey of America, Boulder, CO. 289321.Google Scholar
Barrett, S.W., Arno, S.F., (1991). Classifying fire regimes and defining their topographic controls in the Selway–Bitterroot Wilderness. in: Society of American Foresters, Proceedings of the 11th Conference. pp. 299307.Google Scholar
Barrett, S.W., Arno, S.F., Menakis, J.P., (1997). Fire Episodes in the Inland Northwest (1540–1940) Based on Fire History Data, General Technical Report INT-GTR-370. USDA Forest Service Google 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 simulation climate and comparisons with paleoenvironmental data. Quaternary Science Reviews 17, 549585.CrossRefGoogle Scholar
Bergeron, Y, Richard, P.J.H, Carcaillet, C, Gauthier, S, Flannigan, M, and Prairie, Y.T, (1998). Variability in fire frequency and forest composition in Canada's southeastern boreal forest: a challenge for sustainable forest management. Conservation Ecology 2, available at http://www.consecol.org/vol2/iss2/art6 CrossRefGoogle Scholar
Bradbury, J.P, (1996). Charcoal deposition and redeposition in Elk Lake, Minnesota, USA. The Holocene 3, 339344.CrossRefGoogle Scholar
Brunelle-Daines, A., (2002). Holocene Changes in Fire, Climate and Vegetation in the Northern Rocky Mountains of Idaho and Western Montana. Ph.D. dissertation. University of Oregon, Google Scholar
Carcaillet, C, Gauthier, S, Prairie, Y.T, Bergeron, Y, Richard, P.J.H, and Fréchette, B, (2001). Change of fire frequency in the eastern Canadian boreal forests during the Holocene. does vegetation composition or climate trigger the fire regime?. Journal of Ecology 89, 930946.CrossRefGoogle Scholar
Carrara, P.E, and Trimble, D.A, (1992). A Glacier Peak and Mount Saint Helens J volcanic ash couplet and the timing of deglaciation in the Colville Valley area, Washington. Canadian Journal of Earth Science 29, 23972405.CrossRefGoogle Scholar
Clark, J.S, (1988). Particle motion and the theory of stratigraphic charcoal analysis. source area, transportation, deposition, and sampling. Quaternary Research 30, 8191.CrossRefGoogle Scholar
Dean, W.E Jr. Determination of carbonate and organic matter in calcareous sediments by loss on ignition. comparison to other methods. Journal of Sedimentary Petrology 44, (1974). 242248.Google Scholar
Faegri, K, Kaland, P.E, and Kzywinski, K, (1989). Textbook of Pollen Analysis. Wiley, New York.Google Scholar
Fall, P.L, (1992). Spatial patterns of atmospheric pollen dispersal in the Colorado Rocky Mountains, USA. Review of Paleaeobotany and Palynology 74, 293313.CrossRefGoogle Scholar
Finklin, A.I, (1983). Weather and Climate of the Selway–Bitterroot Wilderness. Northwest Naturalist Books, Idaho.Google Scholar
Flannigan, M.D., Wotton, M., Richard, P., Carcaillet, C., Bergeron, Y., (1998). Fire weather: Past, present and future. in: Ninth Symposium on Global Change Studies, America Meteorological Society. American Meteorological Society, Boston., 11. 305309.Google Scholar
Fule, P.Z, Covington, W.W, and Moore, M.M, (1997). Determining reference conditions for ecosystem management of southwestern ponderosa pine forests. Ecological Applications 7, 895908.CrossRefGoogle Scholar
Gardner, J.J, and Whitlock, C, (2001). Charcoal accumulation following a recent fire in the Cascade Range, northwestern USA, and its relevance for fire-history studies. The Holocene 5, 541549.CrossRefGoogle Scholar
Gates, D.M, (1993). Climate Change and its Biological Consequences. Sinauer Associates, MA.Google Scholar
Graumlich, L.J, (1993). A 1000-year record of temperature and precipitation in the Sierra Nevada. Quaternary Research 39, 249255.CrossRefGoogle Scholar
Grissino-Mayer, H.D, and Swetnam, T.W, (2000). Century-scale climate forcing of fire regimes in the American Southwest. The Holocene 10, 213220.CrossRefGoogle Scholar
Hitchcock, C.L, and Cronquist, A, (1973). Flora of the Pacific Northwest. An Illustrated Manual. University of Washington Press, Seattle.Google Scholar
Hughes, M.K, and Diaz, H.F, (1994). Was there a ‘Medieval Warm Period,’ and if so, where and when?. Climatic Change 26, 109142.CrossRefGoogle Scholar
Hunt, R.S., (1993). Abies. in: Flora of North America Editorial Committee (Eds.), Flora of North America North of Mexico. Vol. 2, . Pteridophytes and Gymnosperms, Oxford University Press, New York., pp. 354362.Google Scholar
Karsian, A.E., (1995). A 6800 Year Vegetation and Fire History in the Bitterroot Mountain Range, Montana. Masters thesis, University of Montana, Google Scholar
Kershaw, L, MacKinnon, A, Pojar, J, (1998). Foulds, N Plants of the Rocky Mountains. Lone Pine Publishing, Canada.Google Scholar
Kipfmueller, K.F., (2003). Fire–Climate–Vegetation Interactions in Subalpine Forests of the Selway– Bitterroot Wilderness Area, Idaho and Montana, USA. Ph.D. dissertation. The University of Arizona, Google Scholar
Kutzbach, J.E, and Guetter, P.J, (1986). The influence of changing orbital patterns and surface boundary conditions on climate simulations for the past 18,000 years. Journal of Atmospheric Science 43, 17261759.2.0.CO;2>CrossRefGoogle Scholar
Kutzbach, J, Gallimore, R, Harrison, S, Behling, P, Selin, R, and Laarif, F, (1998). Climate and biome simulations for the past 21,000 years. Quaternary Science Reviews 17, 473506.CrossRefGoogle 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 Forestry 28, 774787.CrossRefGoogle Scholar
Luckman, B.H, (1993). Glacier fluctuation and tree-ring records for the last millennium in the Canadian Rockies. Quaternary Science Reviews 12, 441450.CrossRefGoogle Scholar
Luckman, B.H, Kearney, M.S, King, R.H, and Beaudoin, A.B, (1986). Revised 14C ages for St. Helens Y tephra at Tonquin Pass, British Columbia. Canadian Journal of Earth Sciences 23, 734736.CrossRefGoogle Scholar
Lynch, E.A, (1998). Origin of a park-forest vegetation mosaic in the Wind River Range, Wyoming. Ecology 79, 13201338.Google Scholar
Mehringer, P.J Jr., Arno, S.F, and Peterson, K.L, (1977). Postglacial history of Lost Trail Pass Bog, Bitterroot Mountains, Montana. Arctic and Alpine Research 9, 345368.CrossRefGoogle Scholar
Millspaugh, S.H., (1997). Late-Glacial and Holocene Variations in Fire Frequency in the Central Plateau and Yellowstone–Lamar Provinces of Yellowstone National Park. Ph.D. dissertation, University of Oregon, Google Scholar
Millspaugh, S.H, Whitlock, C, and Bartlein, P.J, (2000). Variations in fire frequency and climate over the past 17 000 yr in central Yellowstone National Park. Geology 28, 211214.2.0.CO;2>CrossRefGoogle Scholar
Millspaugh, S.H., Whitlock, C. (in press). Postglacial fire, vegetation and climate history of the Yellowstone-Lamar and Central Plateau provinces. Yellowstone National Park, Google Scholar
Mock, C.J, (1996). Climatic controls and spatial variations of precipitation in the Western United States. Journal of Climate 9, 11111125.2.0.CO;2>CrossRefGoogle Scholar
Mohr, J.A, Whitlock, C, and Skinner, C.N, (2000). Postglacial vegetation and fire history. Eastern Klamath Mountains, California, USA. The Holocene 10, 587601.CrossRefGoogle Scholar
National Interagency Fire Center, (2000). Available at http://www.nifc.gov/ Google Scholar
Rollins, M.G, Swetnam, T.W, and Morgan, P, (2001). Evaluating a century of fire patterns in two Rocky Mountain wilderness areas using digital fire atlases. Canadian Journal of Forestry 31, 21072123.CrossRefGoogle Scholar
Segura, G, Hinckley, T.M, and Brubaker, L.B, (1995). Variations in radial growth of declining old-growth stands of Abies amabilis after tephra deposition from Mount St. Helens. Canadian Journal of Forestry 25, 14841492.CrossRefGoogle Scholar
Stine, S, (1994). Extreme and persistent drought in California and Patagonia during medieval time. Nature 369, 546549.CrossRefGoogle Scholar
Stuiver, M, Reimer, P.J, and Braziunas, T.F, (1998). High-precision radiocarbon age calibration for terrestrial and marine samples. Radiocarbon 40, 11271151.CrossRefGoogle Scholar
Swetnam, T.W, and Betancourt, J.L, (1998). Mesoscale disturbance and ecological response to decadal climatic variability in the American Southwest. Journal of Climate 11, 31283147.2.0.CO;2>CrossRefGoogle Scholar
Thilenius, J.F, (1990). Woody plant succession on earthquake-uplifted coastal wetlands of the Copper River Delta, Alaska. Forest Ecology and Management 33-34, 439462.CrossRefGoogle Scholar
Thompson, R.S, Whitlock, C, Bartlein, P.J, Harrison, S.P, and Spaulding, G.W, (1993). Climatic changes in western United States since 18,000 yr B.P.. Wright, H.E Jr., Kutzbach, J.E, Webb, T III, Ruddiman, W.F, and Street-Perrott, F.A Global Climates Since the Last Glacial Maximum. University of Minnesota Press, Minneapolis. 468513.Google Scholar
Thompson, R.S., Anderson, K.H., (1999). and Bartlein, P.J., Atlas of Relations Between Climatic Parameters and Distributions of Important Trees and Shrubs in North America. Professional Paper Volume 1650 A & B. United States Geological Survey, Google Scholar
Tinner, W, and Lotter, A.F, (2001). Central European vegetation response to abrupt climate change at 8.2 ka. Geology 29, 551554.2.0.CO;2>CrossRefGoogle Scholar
Troels-Smith, J., (1955). Characterization of unconsolidated sediments: Geological Survey of Denmark. Series IV, vol. 3, No. 10 Google Scholar
Whitlock, C, (1993). Postglacial vegetation and climate of Grand Teton and Southern Yellowstone National Parks. Ecological Monographs 63, 173198.CrossRefGoogle Scholar
Whitlock, C, and Bartlein, P.J, (1993). Spatial variations of Holocene climatic change in the Yellowstone region. Quaternary Research 39, 231238.CrossRefGoogle Scholar
Whitlock, C, and Larsen, C.P.S, (2002). Charcoal as a fire proxy. Smol, J.P, Birks, H.J.B, Last, W.M Tracking Environmental Change Using Lake Sediments. Biological Techniques and Indicators Vol. 2, Kluwer Academic Publishers, Dordrecht. 8597.Google Scholar
Whitlock, C, and Millspaugh, S.H, (1996). Testing the assumptions of fire-history studies. An examination of modern charcoal accumulation in Yellowstone National Park, USA. The Holocene 6, 715.CrossRefGoogle Scholar
Zdanowicz, C.M, Zielinski, G.A, and Germani, M.S, (1999). Mount Mazama eruption. calendrical age verified and atmospheric impact assessed. Geology 27, 621624.2.3.CO;2>CrossRefGoogle Scholar
Zobel, D.B, and Antos, J.A, (1997). A decade of recovery of understory vegetation buried by volcanic tephra from Mount St. Helens. Ecological Monographs 67, 317344.CrossRefGoogle Scholar
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