Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-13T11:27:46.218Z Has data issue: false hasContentIssue false

Holocene vegetation, fire and climate history of the Sawtooth Range, central Idaho, USA

Published online by Cambridge University Press:  20 January 2017

Cathy Whitlock*
Affiliation:
Department of Earth Sciences, Montana State University, Bozeman, MT 59715, USA
Christy E. Briles
Affiliation:
Department of Anthropology, Texas A&M University, College Station, TX 77843, USA
Matias C. Fernandez
Affiliation:
Ecology, Evolution, and Environmental Biology Department, Columbia University, New York, NY 10027, USA
Joshua Gage
Affiliation:
Department of Earth Sciences, Montana State University, Bozeman, MT 59715, USA
*
Corresponding author.

Abstract

The paucity of low- and middle-elevation paleoecologic records in the Northern Rocky Mountains limits our ability to assess current environmental change in light of past conditions. A 10,500-yr-long vegetation, fire and climate history from Lower Decker Lake in the Sawtooth Range provides information from a new region. Initial forests dominated by pine and Douglas-fir were replaced by open Douglas-fir forest at 8420 cal yr BP, marking the onset of warmer conditions than present. Presence of closed Douglas-fir forest between 6000 and 2650 cal yr BP suggests heightened summer drought in the middle Holocene. Closed lodgepole pine forest developed at 2650 cal yr BP and fires became more frequent after 1450 cal yr BP. This shift from Douglas-fir to lodgepole pine forest was probably facilitated by a combination of cooler summers, cold winters, and more severe fires than before. Five drought episodes, including those at 8200 cal yr BP and during the Medieval Climate Anomaly, were registered by brief intervals of lodgepole pine decline, an increase in fire activity, and mistletoe infestation. The importance of a Holocene perspective when assessing the historical range of variability is illustrated by the striking difference between the modern forest and that which existed 3000 yr ago.

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.)

Footnotes

1 Current address: American Wildlands, P.O. 6669, Bozeman, MT 59715, USA.

References

Alley, R.B., Mayewski, P.A., Sowers, T., Stuiver, M., Taylor, K.C., and Clark, P.U. Holocene climatic instability: a large, widespread event 8200 years ago. Geology 25, (1997). 483486.Google Scholar
Anderson, R.S., Allen, C.D., Toney, J.L., Jass, R.B., and Bair, A.N. Holocene vegetation and fire regimes in subalpine and mixed conifer forests, southern Rocky Mountains, U.S.A.. International Journal of Wildland Fire 17, (2008). 96114.Google Scholar
Arno, S. Forest regions of Montana. USDA Research Paper INT-218. (1979). Google Scholar
Bacon, C.R. Eruptive history of Mount Mazama and Crater Lake caldera, Cascade Range, U.S.A.. Journal of Volcanology and Geothermal Research 18, (1983). 57115.CrossRefGoogle Scholar
Baker, R.G. Late Quaternary vegetation history of the Yellowstone Lake basin, Wyoming. U.S. Geological Survey Professional Paper 729-E: E1–E48. (1976). CrossRefGoogle Scholar
Barnett, T.P., Pierce, D.W., Hidalgo, H.G., Bonfils, C., Santer, B.D., Das, T., Bala, G., Wood, A.W., Nozawa, T., Mirin, A.A., Cayan, D.R., and Dettinger, M.D. Human-induced changes in the hydrology of the western United States. Science 319, (2008). 10801083.Google Scholar
Barrett, S.W., and Arno, S.F. Indian fires in the Northern Rockies: ethnohistory and ecology. Boyd, R.T. Indians, Fire and Land in the Pacific Northwest. (1999). Oregon State University Press, Corvallis, OR. 5064.Google Scholar
Bartlein, P.J., Anderson, P.M., Anderson, K.H., Edwards, M.E., Thompson, R.S., Webb, R.S., Webb, T. III, and Whitlock, C. Paleoclimate simulations for North America over the past 21,000 years: features of simulated climate and comparisons with paleoenvironmental data. Quaternary Science Reviews 17, (1998). 549585.Google Scholar
Beiswenger, J.M. Late Quaternary vegetational history of Grays Lake, Idaho. Ecological Monographs 61, (1991). 165182.Google Scholar
Bennett, K.D., and Willis, K.J. Pollen. Smol, J.P., Birks, H.J.B., and Last, W.M. Tracking Environmental Change Using Lake Sediments. Terrestrial, Algal, and Siliceous Indicators 3, (2002). Kluwer Academic Publishers, Dordrecht. 532.Google Scholar
Breckenridge, R.M., Stanford, L.R., Cotter, J.F.P., Bloomfield, J.M., and Evenson, E.B. Glacial geology of the Stanley Basin. Link, P.K., and Hackett, W.R. Guidebook to the Geology of Central and Southern Idaho. Idaho Geological Survey Bulletin 27, (1988). 209211.Google Scholar
Brunelle, A., Whitlock, C., Bartlein, P.J., and Kipfmuller, K. Postglacial fire, climate, and vegetation history along an environmental gradient in the Northern Rocky Mountains. Quaternary Science Reviews 24, (2005). 22812300.Google Scholar
Brunelle, A., Rehfeldt, G.E., Bentz, B., and Munson, A.S. Holocene records of Dendroctonus bark beetles in high elevation pine forests of Idaho and Montana, USA. Forest Ecology and Management 255, (2007). 836846.Google Scholar
Burns, R.M., and Honkala, B.H. Silvics of North America, volume 1, conifers. USDA Forest Service Agricultural Handbook 654. (1990). Google Scholar
Carrara, P.E. Holocene and latest Pleistocene glacial chronology, Glacier National Park Montana. Canadian Journal of Earth Sciences 24, (1987). 387395.Google Scholar
Cook, E.R., Woodhouse, C.A., Eakin, C.J., Meko, D.M., and Stahle, D.W. Long-term aridity changes in the western United States. Science 306, (2004). 10151018.Google Scholar
Daubenmire, R.F. Plants and Environment: A Textbook of Plant Autecology. (1974). John Wiley & Sons, Inc, 432 pp.Google Scholar
Dean, W.E. 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
Dean, W.E., Rosenbaum, J.R., Forester, R.M., Colman, S.M., Bischoff, J.L., Lie, A., Skipp, G., and Simmons, K. Glacial to Holocene evolution of sedimentation in Bear Lake, Utah-Idaho. Sedimentary Geology 185, (2006). 93112.Google Scholar
Deevey, E.S., and Flint, R.F. Postglacial hypsithermal interval. Science 125, (1957). 182184.Google Scholar
Doerner, J.P., and Carrara, P.E. Late Quaternary vegetation and climatic history of the Long Valley area, west-central Idaho, U.S.A.. Quaternary Research 56, (2001). 103111.Google Scholar
Doher, L.I. Palynomorph preparation procedures currently used in the paleontology and stratigraphy laboratories 830, (1980). U.S. Geological Survey Circular, Washington, DC.Google Scholar
Fischer, W.C., and Clayton, B.D. Fire ecology of Montana forest habitat types east of the Continental Divide. USDA Forest Service Intermountain Forest and Range Experiment Station General Technical Report INT-141. (1983). Google Scholar
Gedye, S.J., Jones, R.T., Tinner, W., Ammann, B., and Oldfield, F. The use of mineral magnetism in the reconstruction of fire history: a case study from Lago di Origlio, Swiss Alps. Palaeogeography, Palaeoclimatology, Palaeoecology 164, (2000). 101110.Google Scholar
Grimm, E.C. Data analysis and display. Huntley, B., Webb, T. III Vegetation History. (1988). Kluwer Academic, Dordrecht, Netherlands. 4376.Google Scholar
Hawksworth, F.G., and Wiens, D. Dwarf Mistletoes: Biology, Pathology, and Systematics. USDA Forest Service, Agriculture Handbook 709. (1996). 709 Google Scholar
Higuera, P.E., Brubaker, L.B., Anderson, P.M., Brown, T.A., Kennedy, A.T., and Hu, F.S. Frequent fires in ancient shrub tundra: implications of paleo-records for arctic environmental change. PLoS ONE 3, (2008). e0001744 Google Scholar
Higuera, P., Whitlock, C., Gage, J., in press. Fire history and climate-fire linkages in subalpine forests of Yellowstone National Park, Wyoming, U.S.A., 1240–1975 AD. The Holocene. doi:10.1177/0959683610374882.Google Scholar
Huerta, M., Whitlock, C., and Yale, J. Holocene Vegetation–Fire–Climate Linkages in Northern Yellowstone National Park, USA. Palaeogeography, Palaeoclimatology, Palaeoecology 271, (2009). 170181.Google Scholar
Kapp, R.O., Davis, O.K., and King, J.E. Pollen and Spores. The American Association of Stratigraphic Palynologists. 2nd Edition (2000). Texas A&M University, College Station, Texas. 279 pp.Google Scholar
Kaushal, S., and Binford, M.W. Relationship between C:N ratios of lake sediments, organic matter sources, and historical deforestation in Lake Pleasant, Massachusetts, USA. Journal of Paleolimnology 22, (1999). 439442.Google Scholar
Logan, J.A., and Powell, J.A. Ghost forests, global warming, and the mountain pine beetle (Coleoptera: Scolytidae). American Entomologist, Fall 2001, (2001). 160172.Google Scholar
Marlon, J., Bartlein, P.J., and Whitlock, C. Fire–fuel–climate linkages in the northwestern U.S. during the Holocene. Holocene 16, (2006). 10591071.CrossRefGoogle Scholar
Mehringer, P.J. Jr., Arno, S.F., and Peterson, K.L. Postglacial history of Lost Trail Pass Bog, Bitterroot Mountains, Montana. Arctic and Alpine Research 9, (1977). 345368.Google Scholar
Miller, M. The history of Sawtooth and Virginia City. Idaho Yesterdays 9, (1965). 1116.Google Scholar
Millspaugh, S.H., Whitlock, C., and Bartlein, P.J. Variations in fire frequency and climate over the last 17,000 years in central Yellowstone National Park. Geology 28, (2000). 211214.Google Scholar
Millspaugh, S.H., Whitlock, C., and Bartlein, P. Postglacial fire, vegetation, and climate history of the Yellowstone-Lamar and Central Plateau provinces, Yellowstone National Park. Wallace, L. After the Fires: The Ecology of Change in Yellowstone National Park. (2004). Yale University Press, 1028.Google Scholar
Minckley, T.A., Bartlein, P.J., Whitlock, C., Shuman, B.N., Williams, J.W., and Davis, O.K. Associations among modern pollen, vegetation, and climate in western North America. Quaternary Science Reviews 27, (2008). 19621991.Google Scholar
Moore, P.O., and Webb, J.A. An Illustrated Guide to Pollen Analysis. (1978). John Wiley and Sons, New York.Google Scholar
Mumma, S.A., (2009). A 20,000-yr-old record of vegetation and climate from Lower Red Rock Lake, Centennial Valley, southwestern Montana. M.S. Thesis. Montana State University, Department of Earth Sciences, Bozeman, MT., 72 pp.Google Scholar
Pierce, J.L., Meyer, G.A., and Jull, A.R. Fire-induced erosion and millennial-scale climate change in northern ponderosa pine forests. Nature 432, (2004). 8790.Google Scholar
Power, M.J., (2006). Recent and Holocene fire, climate, and vegetation linkages in the Northern Rocky Mountains, USA. PhD Dissertation, University of Oregon, Eugene, OR., 243 pp.Google Scholar
Power, M.J., Whitlock, C., Bartlein, P.J., and Stevens, L.R. Fire and vegetation history during the last 3800 years in northwestern Montana. Geomorphology 75, (2006). 420436.Google Scholar
Raffa, K.F., Aukema, B.H., Bentz, B.J., Carroll, A.L., Hicke, J.A., Turner, M.G., and Romme, W.H. Cross-scale drivers of natural disturbances prone to anthropogenic amplification: dynamics of biome-wide bark beetle eruptions. Bioscience 58, (2008). 501517.Google Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Bertrand, C.J.H., Blackwell, P.G., Buck, C.E., Burr, G.S., Cutler, K.B., Damon, P.E., Edwards, R.L., Fairbanks, R.G., Friedrich, M., Guilderson, T.P., Hogg, A.G., Hughen, K.A., Kromer, B., McCormac, F.G., Manning, S.W., Ramsey, C.B., Reimer, R.W., Remmele, S., Southon, J.R., Stuiver, M., Talamo, S., Taylor, F.W., van der Plicht, J., and Weyhenmeyer, C.E. IntCal04 Terrestrial radiocarbon age calibration, 26–0 ka BP. Radiocarbon 46, (2004). 10291058.Google Scholar
Romme, W.H., Everham, E.H., Frelich, L.E., Moritz, M.A., and Sparks, R.E. Are large, infrequent disturbances qualitative different from small frequent disturbances?. Ecosystems 1, (1998). 524534.Google Scholar
Sarna-Wojcicki, A.M., Champion, D.E., and Davis, J.O. Holocene volcanism in the conterminous United States and the role of silicic volcanic ash layers in correlation of latest-Pleistocene and Holocene deposits. Wright, H. Jr. Late Quaternary Environments of the United States 2. (1983). University of Minnesota Press, Minneapolis. 5277.Google Scholar
Shafer, S.H., Bartlein, P.J., and Whitlock, C. (2005). Understanding the spatial heterogeneity of global environmental change in mountainous regions. In: Huber, U.M., Bugman, H.K.M., Reasoner, M. (Eds.), Global Change and Mountain Regions: An Overview of Current Knowledge. Kluwer Academic, Dordrecht., pp. 2131. Kluwer.Google Scholar
Shuman, B., Henderson, A.K., Colman, S.M., Stone, J.R., Fritz, S.C., Stevens, L., Power, M.J., and Whitlock, C. Holocene lake-level trends in the Rocky Mountains, U.S.A.. Quaternary Science Reviews 28, (2009). 18611872.Google Scholar
Steele, R., Pfister, R.D., Ryker, R.A., and Kittams, J.A. Forest habitat types of central Idaho. USDA Forest Service General Technical Report, INT-114. (1981). Intermountain Research Station, 138 pp.Google Scholar
Stevens, L.R., Stone, J.R., Campbell, J., and Fritz, S.C. A 2200-year record of hydrologic variability from Foy Lake, Montana USA, inferred from diatom and geochemical data. Quaternary Research 65, (2006). 264274.Google Scholar
Stone, J.R., and Fritz, S.C. Multi-decadal drought and Holocene climate instability in the Rocky Mountains. Geology 34, (2006). 409412.Google Scholar
Stuiver, M., Reimer, P.J., Reimer, R.W., (2005). CALIB 5.0.. [WWW program and documentation].Google Scholar
Sugita, S. Pollen representation of vegetation in Quaternary sediments: theory and method in patchy vegetation. Journal of Ecology 82, (1994). 881897.Google Scholar
Thackray, G.D., Lundeen, K.A., and Borgert, J.A. Latest Pleistocene alpine glacier advances in the Sawtooth Mountains, Idaho, USA: reflections of midlatitude moisture transport at the close of the last glaciation. Geology 32, (2004). 225228.Google Scholar
Thompson, R.S., Anderson, K.H., and Bartlein, P.J. Atlas of relations between climatic parameters and distributions of important trees and shrubs in North America. U.S. Geological Survey Professional Paper 1650 A&B. (1999). Google Scholar
van Mantgem, P.J., Stephenson, N.L., Byrne, J.C., Daniels, L.D., Franklin, J.F., Fule, P.Z., Harmon, M.E., Larson, A.J., Smith, J.M., Taylor, A.H., and Veblen, T.T. Widespread increase of tree mortality rates in the western United States. Science 323, (2009). 521524.Google Scholar
Westerling, A.L., Hidalgo, H.G., Cayan, D.R., and Swetnam, T.W. Warming and earlier spring increase western US forest wildfire activity. Science 313, (2006). 940943.Google Scholar
Whitlock, C. Postglacial vegetation and climate of Grand Teton and southern Yellowstone National parks. Ecological Monographs 63, (1993). 173198.Google Scholar
Whitlock, C., and Bartlein, P.J. Spatial variations of Holocene climatic change in the Yellowstone region. Quaternary Research 39, (1993). 231238.Google Scholar
Whitlock, C., and Larsen, C.P.S. Charcoal as a fire proxy. Smol, J.P., Birks, H.J.B., and Last, W.M. Tracking Environmental Change Using Lake Sediments:. Terrestrial, Algal, and Siliceous indicators 3, (2002). Kluwer Academic Publishers, Dordrecht. 7597.Google Scholar
Whitlock, C., Skinner, C.N., Minckley, T.A., and Mohr, J.A. Comparison of charcoal and tree-ring records of recent fires in the eastern Klamath Mountains California, USA. Canadian Journal of Forest Research 34, (2004). 21102121.Google Scholar
Whitlock, C., Marlon, J., Briles, C., Brunelle, A., Long, C., and Bartlein, P.J. Long-term relations among fire, fuel, and climate in the north-western US based on lake-sediment studies. International Journal of Wildland Fire 17, (2008). 7283.Google Scholar
Williams, P.L. Glacial geology of the Stanley Basin: Moscow, Idaho Bureau of Mines and Geology, Pamphlet 123, (1961). 29 pp.Google Scholar
Wright, H.E. Jr., Mann, D.H., and Glaser, P.H. Piston cores for peat and lake sediments. Ecology 65, (1983). 657659.Google Scholar