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Late-Holocene response of limber pine (Pinus flexilis) forests to fire disturbance in the Pine Forest Range, Nevada, USA

Published online by Cambridge University Press:  20 August 2012

Robert K. Shriver  and
Thomas A. Minckley
Robert K. Shriver
Affiliation:
Dept. of Botany, University of Wyoming, Laramie, WY 82071, USA
Thomas A. Minckley*
Affiliation:
Dept. of Botany, University of Wyoming, Laramie, WY 82071, USA Roy J. Shlemon Center for Quaternary Studies, University of Wyoming, Laramie, WY 82071, USA
*
⁎Corresponding author at: Dept. of Geography, University of Wyoming, Laramie, WY 82071, USA. Fax: + 1 307 766 2851. Email Address:minckley@uwyo.edu
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Abstract

Despite growing concerns that ecological stressors (fire, insect and pathogen outbreaks) may force vegetation change, few studies have attempted to use paleoecological data to understand small-scale interactions between disturbance and vegetation. Using charcoal and pollen data, we infer past fire episodes and subsequent vegetation responses for a limber pine (Pinus flexilis) forest in northwestern Nevada, USA, to determine local vegetation recovery from disturbance. Using superimposed epoch analysis we examined average-vegetation and individual-taxon responses to eight randomly selected fire events over the past 4.0 ka. Pollen evidence shows that on average fires produce a weak response of declining Pinus while other taxa including Artemisia and Poaceae increase directly after fire episodes. Within 30 yr of a disturbance, pollen data indicate ecosystem recovery to pre-fire composition, consistent with modern studies of fire recovery of limber pine forests. Similar to short-term changes of pollen abundance, long-term vegetation responses indicate Pinus abundance weakly declining and Artemisia increasing when fire episodes are frequent. However, despite fire-episode frequencies varying between 75 and 250 yr, the overall vegetation structure has remained relatively stable over the past 4.0 ka. Our study contributes to the limited information on the disturbance ecology of isolated, subalpine forests in the intermountain West.

Keywords

Limber pineFire historyDisturbance ecologySuperimposed epoch analysisSubalpine forestNevada
Type
Articles
Information
Quaternary Research , Volume 78 , Issue 3 , November 2012 , pp. 465 - 473
Copyright
University of Washington

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Footnotes

1 Current address: University Program in Ecology, Duke University, Durham, NC, 27708, USA.

References

Arno, S.F., and Hammerly, R.P. Timberline: Mountain and Arctic Forest Frontiers. (1984). The Mountaineers, Seattle, WA.Google Scholar
Blarquez, O., and Carcaillet, C. Fire, fuel composition and resilience threshold in subalpine ecosystem. PloS One 5, (2010). Google Scholar
Briles, C.E., Whitlock, C., and Bartlein, P.J. Postglacial vegetation, fire, and climate history of the Siskiyou Mountains, Oregon, USA. Quaternary Research 64, (2005). 44–56.Google Scholar
Brunelle, A., and Whitlock, C. Postglacial fire, vegetation, and climate history in the Clearwater Range, Northern Idaho, USA. Quaternary Research 60, (2003). 307–318.Google Scholar
Conedera, M., Tinner, W., Neff, C., Meurer, M., Dickens, A.F., and Krebs, P. Reconstructing past fire regimes: methods, applications, and relevance to fire management and conservation. Quaternary Science Reviews 28, (2009). 555–576.CrossRefGoogle Scholar
Coop, J.D., and Schoettle, A.W. Regeneration of Rocky Mountain bristlecone pine (Pinus aristata) and limber pine (Pinus flexilis) three decades after stand-replacing fires. Forest Ecology and Management 257, (2009). 893–903.Google Scholar
Coop, J.D., and Schoettle, A.W. Fire and high-elevation, five-needle pine (Pinus aristata and P. flexilis) ecosystems in the southern Rocky Mountains: what do we know?. Keane, R.E., Tomback, D.F., Murray, M.P., and Smith, C.M. The Future of High-elevation, Five-needle White Pines in Western North America: Proceedings of the High Five Symposium. (2011). U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Missoula, MT. 2–28.Google Scholar
Daily, G.C. Nature's Services: Societal Dependance on Natural Ecosystems. (1997). Island Press, Washington, D.C..Google Scholar
Dean, W.E. 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, (1974). 242–248.Google Scholar
Faegri, K., Kaland, P.E., and Kzywinski, K. Textbook of Pollen Analysis. (1989). Wiley, New York.Google Scholar
Fagre, D.B., Charles, C.W., Allen, C.D., Birkeland, C., Chapin, F.S. III, Groffman, P.M., Guntenspergen, G.R., Knapp, A.K., McGuire, A.D., Mulholland, P.J., Peters, D.P.C., Roby, D.D., and Sugihara, G. Case studies. Fagre, D.B., Charles, C.W., Allen, C.D., Birkeland, C., Chapin, F.S. III, Groffman, P.M., Guntenspergen, G.R., Knapp, A.K., McGuire, A.D., Mulholland, P.J., Peters, D.P.C., Roby, D.D., and Sugihara, G. Thresholds of Climate Change in Ecosystems. A Report by the U.S. Climate Change Science Program and the Subcommittee on Global Change Research (2009). U.S. Geological Survey, Reston, VA. 35–40.Google Scholar
Gardner, J.J., and Whitlock, C. Charcoal accumulation following a recent fire in the Cascade Range, northwestern USA, and its relevance for fire-history studies. The Holocene 11, (2001). 541–549.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). 101–110.Google Scholar
Geils, B.W., and Vogler, D.R. A natural history of Cronartium ribicola . Keane, R.E., Tomback, D.F., Murray, M.P., and Smith, C.M. The Future of High-elevation, Five-needle White Pines in Western North America: Proceedings of the High Five Symposium. (2011). U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Missoula, MT. 2–28.Google Scholar
Genries, A., Mercier, L., Lavoie, M., Muller, S.D., Radakovitch, O., and Carcaillet, C. The effect of fire frequency on local cembra pine populations. Ecology 90, (2009). 476–486.Google Scholar
Grimm, E.C. Data analysis and display. Huntley, B., Webb, T. III Vegetation History. (1988). Kluwer Academic, Dordrecht, Netherlands. 43–76.Google Scholar
Hallett, D.J., and Anderson, R.S. Paleofire reconstruction for high-elevation forests in the Sierra Nevada, California, with implications for wildfire synchrony and climate variability in the late Holocene. Quaternary Research 73, (2010). 180–190.Google Scholar
Higuera, P.E., Peters, M.E., Brubaker, L.B., and Gavin, D.G. Understanding the origin and analysis of sediment–charcoal records with a simulation model. Quaternary Science Reviews 26, (2007). 1790–1809.Google Scholar
Higuera, P.E., Brubaker, L.B., Anderson, P.M., Hu, F.S., and Brown, T.A. Vegetation mediated the impacts of postglacial climate change on fire regimes in the south-central Brooks Range, Alaska. Ecological Monographs 79, (2009). 201–219.CrossRefGoogle Scholar
Jacobson, G.L., and Bradshaw, R.H.W. The selection of sites for paleovegetational studies. Quaternary Research 16, (1981). 80–96.Google Scholar
Lertzman, K.P., and Fall, J. From forest stands to landscapes: spatial scales and the roles of disturbances. Peterson, D.L., and Parker, V.T. Ecological Scale: Theory and Applications. (1998). Columbia University Press, New York, New York, USA. 339–367.Google Scholar
Long, C.J., Whitlock, C., Bartlein, P.J., and Millspaugh, S.H. A 9000-year fire history from the Oregon Coast Range, based on a high-resolution charcoal study. Canadian Journal of Forest Research Revue Canadienne De Recherche Forestiere. 28, (1998). 774–787.Google Scholar
Malmstrom, C.M., and Raffa, K.F. Biotic disturbance agents in the boreal forest: considerations for vegetation change models. Global Change Biology 6, (2000). 35–48.Google Scholar
Marlon, J.R., Bartlein, P.J., Carcaillet, C., Gavin, D.G., Harrison, S.P., Higuera, P.E., Joos, F., Power, M.J., and Prentice, I.C. Climate and human influences on global biomass burning over the past two millennia. Nature Geoscience 1, (2008). 697–702.Google Scholar
Marlon, J.R., Bartlein, P.J., Walsh, M.K., Harrison, S.P., Brown, K.J., Edwards, M.E., Higuera, P.E., Power, M.J., Anderson, R.S., Briles, C., Brunelle, A., Carcaillet, C., Daniels, M., Hu, F.S., Lavoie, M., Long, C., Minckley, T., Richard, P.J.H., Scott, A.C., Shafer, D.S., Tinner, W., Umbanhowar, C.E., and Whitlock, C. Wildfire responses to abrupt climate change in North America. Proceedings of the National Academy of Sciences 106, (2009). 2519–2524.CrossRefGoogle ScholarPubMed
McCaughey, W.W., and Schmidt, W.C. Autecology of whitebark pine. Schmidt, W.C., and McDonald, K.J. Symposium on Whitebark Pine Ecosystems: Ecology and Management of a High-mountain Resource. (1990). USDA Forest Service Intermountain Research Station, Ogden, UT. 85–96.Google Scholar
McDonald, K.A., and Brown, J.H. Using montane mammals to model extinctions due to global change. Conservation Biology 6, (1992). 409–415.Google Scholar
McDonald, G.I., and Hoff, R.J. Blister rust: an introduced plague. Tomback, D.F., Arno, S.F., and Keane, R.E. Whitebark Pine Communities: Ecology and Restoration. (2001). Island Press, Washington, DC. 193–220.Google Scholar
Millar, C.I., and Woolfenden, W.B. The role of climate change in interpreting historical variability. Ecological Monographs 9, (1999). 1207–1216.Google Scholar
Millspaugh, S.H., Whitlock, C., and Bartlein, P.J. Variations in fire frequency and climate over the past 17 000 yr in central Yellowstone National Park. Geology 28, (2000). 211–214.Google Scholar
Minckley, T.A., and Shriver, R.K. Fire regime shifts in a Rocky Mountain forest, USA. Journal of Fire Ecology 7, (2011). 66–80.Google Scholar
Minckley, T.A., Whitlock, C., and Bartlein, P.J. Vegetation, fire, and climate history of the northwestern Great Basin during the last 14,000 years. Quaternary Science Reviews 26, (2007). 2167–2184.CrossRefGoogle Scholar
Minckley, T.A., Booth, R.K., and Jackson, S.T. Response of arboreal pollen abundance to late-Holocene drought events in the Upper Midwest, USA. The Holocene 22, (2012). 531–539.Google Scholar
Minckley, T.A., Shriver, R.K., and Shuman, B. Resilience and regime change in a southern Rocky Mountain ecosystem during the past 17000 years. Ecological Monographs 82, (2012). 49–68.Google Scholar
Mohr, J.A., Whitlock, C., and Skinner, C.N. Postglacial vegetation and fire history, eastern Klamath Mountains, California, USA. The Holocene 10, (2000). 587–601.Google Scholar
Moore, P.D., Webb, J.A., and Collinson, M.E. Pollen Analysis. (1991). Blackwell, London.Google Scholar
Morris, J.L., Brunelle, A.R., and Munson, A.S. Pollen evidence of historical forest disturbance on the Wasatch Plateau, Utah. Western North American Naturalist 70, (2010). 175–188.Google Scholar
Overpeck, J.T., Rind, D., and Goldberg, R. Climate-induced changes in forest disturbance and vegetation. Nature 343, (1990). 51–53.Google Scholar
Pierce, J.L., Meyer, G.A., and Timothy Jull, A.J. Fire-induced erosion and millennial-scale climate change in northern ponderosa pine forests. Nature 432, (2004). 87–90.Google Scholar
Power, M.J., Marlon, J., Ortiz, N., Bartlein, P.J., Harrison, S.P., Mayle, F.E., Ballouche, A., Bradshaw, R.H.W., Carcaillet, C., Cordova, C., Mooney, S., Moreno, P.I., Prentice, I.C., Thonicke, K., Tinner, W., Whitlock, C., Zhang, Y., Zhao, Y., Ali, A.A., Anderson, R.S., Beer, R., Behling, H., Briles, C., Brown, K.J., Brunelle, A., Bush, M., Camill, P., Chu, G.Q., Clark, J., Colombaroli, D., Connor, S., Daniau, A.L., Daniels, M., Dodson, J., Doughty, E., Edwards, M.E., Finsinger, W., Foster, D., Frechette, J., Gaillard, M.J., Gavin, D.G., Gobet, E., Haberle, S., Hallett, D.J., Higuera, P., Hope, G., Horn, S., Inoue, J., Kaltenrieder, P., Kennedy, L., Kong, Z.C., Larsen, C., Long, C.J., Lynch, J., Lynch, E.A., McGlone, M., Meeks, S., Mensing, S., Meyer, G., Minckley, T., Mohr, J., Nelson, D.M., New, J., Newnham, R., Noti, R., Oswald, W., Pierce, J., Richard, P.J.H., Rowe, C., Goni, M.F.S., Shuman, B.N., Takahara, H., Toney, J., Turney, C., Urrego-Sanchez, D.H., Umbanhowar, C., Vandergoes, M., Vanniere, B., Vescovi, E., Walsh, M., Wang, X., Williams, N., Wilmshurst, J., and Zhang, J.H. Changes in fire regimes since the Last Glacial Maximum: an assessment based on a global synthesis and analysis of charcoal data. Climate Dynamics 30, (2008). 887–907.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: the dynamics of bark beetle eruptions. Bioscience 58, (2008). 501–517.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, G., Manning, S., 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, 0–26 cal kyr BP. Radiocarbon 46, (2004). 1029–1058.Google Scholar
Shuman, B., Pribyl, P., Minckley, T.A., and Shinker, J.J. Rapid hydrologic shifts and prolonged droughts in Rocky Mountain headwaters during the Holocene. Geophysical Research Letters 37, (2010). L06701 Google Scholar
Sugita, S. Pollen representation of vegetation in Quaternary sediments — theory and method in patchy vegetation. Journal of Ecology 82, (1994). 881–897.Google Scholar
Sugita, S., MacDonald, G.M., and Larsen, C.P.S. Reconstruction of fire disturbance and forest succession from fossil pollen in lake sediments: potentials and limitations. Clark, J.S., Cachier, H., and Goldammer, J.G. Sediment Records of Biomass Burning and Global Change. (1997). Springer-Verlag, Berlin Heidelberg. 387–408.Google Scholar
Sugita, S., Gaillard, M.J., and Brostrom, A. Landscape openness and pollen records: a simulation approach. The Holocene 9, (1999). 409–421.Google Scholar
Swetnam, T.W., Allen, C.D., and Betancourt, J.L. Applied historical ecology: using the past to manage for the future. Ecological Monographs 9, (1999). 1189–1206.Google Scholar
Tausch, R.J., Nowak, C.L., and Mensing, S.A. Climate change and associated vegetation dynamic during the Holocene: the paleoecological record. Chambers, J.C., and Miller, J.R. Great Basin Riaprian Ecosystems. (2004). Island Press, Washington. 24–48.Google Scholar
Tomback, D.F., Achuff, P., Schoettle, A.W., Schwandt, J.W., and Mastrogiuseppe, R.J. The magnificent high-elevation five-needle white pines: ecological roles and future outlook. Keane, R.E., Tomback, D.F., Murray, M.P., and Smith, C.M. The Future of High-elevation, Five-needle White Pines in Western North America: Proceedings of the High Five Symposium. (2011). U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Missoula, MT. 2–28.Google Scholar
van der Knaap, W., van Leeuwen, J., Svitavská-Svobodová, H., Pidek, I., Kvavadze, E., Chichinadze, M., Giesecke, T., Kaszewski, B., Oberli, F., Kalniņa, L., Pardoe, H., Tinner, W., and Ammann, B. Annual pollen traps reveal the complexity of climatic control on pollen productivity in Europe and the Caucasus. Vegetation History and Archaeobotany 19, (2010). 285–307.Google Scholar
Wanner, H., Beer, J., Bütikofer, J., Crowley, T.J., Cubasch, U., Flückiger, J., Goosse, H., Grosjean, M., Joos, F., Kaplan, J.O., Küttel, M., Müller, S.A., Prentice, I.C., Solomina, O., Stocker, T.F., Tarasov, P., Wagner, M., and Widmann, M. Mid- to Late Holocene climate change: an overview. Quaternary Science Reviews 27, (2008). 1791–1828.Google Scholar
Westerling, A.L., Gershunov, A., Brown, T.J., Cayan, D.R., and Dettinger, M.D. Climate and wildfire in the western United States. Bulletin of the American Meteorological Society 84, (2003). 595–604.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). 940–943.Google Scholar
Whitlock, C. Postglacial vegetation and climate of Grand Teton and southern Yellowstone National Parks. Ecological Monographs 63, (1993). 173–198.CrossRefGoogle Scholar
Whitlock, C., Marlon, J., Briles, C., Brunelle, A., Long, C., and Bartlein, P. 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). 72–83.Google Scholar
Williams, J.W., and Jackson, S.T. Novel climates, no-analog communities, and ecological surprises. Frontiers in Ecology and the Environment 5, (2007). 475–482.Google Scholar
Williams, J.W., Jackson, S.T., and Kutzbacht, J.E. Projected distributions of novel and disappearing climates by 2100 AD. Proceedings of the National Academy of Sciences of the United States of America 104, (2007). 5738–5742.Google Scholar