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A 14,300-year-long record of fire–vegetation–climate linkages at Battle Ground Lake, southwestern Washington

Published online by Cambridge University Press:  20 January 2017

Megan K. Walsh ,
Cathy Whitlock  and
Patrick J. Bartlein
Megan K. Walsh*
Affiliation:
Department of Geography, University of Oregon, Eugene, OR 97403, USA
Cathy Whitlock
Affiliation:
Department of Earth Sciences, Montana State University, Bozeman MT 59717, USA
Patrick J. Bartlein
Affiliation:
Department of Geography, University of Oregon, Eugene, OR 97403, USA
*
*Corresponding author. Department of Geography, University of Oregon, Eugene, OR 97403, USA. Fax: +1 541 346 2067. E-mail address:[email protected] (M.K. Walsh).
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Abstract

High-resolution macroscopic charcoal analysis was used to reconstruct a 14,300-year-long fire history record from the lower Columbia River Valley in southwestern Washington, which was compared to a previous vegetation reconstruction for the site. In the late-glacial period (ca. 14,300-13,100 cal yr BP), Pinus/Picea-dominated parkland supported little to no fire activity. From the late-glacial to the early Holocene (ca. 13,100-10,800 cal yr BP), Pseudotsuga/Abies-dominated forest featured more frequent fire episodes that burned mostly woody vegetation. In the early to middle Holocene (ca. 10,800-5200 cal yr BP), Quercus-dominated savanna was associated with frequent fire episodes of low-to-moderate severity, with an increased herbaceous (i.e., grass) charcoal content. From the middle to late Holocene (ca. 5200 cal yr BP to present), forest dominated by Pseudotsuga, Thuja-type, and Tsuga heterophylla supported less frequent, but mostly large or high-severity fire episodes. Fire episodes were least frequent, but were largest or most severe, after ca. 2500 cal yr BP. The fire history at Battle Ground Lake was apparently driven by climate, directly through the length and severity of the fire season, and indirectly through climate-driven vegetation shifts, which affected available fuel biomass.

Keywords

Fire historyMacroscopic charcoalPollenLate-glacialHoloceneLower Columbia River ValleyWashington
Type
Original Articles
Information
Quaternary Research , Volume 70 , Issue 2 , September 2008 , pp. 251 - 264
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
Aikens, M.C., (1993). Archaeology of Oregon.. US Department of the Interior Bureau of Land Management, Portland.Google Scholar
Alley, R.B., (2000). The Younger Dryas cold interval as viewed from central Greenland.. Quaternary Science Reviews 19, 213–226.Google Scholar
Allworth, L.M., (1976). Battle Ground…In and Around.. Taylor Publishing Company, Dallas.Google Scholar
Ames, K.M., (2003). The Northwest Coast.. Evolutionary Anthropology 12, 19–33.Google Scholar
Barnosky, C.W., (1985). Late Quaternary vegetation near Battle Ground Lake, southern Puget Trough, Washington.. Geological Society of America Bulletin 96, 263–271.Google Scholar
Bartlein, P.J., Anderson, K.H., Anderson, P.M., Edwards, M.E., Mock, C.J., Thompson, R.S., Webb, T. III, Whitlock, C., (1998). Paleoclimatic simulations for North America over the past 21,000 years: features of the simulated climate and comparisons with paleoenvironmental data.. Quaternary Science Reviews 17, 549–585.Google Scholar
Berger, A., Loutre, M.F., (1991). Insolation values for the last 10 million years.. Quaternary Science Reviews 10, 297–317.Google Scholar
Boyd, R.T., (1986). Strategies of Indian burning in the Willamette Valley.. Canadian Journal of Anthropology 5, 67–86.Google Scholar
Boyd, R.T., Hajda, Y.P., (1984). Seasonal population movement along the lower Columbia River: the social and ecological context.. American Ethnologist 14, 309–326.Google Scholar
Brown, K.J., Hebda, R.J., (2002a). Origin, development, and dynamics of coastal temperate conifer rainforests of southern Vancouver Island, Washington.. Canadian Journal of Forest Research 32, 353–372.Google Scholar
Brown, K.J., Hebda, R.J., (2002b). Ancient fires on southern Vancouver Island, British Columbia, Canada: a change in causal mechanisms at about 2000 ybp.. Environmental Archaeology 7, 1–12.Google Scholar
Brown, K.J., Hebda, R.J., (2003). Coastal rainforest connections disclosed through a Late Quaternary vegetation, climate, and fire history investigation from the Mountain Hemlock Zone on southern Vancouver Island, British Columbia, Canada.. Review of Palaeobotany and Palynology 123, 247–269.Google Scholar
Brunelle, A., Whitlock, C., (2003). Postglacial fire, vegetation, and climate history in the Clearwater Range, Northern Idaho, USA.. Quaternary Research 60, 307–318.Google Scholar
Carcaillet, C., Almquist, H., Asnong, H., Bradshaw, R.H.W., Carrión, J.S., Gaillard, M.-J., Gajewski, K., Haas, J.N., Haberle, S.G., Hadorn, P., Müller, S.D., Richard, P.J.H., Richoz, I., Rösch, M., Sánchez Goñi, M.F., von Stedingk, H., Stevenson, A.C., Talon, B., Tardy, C., Tinner, W., Tryterud, E., Wick, L., Willis, K.J., (2002). Holocene biomass burning and global dynamics of the carbon cycle.. Chemosphere 49, 845–863.Google Scholar
Cook, E.R., Woodhouse, C.A., Eakin, C.M., Meko, D.M., Stahle, D.W., (2004). Long-term aridity changes in the western United States.. Science 306, 1015–1018.Google Scholar
Crandall, D.R., Miller, R.D., (1974). Quaternary stratigraphy and extent of glaciation in the Mount Rainier region, Washington.. US Geological Survey Professional Paper 450-D, 59.Google Scholar
Cwynar, L.C., (1987). Fire and the forest history of the north Cascade Range.. Ecology 68, 791–802.Google Scholar
Dean, W.E. Jr. (1974). Determination of carbonate and organic matter in calcareous sediments by loss on ignition comparison with other methods.. Journal of Sedimentary Petrology 44, 242–248.Google Scholar
Faegri, K., Kaland, P.E., Krzywinski, K., (1989). Textbook of Pollen Analysis.. John Wiley and Sons, New York.Google Scholar
Franklin, J.F., Dyrness, C.T., (1988). Natural Vegetation of Oregon and Washington.. Oregon State University Press, Corvallis.Google Scholar
Gardner, J.J., Whitlock, C., (2001). Charcoal accumulation following a recent fire in the Cascade Range, northwestern USA, and its relevance for fire-history studies.. The Holocene 11, 541–549.Google Scholar
Gavin, D.G., Hu, F.S., Lertzman, K., Corbett, P., (2006). Weak climatic control of stand-scale fire history during the late Holocene.. Ecology 87, 1722–1732.Google Scholar
Gedalof, Z., Peterson, D.L., Mantua, N.L., (2005). Atmospheric, climatic, and ecological controls on extreme wildfire years in the northwestern United States.. Ecological Applications 15, 154–174.Google Scholar
Graumlich, L.J., (1993). A 1000-year record of temperature and precipitation in the Sierra Nevada.. Quaternary Research 39, 249–255.Google Scholar
Graumlich, L.J., Brubaker, L.B., (1986). Reconstruction of annual temperature (1590–1979) for Longmire, Washington, derived from tree rings.. Quaternary Research 25, 223–234.Google Scholar
Gray, A., (1990). Forest Structure on the Siouxon Burn, Southern Washington Cascades: Comparison of Single and Multiple burns, M.S.. thesis, University of Washington, Seattle.Google Scholar
Grigg, L.D., Whitlock, C., (1998). Late-glacial vegetation and climate change in western Oregon.. Quaternary Research 49, 287–298.Google Scholar
Grigg, L.D., Whitlock, C., (2002). Patterns and causes of millennial-scale climate change in the Pacific Northwest during Marine Isotope Stages 2 and 3.. Quaternary Science Reviews 21, 2067–2083.Google Scholar
Grove, A.T., (2001). The “Little Ice Age” and its geomorphological consequences in Mediterranean Europe.. Climatic Change 48, 121–136.Google Scholar
Hallett, D.J., Lepofsky, D.S., Mathewes, R.W., Lertzman, K.P., (2003). 11,000 years of fire history and climate in the mountain hemlock rain forests of southwestern British Columbia based on sedimentary charcoal.. Canadian Journal of Forest Research 33, 292–312.Google Scholar
Heusser, C.J., Heusser, L.E., (1980). Sequence of pumicious tephra layers and late Quaternary environmental record near Mount St.. Helens. Science 210, 1007–1009.Google Scholar
Heusser, C.J., Heusser, L.E., Peteet, D.M., (1985). Late-Quaternary climatic change on the American North Pacific Coast.. Nature 315, 485–487.Google Scholar
Higuera, P.E., Brubaker, L.B., Anderson, P.M., Brown, T.A., Kennedy, A.T., Hu, F.S., (2008). Frequent fires in ancient shrub tundra: implications of paleorecords for arctic environmental change.. PLoS One 3, e0001744.Google Scholar
Higuera, P.E., Peters, M.E., Brubaker, L.A., Gavin, D.G., (2007). Understanding the origin and analysis of sediment-charcoal records with a simulation model.. Quaternary Science Reviews 26, 1790–1809.Google Scholar
Hitchcock, C.L., Cronquist, A., (1973). Flora of the Pacific Northwest.. University of Washington Press, Seattle.Google Scholar
Hulse, D., Gregory, S., Baker, J., (2002). Willamette River Basin Planning Atlas: Trajectories of Environmental and Ecological Change.. Oregon State University Press, Corvallis.Google Scholar
Jensen, K., Lynch, E.A., Calcote, R., Hotchkiss, S.C., (2007). Interpretation of charcoal morphotypes in sediments from Ferry Lake, Wisconsin, USA: do different plant fuel sources produce distinctive charcoal morphotypes? The Holocene 17, 907–915.Google Scholar
Juvigné, E.H., (1986). Late-Quaternary sediments at Battle Ground Lake, southern Puget Trough, Washington.. Northwest Science 60, 210–217.Google Scholar
Kaufman, D.S., Porter, S.C., Gillespie, A.R., (2004). Quaternary alpine glaciation in Alaska, the Pacific Northwest, Sierra Nevada, and Hawaii.. Gillespie, A.R., Porter, S.C., Atwater, B.F. The Quaternary Period in the United States Elsevier, Amsterdam., pp. 77–104.Google Scholar
Leavitt, S.W., (1994). Major wet interval in White Mountains Medieval Warm Period evidenced in δ13C of bristlecone pine tree rings.. Climatic Change 26, 299–307.Google Scholar
Leopold, E.B., Boyd, R.T., (1999). An ecological history of old prairie areas in southwestern Washington.. Boyd, R.T. Indians, Fire, and the Land in the Pacific Northwest 94–138.Google Scholar
Long, C.J., Whitlock, C., (2002). Fire and vegetation history from the coastal rain forest of the western Oregon Coast Range.. Quaternary Research 58, 215–225.Google Scholar
Long, C.J., Whitlock, C., Bartlein, P.J., 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, 774–782.Google Scholar
Luckman, B.H., (1995). Calendar-dated, early “Little Ice Age” glacier advance at Robson Glacier, British Columbia, Canada.. The Holocene 5, 149–159.Google Scholar
Mann, M.E., (2002). Medieval Climatic Optimum.. MacCracken, M.C., Perry, J.S. Encyclopedia of Global Environmental Change, Volume 1, The Earth System: Physical and Chemical Dimensions of Global Environmental Change John Wiley and Sons, Chichester., pp. 514–516.Google Scholar
Maret, M.P., Wilson, M.V., (2005). Fire and litter effects on seedling establishment in western Oregon upland prairies.. Restoration Ecology 13, 562–568.Google Scholar
Marlon, J., Bartlein, P.J., Whitlock, C., (2006). Fire-fuel-climate linkages in the northwestern USA during the Holocene.. The Holocene 16, 1059–1071.Google Scholar
Mathewes, R.W., (1993). Evidence for Younger Dryas-age cooling on the north Pacific coast of America.. Quaternary Science Reviews 12, 321–331.Google Scholar
McKenzie, D., Gedalof, Z., Peterson, D.L., Mote, P., (2004). Climatic change, wildfire, and conservation.. Conservation Biology 18, 890–902.Google Scholar
Millspaugh, S.H., Whitlock, C., (1995). A 750-year fire history based on lake sediment records in central Yellowstone National Park, USA.. The Holocene 5, 283–292.Google Scholar
Mitchell, V.L., (1976). The regionalization of climate in the western United States.. Journal of Applied Meteorology 15, 920–927.Google Scholar
Mock, C.J., (1996). Climatic controls and spatial variations of precipitation in the western United States.. Journal of Climate 9, 1111–1125.Google Scholar
Mohr, J.A., Whitlock, C., Skinner, C.J., (2000). Postglacial vegetation and fire history, eastern Klamath Mountains, California.. The Holocene 10, 587–601.Google Scholar
Morris, W.G., (1934). Forest fires in western Oregon and western Washington.. Oregon Historical Quarterly 35, 313–339.Google Scholar
Mullineaux, D.R., (1986). Summary of pre-1980 tephra-fall deposits erupted from Mount St.. Helens, Washington State, USA. Bulletin of Volcanology 48, 17–26.Google Scholar
Patterson, W.A. III, Edwards, K.J., Maguire, D.J., (1987). Microscopic charcoal as a fossil indicator of fire.. Quaternary Science Reviews 6, 3–23.Google Scholar
Pendergrass, K.L., Miller, P.M., Kauffman, J.B., (1998). Prescribed fire and the response of woody species in Willamette Valley wetland prairies.. Restoration Ecology 6, 303–311.Google Scholar
Pettigrew, R.M., (1990). Prehistory of the Lower Columbia and Willamette Valley.. Suttles, W.P. Handbook of North American Indians Volume 7, Northwest Coast Smithsonian Institution, Washington, D.C., pp. 518–529.Google Scholar
Sea, D.S., Whitlock, C., (1995). Postglacial vegetation and climate of the Cascade Range, central Oregon.. Quaternary Research 43, 370–381.Google Scholar
Sharp, J., Mass, C.F., (2004). Columbia Gorge gap winds: their climatological influence and synoptic evolution.. Weather and Forecasting 19, 970–992.Google Scholar
Stine, S., (1994). Extreme and persistent drought in California and Patagonia during medieval time.. Nature 369, 546–549.Google Scholar
Stuiver, M., Reimer, P.J., (2005). CALIB Radiocarbon Calibration version 5.0.2 html. Available at http://calib.qub.ac.uk/calib/.Google Scholar
Thilenius, J.F., (1968). The Quercus garryana forests of the Willamette Valley, Oregon.. Ecology 49, 1124–1133.Google Scholar
Thompson, R.S., Whitlock, C., Bartlein, P.J., Harrison, S.P., Spaulding, W.G., (1993). Climate changes in the western United States since 18,000 yr BP.. Wright, H.E. Jr., Kutzbach, J.E., Webb, T. III, Ruddiman, W.F., Street-Perrott, F.A., Bartlein, P.J. Global Climates Since the Last Glacial Maximum University of Minnesota Press, Minneapolis., pp. 468–513.Google Scholar
Tsukada, M., Sugita, S., Hibbert, D.M., (1981). Paleoecology in the Pacific Northwest I. Late Quaternary vegetation and climate.. Proceedings-International Association of Theoretical and Applied Limnology 21, 730–737.Google Scholar
Turner, N.J., Kuhnlein, H.V., (1983). Camas (Camassia spp.) and riceroot (Fritillaria spp.): two liliaceous “root” foods of the Northwest Coast Indians.. Ecology of Food and Nutrition 13, 199–219.Google Scholar
Vacco, D.A., Clark, P.U., Mix, A.C., Cheng, H., Lawrence Edwards, R., (2005). A speleothem record of Younger Dryas cooling, Klamath Mountains, Oregon, USA.. Quaternary Research 64, 249–256.Google Scholar
Weisberg, P.J., Swanson, F.J., (2003). Regional synchroneity in fire regimes of the western Cascades, USA.. Forest Ecology and Management 172, 17–28.Google Scholar
Western Regional Climate Center (2007). Available athttp://www.wrcc.dri.edu.Google Scholar
Whitlock, C., (1992). Vegetational and climatic history of the Pacific Northwest during the last 20,000 years: implications for understanding present-day biodiversity.. Northwest Environmental Journal 8, 5–28.Google Scholar
Whitlock, C., Bartlein, P.J., (2004). Holocene fire activity as a record of past environmental change.. Gillespie, A.R., Porter, S.C., Atwater, B.F. The Quaternary Period in the United States Elsevier, Amsterdam., pp. 479–490.Google Scholar
Whitlock, C., Bianchi, M.M., Bartlein, P.J., Markgraf, V., Marlon, J., Walsh, M., McCoy, N., (2006). Postglacial vegetation, climate, and fire history along the east side of the Andes (lat 41–42.5°S), Argentina.. Quaternary Research 66, 187–201.Google Scholar
Whitlock, C., Larsen, C.P.S., (2001). 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 Volume 2 Kluwer Academic Publishers, Dordrecht., pp. 75–97.Google Scholar
Whitlock, C., Marlon, J., Briles, C., Brunelle, A., Long, C., Bartlein, P., (2008). Long-term relations among fire, fuel, and climate in the north-western US based on lake-sediment studies.. International Journal of Wildland Fire 17, 72–83.Google Scholar
Whitlock, C., 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, 7–15.Google Scholar
Whitlock, C., Shafer, S.L., Marlon, J., (2003). The role of climate and vegetation change in shaping past and future fire regimes in the northwestern US and the implications for ecosystem management.. Forest Ecology and Management 178, 5–21.Google Scholar
Wiles, G.C., Barclay, D.J., Calkin, P.E., (1999). Tree-ring-dated “Little Ice Age” histories of maritime glaciers from western Prince William Sound, Alaska.. The Holocene 9, 163–173.Google Scholar
Wood, C.A., Kienle, J., (1990). Volcanoes of North America: United States and Canada.. Cambridge University Press, England.Google Scholar
Worona, M.A., Whitlock, C., (1995). Late Quaternary vegetation and climate history near Little Lake, central Coast Range, Oregon.. GSA Bulletin 107, 867–876.Google Scholar
Wright, H.E. Jr., Mann, D.H., Glaser, P.H., (1983). Piston cores from peat and lake sediments.. Ecology 65, 657–659.Google Scholar
Zdanowicz, C.M., Zielinski, G.A., Germani, M.S., (1999). Mount Mazama eruption: calendrical age verified and atmospheric impact assessed.. Geology 27, 621–624.Google Scholar
Zobel, D.B., Antos, J.A., (1997). A decade of recovery of understory vegetation buried by volcanic tephra from Mount St.. Helens. Ecological Monographs 67, 317–344.Google Scholar