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Postglacial vegetation history of Orcas Island, northwestern Washington

Published online by Cambridge University Press:  20 January 2017

Estella B. Leopold ,
Peter W. Dunwiddie ,
Cathy Whitlock ,
Rudy Nickmann  and
William A. Watts
Estella B. Leopold
Affiliation:
Biology Department, University of Washington, Seattle, WA 98195, USA
Peter W. Dunwiddie*
Affiliation:
Biology Department, University of Washington, Seattle, WA 98195, USA
Cathy Whitlock
Affiliation:
Department of Earth Sciences and Montana Institute on Ecosystems, Montana State University, Bozeman, MT 59715, USA
Rudy Nickmann
Affiliation:
15 Somers Avenue, Bergenfield, NJ 07621, USA
William A. Watts
Affiliation:
School of Botany, Trinity College, Dublin, USA
*
⁎Corresponding author. E-mail address:[email protected] (P.W. Dunwiddie).
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Abstract

The revegetation of islands following retreat of Pleistocene glaciers is of great biogeographical interest. The San Juan Islands, Washington, feature regionally distinctive xerophytic plant communities, yet their vegetation history, as it relates to past climate and sea level, is poorly known. We describe a 13,700-year-old pollen record from Killebrew Lake Fen and compare the vegetation reconstruction with others from the region. The data suggest that the narrow channels surrounding Orcas Island were not a barrier to early postglacial immigration of plants. Between 13,700 and 12,000 cal yr BP, Pinus, Tsuga, Picea, Alnus viridis, and possibly Juniperus maritima were present in a mosaic that supported Bison antiquus and Megalonyx. The rise of Alnus rubra-type pollen and Pteridium spores at ca. 12,000 cal yr BP suggests a warming trend and probably more fires. Temperate conifer taxa, including Cupressaceae, Pseudotsuga, Tsuga heterophylla, and Abies, increased after 11,000 cal yr BP and especially in the last 7000 cal yr BP. After 6000 cal yr BP, Pseudotsuga and Cupressaceae dominated the vegetation. The last 1500 yr were the wettest period of the record. Due to its rain shadow location, Orcas Island experienced drier conditions than on the mainland during most of the postglacial period.

Keywords

Island biogeographyPostglacial pollenNorthern Puget LowlandBison antiquus habitatSan Juan Islands
Type
Original Articles
Information
Quaternary Research , Volume 85 , Issue 3 , May 2016 , pp. 380 - 390
Copyright
University of Washington

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Footnotes

1 Deceased.

References

Adams, R.P., Hunter, G., Fairhall, T.A.(2010). Discovery and SNPs analyses of populations of Juniperus maritima in the Olympic Peninsula, a Pleistocene refugium?. Phytologia 92, 68–81.Google Scholar
Allen, G.B. (1995). Vegetation and Climate History of Southeast Vancouver Island, British Columbia.M.S. thesisUniversity of Victoria, BC, Google Scholar
Allen, G.B., Brown, K.J., Hebda, R.J.(1999). Surface pollen spectra from southern Vancouver Island, British Columbia, Canada. Canadian Journal of Botany 77, 786–799.Google Scholar
Alley, N.F., Chatwin, S.C.(1979). Late Pleistocene history and geomorphology, Southwestern Vancouver Island, British-Columbia. Canadian Journal of Earth Sciences 16, 1645–1657.CrossRefGoogle Scholar
Barnosky, C.W. (1981). A record of late Quaternary vegetation from Davis Lake, southern Puget Lowland, Washington. Quaternary Research 16, 221–239.CrossRefGoogle Scholar
Barron, J.A., Heusser, L., Herbert, T., Lyle, M.(2003). High-resolution climatic evolution of coastal northern California during the past 16,000 years. Paleoceanography 18, 10.1029/2002PA000768Google Scholar
Bartlein, P.J., Anderson, P.M., Anderson, K.H., Edwards, M.E., Thompson, R.S., Webb, R.S., Webb III, T., Whitlock, C.(1998). Paleoclimate simulations for North America over the past 21,000 years: features of simulated climate and comparisons with paleoenvironmental data. Quaternary Science Reviews 17, 549–585.Google Scholar
Blaauw, M., Christen, J.A.(2011). Bacon Manual – v2.2.http://www.chrono.qub.ac.uk/blaauw/bacon.html(accessed 06.06.15.)Google Scholar
Brown, K.J., Hebda, R.J.(2002). Origin, development, and dynamics of coastal temperate conifer rainforests of southern Vancouver Island, Canada. Canadian Journal of Forest Research 32, 353–372.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.CrossRefGoogle Scholar
Buckingham, N.M., Schreiner, E.G., Kaye, T.N., Burger, J.E., Tisch, E.L.(1995). Flora of the Olympic Peninsula. Northwest Interpretative Association, Washington.Google Scholar
Burns, R.M., Honkala, B.H.(1990). Silvics of North America: 1. Conifers.U.S. Department of Agriculture, Forest ServiceAgricultural Handbook 654 Google Scholar
Craine, J.M., McLauchlan, K.K.(2004). The influence of biotic drivers on North American palaeorecords: alternatives to climate. The Holocene 14, 787–791.CrossRefGoogle Scholar
Cwynar, L.C. (1987). Fire and the forest history of the North Cascade range. Ecology 68, 791–802.CrossRefGoogle Scholar
Egan, J., Staff, R., Blackford, J.(2015). A revised age estimate of the Holocene Plinian eruption of Mount Mazama, Oregon using Bayesian statistical modeling. The Holocene 25, 1054–1067.10.1177/0959683615576230Google Scholar
Engstrom, D.R., Hansen, B.C.S., Wright Jr., H.E.(1990). A possible Younger Dryas record in Southeastern Alaska. Science 250, 1383–1385.Google Scholar
Faegri, K., Krzwinksi, K., Iversen, J., Kaland, P.E.(1992). Textbook of Pollen Analysis. fourth ed. The Blackburn Press, Caldwell, NJ.Google Scholar
Franklin, J.F., Dyrness, C.T.(1973). Natural Vegetation of Oregon and Washington.U.S. Department of Agriculture, Forest Service General Technical Report PNW-GTR-008Google Scholar
Gavin, D.G., Brubaker, L.B.(2015). Late Pleistocene and Holocene environmental change on the Olympic Peninsula, Washington. Ecological Studies 222, Springer, New York. 142 ppGoogle Scholar
Gavin, D.G., Brubaker, L.B., Greenwald, D.N.(2013). Postglacial climate and fire-mediated vegetation change on the Western Olympic Peninsula, Washington. Ecological Monographs 83, 471–489.Google Scholar
Gavin, D.G., McLachlan, J.S., Brubaker, L.B., Young, K.A.(2001). Postglacial history of subalpine forests, Olympic Peninsula, Washington, USA. The Holocene 11, 177–188.Google Scholar
Grigg, L.D., Whitlock, C.(1998). Late-glacial climate and vegetation changes in western Oregon. Quaternary Research 49, 287–298.CrossRefGoogle Scholar
Grimm, E.C. (1987). CONISS: a FORTRAN 77 program for stratigraphically constrained cluster analysis by the method of incremental sum of squares. Computers and Geosciences 13, 13–35.CrossRefGoogle Scholar
Gustafson, C.E., Gilbow, D.W., Daugherty, R.D.(1979). The Manis mastodon site: early man on the Olympic Peninsula. Canadian Journal of Archaeology 3, 157–164.Google Scholar
Hansen, H. (1943). A pollen study of two bogs on Orcas Island of the San Juan Islands, Washington. Bulletin of the Torrey Botanical Club 70, 236–243.Google Scholar
Hansen, B.S., Easterbrook, D.J.(1974). Stratigraphy and palynology of late Quaternary sediments in the Puget Lowland, Washington. Geological Society of America Bulletin 85, 587–602.Google Scholar
Hebda, R.J., Mathewes, R.W.(1984). Holocene history of cedar and native Indian cultures of the North American Pacific coast. Science 225, 711–713.Google Scholar
Heusser, C.J. (1974). Quaternary vegetation, climate, and glaciation of the Hoh River Valley, Washington. Geological Society of America Bulletin 85, 1547–1560.Google Scholar
Heusser, C.J., Heusser, L.E., Peteet, D.M.(1999). Humptulips revisited: a revised interpretation of Quaternary vegetation and climate of western Washington, USA. Palaeogeography, Palaeoclimatology, Palaeoecology 150, 191–221.Google Scholar
Hicock, S.R., Hebda, R.J., Armstrong, J.E.(1982). Lag of the Fraser glacial maximum in the Pacific Northwest; pollen and macrofossil evidence from western Fraser Lowland, British Columbia. Canadian Journal of Earth Sciences 19, 2288–2296.CrossRefGoogle Scholar
Higuera, P.E., Sprugel, D.G., Brubaker, L.B.(2005). Reconstructing fire regimes with charcoal from small-hollow sediments: a calibration with tree-ring records and fire. The Holocene 15, 238–251.Google Scholar
Hutchinson, I., James, T.S., Reimer, P.J., Bornhold, B.D., Clague, J.J.(2004). Marine and limnic radiocarbon reservoir corrections for studies of late- and postglacial environments in Georgia Basin and Puget Lowland, British Columbia, Canada and Washington, USA. Quaternary Research 61, 193–203.Google Scholar
James, T., Gowan, E.J., Hutchinson, I., Clague, J.J., Barrie, J.V., Conway, K.W.(2009). Sea-level change and paleogeographic reconstructions, southern Vancouver Island, British Columbia, Canada. Quaternary Science Reviews 28, 1200–1216.Google Scholar
Johnson, C.N. (2009). Ecological consequences of Late Quaternary extinctions of megafauna. Proceedings of the Royal Society, B (Biological Sciences) 276, 2509–2519.Google Scholar
Kenady, S.M., Wilson, M.C., Schalk, R.F., Mierendorf, R.R.(2011). Late Pleistocene butchered Bison antiquus from Ayer Pond, Orcas Island, Pacific Northwest: age confirmation and taphonomy. Quaternary International 233, 130–141.Google Scholar
Lacourse, T., Delepine, J.M., Hoffman, E.H., Mathewes, R.W.(2012). A 14,000 year vegetation history of a hypermaritime island on the outer Pacific coast of Canada based on fossil pollen, spores and conifer stomata. Quaternary Research 78, 572–582.Google Scholar
Leopold, E.B., Birkebak, J., Reinink-Smith, L., Jayachandar, A.P., Narváez, P., Zaborac-Reed, S.J.(2012). Pollen morphology of the three subgenera of Alnus . Palynology 36, 131–151.Google Scholar
Leopold, E.B., Boyd, R.(1999). An ecological history of old prairie areas in southwestern Washington.Boyd, R. Indians, Fire, and the Land. Oregon State University Press, Corvallis.139–163.Google Scholar
Leopold, E.B., Nickman, R.J., Hedges, J.L., Ertel, J.R.(1982). Pollen and lignin records of Late Quaternary vegetation, Lake Washington. Science 218, 1305–1307.Google Scholar
Lucas, J.D., Lacourse, T.(2013). Holocene vegetation history and fire regimes of Pseudotsuga menziesii forests in the Gulf Islands National Park Reserve, southwestern British Columbia, Canada. Quaternary Research 79, 366–376.CrossRefGoogle Scholar
Mathewes, R.W. (1973). A palynological study of postglacial vegetation changes in the University Research Forest, southwestern British Columbia. Canadian Journal of Botany 51, 2085–2103.CrossRefGoogle 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
Mathewes, R.W., Heusser, L.E.(1981). A 12,000- year palynological record of temperature and precipitation trends in southwestern British Columbia. Canadian Journal of Botany 59, 707–710.CrossRefGoogle Scholar
McLachlan, J., Brubaker, L.B.(1995). Local and regional vegetation change on the northeastern Olympic Peninsula during the Holocene. Canadian Journal of Botany 73, 1618–1627.Google Scholar
Mosher, D.C., Hewitt, A.T.(2004). Late Quaternary deglaciation and sea-level history of eastern Juan de Fuca Strait, Cascadia. Quaternary International 121, 23–29.Google Scholar
Muscheler, R., Kromer, B., Björck, S., Svensson, A., Friedrich, M., Kaiser, K.F., Southon, J.(2008). Tree rings and ice cores reveal 14C calibration uncertainties during the Younger Dryas. Nature Geoscience 1, 263–267.Google Scholar
Palmer, S., Walker, I.R., Heinrichs, M., Hebda, R., Scudder, G.(2002). Postglacial midge community change and Holocene palaeotemperature reconstructions near treeline, southern British Columbia (Canada). Journal of Paleolimnology 28, 469–490.Google Scholar
Pellatt, M.G., Hebda, R.J., Mathewes, R.W.(2001). High-resolution Holocene vegetation history and climate from Hole 1034B. ODP LEG 169S, Saanich Inlet, Canada. Marine Geology 174, 211–226.Google Scholar
Pellatt, M.G., Mathewes, R.W., Clague, J.J.(2002). Implications of a late-glacial pollen record for the glacial and climatic history of the Fraser Lowland, British Columbia. Palaeogeography, Palaeoclimatology, Palaeoecology 180, 147–157.CrossRefGoogle Scholar
Petersen, K.L., Mehringer, P.J., Gustafson, C.E.(1983). Late-glacial vegetation and climate at the Manis Mastodon site, Olympic Peninsula, Washington. Quaternary Research 20, 215–231.CrossRefGoogle Scholar
Reimer, P.J., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Bronk Ramsey, C., Buck, C.E., Burr, G.S., Cheng, H., Edwards, R.L., Friedrich, M., Grootes, P.M., Guilderson, P.I., Haflidason, H., Hajdas, I., Hatte, C., Heaton, T.J., Hoffman, D.L., Hogg, A.G., Hughen, K.A., Kaiser, K.F., Kromer, B., Manning, S.W., Niu, M., Reimer, R.W., Richards, D.A., Scott, E.M., Southon, J.R., Staff, R.A., Turney, C.S.M., van der Plicht, J.(2013). IntCal13 and Marine13 radiocarbon age calibration curves, 0-50,000 years cal BP. Radiocarbon 55, 1869–1887.Google Scholar
Sugimura, W.V., Sprugel, D.G., Brubaker, L.B., Higuera, P.E.(2008). Millennial-scale changes in local vegetation and fire regimes on Mount Constitution, Orcas Island, Washington, USA, using small hollow sediments. Canadian Journal of Forest Research 38, 539–552.Google Scholar
Thorson, R.M. (1980). Ice-sheet glaciation of the Puget Lowland, Washington, during the Vashon Stade (Late Pleistocene). Quaternary Research 13, 303–321.Google Scholar
Turner, N.J. (1995). Food Plants of Coastal First Peoples. Royal British Columbia Museum Handbook. University of British Columbia Press, Vancouver, BC.Google Scholar
(2014). University of Washington Herbarium, Burke Museum.(2014).Washington State County & Regional Species Lists. (http://biology.burke.washington.edu/herbarium/resources/specieslists.php, 15 October 2014).Google Scholar
(2014). USDA, NRCS.(2014).The PLANTS Database (http://plants.usda.gov, 15 October 2014). National Plant Data Team, Greensboro, NC 27401–4901 USA.Google Scholar
Vacco, D.A., Clark, P.U., Mix, A.C., Cheng, H., Edwards, R.L.(2005). A speleothem record of Younger Dryas cooling, Klamath mountains, Oregon, USA. Quaternary Research 64, 249–256.Google Scholar
Waggoner, V., Hinkes, M.(1986). Summer and fall browse utilization by an Alaskan bison herd. Journal of Wildlife Management 50, 322–324.CrossRefGoogle Scholar
Walsh, M.K., Marlon, J.R., Goring, S.J., Brown, K.J., Gavin, D.G.(2015). A regional perspective on Holocene fire–climate–human interactions in the Pacific Northwest of North America. Annals of the Association of American Geographers 105, 6 1135–1157.10.1080/00045608.2015.1064457CrossRefGoogle Scholar
Waters, M.R., Stafford, T.W., McDonald, H.G.(2011). Pre-Clovis mastodon hunting 13,800 years ago at the Manis Site, Washington. Science 334, 351–353.Google Scholar
Weiser, A., Lepofsky, D.(2009). Ancient land use and management of Ebey's Prairie, Whidbey Island, Washington. Journal of Ethnobiology 29, 184–212.Google Scholar
Wilson, M.C., Kenady, S.M., Schalk, R.F.(2009). Late Pleistocene Bison antiquus from Orcas Island, Washington, and the biogeographic importance of an early postglacial land mammal dispersal corridor from the mainland to Vancouver Island. Quatarnary Research 71, 49–61.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