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Quaternary Palynology of the Pacific Slope of Washington

Published online by Cambridge University Press:  20 January 2017

Calvin J. Heusser
Calvin J. Heusser*
Affiliation:
Department of Biology, New York University, Box 608, Tuxedo, New York 10987 USA
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Abstract

Quaternary deposits on the Pacific slope of Washington range in age from the earliest known interglaciation, the Alderton, through the Holocene. Pollen stratigraphy of these deposits is represented by 12 major pollen zones and is ostensibly continuous through Zone 8 over more than 47,000 radiocarbon yr. Before this, the stratigraphy is discontinuous and the chronology less certain. Environments over the time span of the deposits are reconstructed by the comparison of fossil and modern pollen assemblages and the use of relevant meteorological data. The Alderton Interglaciation is characterized by forests of Douglas fir (Pseudotsuga menziesii), alder (Alnus), and fir (Abies). During the next younger interglaciation, the Puyallup, forests were mostly of pine, apparently lodgepole (Pinus contorta), except midway in the interval when fir, western hemlock (Tsuga heterophylla), and Douglas fir temporarily replaced much of the pine. Vegetation outside the limits of Salmon Springs ice (>47,00034,000 yr BP) varied chiefly between park tundra and forests of western hemlock, spruce (Picea), and pine. The Salmon Springs nonglacial interval at the type locality records early park tundra followed by forests of pine and of fir. During the Olympia Interglaciation (34,000–28,000 yr BP), pine invaded the Puget Lowland, whereas western hemlock and spruce became manifest on the Olympic Peninsula. Park tundra was widespread during the Fraser Glaciation (28,000–10,000 yr BP) with pine becoming more important from about 15,000 to 10,000 yr BP. Holocene vegetation consisted first of open communities of Douglas fir and alder; later, closed forests succeeded, formed principally of western hemlock on the Olympic Peninsula and of western hemlock and Douglas fir in the Puget Lowland. Over the length of the reconstructed environmental record, climate shifted between cool and humid or relatively warm, semihumid forest types and cold, relatively dry tundra or park tundra types. During times of glaciation, average July temperatures are estimated to have been at least 7°C lower than today. Only during the Alderton Interglaciation and during the Holocene were temperatures higher for protracted periods than at present.

Type
Research Article
Information
Quaternary Research , Volume 8 , Issue 3 , November 1977 , pp. 282 - 306
Copyright
University of Washington

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References

Adam, D.P., Sims, J., (1976). A long, continuous pollen record from Clear Lake, California. Geological Society of America. 8, 349 (Abstracts with Programs).Google Scholar
Armstrong, J.E., Crandell, D.R., Easterbrook, D.J., Noble, J.B., (1965). Late-Pleistocene stratigraphy and chronology in southwestern British Columbia and northwestern Washington. Geological Society of America Bulletin. 76, 321-330.Google Scholar
Bloom, A.L., Broecker, W.S., Chappell, J.M.A., Matthews, R.K., Mesolella, K.J., (1974). Quaternary sea level fluctuations on a tectonic coast: new 230Th/234U dates from the Huon Peninsula, New Guinea. Quaternary Research. 4, 185-205.Google Scholar
Bretz, J.H., (1913). Glaciation of the Puget Sound region. Washington Geological Survey Bulletin. 8, 244.Google Scholar
Broecker, W.S., Kulp, J.L., (1957). Lamont natural radiocarbon measurements IV. Science. 126, 1324-1334.CrossRefGoogle ScholarPubMed
Carson, R.J., Spence, W.H., Birdseye, R.U., (1976). Late Pleistocene tephra layers in the western Puget Lowland, Washington. Geological Society of America. 8, 358 (Abstracts with Programs).Google Scholar
Costin, A.B., (1968). Alpine ecosystems of the Australasian region. Wright, H.E. Jr., Osborn, W.H., Arctic and Alpine Environments. Indiana University Press, Bloomington, 55-87.Google Scholar
Crandell, D.R., (1963) Surficial Geology and Geomorphology of the Lake Tapps Quadrangle, Washington. U.S. Geological Survey Professional Paper 388-A.Google Scholar
Crandell, D.R., (1965). The glacial history of western Washington and Oregon. Wright, H.E. Jr., Frey, D.G., The Quaternary of the United States. Princeton University Press, Princeton, New Jersey, 341-353.Google Scholar
Crandell, D.R., (1974) Quaternary Stratigraphy and Extent of Glaciation in the Mount Rainier Region, Washington. U.S. Geological Survey Professional Paper 847.Google Scholar
Crandell, D.R., Mullineaux, D.R., Waldron, H.H., (1958). Pleistocene sequence in southeastern part of the Puget Lowland, Washington. American Journal of Science. 256, 384-397.Google Scholar
Davis, M.B., (1973). Pollen evidence of changing land use around the shores of Lake Washinton. Northwest Science. 47, 133-148.Google Scholar
Dreimanis, A., Karrow, P.F., (1972). Glacial history of the Great Lakes-St. Lawrence region, the classification of the Wisconsin(an) Stage, and its correlatives. International Geological Congress, 24th Session. 5-15 Section 12.Google Scholar
Easterbrook, D.J., (1969). Pleistocene chronology of the Puget Lowland and San Juan Islands, Washington. Geological Society of America Bulletin. 80, 2273-2286.Google Scholar
Easterbrook, D.J., (1973). Paleomagnetic events recorded in late Pleistocene sediments. Geological Society of America. 5, 478 (Abstracts with Programs).Google Scholar
Easterbrook, D.J., (1976). Stratigraphy and palynology of late Quaternary Sediments in the Puget Lowland, Washington: Discussion and reply. Geological Society of America Bulletin. 87, 155-156.Google Scholar
Easterbrook, D.J., Crandell, D.R., Leopold, E.B., (1967). Pre-Olympia Pleistocene stratigraphy and chronology in the central Puget Lowland, Washington. Geological Society of America Bulletin. 78, 13-20.CrossRefGoogle Scholar
Easterbrook, D.J., Othberg, K.L., (1973). Paleomagnetism of late Pleistocene sediments, Puget Lowland, Washington. Geological Society of America. 5, 36 (Abstracts with Programs).Google Scholar
Emiliani, C., (1961). Cenozoic climatic changes as indicated by the stratigraphy and chronology of deep-sea cores of Globigerina facies. Annals of the New York Academy of Science. 95, 521-536.Google Scholar
Flint, R.F., (1971) Glacial and Quaternary Geology. Wiley, New York. Google Scholar
Florer, L.E., (1972). Quaternary paleoecology and stratigraphy of the sea cliffs, western Olympic Peninsula, Washington. Quaternary Research. 2, 202-216.Google Scholar
Florer, L.E., (1973). Pollen analysis of marine sediments off the Washington coast. Marine Geology. 14, 73-78.Google Scholar
Florer-Heusser, L.E., (1975). Late-Cenozoic marine palynology of Northeast Pacific Ocean cores. Suggate, R.P., Cresswell, M.M., Quaternary Studies. The Royal Society of New Zealand, Wellington, 133-138.Google Scholar
Franklin, J.F., Dyrness, C.T., (1973). Natural vegetation of Oregon and Washington. J.S. Department of Agriculture Forest Service General Technical Report PNW-8. .Google Scholar
Fulton, R.J., (1968). Olympia Interglaciation, Purcell Trench, British Columbia. Geological Society of America Bulletin. 79, 1075-1080.Google Scholar
Fulton, R.J., (1971) Radiocarbon Chronology of Southern British Columbia. Canada Geological Survey Paper 71-37.CrossRefGoogle Scholar
Fulton, R.J., Armstrong, J.E., Fyles, J.G., (1976). Stratigraphy and palynology of late Quaternary sediments in the Puget Lowland, Washington: Discussion and reply. Geological Society of America Bulletin. 87, 153-155.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
Hansen, H.P., 1938a. Pollen analysis of some interglacial peat from Washington. University of Wyoming Publications. 5, 11-18.Google Scholar
Hansen, H.P., 1938b. Postglacial forest succession and climate in the Puget Sound region. Ecology. 19, 528-542.Google Scholar
Hansen, H.P., (1947). Postglacial forest succession, climate, and chronology in the Pacific Northwest. American Philosophical Society Transactions. 37.CrossRefGoogle Scholar
Hansen, H.P., (1974). Pollen analysis of a deep section from Lake Washington, Seattle. Birbal Sahni Institute of Palaeobotany Special Publication. 5, 1-4.Google Scholar
Hansen, H.P., Mackin, J.H., (1940). A further study of interglacial peat from Washington. Torrey Botanical Club Bulletin. 67, 131-142.Google Scholar
Hansen, H.P., Mackin, J.H., (1949). A pre-Wisconsin forest succession in the Puget Lowland, Washington. American Journal of Science. 247, 833-855.Google Scholar
Heusser, C.J., (1960) Late Pleistocene Environments of North Pacific North America. American Geographical Society Special Publication 35.Google Scholar
Heusser, C.J., (1964). Palynology of four bog sections from the western Olympic Peninsula, Washington. Ecology. 45, 23-40.Google Scholar
Heusser, C.J., (1965). A Pleistocene phytogeographical sketch of the Pacific Northwest and Alaska. Wright, H.E. Jr., Frey, D.G., The Quaternary of the United States. Princeton University Press, Princeton, New Jersey, 469-483.Google Scholar
Heusser, C.J., (1969). Modern pollen spectra from the Olympic Peninsula, Washington. Torrey Botanical Club Bulletin. 96, 407-417.Google Scholar
Heusser, C.J., (1972). Palynology and phytogeographical significance of a late-Pleistocene refugium near Kalaloch, Washington. Quaternary Research. 2, 189-201.Google Scholar
Heusser, C.J., 1973a. Environmental sequence following the Fraser advance of the Juan de Fuca lobe, Washington. Quaternary Research. 3, 284-306.CrossRefGoogle Scholar
Heusser, C.J., 1973b. Age and environment of allochthonous peat clasts from the Bogachiel River Valley, Washington. Geological Society of America Bulletin. 84, 797-804.Google Scholar
Heusser, C.J., 1973c. Modern pollen spectra from Mount Rainier, Washington. Northwest Science. 47, 1-8.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., Florer, L.E., (1973). Correlation of marine and continental Quaternary pollen records from the Northeast Pacific and western Washington. Quaternary Research. 3, 661-670.Google Scholar
Heusser, L.E., Balsam, W.L., (1977). Pollen distribution in the Northeast Pacific Ocean. Quaternary Research. 6, 45-62.Google Scholar
Heusser, L.E., Shackleton, N.J., Moore, T.C., Balsam, W.L., (1975). Land and marine records in the Pacific Northwest during the last glacial interval. Geological Society of America. 7, 1113-1114 (Abstracts with Programs).Google Scholar
Hitchcock, C.L., Cronquist, A., (1973) Flora of the Pacific Northwest. University of Washington Press, Seattle. Google Scholar
LaChapelle, E.R., (1960) The Blue Glacier Project 1959 and 1960. 54 Office of Naval Research Contract 477(18)(NR307-244) Final Report.Google Scholar
Leeden, F.van der, Troise, F.L., (1974) Climates of the States. Water Information Center, Inc.,, Port Washington, New York, Volume II-Western States.Google Scholar
Leopold, E.B., Crandell, D.R., (1957). Pre-Wisconsin interglacial pollen spectra from Washington State, USA. Geobotanisches Institut Rübel in Zürich Veröffentlichung. 34, 76-79.Google Scholar
Marcus, M.G., (1965). Summer temperature relationships along a transect in the St. Elias Mountains, Alaska and Yukon Territory. Man and Earth, Series in Earth Sciences, University of Colorado Studies. 3, 15-30.Google Scholar
Marcus, M.G., Ragle, R.H., (1970). Snow accumulation in the Icefield Ranges, St. Elias Mountains, Yukon. Arctic and Alpine Research. 2, 277-292.Google Scholar
Noble, J.B., Wallace, E.F., (1966). Geology and ground-water resources of Thurston County, Washington. Division of Water Resources Water Supply Bulletin. 10, Volume 2.Google Scholar
Phillips, E.L., (1965). Climate of Washington. Climatography of the United States No. 6045. U.S. Department of Commerce Weather Bureau, 1-27.Google Scholar
Plafker, G., Miller, D.J., (1958). Glacial features and surficial deposits of the Malaspina district, Alaska. U.S. Geological Survey Miscellaneous Geologic Investigations Map I-271. .Google Scholar
Porter, S.C., (1976). Pleistocene glaciation in the southern part of the North Cascade Range, Washington. Geological Society of America Bulletin. 87, 61-75.Google Scholar
Porter, S.C., Stuiver, M., Wang, I.C., (1977). Chronology of Hawaiian glaciations. Science. 195, 61-63.Google Scholar
Randle, K., Goles, G.G., Kittleman, L.R., (1971). Geochemical and petrological characterization of ash samples from Cascade Range volcanoes. Quaternary Research. 1, 261-282.Google Scholar
Schmidt, R.L., (1957). The silvics and plant geography of the genus Abies in the coastal forests of British Columbia. Department of Lands and Forests British Columbia Forest Service Technical Bulletin T. 46. .Google Scholar
Shackleton, N.J., Opdyke, N., (1973). Oxygen isotope and palaeomagnetic stratigraphy of equatorial Pacific core V28238: Oxygen isotope temperatures and ice volumes on a 105-year and 106-year scale. Quaternary Research. 3, 39-55.Google Scholar
Steinen, R.P., Harrison, R.S., Matthews, R.K., (1973). Eustatic low stand of sea level between 125,000 and 105,000 B. P.: Evidence from the subsurface of Barbados, West Indies. Geological Society of America Bulletin. 84, 63-70.Google Scholar
1960. U.S. Department of Commerce Weather Bureau. Climatological data. Annual Summary 1959. 63, 220-230 Washington.Google Scholar
1961. U.S. Department of Commerce Weather Bureau. Climatological data. Annual Summary 1960. 64, 224-234 Washington.Google Scholar
1962. U.S. Department of Commerce Weather Bureau. Climatological data. . Annual Summary 1961. 65, 228-238 Washington.Google Scholar
1963. U.S. Department of Commerce Weather Bureau. Climatological data. . Annual Summary 1962. 66, 226-236 Washington.Google Scholar
1964. U.S. Department of Commerce Weather Bureau. Climatological data. . Annual Summary 1963. 67, 210-222 Washington.Google Scholar
1965. U.S. Department of Commerce Weather Bureau. Climatological data. Annual Summary 1964. 68, 232-244 Washington.Google Scholar
1966. U.S. Department of Commerce Environmental Science Services Administration. Climatological data. Annual Summary 1965. 69, 228-240 Washington.Google Scholar
1967. U.S. Department of Commerce Environmental Science Services Administration. Climatological data. Annual Summary 1966. 70, 209-221 Washington.Google Scholar
1968. U.S. Department of Commerce Environmental Science Services Administration. Climatological data. Annual Summary 1967. 71, 207-219 Washington.Google Scholar
1969. U.S. Department of Commerce Environmental Science Services Administration. Climatological data. Annual Summary 1968. 72, 217-227 Washington.Google Scholar
1970. U.S. Department of Commerce Environmental Science Services Administration. Climatological data. Annual Summary 1969. 73, 219-231 Washington.Google Scholar
1971. U.S. Department of Commerce National Oceanic and Atmospheric Administration, Climatological data. Annual Summary 1970. 74, 223-236 Washington.Google Scholar
Wolfe, J.A., (1969). Neogene floristic and vegetational history of the Pacific Northwest. Madroño. 20, 83-110.Google Scholar
Wright, H.E. Jr., (1972). Interglacial and postglacial climates: The pollen record. Quaternary Research. 2, 274-282.Google Scholar