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Late Quaternary History of Tundra Vegetation in Northwestern Alaska

Published online by Cambridge University Press:  20 January 2017

Patricia M. Anderson
Affiliation:
Quaternary Research Center, AK-60, University of Washington, Seattle, Washington 98195
Patrick J. Bartlein
Affiliation:
Department of Geography, University of Oregon, Eugene, Oregon 97403
Linda B. Brubaker
Affiliation:
College of Forest Resources, AR-10, University of Washington, Seattle, Washington 98195

Abstract

Pollen analysis of a new core from Joe Lake indicates that the late Quaternary vegetation of northwestern Alaska was characterized by four tundra and two forest-tundra types. These vegetation types were differentiated by combining quantitative comparisons of fossil and modern pollen assemblages with traditional, qualitative approaches for inferring past vegetation, such as the use of indicator species. Although imprecisely dated, the core probably spans at least the past 40,000 yr. A graminoid-Salix tundra dominated during the later and early portions of the glacial record. The middle glacial interval and the transition from glacial to interglacial conditions are characterized by a graminoid-Betula-Salix tundra. A Populus forest-Betula shrub tundra existed during the middle potion of this transition, being replaced in the early Holocene by a Betula-Alnus shrub tundra. The modern Picea forest-shrub tundra was established by the middle Holocene. These results suggest that the composition of modem tundra communities in northwestern Alaska developed relatively recently and that throughout much of the late Quaternary, tundra communities were unlike the predominant types found today in northern North America. Although descriptions of vegetation variations within the tundra will always be restricted by the innate taxonomic limitations of their herb-dominated pollen spectra, the application of multiple interpretive approaches improves the ability to reconstruct the historical development of this vegetation type.

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Articles
Copyright
University of Washington

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References

Abelson, P. H. (1989). The arctic: A key to world climate. Science 243, 873.Google Scholar
Anderson, P. M. (1988). Late Quaternary pollen records from the Kobuk and Noatak River drainages, northwestern Alaska. Quaternary Research 29, 263276.CrossRefGoogle Scholar
Anderson, P. M., and Brubaker, L. B. (1986). Modem pollen assemblages from northern Alaska. Review of Palaeobotany and Palynology 46, 273291.CrossRefGoogle Scholar
Anderson, P. M., and Brubaker, L. B. (1993). Vegetation history of northcentral Alaska: A mapped summary of late-Quatemary pollen data. Quaternary Science Reviews 12, in press.Google Scholar
Anderson, P. M. Bartlein, P. J. Brubaker, L. B. Gajewski, K., and Ritchie, J. C. (1989). Modem analogues of late-Quaternary pollen spectra from the western interior of North America. Journal of Biogeography 16, 573596.CrossRefGoogle Scholar
Anderson, P. M. Bartlein, P. J. Brubaker, L. B. Gajewski, K., and Ritchie, J. C. (1991). Vegetation-pollen-climate relationships for the arcto-boreal region of North America and Greenland. Journal of Biogeography 18, 565582.CrossRefGoogle Scholar
Andrews, J. T., and Brubaker, L. B. (1991). Paleoclimate of arctic lakes and estuaries: A new NSF initiative. £05 72(32), 331.Google Scholar
Barnosky, C. W. Anderson, P. M., and Bartlein, P. J. (1987). The northwestern U.S. during deglaciation: Vegetational history and paleoclimatic implications. In “North America and Adjacent Oceans during the Last Deglaciation” (Ruddiman, W. and Wright, H. Jr., Eds.), pp. 289321. Geological Society of America, Boulder.Google Scholar
Bartlein, P. J. Anderson, P. M. Edwards, M. E., and McDowell, P. F. (1991). A framework for interpreting paleoclimatic variations in eastern Beringia. Quaternary International 10-12, 7383.Google Scholar
Birks, H. J. B., and Birks, H. H. (1980). “Quaternary Palaeoecology.” Edward Arnold, London.Google Scholar
Brubaker, L. B. Garfinkel, H. L., and Edwards, M. E. (1983). A late Wisconsin and Holocene vegetation history from the central Brooks Range: Implications for Alaskan paleoecology. Quaternary Research 20, 194214.CrossRefGoogle Scholar
Bryson, R. A. (1966). Airmasses, streamlines and the boreal forest. Geographical Bulletin 8, 228269.Google Scholar
Colinvaux, P. A. (1964). The environment of the Bering Land Bridge. Ecological Monographs 34, 297329.Google Scholar
Committee on Global Change (1988). “Toward an Understanding of Global Change: Initial Priorities for U.S. Contributions to the International Geosphere-Biosphere Program.” National Academy Press, Washington, DC.Google Scholar
Cwynar, L. C. (1982). A late-Quaternary vegetation history from Hanging Lake, northern Yukon. Ecological Monographs 52, 124.Google Scholar
Cwynar, L. C., and Spear, R. W. (1991). Reversion of forest to tundra in the central Yukon. Ecology 12, 202212.CrossRefGoogle Scholar
Cwynar, L. C. Burden, E., and McAndrews, J. (1979). An inexpensive sieving method for concentrating pollen and spores from fine-grained sediments. Canadian Journal of Earth Science 16, 11151120.Google Scholar
Davis, M. B. (1989). Lags in vegetation response to greenhouse warming. Climatic Change 15, 7582.Google Scholar
Guiot, J. Harrison, S. P., and Prentice, I. C. (1993). Reconstruction of Holocene precipitation patterns in Europe using pollen and lake-level data. Quaternary Research 40, 139149.CrossRefGoogle Scholar
Guthrie, R. D. (1990). “Frozen Fauna of the Mammoth Steppe: The Story of Blue Babe.” Univ. of Chicago Press, Chicago.Google Scholar
Hamilton, T. (1986). Late Cenozoic glaciation of the central Brooks Range. In “Glaciation in Alaska: The Geologic Record” (Hamilton, T. Reed, K., and Thorson, R., Eds.), pp. 950. Alaska Geological Society, Anchorage.Google Scholar
Hare, F. K., and Ritchie, J. C. (1972). The boreal bioclimates. Geographical Review 62, 333365.CrossRefGoogle Scholar
Hopkins, D. M. (1982). Aspects of the paleogeography of Beringia during the late Pleistocene. In “Paleoecology of Beringia” (Hopkins, D. Matthews, J. Jr. Schweger, C., and Young, S., Eds.), pp. 328. Academic Press, New York.Google Scholar
Hopkins, D. M. Matthews, J. V. Jr. Schweger, C. E., and Young, S. B. (Eds.) (1982). “Paleoecology of Beringia.” Academic Press, New York.Google Scholar
Lamb, H. F., and Edwards, M. E. (1988). The arctic. In “Vegetation History” (Huntley, B. and Webb, T. III, Eds.), pp. 519555. Kluwer, Dordrecht.Google Scholar
Larsen, J. A. (1965). The vegetation of the Ennadai Lake area, N.W.T.. Studies in subarctic and arctic bioclimatology. Ecological Monographs 35, 3759.Google Scholar
MacDonald, G. M. Edwards, T. W. D. Moser, K. A. Pienitz, R., and Smol, J. P. (1993). Rapid response of treeline vegetation and lakes to past climate warming. Nature 361, 243246.Google Scholar
Murray, D. F. (1978). Vegetation, floristics, and phytogeography of northern Alaska. In “Vegetation and Production Ecology of an Alaskan Arctic Tundra (Ecological Studies)” (Tieszan, L. L., Ed.), pp. 1936. Springer, New York.Google Scholar
Overpeck, J. T. Bartlein, P. J., and Webb, T. III (1991). Potential magnitude of future vegetation change in eastern North America: comparisons with the past. Science 254, 692695.Google Scholar
Overpeck, J. T. Prentice, I. C., and Webb, T. III (1985). Quantitative interpretation of fossil pollen spectra: Dissimilarity coefficients and the method of modem analogs. Quaternary Research 23, 87108.Google Scholar
Overpeck, J. T. Webb, R. S., and Webb, T. III (1992). Mapping eastern North America vegetation change of the past 18 ka: No-analogs and the future. Geology 20, 10711074.Google Scholar
Patton, W. Jr. Miller, T., and Tailleur, I. (1968). Regional geologic map of the Shungnak and southern part of the Ambler River quandrangles, Alaska. “Miscellaneous Geologic Investigations Map 1-554.” U.S. Geological Survey, Washington, DC.Google Scholar
Porter, S. Pierce, K., and Hamilton, T. (1983). Late Wisconsin mountain glaciation in the western United States. In “Late Quaternary Environments of the United States, Volume 1, The Late Pleistocene” (Porter, S. C., Ed.), pp. 71111. Univ. of Minnesota Press, Minneapolis.Google Scholar
Post, W. M. (Ed.) (1989). “Report of a Workshop on Climate Feedbacks and the Role of Peatlands, TLindra, and the Boreal Ecosystems in the Global Carbon Cycle.” ORNL Environmental Sciences Division Publication 9999.Google Scholar
Ritchie, J. C., and Cwynar, L. C. (1982). The late Quaternary vegetation of the north Yukon. In “Paleoecology of Beringia” (Hopkins, D. Matthews, J. Jr. Schweger, C., and Young, S., Eds.), pp. 113126. Academic Press, New York.CrossRefGoogle Scholar
Ritchie, J. C. Cwynar, L. C., and Spear, R. W. (1983). Evidence from north-west Canada for an early Holocene Milankovitch thermal maximum. Nature 305, 126128.Google Scholar
Shaver, G. Billings, W. Chapin, F. III Giblin, A. Nadelhoffer, K. Oechel, W., and Rastetter, E. B. (1992). Global change and carbon balance of arctic ecosystems. Bioscience 42, 433441.CrossRefGoogle Scholar
Viereck, L. Dymess, C. Batten, A., and Wenzlick, K. (1992). “The Alaska Vegetation Classification.” U.S. Forest Service General Technical Report PNW-GTR-286. Washington, DC.Google Scholar
Wright, H. E. Jr. Mann, D. H., and Glaser, P. H. (1984). Piston corers for peat and lake sediments. Ecology 65, 657659.CrossRefGoogle Scholar
Young, S. B. (1971). The vascular flora of St. Lawrence Island with special reference to floristic zonation in the arctic regions. Contributions from the Gray Herbarium 201, 11115.Google Scholar