Hostname: page-component-586b7cd67f-rcrh6 Total loading time: 0 Render date: 2024-11-25T17:12:54.108Z Has data issue: false hasContentIssue false

Vegetation History of Pleasant Island, Southeastern Alaska, since 13,000 yr B.P.

Published online by Cambridge University Press:  20 January 2017

Barbara C. S. Hansen
Affiliation:
Limnological Research Center, University of Minnesota, 310 Pillsbury Dr. SE, Minneapolis, Minnesota, 55455
Daniel R. Engstrom
Affiliation:
Limnological Research Center, University of Minnesota, 310 Pillsbury Dr. SE, Minneapolis, Minnesota, 55455

Abstract

A 13,000-year history of late-Quaternary vegetational and climatic change has been derived from lacustrine sediments from Pleasant Island in the Glacier Bay region of southeastern Alaska. Early arrival of lodgepole pine and mountain hemlock, indicated by the presence of pollen and conifer stomata, suggests expansion from refugia in the Alexander Archipelago. A short-term climatic reversal, possibly correlated with the European Younger Dryas, is inferred from the expansion of tundra elements and deposition of inorganic sediments between 10,600 and 9900 14C yr B.P. Two peat cores from the lake catchment verify Holocene vegetation changes and aid in the separation of biogenic from climatic forces affecting vegetation history. Differences in pollen representation among the three cores illustrate the variation among pollen-collecting substrates, as well as the spatial heterogeneity of peatland development and its dependence on local hydrology. Initial peat accumulation and soil paludification, occasioned by increases in temperature and precipitation in the early Holocene, allowed western and mountain hemlock to replace sitka spruce 8500–8000 yr B. P. Open muskeg became widespread about 7000 yr B. P. and allowed lodgepole pine to reinvade the region after a 2000-yr absence. The extensive replacement of fen elements by bog taxa at 3400 yr B. P. suggests increased paludification due to changing hydrologic conditions; its correlation with the upland expansion of Tsuga heterophylla suggests the onset of a cooler/wetter Neoglacial climate in southeastern Alaska.

Type
Research Article
Copyright
University of Washington

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Ager, T. A. (1983). Holocene vegetational history of Alaska. In “Late-Quaternary Environments of the United States“ (Wright, H. E. Jr., Ed.), pp. 128141. University of Minnesota Press, Minneapolis.Google Scholar
Ammann, B., and Wick, L. (1993). Analysis of fossil stomata of conifers as indicators of the alpine tree line fluctuations during the Holocene. Paläoklimaforschung 9, 175185.Google Scholar
Bard, E., Arnold, M., Fairbanks, R. G., and Hamelin, B. (1993).230Th- 234U and 14C ages obtained by mass spectrometry on corals. Radiocarbon 35, 191199.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, The Geology of North America, v. K-3“ (Wright, H. E. Jr.,, and W. F. Ruddiman, Eds.), pp. 289321. Geological Society of America, Boulder.Google Scholar
Bigelow, N., Begét, J., and Powers, R. (1990). Latest Pleistocene increase in wind intensity recorded in eolian sediments from central Alaska. Quaternary Research 34, 160168.Google Scholar
Bormann, B. T., and Sidle, R. C. (1990). Changes in productivity and distribution of nutrients in a chronosequence at Glacier Bay National Park, Alaska. Journal of Ecology 78, 561578.Google Scholar
Clague, J. J., Mathewes, R. W., Buhay, W. M., and Edwards, T. W. D. (1992). Early Holocene climate at Castle Peak, southern Coast Mountains, British Columbia, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology 95, 153167.Google Scholar
COHMAP Members. (1988). Climatic changes of the last 18,000 years: observations and model simulations. Science 241, 10431052.Google Scholar
Cooper, W. S. (1923). The recent ecological history of Glacier Bay, Alaska: II. The present vegetation cycle. Ecology 4, 223246.Google Scholar
Cooper, W. S. (1931). A third expedition to Glacier Bay, Alaska. Ecology 12, 6195.CrossRefGoogle Scholar
Cooper, W. S. (1937). The problem of Glacier Bay, Alaska: a study of glacier variations. The Geographical Review 27, 3762.Google Scholar
Cooper, W. S. (1939). A fourth expedition to Glacier Bay, Alaska. Ecology 20, 130155.CrossRefGoogle Scholar
Cushing, E. J. (1963). Late-glacial pollen stratigraphy in east-central Minnesota. Unpublished Ph.D. thesis, University of Minnesota, Minneapolis. Google Scholar
Cwynar, L. C. (1987). Fire and forest history of the north Cascade Range. Ecology 68, 791802.Google Scholar
Cwynar, L. C. (1990). A late Quaternary vegetation history from Lily Lake, Chilkat Peninsula, southeast Alaska. Canadian Journal of Botany 68, 11061112.CrossRefGoogle Scholar
Cwynar, L. C., Burden, E., and McAndrews, J. H. (1979). An inexpensive sieving method for concentrating pollen and spores from fine-grained sediments. Canadian Journal of Earth Sciences 16, 11151120.Google Scholar
Engstrom, D. R., and Fritz, S. C. (1990). Early lake ontogeny following Neoglacial ice recession at Glacier Bay, Alaska. In “Proceedings of the Second Glacier Bay Science Symposium“ (Milner, A. M. and Wood, J. D. Jr., Eds.), pp. 127132. National Park Service, Anchorage, Alaska.Google Scholar
Engstrom, D. R., and Hansen, B. C. S. (1985). Postglacial vegetational change and soil development in southeastern Labrador as inferred from pollen and chemical stratigraphy. Canadian Journal of Botany 63, 543561.Google Scholar
Engstrom, D. R., Hansen, B. C. S., and Wright, H. E. Jr., (1990). A possible Younger Dryas record in southeastern Alaska. Science 250, 13831385.Google Scholar
Faegri, K., and Iversen, J. (1975). “Textbook of Pollen Analysis.“ Hafner Press, New York.Google Scholar
Fowells, H. A. (1965). “Silvics of Forest Trees of the United States.“ U.S. Department of Agriculture, Washington, DC.Google Scholar
Goodwin, R. G. (1988). Holocene glaciolacustrine sedimentation in Muir Inlet and ice advance in Glacier Bay, Alaska, U.S.A. Arctic and Alpine Research 20, 5569.Google Scholar
Hansen, B. C. S. (1995). Conifer stomate analysis as a paleoecological tool: an example from the Hudson Bay Lowlands. Canadian Journal of Botany 73, 244252.Google Scholar
Hansen, B. C. S., and Easterbrook, D. J. (1974). Stratigraphy and palynology of Late-Quaternary sediments in the Puget Lowland, Washington. Geological Society of America Bulletin 85, 587602.2.0.CO;2>CrossRefGoogle Scholar
Hebda, R. J. (1983). Late-glacial and postglacial vegetation history at Bear Cove Bog, northeast Vancouver Island, British Columbia. Canadian Journal of Botany 61, 31723192.Google Scholar
Hebda, R. J., and Allen, G. B. (1993). Modern pollen spectra from west central British Columbia. Canadian Journal of Botany. 71, 14861495.Google Scholar
Heusser, C. J. (1955). Pollen profiles from the Queen Charlotte Islands, British Columbia. Canadian Journal of Botany 33, 429449.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. (1983). Holocene vegetational history of the Prince William Sound region, south-central Alaska. Quaternary Research 19, 337355.Google Scholar
Heusser, C. J. (1985). Quaternary pollen records from the Pacific Northwest coast: Aleutians to the Oregon-California boundary. In “Pollen Records of Late-Quaternary North American Sediments“ (Bryant, V. M. Jr., and Holloway, R. G., Eds.), pp. 141166. American Association of Strati-graphic Palynologists Foundation, Dallas, Texas.Google Scholar
Heusser, C. J. (1989). North Pacific coastal refugia—the Queen Charlotte Islands in perspective. In “The Outer Shores, Proceedings of the Queen Charlotte Islands First International Symposium“ (Scudder, G. G. E. and Gessler, N., Eds.). University of British Columbia, Vancouver.Google Scholar
Heusser, C. J., Heusser, L. E., and Peteet, D. M. (1985). Late-Quaternary climatic change on the American North Pacific coast. Nature 315, 485487.Google Scholar
Janssen, C. R. (1984). Modern pollen assemblages and vegetation in the Myrtle Lake peatland, Minnesota. Ecological Monographs 54, 213252.Google Scholar
Kromer, B., and Becker, B. (1993). German Oak and Pine 14C calibration, 7200 BC–9400 BC. Radiocarbon 35, 125135.Google Scholar
Lawrence, D. B. (1958). Glaciers and vegetation in southeastern Alaska. American Scientist 46, 89122.Google Scholar
Linick, T.W., Long, A., Damon, P. E., and Ferguson, C. W. (1986). High-precision radiocarbon dating of bristlecone pine from 6554 to 5350 BC. Radiocarbon 28, 943953.Google Scholar
MacDonald, G. M. (1987). Postglacial development of the subalpine-boreal transition forest of western Canada. Journal of Ecology 75, 303320.Google Scholar
MacDonald, G. M., and Cwynar, L. C. (1985). A fossil pollen based reconstruction of the late Quaternary history of lodgepole pine (Pinus contorta ssp. latifolia) in the Western interior of Canada. Canadian Journal of Botany 15, 10391044.Google Scholar
Mann, D. H. (1983). The Quaternary history of the Lituya Glacial Refugium, Alaska. Unpublished Ph.D. thesis, University of Washington. Google Scholar
Mann, D. H. (1986). Wisconsin and Holocene glaciation of southeast Alaska. In “Glaciation in Alaska—The Geologic Record“ (Hamilton, T. D., Reed, K. M. and Thorson, R. M., Eds.), pp. 237265. Alaska Geological Society, Anchorage.Google Scholar
Mann, D. H., and Ugolini, F. C. (1985). Holocene glacial history of the Lituya District, southeast Alaska. Canadian Journal of Earth Sciences 22, 913928.Google Scholar
Mathewes, R. W. (1989). The Queen Charlotte Islands refugium: a paleo-ecological perspective. In “Quaternary Geology of Canada and Greenland, The Geology of North America, v. K-1“ (Fulton, R. J., Ed.), pp. 486490. Geological Society of America, Boulder, Colorado.Google Scholar
Mathewes, R. W., and Clague, J. J. (1982). Stratigraphic relationships and paleoecology of a late-glacial peat bed from the Queen Charlotte Islands, British Columbia. Canadian Journal of Earth Sciences 19, 11851195.Google Scholar
Mathewes, R. W., and Heusser, L. E. (1981). A 12000 year palynological record of temperature and precipitation trends in southwestern British Columbia. Canadian Journal of Botany 59, 707710.Google Scholar
Mathewes, R. W., Heusser, L. E., and Patterson, R. T. (1993). Evidence for a Younger Dryas like cooling event on the British-Columbia coast. Geology 21, 101104.Google Scholar
McKenzie, G. D., and Goldthwait, R. P. (1971). Glacial history of the last eleven thousand years in Adams inlet, southeastern Alaska. Geological Society of America Bulletin 82, 17671782.Google Scholar
Noble, M. G., Lawrence, D. B., and Streveler, G. P. (1984). Sphagnum invasion beneath an evergreen forest canopy in southeastern Alaska. The Bryologist 87, 119127.Google Scholar
Pearson, G. W., Becker, B., and Qua, F. (1993). High-precision 14C measurement of German and Irish oaks to show the natural 14C variations from 7890 to 5000 BC. Radiocarbon 35, 93–104.Google Scholar
Pearson, G. W., and Stuiver, M. (1993). High-precision bidecadal calibration of the radiocarbon time scale 500–2500 BC. Radiocarbon 35, 2533.Google Scholar
Peteet, D. M. (1986). Modern pollen rain and vegetational history of the Malaspina Glacier District, Alaska. Quaternary Research 25, 100120.Google Scholar
Peteet, D. M. (1991). Postglacial migration history of lodgepole pine near Yakutat, Alaska. Canadian Journal of Botany 69, 786796.Google Scholar
Peteet, D., Alley, R., Bond, G., Chappellaz, J., Clapperton, C., Del Genio, A., and Keigwin, L. (1993). Global Younger Dryas? EOS, Transactions American Geophysical Union 74, 587589.Google Scholar
Reiners, W. A., Worley, I. A., and Lawrence, D. B. (1971). Plant diversity in a chronosequence at Glacier Bay, Alaska. Ecology 52, 5569.Google Scholar
Riehle, J. R., Mann, D. H., Peteet, D. M., Engstrom, D. R., and Brew, D. A. (1992). The Mount Edgecumbe tephra deposits, a marker horizon in southeastern Alaska near the Pleistocene-Holocene boundary. Quaternary Research 37, 183202.Google Scholar
Ritchie, J. C. (1987). “Postglacial Vegetation of Canada.“ Cambridge University Press, Cambridge.Google Scholar
Stuiver, M., and Pearson, G. W. (1993). High-precision bidecadal calibration of the radiocarbon time scale, AD 1950–500 BC and 2500–6000 BC. Radiocarbon 35, 123.Google Scholar
Stuiver, M., and Reimer, P. J. (1993). Extended 14C database and revised CALIB radiocarbon calibration program. Radiocarbon 35, 215230.Google Scholar
Trautmann, W. (1953). Zur unterscheidung fossiler Spaltöffnungen der mit-teleuropäischen Coniferen. Flora 140, 523533.Google Scholar
Wainman, N., and Mathewes, R. W. (1987). Forest history of the last 12000 years based on plant macrofossil analysis of sediment from Marion Lake, southwestern British Columbia. Canadian Journal of Botany 65, 217921287.Google Scholar
Warner, B. G., Mathewes, R. W., and Clague, J. J. (1982). Ice-free conditions on the Queen Charlotte Islands, British Columbia, at the height of late Wisconsin glaciation. Science 218, 675677.Google Scholar
Wright, H. E. Jr., , Mann, D. H., and Glaser, P. H. (1984). Piston corers for peat and lake sediments. Ecology 65, 657659.Google Scholar