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Interstadial Conifer Wood from Northern Maine

Published online by Cambridge University Press:  20 January 2017

R. Scott Anderson ,
Ronald B. Davis ,
Robert Stuckenrath  and
Harold W. Borns Jr.
R. Scott Anderson
Affiliation:
Quaternary Studies Program, Department of Geology, and Bilby Research Center, Northern Arizona University, Flagstaff, Arizona 86011
Ronald B. Davis
Affiliation:
Department of Botany and Plant Pathology, and Institute for Quaternary Studies, University of Maine, Orono, Maine 04469
Robert Stuckenrath
Affiliation:
Institute for Quaternary Studies, University of Maine, Orono, Maine 04469, and Radiocarbon Dating Laboratory, University of Pittsburgh, Applied Research Center, 365 William Pitt Way, Pittsburgh, Pennsylvania 15238
Harold W. Borns Jr.
Affiliation:
Department of Geological Sciences and Institute for Quaternary Studies, University of Maine, Orono, Maine 04469
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Abstract

Conifer wood, probably spruce (Picea sp.), of middle Wisconsinan age (29,200 ± 500 yr B.P.) was recovered from late-glacial lake sediments from Upper South Branch Pond, Maine. If the wood was derived from a local source, deglaciation of part of northern New England is suggested for this time. The occurrence also has implications for understanding the problem associated with radiocarbon dating of bulk lake sediment containing small amounts of organic matter.

Type
Short Paper
Information
Quaternary Research , Volume 30 , Issue 1 , July 1988 , pp. 98 - 101
Copyright
University of Washington

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References

Anderson, R.S., Davis, R.B., Miller, N.G., Stuckenrath, R., (1986). History of late- and postglacial vegetation and disturbance around Upper South Branch Pond, northern Maine. Canadian Journal of Botany. 64, 1977-1986.Google Scholar
Anderson, R.S., Homola, R.L., Davis, R.B., Jacobson, G.L. Jr., (1984). Fossil remains of the mycorrhizal fungal Glomus fasciculatum complex in postglacial lake sediments from Maine. Canadian Journal of Botany. 62, 2325-2328.CrossRefGoogle Scholar
örck, and Håkansson, , Björck, S., Håkansson, S., 1982. Radiocarbon dates from late Weichselian lake sediments in southern Sweden as a basis for chronostratigraphic subdivision. Boreas. 11, 141-150.Google Scholar
Borns, H.W. Jr., Calkin, P.E., (1977). Quaternary glaciation, west-central Maine. Geological Society of America Bulletin. 88, 177301784.Google Scholar
Borns, H.W. Jr., LaSalle, P., Thompson, W.B., (1985). Late Pleistocene History of Northeastern New England and Adjacent Quebec. Geological Society of America, Special Paper 197.Google Scholar
Caldwell, D.W., (1959). Glacial Lake and Glacial Marine Clay in the Farmington Area, Maine. Maine Geological Survey, Special Geological Studies, Series 3.Google Scholar
Caldwell, D.W., The surficial geology of the River Valley from Farmington to Norridgewock, Maine. Griscom, A., Milton, D., (1960). New England Intercollegiate Geological Conference Guidebook, 52nd Annual Meeting. 19-24.Google Scholar
Davis, R.B., Jacobson, G.L. Jr., (1985). Late glacial and early Holocene landscapes in northern New England and adjacent areas of Canada. Quaternary Research. 23, 341-368.Google Scholar
de Vernal, A., Causse, C., Hillaire-Marcel, C., Mott, R.J., Occhietti, S., (1986). Palynostratigraphy and Th U ages of upper Pleistocene interglacial and interstadial deposits on Cape Breton Island, Eastern Canada. Geology. 14, 554-557.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. 24th International Geological Congress Report. 5-15, Sect. 12.Google Scholar
Dreimanis, A., Terasmae, J., McKenzie, G.D., (1966). The Port Talbot interstade of the Wisconsin glaciation. Canadian Journal of Earth Sciences. 3, 305-325.CrossRefGoogle Scholar
Genes, A.N., Newman, W.A., Brewer, T.B., (1981). Late Wisconsinan glaciation models of northern Maine and adjacent Canada. Quaternary Research. 16, 48-65.Google Scholar
Grant, D.R., (1971). Glacial Deposits, Sea Level Changes and Pre-Wisconsin Deposits in Southwest Nova Scotia. 110-113, Geblogical Survey of Canada, Paper 71-1B.Google Scholar
Grant, D.R., King, L.H., A stratigraphic framework for the Quaternary history of the Atlantic Provinces, Canada. Fulton, R.J., (1984). Quaternary Stratigraphy of Canada: A Canadian Contribution to IGCP Project 24. Geological Survey of Canada, Paper 84-10. 173-191.Google Scholar
Gratton, D., Dubois, J.-M., Painchaud, A., Gwyn, H., (1986). L'ile d'Anticosti; a-t-elle ete recemment englacee?. Geos (Ottawa). 15, 21-23.Google Scholar
Lasalle, P., Quaternary Stratigraphy of Quebec. Fulton, R.J., (1984). Quaternary Stratigraphy of Canada: A Canadian Contribution of IGCP Project 24. Geological Survey of Canada, Paper 84-10. 151-171.Google Scholar
Lowell, T.V., Becker, D.A., Calkin, P.E., (1986). Quaternary stratigraphy in northwestern Maine: A progress report. Geographie Physique et Quaternaire. 40, 71-84.Google Scholar
McDonald, B.C., Shilts, W.W., (1971). Quaternary stratigraphy and events in southeastern Quebec. Geological Society of America Bulletin. 82, 683-698.CrossRefGoogle Scholar
Mott, R.J., Grant, D.R., (1985). Pre-late Wisconsinan paleoenvironments in Atlantic Canada. Geographie Physique et Quaternaire. 39, 239-254.Google Scholar
Prescott, G.C. Jr., (1973). Groundwater Favorability and Surficial Geology of the Lower St. John River Valley, Maine. U.S. Geological Survey, Atlas HA-485.Google Scholar
Prest, V.K., (1977). General stratgraphic framework of the Quanternary in eastern Canada. Geographie Physique et Quaternaire. 3, 7-14.Google Scholar
Sirkin, L., Stuckenrath, R., (1980). The Portwashingtonian warm interval in the northern Atlantic coastal plain. Geological Society of America Bulletin. 91, 332-336.Google Scholar