While early Holocene sites are rare in northeastern North America, and by implication early Holocene populations were relatively low, Middle Archaic sites (7000–9000 BP) are particularly abundant in the “Lakes” region of southwestern Maine and southeastern New Hampshire. Since sea level in this region (western Gulf of Maine) was as much as 50 m below present at that time, site abundance in the “Lakes” region may be explained by an unusual set of conditions which allowed populations of anadromous fish to develop earlier than elsewhere. Data from the Sebago Lake region of southwestern Maine suggest the development of a subsistence regime in Middle Archaic times based on intensive exploitation of anadromous fish, turtles, and aquatic mammals. In addition, it is likely that “landlocked” salmon populations became established at this time, resulting in a diverse, abundant, and stable resource base that supported sedentary encampments, particularly near outlets to important spawning grounds.
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References
1.
AtkinsC. G.1884Notes on Landlocked Salmon, Transactions of the American Fisheries Society, pp. 40–56.
2.
BloomA. L.1959The Geology of Sebago Lake State Park, Maine Geological Survey, Augusta.
3.
BloomA. L.1960Late Pleistocene Changes of Sea Level in Southwestern Maine, Maine Geological Survey, Augusta.
4.
BolianC. E.1980The Early and Middle Archaic of the Lakes Region, New Hampshire, in Early and Middle Archaic Cultures in the Northeast, StarbuckD. R. and BolianC. E. (eds.), Department of Anthropology, Franklin Pierce College, Rindge, New Hampshire, (Occasional Publications in Anthropology No. 7) pp. 115–134.
5.
CrossenK. J.1983Glaciomarine Deltas in Southwestern Maine: Deposition, Rebound, and Neotectonic Implications, M.S. Thesis, University of Maine, Orono.
6.
DeRocheS. E.1967The Presumpscot River: A Biological Survey Report, Department of Inland Fisheries and Game, Augusta, Maine.
7.
DeRocheS. E.1976The Sebago Lake Study, Maine Department of Inland Fisheries and Wildlife, Augusta, (Fisheries Research Bulletin No. 9).
8.
DincauzeD. F.1976The Neville Site: 8,000 Years at Amoskeag, Manchester, New Hampshire, Harvard University, Cambridge, Maine, (Peabody Museum Monographs No. 4).
9.
DincauzeD. F. and MulhollandM. T.1977Early and Middle Archaic Site Distributions and Habitats in Southern New England, in Amerinds and Their Paleoenvironments in Northeastern North America, NewmanW. S. and SalwenB. (eds.), New York Academy of Sciences, New York (Annals of the NY Academy of Sciences No. 288).
10.
DoyleF. H. and HansonR. E.1935Sketches of the History of Windham Maine, H. S. Cobb, Westbrook.
11.
DoyleR. A.HamiltonN. D.PetersenJ. B., and SangerD.1983Late Paleo-Indian Remains from Western Maine and their Correlations in Northeastern Prehistory, paper presented to the Society for American Archaeology, Pittsburgh.
12.
FittingJ. E.1968Environmental Potential and the Postglacial Readaptation in Eastern North America, American Antiquity, 33, pp. 441–445.
13.
FladmarkK. R.1983A Comparison of Sea-Levels and Prehistoric Cultural Developments on the East and West Coasts of Canada, in The Evolution of Maritime Cultures on the Northeast and Northwest Coasts of North America, NashR. J. (ed.) Department of Archaeology, Simon Fraser University, Burnaby, BC, (Publication No. 11).
14.
FobesC. S.1894The Story of the Presumpscot, Maine Historical Society, 2nd series, Vol. 5, pp. 361–385.
15.
HamiltonN. D. and YesnerD. R.1983Prehistoric Maritime Adaptations in Western Maine: The Great Diamond Island Site, paper presented to the Society for American Archaeology, Pittsburgh.
16.
HansonL. S.BreynaertR., and CaldwellD. W.1982Landlocked Salmon, A Relic of the Marine Submergence in Maine, Geological Society of American Abstracts with Programs14.
17.
HaveyK. A. and WarnerK.1970The Landlocked Salmon (Slamo Salar): Its Life History and Management in Maine, Maine Department of Inland Fisheries and Game, Augusta.
18.
HitchcockC. H.1874The Geology of Portland, Proceedings of the American Association for the Advancement of Science, 2, pp. 163–175.
19.
HylandF.ThompsonW. B., and StuckenrathR.Jr.1978Late Wisconsinan Wood and Other Tree Remains in the Presumpscot Formation, Portland, Maine, Maritime Sediments, 14, pp. 103–120.
20.
JacobsenG. L.TolonenM.AndersonR. S., and DavisR. B.1981Vegetational Development in Southern Maine During the Past 14,000 Years, Ecological Society of America Annual Meeting, Abstracts, Bloomington, Indiana, p. 127.
21.
JonesH. G.1949Sebago Lake Land, Bowker Press, Portland.
22.
McManamonF. P.1980Middle Archaic Chipped Stone Variation: Collections Research and Hypothesis Testing, in Early and Middle Archaic Cultures in the Northeast, StarbuckD. R. and BolianC. E. (eds.), Department of Anthropology, Franklin Pierce College, Rindge, New Hampshire, (Occasional Publications in Northeastern Anthropology No. 7), pp. 39–57.
23.
MorseE. S.1869Landslides in the Vicinity of Portland, Maine, Boston Society of Natural History, Boston.
24.
OldaleR. N.WommackL. E., and WhitneyA. B.1983Evidence for a Postglacial Low Relative Sea-Level Stand in the Drowned Delta of the Merrimack River, Western Gulf of Maine, Quaternary Research, 19, pp. 325–337.
25.
PowerG.1958The Evolution of Freshwater Races of the Atlantic Salmon (Salmo Salar), Arctic, 11, pp. 86–92.
26.
SangerD.1979Some Thoughts on the Scarcity of Archaeological Sites in Maine Between 10,000 and 5,000 Years Ago, in Discovering Maine's Archaeological Heritage, SangerD. (ed.), Maine Historic Preservation Commission, Augusta, pp. 23–34.
27.
SargentH. R.1980Archaeological Salvage at the Weirs, Laconia, New Hampshire, New Hampshire Water Supply and Pollution Control Commission, Concord.
28.
StuiverM. and BornsH. W.Jr.1975Late Quaternary Marine Invasion in Maine: Its Chronology and Associated Crustal Movement, Geological Society of America Bulletin, 86, pp. 99–104.
29.
U.S. ARMY CORPS OF ENGINEERS1975Flood Plain Information, Presumpscot River, U.S. Government Printing Office, Washington, D.C.
30.
UpsonJ. E. and SpencerC. W.1964Bedrock Valleys of the New England Coast as Related to Fluctuations of Sea Level, U. S. Government Printing Office, Washington, D.C., (U.S. Geological Survey Professional Paper No. 454-M).
31.
WhiteheadD. R.RochesterH.RissingS. W.DouglassC. B., and SheehanM. C.1973Late Glacial and Postglacial Productivity Changes in a New England Pond, Science, 181, pp. 744–746.
32.
WilderD. J.1947A Comparative Study of the Atlantic Salmon and the Lake Salmon, Canadian Journal of Research, 25, pp. 175–189.
33.
YesnerD. R.1980Archaeology of Casco Bay: A Preliminary Report, Maine Archaeological Society Bulletin, 20, pp. 60–74.
34.
YesnerD. R.1982Points, Pots, and People: Cultural Continuities Across the Archaic-Woodland Interface in Southwestern Maine, paper prepared in the Northeastern Anthropological Association, Syracuse.
35.
YesnerD. R.1983On Explaining Changes in Prehistoric Coastal Economies: The View from Casco Bay, in The Evolution of Maritime Cultures on the Northeast and Northwest Coasts of North America, NashR. J. (ed.), Department of Archaeology, Simon Fraser University, Burnaby, (Publication No. 11), pp. 79–90.
