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- W1980509362 abstract "A number of peat deposits, mainly associated with raised beaches, were studied in the Sugluk region of northern Ungava. The peats were exposed in sections cut by river erosion and usually showed a succession of marine sands, peats and windblown sand. Samples were taken for the analysis of pollen and macroscopic remains. The conclusions may be summarized as follows: (1) Pollen analysis suggests that, during the period represented by the deposits, the area has been covered by treeless tundra. (2) The alteration of dated peats and sands can be interpreted in relation to the climatic scheme worked out by Nichols (1967) for Keewatin. There was: (a) a warm period represented by peaty deposits dated about 4,000 years and 2,800 years B.P.; (b) a cold period from about 1,600–2,800 years B.P., with deposition of windblown sand at one site; (c) a warm and moist period from 1,600 to 670 years BP. characterised by a considerable development of peat; (d) a second cold period characterised by the cessation of peat growth and the development of sand tunes. (3) The development of living Sphagnum appears to have followed the amelioration of climate in this century." @default.
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- W1980509362 date "1969-09-01" @default.
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- W1980509362 title "A palaeobotanical investigation of postglacial deposits in the sugluk area of northern Ungava (Quebec, Canada)" @default.
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- W1980509362 doi "https://doi.org/10.1016/0034-6667(69)90012-8" @default.
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