1981
DOI: 10.4095/109356
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Geological Survey of Canada radiocarbon dates XXI

Abstract: This list includes 105 radiocarbon age determinations on 104 geological samples made by the Radiocarbon Dating Laboratory. They are on samples from various are as follows: Labrador Shelf (2); Newfoundland (12); Nova Scotia (2); New Brunswick (1): Quebec (3); Ontario(1); Manitoba(1); Alberta (2); British Columbia (15); Yukon Territory (35); Northwest Territories, Mainland (10); Northwest Territories, Arctic Archipelago (21). Details of background and standard for the 2 L and 5 L counters during the period from … Show more

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Cited by 17 publications
(13 citation statements)
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“…The rate of retreat to this position is unknown because of the current lack of dates from the outer part of the inlet. However, a date of 9.3 ka BP (GSC-3183, Lowdon and Blake 1981) obtained on shells at Clarence Head, 120 km to the east on Smith Sound (Fig. 1), provides a similar, minimum age for marine limit in central Makinson Inlet.…”
Section: Deglaciation and Pattern Of Isochronesmentioning
confidence: 84%
“…The rate of retreat to this position is unknown because of the current lack of dates from the outer part of the inlet. However, a date of 9.3 ka BP (GSC-3183, Lowdon and Blake 1981) obtained on shells at Clarence Head, 120 km to the east on Smith Sound (Fig. 1), provides a similar, minimum age for marine limit in central Makinson Inlet.…”
Section: Deglaciation and Pattern Of Isochronesmentioning
confidence: 84%
“…There are indications that bog development and associated permafrost formation began earlier in the north and gradually spread southward. Within 1170±150 6510±150 5070±60 6160±90 2800±100 4250±100 6070±100 6280±80 1320±60 7590±80 6940±110 9820±220 2080±60 4750±60 2920±130 6770±140 8260±110 10100±130 1890±60 4810±60 3150±90 6020±100 2200±80 4030±100 2130±80 3850±400 920±80 3890±160 2300±100 Lowdon et ai, 1967Lowdon era/., 1967Tarnocai & Zoltai, 1988Tamocai & Zoltai, 1988Tarnocai & Zoltai, 1988Tarnocai & Zoltai, 1988 This paper This paper Blake, 1987Blake, 1987Dyck & Fyles, 1963Dyck & Fyles, 1963Blake, 1988Blake, 1988Lowdon & Blake, 1981Lowdon & Blake, 1981 This paper This paper Tarnocai & Zoltai, 1988Tarnocai & Zoltai, 1988Tarnocai & Zoltai, 1988Tarnocai & Zoltai, 1988Zoltai et al, 1992Zoltai et al, 1992 This paper This paper This paper This paper This paper This paper Alberta, bog development occurred earlier in the north (about 5 ka) than farther south in the present LPZ (about 2.2 ka, Zoltai and Vitt, 1990). …”
Section: Discussionmentioning
confidence: 99%
“…The McConnell glaciation is firmly dated to OIS 2 (Late Wisconsin). Radiocarbon ages from wood and fossils underlying McConnell till indicate that the McConnell glaciation began after 29,600±300 14 C yr BP (Matthews et al, 1990), but glaciers did not advance into major valleys before 26,350±280 14 C yr BP (Jackson and Harington, 1991), and a fully developed CIS did not exist until after 23,900±1140 14 C yr BP (Lowdon and Blake, 1981). Published radiocarbon ages indicate that the St. Elias lobe of the CIS was in retreat by 13,660±180 14 C yr BP (Rampton, 1971) and the Selwyn lobe by 12,590±120 14 C yr BP (Ward, 1989) (Fig.…”
Section: The Cordilleran Ice Sheetmentioning
confidence: 99%