Cited by 76

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Accelerator-Mass-Spectrometer Ages for the Younger Dryas Event in Atlantic Canada

Mayle, Francis E., Levesque, André J., Cwynar, Les C.·1993·Quaternary Research

Abstract

In Atlantic Canada, bulk-sediment dates for the onset of a late-glacial cooling, widely regarded as the Younger Dryas event, are highly variable, ranging from 14,300 ± 270 to 10,800 ± 100 yr B.P. We present the first accelerator-mass-spectrometer (AMS) 14 C dates from Atlantic Canada, at or close to the boundaries of this event, from six sites in New Brunswick and Nova Scotia. The mean of five dates places the onset of this cooling at ca. 10,770 yr B.P.; the inclusion of a sixth, perhaps anomalously old date, changes the mean to 10,880 yr B.P. The termination averages (three dates) ca. 10,000 yr B.P. These dates place the timing of the Younger Dryas event in Atlantic Canada closer in line with the traditional chronozone boundaries of 11,000 and 10,000 yr B.P. in Northwest Europe.

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Crossref · 10.1006/qres.1993.1042

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  • The Younger Dryas has been convincingly documented from terrestrial sites near the Atlantic Coast of northern North America.

    “Only recently has the Younger Dryas been convincingly documented from terrestrial sites near the Atlantic Coast of northern North America (Mott et al., 1986;Peteet et al., 1990;Mayle et al., 1993).”

    From Late-Quaternary history of the alpine flora of the New Hampshire White Mountains (2002) · cites this paper as Mayle et al., 1993

Citations

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No references could be resolved yet.

Research works printed but not linked: 24

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Metadata

Authors
Mayle, F. E., Levesque, A. J., & Cwynar, L. C.
Venue
Quaternary Research
Published
1993-05
Volume
39
Issue
3
Pages
355-360
ISSN
  • 0033-5894
  • 1096-0287
Cited by
76
References
0
Language
en

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