Evidence from Nipawin Bay in Frobisher Lake, Saskatchewan, for three highstand and three lowstand lake phases between 9 and 10 (10.1 and 11.5 cal) ka BP

Author:

Anderson T.W.

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference50 articles.

1. Evidence for ice margin retreat and proglacial lake (Agassiz?) drainage by about 11 ka, Clearwater River spillway area, Saskatchewan;Anderson;Current Research, Part B, Geological Survey of Canada, Paper 92–1B,1992

2. Beckman Coulter, 2010. http://www.beckmancoulter.com/coultercounter/homepage_tech_laserdiff.jsp.

3. Early Holocene drowned lagoonal deposits from the Kattegat, southern Scandinavia;Bennike;Boreas,2000

4. Plant macrofossils in Quaternary lake sediments;Birks,1980

5. The Lake Superior varve stratigraphy and implications for eastern Lake Agassiz outflow from 10,700 to 8900 cal ybp (9.5-8.0 14C ka);Breckenridge;Palaeogeography, Palaeoclimatology, Palaeoecology,2007

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