Variations in the oxygen-isotope composition of ancient Lake Superior between 10,600 and 8,800 cal BP
Author:
Publisher
Springer Science and Business Media LLC
Subject
Earth-Surface Processes,Aquatic Science
Link
http://link.springer.com/content/pdf/10.1007/s10933-011-9552-7.pdf
Reference49 articles.
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2. Boyd M, Teller JT, Yang Z, Kingsmill L, Shultis C (2010) An 8, 900-year-old forest drowned by Lake Superior: hydrological and paleoecological implications. J Paleolimnol. doi: 10.1007/s10933–010-9461–1
3. Breckenridge A (2007) 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). Palaeogeogr Palaeoclimatol Palaeoecol 246:45–61
4. Breckenridge A, Johnson TC (2009) Paleohydrology of the upper Laurentian Great Lakes from the late glacial to early Holocene. Quat Res 71:397–408
5. Breckenridge A, Johnson TC, Beske-Diehl S, Mothersill JS (2004) The timing of regional late glacial events and postglacial sedimentation rates from Lake Superior. Quat Sci Rev 23:2355–2367
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