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Please use this identifier to cite or link to this item: http://hdl.handle.net/1993/4098

Title: Holocene paleohydrology from Lake of the Woods and Shoal Lake cores using ostracodes, thecamoebians and sediment properties
Authors: Mellors, Trevor
Supervisor: Teller, James (Geological Sciences)
Examining Committee: Last, William (Geological Sciences) Buhay, William (University of Winnipeg)
Graduation Date: October 2010
Keywords: Ostracodes
Thecamoebians
Isostatic Rebound
Climate Instabily
Lake of the Woods
Shoal Lake
Holocene
Hypsithermal
Laurentide Ice Sheet
Lake Agassiz
Marquette Readvance
Charcoal
Paleohydrology
Sediments
Issue Date: 7-Sep-2010
Abstract: Ten sediment cores (2.0-8.5 m long) from various locations in Lake of the Woods (LOTWs) and Shoal Lake (SL) were recovered in August 2006, using a Kullenberg piston corer. From the study of the macrofossils (primarily ostracodes and thecamoebians) and the sediments in six processed cores, variations in paleoconditions were observed both spatially and temporally, and the timing of these changes were identified in over 10,000 years of postglacial history. Ostracodes disappeared from the LOTWs record from about 9000 to 7600 calendar years before present (BP) (about 5800 in SL), after LOTWs became isolated from glacial Lake Agassiz. Thecamoebians appeared in many cores around 2000 calendar years BP, with the earliest appearance at 9200. Buried paleosols in three cores indicate portions of the lake dried on several occasions during the Hypsithermal, perhaps indicating the region’s future climate response. One core contained a pink clay bed indicative of the Marquette readvance about 11,300 years (BP), and the subsequent input of water from the Superior basin.
URI: http://hdl.handle.net/1993/4098
Appears in Collection(s):FGS - Electronic Theses & Dissertations (Public)

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