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Paleolimnology and paleoclimate studies in Upper Klamath Lake, Oregon

December 31, 2004

The subsiding Upper Klamath Lake Basin contains sediments that were continuously deposited in a shallow, freshwater lake for more than 40 000 years. Well dated by radiometric methods and containing volcanic ashes of known age, these sediments constitute a valuable paleoclimate record. Sediment constituents and properties that reflect past climatic conditions in the area include pollen, diatoms, sediment geochemistry, and sediment magnetic properties. Many of these proxy measurements are also useful for comparing natural conditions in the lake to conditions following human settlement. Because of its location, the paleoclimate record from Upper Klamath Lake is valuable for comparisons to offshore marine records and as part of latitudinal transects of paleoclimate records along the west coast of the Americas.

Publication Year 2004
Title Paleolimnology and paleoclimate studies in Upper Klamath Lake, Oregon
DOI 10.1023/B:JOPL.0000019235.72107.92
Authors S.M. Colman, J. Platt Bradbury, Joseph G. Rosenbaum
Publication Type Article
Publication Subtype Journal Article
Series Title Journal of Paleolimnology
Index ID 70195412
Record Source USGS Publications Warehouse
USGS Organization Woods Hole Coastal and Marine Science Center