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Synchronous climatic change inferred from diatom records in four western Montana lakes in the U.S. Rocky Mountains

Published online by Cambridge University Press:  20 January 2017

Brandi Bracht-Flyr  and
Sherilyn C. Fritz
Brandi Bracht-Flyr
Affiliation:
Department of Earth and Atmospheric Sciences, University of Nebraska-Lincoln, Lincoln, NE, 68588–0340, USA
Sherilyn C. Fritz*
Affiliation:
Department of Earth and Atmospheric Sciences, University of Nebraska-Lincoln, Lincoln, NE, 68588–0340, USA School of Biological Sciences, University of Nebraska-Lincoln, Lincoln, NE, 68588–0340, USA
*
*Corresponding author at: Department of Earth and Atmospheric Sciences, University of Nebraska-Lincoln, Lincoln, NE, 68588–0340, USA. E-mail address:brachtflyr@huskers.unl.edu (B. Bracht-Flyr), sfritz2@unl.edu (S.C. Fritz).
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Abstract

Late-Holocene environmental and climatic conditions were reconstructed from diatom assemblages in sediment cores from four western Montana lakes: Crevice Lake, Foy Lake, Morrison Lake, and Reservoir Lake. The lakes show synchroneity in timing of shifts in diatom community structure, but the nature of these changes differs among the lakes. Two of the sites provide highly resolved records of hydrologic balance, while the other two stratigraphic sequences primarily record temperature impact on lake thermal structure. All four lakes show significant change in five discrete intervals: 2200–2100, 1700–1600, 1350–1200, 800–600, and 250 cal yr BP. The similarities in the timing of change suggest overlying regional climatic influences on lake dynamics. The 800–600 cal yr BP shift is evident in other paleorecords throughout the Great Plains and western US, associated with the transition from the Medieval Climate Anomaly to the Little Ice Age. Large-scale climatic mechanisms that influence these lake environments may result from atmospheric circulation patterns that are driven by interactions between Pacific and Atlantic sea-surface temperatures, which are then locally modified by topography.

Keywords

DiatomLake-levelPaleoclimateHolocenewestern North AmericaLittle Ice AgeMedieval Climate Anomaly
Type
Original Articles
Information
Quaternary Research , Volume 77 , Issue 3 , May 2012 , pp. 456 - 467
Copyright
University of Washington

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