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Freshwater control of ice-rafted debris in the last glacial period at Mono Lake, California, USA

Published online by Cambridge University Press:  20 January 2017

Susan R. H. Zimmerman ,
Crystal Pearl ,
Sidney R. Hemming ,
Kathryn Tamulonis ,
N. Gary Hemming  and
Stephanie Y. Searle
Susan R. H. Zimmerman*
Affiliation:
Dept. of Earth and Environmental Sciences, Columbia University, New York, NY 10027, USA
Crystal Pearl
Affiliation:
School of Earth and Environmental Sciences, Queens College, City University of New York, Flushing, NY 11367, USA
Sidney R. Hemming
Affiliation:
Dept. of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory, Columbia University, Palisades, NY 10964, USA
Kathryn Tamulonis
Affiliation:
Dept. of Geology, Dickinson College, Carlisle, PA 17013, USA
N. Gary Hemming
Affiliation:
School of Earth and Environmental Sciences, Queens College, City University of New York, Flushing, NY 11367, USA
Stephanie Y. Searle
Affiliation:
Dept. of Earth and Environmental Sciences, Columbia University, New York, NY 10027, USA
*
⁎Corresponding author at: Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, CA 94550 and Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA. Fax: + 1 925 423 7884. E-mail address:[email protected] (S.R.H. Zimmerman).
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Abstract

The type section silts of the late Pleistocene Wilson Creek Formation at Mono Lake contain outsized clasts, dominantly well-rounded pebbles and cobbles of Sierran lithologies. Lithic grains > 425 μm show a similar pattern of variability as the > 10 mm clasts visible in the type section, with decreasing absolute abundance in southern and eastern outcrops. The largest concentrations of ice-rafted debris (IRD) occur at 67–57 ka and 46–32 ka, with strong millennial-scale variability, while little IRD is found during the last glacial maximum and deglaciation.

Stratigraphic evidence for high lake level during high IRD intervals, and a lack of geomorphic evidence for coincidence of lake and glaciers, strongly suggests that rafting was by shore ice rather than icebergs. Correspondence of carbonate flux and IRD implies that both were mainly controlled by freshwater input, rather than disparate non-climatic controls. Conversely, the lack of IRD during the last glacial maximum and deglacial highstands may relate to secondary controls such as perennial ice cover or sediment supply. High IRD at Mono Lake corresponds to low glacial flour flux in Owens Lake, both correlative to high warm-season insolation. High-resolution, extra-basinal correlation of the millennial peaks awaits greatly improved age models for both records.

Keywords

Mono LakeLate PleistoceneIRDLake levelPaleoclimateIce raftingGreat Basin
Type
Research Article
Information
Quaternary Research , Volume 76 , Issue 2 , September 2011 , pp. 264 - 271
Copyright
University of Washington. Published by Elsevier Inc.

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Footnotes

1 Now at: Schlumberger Carbon Services, Sugar Land TX 77478.
2 Now at: School of Biological Sciences, University of Canterbury, Christchurch, NZ 8140.

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