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Swanger KM, Lamp JL, Winckler G, et al. Glacier advance during Marine Isotope Stage 11 in the McMurdo Dry Valleys of Antarctica. Sci Rep. 2017;7:41433doi: 10.1038/srep41433.
Swanger, K. M., Lamp, J. L., Winckler, G., Schaefer, J. M., & Marchant, D. R. (2017). Glacier advance during Marine Isotope Stage 11 in the McMurdo Dry Valleys of Antarctica. Scientific reports, 741433. https://doi.org/10.1038/srep41433
Swanger, Kate M, et al. "Glacier advance during Marine Isotope Stage 11 in the McMurdo Dry Valleys of Antarctica." Scientific reports vol. 7 (2017): 41433. doi: https://doi.org/10.1038/srep41433
Swanger KM, Lamp JL, Winckler G, Schaefer JM, Marchant DR. Glacier advance during Marine Isotope Stage 11 in the McMurdo Dry Valleys of Antarctica. Sci Rep. 2017 Jan 31;7:41433. doi: 10.1038/srep41433. PMID: 28139676; PMCID: PMC5282522.
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Sci Rep. 2017 Jan 31;7:41433. doi: 10.1038/srep41433.

Glacier advance during Marine Isotope Stage 11 in the McMurdo Dry Valleys of Antarctica.

Scientific reports

Kate M Swanger, Jennifer L Lamp, Gisela Winckler, Joerg M Schaefer, David R Marchant

Affiliations

  1. Department of Environmental, Earth and Atmospheric Sciences, University of Massachusetts, 1 University Avenue, Lowell, MA 01854, USA.
  2. Lamont-Doherty Earth Observatory, The Earth Institute at Columbia University, Route 9W, Palisades, NY 10964, USA.
  3. Department of Earth and Environment, Boston University, 685 Commonwealth Avenue, Boston, MA 02215, USA.

PMID: 28139676 PMCID: PMC5282522 DOI: 10.1038/srep41433

Abstract

We mapped six distinct glacial moraines alongside Stocking Glacier in the McMurdo Dry Valleys, Antarctica. Stocking Glacier is one of several alpine glaciers in the Dry Valleys fringed by multiple cold-based drop moraines. To determine the age of the outermost moraine, we collected 10 boulders of Ferrar Dolerite along the crest of the moraine and analyzed mineral separates of pyroxene for cosmogenic

Conflict of interest statement

The authors declare no competing financial interests.

References

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