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Three soil chronosequences in recessional glacial deposits near the polar plateau, in the Central Transantarctic Mountains, Antarctica

Published online by Cambridge University Press:  26 March 2014

Joshua W. Scarrow ,
Megan R. Balks  and
Peter C. Almond
Joshua W. Scarrow*
Affiliation:
Earth and Ocean Sciences, University of Waikato, Hamilton 3240, New Zealand
Megan R. Balks
Affiliation:
Earth and Ocean Sciences, University of Waikato, Hamilton 3240, New Zealand
Peter C. Almond
Affiliation:
Faculty of Agriculture and Life Sciences, Lincoln University, Lincoln 7647, New Zealand
*
[email protected]
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Abstract

Soil chronosequences in till deposits emplaced during glacial retreat in the Central Transantarctic Mountains are described. Discrepancies between the degree of soil development and reported cosmogenic surface exposure ages suggest slower, weaker soil development in this region than encountered in other areas of Antarctica. The study sites (Dominion Range, Mount Achernar and Ong Valley) were located between 83° and 85°S, at altitudes of 1600–2200 m, on the edge of the polar plateau. Soil landscape maps show a gradation of soil properties across landscape units that were designated as homogenous/single-event drifts in previous smaller-scale studies. Along transects away from the current ice edge, the depth to underlying ice thickened (from 2 cm to > 80 cm), soil became more weathered, saltier and less alkaline, and horizonation became more pronounced. Soil thickness, clast abundance and soil chemistry are all consistent with a two-layer mode of soil formation. We suggest that a thin, clast-rich surface horizon, originating from weathering of supraglacial debris, overlies a thick, clast-poor sublimation till. The supraglacial debris has a finite contribution to soil volume, whereas sublimation offers an ongoing source of soil material that thickens the soil from its base.

Keywords

Beardmorecold desertCryosolGelisolsublimationultraxerous
Type
Earth Sciences
Information
Antarctic Science , Volume 26 , Supplement 5 , October 2014 , pp. 573 - 583
Copyright
© Antarctic Science Ltd 2014 

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References

Aislabie, J., Bockheim, J., McLeod, M., Hunter, D., Stevenson, B. & Barker, G.M. 2012. Microbial biomass and community structure changes along a soil development chronosequence near Lake Wellman, southern Victoria Land. Antarctic Science, 24, 154–164.CrossRefGoogle Scholar
Almond, P.C. & Tonkin, P.J. 1999. Pedogenesis by upbuilding in an extreme leaching and weathering environment, and slow loess accretion, south Westland, New Zealand. Geoderma, 92, 1–36.CrossRefGoogle Scholar
Barrett, P.J., Lindsay, J.F. & Gunner, J. 1970. Reconnaissance geologic map of the Mount Rabot quadrangle, Transantarctic Mountains, Antarctica. Washington, DC: United States Geological Survey.Google Scholar
Barrett, P.J. & Elliot, D.H. 1973. Reconnaissance geologic map of the Buckley Island quadrangle, Transantarctic Mountains, Antarctica. Washington, DC: United States Geological Survey.Google Scholar
Bockheim, J.G. 1990. Soil development rates in the Transantarctic Mountains. Geoderma, 47, 59–77.Google Scholar
Bockheim, J.G. 1997. Properties and classification of cold desert soils from Antarctica. Soil Science Society of America Journal, 61, 224–231.Google Scholar
Bockheim, J.G. 2008. Functional diversity of soils along environmental gradients in the Ross Sea region, Antarctica. Geoderma, 144, 32–42.CrossRefGoogle Scholar
Bockheim, J.G. 2010. Evolution of desert pavements and the vesicular layer in soils of the Transantarctic Mountains. Geomorphology, 118, 433–443.Google Scholar
Campbell, I.B. & Claridge, G.G.C. 1975. Morphology and age relationships of Antarctic soils. Royal Society of New Zealand Bulletin, 13, 83–88.Google Scholar
Campbell, I.B. & Claridge, G.G.C. 1987. Antarctica: soils, weathering processes and environment. Amsterdam: Elsevier, 406 pp.Google Scholar
Claridge, G.G.C. & Campbell, I.B. 1968. Soils of the Shackleton Glacier region, Queen Maud Range, Antarctica. New Zealand Journal of Science, 11, 171–218.Google Scholar
Denton, G.H., Bockheim, J.G., Wilson, S.C. & Leide, J.E. 1989a. Late quaternary ice-surface fluctuations of Beardmore Glacier, Transantarctic Mountains. Quaternary Research, 31, 183–209.Google Scholar
Denton, G.H., Bockheim, J.G., Wilson, S.C. & Stuiver, M. 1989b. Late Wisconsin and early Holocene glacial history, inner Ross Embayment, Antarctica. Quaternary Research, 31, 151–182.CrossRefGoogle Scholar
Elliot, D.H., Barrett, P.J. & Mayewski, P.A. 1974. Reconnaissance geologic map of the Plunket Point quadrangle, Transantarctic Mountains, Antarctica. Washington, DC: United States Geological Survey.Google Scholar
Heimsath, A.M., Dietrich, W.E., Nishiizumi, K. & Finkel, R.C. 1997. The soil production function and landscape equilibrium. Nature, 388, 358–361.Google Scholar
Hofstee, E.H., Balks, M.R., Petchey, F. & Campbell, D.I. 2006. Soils of Seabee Hook, Cape Hallet, northern Victoria Land, Antarctica. Antarctic Science, 18, 473–486.Google Scholar
Howard-Williams, C., Peterson, D., Lyons, W.B., Cattaneo-Vietti, R. & Gordon, S. 2006. Measuring ecosystem response in a rapidly changing environment: the Latitudinal Gradient Project. Antarctic Science, 18, 465–471.Google Scholar
Humphreys, G.S. & Wilkinson, M.T. 2007. The soil production function: a brief history and its recovery. Geoderma, 139, 73–78.Google Scholar
McLeod, M., Bockheim, J., Balks, M. & Aislabie, J. 2009. Soils of western Wright Valley, Antarctica. Antarctic Science, 21, 355–365.CrossRefGoogle Scholar
Ng, F., Hallet, B., Sletten, R.S. & Stone, J.O. 2005. Fast-growing till over ancient ice in Beacon Valley, Antarctica. Geology, 33, 121–124.Google Scholar
Scarrow, J.W. 2013. Soil chronosequences and bacterial communities of the Central Transantarctic Mountains, Antarctica. MSc thesis. University of Waikato, 201 pp. [Unpublished].Google Scholar
Schoeneberger, P.J., Wysocki, D.A., Benham, E.C. & Broderson, W.D., eds. 2002. Field book for describing and sampling soils. Version 3.0. Lincoln, NE: Natural Resources Conservation Service, National Soil Survey Center.Google Scholar
Soil Survey Staff. 2010. Keys to soil taxonomy, 11th ed. Washington, DC: USDA-NRCS.Google Scholar
Storey, B.C., Fink, D., Hood, D., Joy, K., Shulmeister, J., Riger-Kusk, M. & Stevens, M.I. 2010. Cosmogenic nuclide exposure age constraints on the glacial history of the Lake Wellman area, Darwin Mountains, Antarctica. Antarctic Science, 22, 603–618.Google Scholar
Ugolini, F.C. & Bockheim, J.G. 2008. Antarctic soils and soil formation in a changing environment: a review. Geoderma, 144, 1–8.CrossRefGoogle Scholar
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