Articles | Volume 2, issue 2
SOIL, 2, 221–240, 2016

Special issue: Soil as a record of the past

SOIL, 2, 221–240, 2016
Original research article
07 Jun 2016
Original research article | 07 Jun 2016

Arctic soil development on a series of marine terraces on central Spitsbergen, Svalbard: a combined geochronology, fieldwork and modelling approach

W. Marijn van der Meij et al.

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Cited articles

Aitken, M. J.: An introduction to optical dating: the dating of Quaternary sediments by the use of photon-stimulated luminescence, Oxford University Press, Oxford, 280 pp., 1998.
Alexanderson, H., Ingólfsson, Ó., Murray, A. S., and Dudek, J.: An interglacial polar bear and an early Weichselian glaciation at Poolepynten, western Svalbard, Boreas, 42, 532–543, 2013.
Andò, S., Garzanti, E., Padoan, M., and Limonta, M.: Corrosion of heavy minerals during weathering and diagenesis: A catalog for optical analysis, Sediment. Geol., 280, 165–178, 2012.
André, M.-F.: Holocene climate fluctuations and geomorphic impact of extreme events in Svalbard, Geograf. Ann. A, 77, 241–250, 1995.
Arctic Climate Impact Assessment: Impacts of a Warming Arctic – Arctic Climate Impact Assessment, Cambridge University Press, Cambridge, UK, 139 pp., 2004.
Short summary
This study combined fieldwork, geochronology and modelling to get a better understanding of Arctic soil development on a landscape scale. Main processes are aeolian deposition, physical and chemical weathering and silt translocation. Discrepancies between model results and field observations showed that soil and landscape development is not as straightforward as we hypothesized. Interactions between landscape processes and soil processes have resulted in a complex soil pattern in the landscape.