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Solid Earth An interactive open-access journal of the European Geosciences Union
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Volume 5, issue 2
Solid Earth, 5, 901–914, 2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue: Soil processes in cold-climate environments

Solid Earth, 5, 901–914, 2014
© Author(s) 2014. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 01 Sep 2014

Research article | 01 Sep 2014

Sedimentological characteristics of ice-wedge polygon terrain in Adventdalen (Svalbard) – environmental and climatic implications for the late Holocene

M. Oliva1, G. Vieira1, P. Pina2, P. Pereira3, M. Neves3, and M. C. Freitas4 M. Oliva et al.
  • 1Institute of Geography and Spatial Planning – Centre for Geographical Studies, University of Lisbon, Lisbon, Portugal
  • 2CERENA/University of Lisbon, Lisbon, Portugal
  • 3Environmental Management Center, Mykolas Romeris University, Ateities St. Vilnius, Lithuania
  • 4Universidade de Lisboa, Faculdade de Ciências, Centro de Geologia, Lisbon, Portugal

Abstract. Ice wedges are widespread periglacial features in the landscape of Adventdalen, Svalbard. The networks of ice wedges have created areas with well-developed polygonal terrains in the lowest fluvial terraces in this valley. We have examined the sedimentological characteristics of the northern and southern banks of the Advent river for palaeoenvironmental purposes. The base of two sedimentary sections reported radiocarbon dates of 3.3 and 3.9 ka BP, respectively. The northern site is constituted by three very different lithostratigraphical units, which suggests that their formation should be related to different environmental and climate conditions. By contrast, the southern section shows a rather homogeneous composition, with no significant variations in grain size and organic matter content. In both cases the uppermost sediments are constituted by a thick aeolian deposit. According to our data, warmer climate conditions may have prevailed during the mid Holocene until 3.3 ka BP with widespread peat formation in the valley bottom. Subsequently, a period with alternating soil formation and aeolian sedimentation took place from 3 to 2.5 ka BP, probably due to increasing climatic severity. During the last millennium a long-term cooling trend has favoured aeolian deposition in the lowest part of Adventdalen.

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