The browser you are using is not supported by this website. All versions of Internet Explorer are no longer supported, either by us or Microsoft (read more here: https://www.microsoft.com/en-us/microsoft-365/windows/end-of-ie-support).

Please use a modern browser to fully experience our website, such as the newest versions of Edge, Chrome, Firefox or Safari etc.

Helena Alexandersson

Helena Alexanderson

Professor

Helena Alexandersson

Sediments of MIS 5e age suggested by new OSL dates from the Skilvika section, west Svalbard

Author

  • Helena Alexanderson
  • Jon Y. Landvik

Summary, in English

The sediment succession at Skilvika, west Svalbard, represents one of the key stratigraphic records of the Late Quaternary palaeoenvironments and glaciation history of the Svalbard/Barents Sea area. A formation of raised marine sediments, interfingering with and capped by glacial deposits of local origin, have previously been assumed to be of an Early Weichselian age, likely marine isotope stage (MIS) 5c. Here we present a new series of optically stimulated luminescence (OSL) ages that suggest the events took place in MIS 5e. This advocates a revision of the correlation with other key stratigraphic sites on Svalbard.

Department/s

  • Quaternary Sciences

Publishing year

2018-09-24

Language

English

Publication/Series

Polar Research

Volume

37

Issue

1

Document type

Journal article

Publisher

Wiley-Blackwell

Topic

  • Geology

Keywords

  • Arctic
  • glaciation history
  • luminescence dating
  • MIS 5
  • MIS: marine isotope stageOD: overdispersionOSL: optically stimulated luminescenceTL: thermoluminescence

Status

Published

Project

  • Glacial history of Svalbard

ISBN/ISSN/Other

  • ISSN: 0800-0395