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A 10,300-year-old permafrost core from the active rock glacier Lazaun, southern Ötztal Alps (South Tyrol, northern Italy)

Published online by Cambridge University Press:  20 January 2017

Karl Krainer ,
David Bressan ,
Benjamin Dietre ,
Jean Nicolas Haas ,
Irka Hajdas ,
Kathrin Lang ,
Volkmar Mair ,
Ulrike Nickus ,
Daniel Reidl  and
Hansjörg Thies
...Show all authors
Karl Krainer*
Affiliation:
Institute of Geology and Paleontology, University of Innsbruck, Austria
David Bressan
Affiliation:
Institute of Geology and Paleontology, University of Innsbruck, Austria
Benjamin Dietre
Affiliation:
Institute of Botany, University of Innsbruck, Austria
Jean Nicolas Haas
Affiliation:
Institute of Botany, University of Innsbruck, Austria
Irka Hajdas
Affiliation:
Laboratory of Ion Beam Physics, ETH Zürich, Switzerland
Kathrin Lang
Affiliation:
Office for Geology and Building Materials Testing, Autonomous Province of Bolzano, Italy
Volkmar Mair
Affiliation:
Office for Geology and Building Materials Testing, Autonomous Province of Bolzano, Italy
Ulrike Nickus
Affiliation:
Institute of Meteorology and Geophysics, University of Innsbruck, Austria
Daniel Reidl
Affiliation:
Institute of Botany, University of Innsbruck, Austria
Hansjörg Thies
Affiliation:
Institute of Ecology, University of Innsbruck, Austria
David Tonidandel
Affiliation:
Office for Geology and Building Materials Testing, Autonomous Province of Bolzano, Italy
*
*Corresponding author at: Institute of Geology, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria. E-mail address:Karl.Krainer@uibk.ac.at (K. Krainer).
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Abstract

Two cores were drilled on rock glacier Lazaun in the southern Ötztal Alps (N Italy). The average ice content of core Lazaun I is 43 vol.% and of core Lazaun II is 22 vol.%. Radiocarbon dating of plant macrofossil remains of core Lazaun I yielded ages ranging from 8960 cal yr BP at a depth of ca. 23.5 m to 2240 cal yr BP at a depth of 2.8 m, indicating that the ice near the base is approximately 10,300 yr old. The rock glacier was intact since that time and the ice persisted even during warm periods of the Holocene. An ice-free debris layer between 16.8 and 14.7 m separates the rock glacier into two frozen bodies. Inclinometer measurements indicate that both frozen bodies are active and that deformation occurs within a shear horizon at a depth of 20–25 m at the base of the lower frozen body and to a minor extent at a depth of approximately 14 m at the base of the upper frozen body. The ice-free debris layer in the middle of the Lazaun rock glacier indicates a more than five centennial long drought period, which dates to about 4300–3740 cal yr BP.

Keywords

Rock glacierLazaunÖtztal AlpsHolocene drought
Type
Research Article
Information
Quaternary Research , Volume 83 , Issue 2 , March 2015 , pp. 324 - 335
Copyright
University of Washington

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