EGU22-1637
https://doi.org/10.5194/egusphere-egu22-1637
EGU General Assembly 2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.

Cryostratigraphy, chronology, and ground-ice stable isotopes of the Batagay megaslump in east Siberia indicate climate–permafrost interactions during the Middle and Late Pleistocene

Thomas Opel1, Sebastian Wetterich1,2, Hanno Meyer1, and Julian Murton3
Thomas Opel et al.
  • 1Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Polar Terrestrial Environmental Systems, Potsdam, Germany (thomas.opel@awi.de)
  • 2Technische Universität Dresden, Institute of Geography, Heisenberg Chair of Physical Geography with Focus on Paleoenvironmental Research, Dresden, Germany
  • 3Permafrost Laboratory, Department of Geography, University of Sussex, Brighton, United Kingdom

How to cite: Opel, T., Wetterich, S., Meyer, H., and Murton, J.: Cryostratigraphy, chronology, and ground-ice stable isotopes of the Batagay megaslump in east Siberia indicate climate–permafrost interactions during the Middle and Late Pleistocene, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-1637, https://doi.org/10.5194/egusphere-egu22-1637, 2022.

This abstract has been withdrawn on 01 Apr 2022.