EGU22-2907, updated on 17 Mar 2025
https://doi.org/10.5194/egusphere-egu22-2907
EGU General Assembly 2022
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Lacustrine diatom oxygen isotopes as Holocene palaeo precipitation proxy for the Polar Urals, Russia
Hanno Meyer1, Svetlana S. Kostrova1, Meister Philip1, Lenz Marlene M.2, Nazarova Larisa1,3, Kuhn Gerhard1, Syrykh Luidmila S.4, and Dvornikov Yuri5
Hanno Meyer et al.
  • 1Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Potsdam and Bremerhaven, Germany (hanno.meyer@awi.de)
  • 2Institute of Geology and Mineralogy, University of Cologne, Zülpicher Str. 49a, Cologne 50674, Germany
  • 3Kazan Federal University, Kremlyovskaya str. 18, Kazan 420018, Russia
  • 4Herzen State Pedagogical University of Russia, Moika 48, St. Petersburg 191186, Russia
  • 5Department of Landscape Design and Sustainable Ecosystems, Agrarian-Technological Institute, Рeoples’ Friendship University of Russia (RUDN University), 6 Miklukho-Maklaya St, Moscow, 117198, Russia.

How to cite: Meyer, H., Kostrova, S. S., Philip, M., Marlene M., L., Larisa, N., Gerhard, K., Luidmila S., S., and Yuri, D.: Lacustrine diatom oxygen isotopes as Holocene palaeo precipitation proxy for the Polar Urals, Russia, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-2907, https://doi.org/10.5194/egusphere-egu22-2907, 2022.

This abstract has been withdrawn on 01 Apr 2022.