Journal of Paleolimnology

, Volume 58, Issue 2, pp 213–229 | Cite as

Nesseltalgraben, a new reference section of the last glacial period in southern Germany

  • Christoph Mayr
  • Birgit Brandlmeier
  • Volker Diersche
  • Philipp Stojakowits
  • Uwe Kirscher
  • Renate Matzke-Karasz
  • Valerian Bachtadse
  • Michael Eigler
  • Ulrich Haas
  • Bernhard Lempe
  • Paula J. Reimer
  • Christoph Spötl
Original paper
  • 146 Downloads

Abstract

In the northern Alpine region only a few lacustrine sediment sequences are known from the period of the last glacial, regionally assigned as Würmian. Even less is known about Alpine palaeoenvironments prior to the last glacial maximum (LGM). The recently discovered sediment sections at the Nesseltalgraben site (northern Alps, southern Germany) presented here, comprise an approximately 27-m-high, predominantly lacustrine composite profile below coarse clastic sediments assigned to the LGM and underlain by Permian–Triassic evaporitic and sandy clayey sediments of the Haselgebirge and Werfen-Formation. The Würmian lake sediments consist of carbonate mud layers representing cooler phases, and organic rich layers (compressed peat, organic mud), that were deposited during warmer periods. Bulk organic geochemical analyses suggest that predominantly algal organic matter was deposited during the cooler periods, while higher fractions of terrestrial vascular plants were admixed during warmer phases. A diamict represents an erosional unconformity and cuts the sediment sequence into a lower and an upper part. Paleomagnetic, palynostratigraphic and radiocarbon analyses place the lower part into the Marine Isotope Stage (MIS) 5c (Lower Würmian), while the upper part covers at least the period from 45 to 31 ka cal BP (MIS 3, Middle Würmian). Different explanations for the origin and spatiotemporal extent of the palaeolake are discussed. The most plausible sedimentary deposition is the formation of the small-scaled lake in a sinkhole in the evaporitic Haselgebirge Formation. The results highlight the significance of the Nesseltalgraben site as a new reference section of the last glacial period in the Northern Calcareous Alps and call for the necessity of further geochronological and paleoenvironmental studies at that site.

Keywords

Lake sediments Berchtesgaden Würmian Geochemistry Carbon isotopes Pollen Magnetostratigraphy Northern Calcareous Alps 

Notes

Acknowledgements

We are much indebted to Josef März (Berchtesgaden) for generously supporting the fieldwork and analyses. He discovered the Nesseltalgraben site and was one of the driving forces for initiating this study. The palynological studies were partly financed by the Bavarian Environment Agency (Bayerisches Landesamt für Umwelt) in the framework of the EU-funded project “Informationsoffensive Oberflächennahe Geothermie”. We acknowledge research funding by the Deutsche Forschungsgemeinschaft (DFG) (MA 4235/10-1).

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Copyright information

© Springer Science+Business Media Dordrecht 2017

Authors and Affiliations

  • Christoph Mayr
    • 1
    • 2
    • 3
  • Birgit Brandlmeier
    • 2
  • Volker Diersche
    • 4
  • Philipp Stojakowits
    • 5
  • Uwe Kirscher
    • 6
    • 7
  • Renate Matzke-Karasz
    • 2
    • 3
  • Valerian Bachtadse
    • 7
  • Michael Eigler
    • 2
  • Ulrich Haas
    • 8
  • Bernhard Lempe
    • 9
  • Paula J. Reimer
    • 10
  • Christoph Spötl
    • 11
  1. 1.Institut für GeographieFriedrich-Alexander-Universität Erlangen-NürnbergErlangenGermany
  2. 2.Department für Geo- & Umweltwissenschaften, Paläontologie and GeobiologieLudwig-Maximilians-Universität MünchenMunichGermany
  3. 3.GeoBio-CenterLudwig-Maximilians-Universität MünchenMunichGermany
  4. 4.Bayerisch GmainGermany
  5. 5.Institut für GeographieUniversität AugsburgAugsburgGermany
  6. 6.Earth Dynamics Research Group, Department of Applied Geology, ARC Centre of Excellence for Core to Crust Fluid Systems (CCFS) and The Institute for Geoscience Research (TIGeR)Curtin UniversityPerthAustralia
  7. 7.Department für Geo- & Umweltwissenschaften, GeophysikLudwig-Maximilians-Universität MünchenMunichGermany
  8. 8.Bayerisches Landesamt für UmweltAugsburgGermany
  9. 9.Lehrstuhl für IngenieurgeologieTechnische Universität MünchenMunichGermany
  10. 10.Centre for Climate, the Environment and Chronology (14CHRONO), School of Natural and Built EnvironmentQueen’s University BelfastBelfastUK
  11. 11.Institut für GeologieLeopold-Franzens Universität InnsbruckInnsbruckAustria

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