The Crvenka loess-paleosol sequence: A record of continuous grassland domination in the southern Carpathian Basin during the Late Pleistocene

Slobodan B. Marković, Pál Sümegi, Thomas Stevens, Randall J. Schaetzl, Igor Obreht, Wei Chu, Björn Buggle, Michael Zech, Roland Zech, Christian Zeeden, Milivoj B. Gavrilov, Zoran Perić, Zorica Svirčev, Frank Lehmkuhl

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11 Citations (Scopus)

Abstract

In this study, we compare two independent paleoenvironmental proxies for a loess sequence in northern Serbia, in the southern Carpathian Basin: novel n-alkane biomarkers and traditional land snail assemblages. Both are associated with other, more widely used proxy data for loess sections, such as environmental magnetism, grain size, and geochemical indices. Together, these paleoenvironmental proxy records provide evidence for the continued dominance of grasslands during the Late Pleistocene in the Southern Carpathian Basin. It is contrary to other European loess provinces, which are characterized by high diversity of Late Pleistocene environments (ranging from tundra-like to deciduous forest habitats). These findings highlight the southeastern part of Carpathian Basin as an important, but still insufficiently investigated, biogeographical refugium, and biodiversity preservation zone. The reason for this is a mostly stable paleoclimate for much of the Late Pleistocene.

Original languageEnglish
Pages (from-to)33-46
Number of pages14
JournalPalaeogeography, Palaeoclimatology, Palaeoecology
Volume509
DOIs
Publication statusPublished - Nov 15 2018

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Keywords

  • Biomarkers
  • Grassland
  • Loess
  • Mollusks
  • Serbia

ASJC Scopus subject areas

  • Oceanography
  • Ecology, Evolution, Behavior and Systematics
  • Earth-Surface Processes
  • Palaeontology

Cite this

Marković, S. B., Sümegi, P., Stevens, T., Schaetzl, R. J., Obreht, I., Chu, W., Buggle, B., Zech, M., Zech, R., Zeeden, C., Gavrilov, M. B., Perić, Z., Svirčev, Z., & Lehmkuhl, F. (2018). The Crvenka loess-paleosol sequence: A record of continuous grassland domination in the southern Carpathian Basin during the Late Pleistocene. Palaeogeography, Palaeoclimatology, Palaeoecology, 509, 33-46. https://doi.org/10.1016/j.palaeo.2018.03.019