Articles | Volume 14, issue 11
https://doi.org/10.5194/cp-14-1607-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-14-1607-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Leaf wax n-alkane distributions record ecological changes during the Younger Dryas at Trzechowskie paleolake (northern Poland) without temporal delay
Institute of Earth and Environmental Sciences, University of Potsdam,
14476 Potsdam-Golm, Germany
Florian Ott
Section 5.2: Climate Dynamics and Landscape Evolution, GFZ German
Research Centre for Geosciences, 14473 Potsdam, Germany
Department of Archaeology, Max Planck Institute for the Science of
Human History, 07745 Jena, Germany
Michał Słowiński
Department of Environmental Resources and Geohazards, Institute of
Geography and Spatial Organisation, Polish Academy of Sciences, 00-818
Warsaw, Poland
Agnieszka M. Noryśkiewicz
Institute of Archaeology, Faculty of History, Nicolaus Copernicus University, 87-100
Toruń, Poland
Achim Brauer
Section 5.2: Climate Dynamics and Landscape Evolution, GFZ German
Research Centre for Geosciences, 14473 Potsdam, Germany
Dirk Sachse
Organic Surface Geochemistry Lab, Section 5.1: Geomorphology, GFZ
German Research Centre for Geosciences, 14473 Potsdam, Germany
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- How dry was the Younger Dryas? Evidence from a coupled <i>δ</i><sup>2</sup>H–<i>δ</i><sup>18</sup>O biomarker paleohygrometer applied to the Gemündener Maar sediments, Western Eifel, Germany J. Hepp et al. 10.5194/cp-15-713-2019
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- Synchronous or Not? The Timing of the Younger Dryas and Greenland Stadial-1 Reviewed Using Tephrochronology S. Larsson et al. 10.3390/quat5020019
- The Late Glacial pedogenesis interrupted by aeolian activity in Central Poland – records from the Lake Gościąż catchment B. Kruczkowska et al. 10.1016/j.catena.2019.104286
- Seasonal variability in temperature trends and atmospheric circulation systems during the Eemian (Last Interglacial) based on n-alkanes hydrogen isotopes from Northern Finland C. Katrantsiotis et al. 10.1016/j.quascirev.2021.107250
- Alkane variation in peat reveals palaeohydrological changes since the Little Ice Age in eastern China Y. Pang et al. 10.1016/j.palaeo.2021.110727
Discussed (final revised paper)
Discussed (preprint)
Latest update: 20 Nov 2024
Short summary
Abundances of plant biomarkers are compared with pollen data in a 3000-year climate archive covering the Late Glacial to Holocene transition in northern Poland. Both parameters synchronously show the rapid onset (12680–12600 yr BP) and termination
(11580–11490 yr BP) of the Younger Dryas cold interval in the study area. This demonstrates the suitability of such proxies to record pronounced changes in vegetation cover without significant delay.
Abundances of plant biomarkers are compared with pollen data in a 3000-year climate archive...