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.
Research article
| 
02 Nov 2018
Research article |
| 02 Nov 2018
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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Cited
18 citations as recorded by crossref.
- Climatic and hydrologic variability in the northern Mediterranean across the onset of the Messinian salinity crisis M. Sabino et al. 10.1016/j.palaeo.2020.109632
- Biomarker proxies for reconstructing Quaternary climate and environmental change E. McClymont et al. 10.1002/jqs.3559
- Molecular and stable isotope analysis (δ13C, δ2H) of sedimentary n-alkanes in the St. Lawrence Estuary and Gulf, Quebec, Canada: Importance of even numbered n-alkanes in coastal systems A. Imfeld et al. 10.1016/j.orggeochem.2022.104367
- Organic geochemical and palaeobotanical reconstruction of a late-Holocene archaeological settlement in coastal eastern India S. Kumar Das et al. 10.1177/09596836211025970
- DO RADIOCARBON AGES OF PLANT WAX BIOMARKERS AGREE WITH 14C-TOC/OSL-BASED AGE MODELS IN AN ARID HIGH-ALTITUDE LAKE SYSTEM? B. Aichner et al. 10.1017/RDC.2021.78
- 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
- n-Alkanes variability in natural populations of Picea omorika (Pančić) Purk. From Bosnia and Herzegovina B. Nikolić et al. 10.1016/j.bse.2022.104544
- Assessment of long-chain n-alkanes as a paleoclimate proxy in the Bering Sea sediments O. Seki et al. 10.1016/j.pocean.2021.102687
- Neolithic livestock practices in high mountain areas: A multi-proxy study of pastoral enclosures of Molleres II (Eastern Pyrenees) V. Pescini et al. 10.1016/j.quaint.2023.04.008
- Younger Dryas glaciomarine sedimentation, push-moraine formation and ice-margin behavior in the Middle Swedish end-moraine zone west of Billingen, central Sweden M. Johnson et al. 10.1016/j.quascirev.2019.105913
- n-Alkane Distribution—A Paleovegetation Change Indicator during the Period from Late Glacial to Late Holocene on Russian Plain (Bryansk Region) E. Stolpnikova et al. 10.3390/geosciences10030086
- Paleoclimatic fluctuations inferred from leaf wax n-alkane records in Central Tibet in the late Oligocene to early Miocene M. Cao et al. 10.1016/j.palaeo.2019.109504
- Centennial-scale age offsets of plant wax n-alkanes in Adirondack lake sediments E. Freimuth et al. 10.1016/j.gca.2021.02.022
- Water depth control on n-alkane distribution and organic carbon isotope in mid-latitude Asian lakes J. Jiang et al. 10.1016/j.chemgeo.2021.120070
- 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
18 citations as recorded by crossref.
- Climatic and hydrologic variability in the northern Mediterranean across the onset of the Messinian salinity crisis M. Sabino et al. 10.1016/j.palaeo.2020.109632
- Biomarker proxies for reconstructing Quaternary climate and environmental change E. McClymont et al. 10.1002/jqs.3559
- Molecular and stable isotope analysis (δ13C, δ2H) of sedimentary n-alkanes in the St. Lawrence Estuary and Gulf, Quebec, Canada: Importance of even numbered n-alkanes in coastal systems A. Imfeld et al. 10.1016/j.orggeochem.2022.104367
- Organic geochemical and palaeobotanical reconstruction of a late-Holocene archaeological settlement in coastal eastern India S. Kumar Das et al. 10.1177/09596836211025970
- DO RADIOCARBON AGES OF PLANT WAX BIOMARKERS AGREE WITH 14C-TOC/OSL-BASED AGE MODELS IN AN ARID HIGH-ALTITUDE LAKE SYSTEM? B. Aichner et al. 10.1017/RDC.2021.78
- 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
- n-Alkanes variability in natural populations of Picea omorika (Pančić) Purk. From Bosnia and Herzegovina B. Nikolić et al. 10.1016/j.bse.2022.104544
- Assessment of long-chain n-alkanes as a paleoclimate proxy in the Bering Sea sediments O. Seki et al. 10.1016/j.pocean.2021.102687
- Neolithic livestock practices in high mountain areas: A multi-proxy study of pastoral enclosures of Molleres II (Eastern Pyrenees) V. Pescini et al. 10.1016/j.quaint.2023.04.008
- Younger Dryas glaciomarine sedimentation, push-moraine formation and ice-margin behavior in the Middle Swedish end-moraine zone west of Billingen, central Sweden M. Johnson et al. 10.1016/j.quascirev.2019.105913
- n-Alkane Distribution—A Paleovegetation Change Indicator during the Period from Late Glacial to Late Holocene on Russian Plain (Bryansk Region) E. Stolpnikova et al. 10.3390/geosciences10030086
- Paleoclimatic fluctuations inferred from leaf wax n-alkane records in Central Tibet in the late Oligocene to early Miocene M. Cao et al. 10.1016/j.palaeo.2019.109504
- Centennial-scale age offsets of plant wax n-alkanes in Adirondack lake sediments E. Freimuth et al. 10.1016/j.gca.2021.02.022
- Water depth control on n-alkane distribution and organic carbon isotope in mid-latitude Asian lakes J. Jiang et al. 10.1016/j.chemgeo.2021.120070
- 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 (preprint)
Latest update: 24 Sep 2023
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...
