Articles | Volume 14, issue 11
Clim. Past, 14, 1607–1624, 2018
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.
Clim. Past, 14, 1607–1624, 2018
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
Bernhard Aichner et al.
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Cited
14 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
- 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
- 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
- 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
- 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
14 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
- 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
- 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
- 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
- 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: 28 Jun 2022
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...
