Articles | Volume 15, issue 2
https://doi.org/10.5194/cp-15-713-2019
© Author(s) 2019. 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-15-713-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
How dry was the Younger Dryas? Evidence from a coupled δ2H–δ18O biomarker paleohygrometer applied to the Gemündener Maar sediments, Western Eifel, Germany
Johannes Hepp
CORRESPONDING AUTHOR
Department of Geomorphology and BayCEER, University of Bayreuth, Universitätsstrasse 30,
95440 Bayreuth, Germany
Institute of Agronomy and Nutritional Sciences, Soil Biogeochemistry, Martin Luther University Halle-Wittenberg, Von-Seckendorff-Platz 3, 06120 Halle, Germany
present address: Department of Geomorphology and BayCEER, University of Bayreuth, Universitätsstrasse 30, 95440 Bayreuth, Germany
Lorenz Wüthrich
Institute of Geography and Oeschger Center for Climate Change Research, University of Bern, Hallerstrasse 12, 3012 Bern, Switzerland
Tobias Bromm
Institute of Agronomy and Nutritional Sciences, Soil Biogeochemistry, Martin Luther University Halle-Wittenberg, Von-Seckendorff-Platz 3, 06120 Halle, Germany
Marcel Bliedtner
Institute of Geography and Oeschger Center for Climate Change Research, University of Bern, Hallerstrasse 12, 3012 Bern, Switzerland
present address: Institute of Geography, Department of Physical Geography, Friedrich Schiller University of Jena, Löbdergraben 32, 07743 Jena, Germany
Imke Kathrin Schäfer
Institute of Geography and Oeschger Center for Climate Change Research, University of Bern, Hallerstrasse 12, 3012 Bern, Switzerland
Bruno Glaser
Institute of Agronomy and Nutritional Sciences, Soil Biogeochemistry, Martin Luther University Halle-Wittenberg, Von-Seckendorff-Platz 3, 06120 Halle, Germany
Kazimierz Rozanski
Faculty of Physics and Applied Computer Science, AGH University of Science and Technology, Al. Mickiewicza 30, 30-059 Kraków, Poland
Frank Sirocko
Institute of Geosciences, Group of Climate and Sediments, Johannes Gutenberg University of Mainz, J.-J.-Becher-Weg 21, 55128 Mainz, Germany
Roland Zech
Institute of Geography and Oeschger Center for Climate Change Research, University of Bern, Hallerstrasse 12, 3012 Bern, Switzerland
present address: Institute of Geography, Department of Physical Geography, Friedrich Schiller University of Jena, Löbdergraben 32, 07743 Jena, Germany
Michael Zech
Institute of Agronomy and Nutritional Sciences, Soil Biogeochemistry, Martin Luther University Halle-Wittenberg, Von-Seckendorff-Platz 3, 06120 Halle, Germany
Institute of Geography, Dresden University of Technology, Helmholtzstrasse 10, 01062 Dresden, Germany
present address: Institute of Geography, Dresden University of Technology, Helmholtzstrasse 10, 01062 Dresden, Germany
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- The potential of δ2H-alkanes and δ18Osugar for paleoclimate reconstruction – A regional calibration study for South Africa P. Strobel et al. 10.1016/j.scitotenv.2020.137045
- Source-bordering aeolian dune formation along the Scheldt River (southern Netherlands – northern Belgium) was caused by Younger Dryas cooling, high river gradient and southwesterly summer winds C. Kasse et al. 10.1017/njg.2020.15
- Fine-Tuning of Sub-Annual Resolution Spectral Index Time Series from Eifel Maar Sediments, Western Germany, to the NGRIP δ18O Chronology, 26–60 ka J. Albert et al. 10.3390/quat7030033
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- Human response to the Younger Dryas along the southern North Sea basin, Northwest Europe P. Crombé et al. 10.1038/s41598-024-68686-z
- Latest Pleistocene glacier advances and post-Younger Dryas rock glacier stabilization in the Mt. Kriváň group, High Tatra Mountains, Slovakia J. Zasadni et al. 10.1016/j.geomorph.2020.107093
- Revisiting afro-alpine Lake Garba Guracha in the Bale Mountains of Ethiopia: rationale, chronology, geochemistry, and paleoenvironmental implications L. Bittner et al. 10.1007/s10933-020-00138-w
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- Validation of a coupled <i>δ</i><sup>2</sup>H<sub><i>n</i>-alkane</sub>–<i>δ</i><sup>18</sup>O<sub>sugar</sub> paleohygrometer approach based on a climate chamber experiment J. Hepp et al. 10.5194/bg-18-5363-2021
- δ2Hn-alkane and δ18Osugar biomarker proxies from leaves and topsoils of the Bale Mountains, Ethiopia, and implications for paleoclimate reconstructions B. Lemma et al. 10.1007/s10533-021-00773-z
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- Quantitative reconstruction of the relative humidity by a coupled δ18O-δ2H approach during the Younger Dryas in central China Y. Yang et al. 10.1016/j.quascirev.2022.107879
- Rapid flood intensification and environmental response of the Lower Meuse during the Allerød-Younger Dryas climate transition F. Peng et al. 10.1016/j.geomorph.2020.107469
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- The hydrogen isotopic compositions of sedimentary mid-chain n-alkanes record ecological change at a Portuguese paleowetland A. Taylor et al. 10.1016/j.quaint.2019.09.009
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- Reconstructing Late Quaternary precipitation and its source on the southern Cape coast of South Africa: A multi-proxy paleoenvironmental record from Vankervelsvlei P. Strobel et al. 10.1016/j.quascirev.2022.107467
- Holocene landscape evolution, palaeoclimate and human impact in the Fotsch Valley, Stubai Alps, Austria: Interrogating biomarkers, stable isotopes, macrofossils and palynological indicators from a subalpine mire archive M. Lerch et al. 10.1177/09596836231176485
- Holocene fire dynamics and their climatic controls on the southern Cape coast of South Africa - A 7.2 ka multi-proxy record from the peatland Vankervelsvlei P. Strobel et al. 10.1016/j.quascirev.2023.108464
23 citations as recorded by crossref.
- Cryogenic cave carbonates in the Dolomites (northern Italy): insights into Younger Dryas cooling and seasonal precipitation G. Koltai et al. 10.5194/cp-17-775-2021
- Helium‐flushed sheathed nickel tube reactor for continuous flow oxygen stable isotope compound‐specific analysis C. Johnson & V. Galy 10.1002/rcm.9252
- Comparison of paleobotanical and biomarker records of mountain peatland and forest ecosystem dynamics over the last 2600 years in central Germany C. Thomas et al. 10.5194/bg-20-4893-2023
- The potential of δ2H-alkanes and δ18Osugar for paleoclimate reconstruction – A regional calibration study for South Africa P. Strobel et al. 10.1016/j.scitotenv.2020.137045
- Source-bordering aeolian dune formation along the Scheldt River (southern Netherlands – northern Belgium) was caused by Younger Dryas cooling, high river gradient and southwesterly summer winds C. Kasse et al. 10.1017/njg.2020.15
- Fine-Tuning of Sub-Annual Resolution Spectral Index Time Series from Eifel Maar Sediments, Western Germany, to the NGRIP δ18O Chronology, 26–60 ka J. Albert et al. 10.3390/quat7030033
- Revisiting the subalpine Mesolithic site Ullafelsen in the Fotsch Valley, Stubai Alps, Austria – new insights into pedogenesis and landscape evolution from leaf-wax-derived <i>n</i>-alkanes, black carbon and radiocarbon dating M. Zech et al. 10.5194/egqsj-70-171-2021
- Human response to the Younger Dryas along the southern North Sea basin, Northwest Europe P. Crombé et al. 10.1038/s41598-024-68686-z
- Latest Pleistocene glacier advances and post-Younger Dryas rock glacier stabilization in the Mt. Kriváň group, High Tatra Mountains, Slovakia J. Zasadni et al. 10.1016/j.geomorph.2020.107093
- Revisiting afro-alpine Lake Garba Guracha in the Bale Mountains of Ethiopia: rationale, chronology, geochemistry, and paleoenvironmental implications L. Bittner et al. 10.1007/s10933-020-00138-w
- Precipitation and Lake Water Evaporation Recorded by Terrestrial and Aquatic n‐Alkane δ2H Isotopes in Lake Khar Nuur, Mongolia P. Strobel et al. 10.1029/2021GC010234
- Leaf Waxes and Hemicelluloses in Topsoils Reflect the δ2H and δ18O Isotopic Composition of Precipitation in Mongolia J. Struck et al. 10.3389/feart.2020.00343
- Validation of a coupled <i>δ</i><sup>2</sup>H<sub><i>n</i>-alkane</sub>–<i>δ</i><sup>18</sup>O<sub>sugar</sub> paleohygrometer approach based on a climate chamber experiment J. Hepp et al. 10.5194/bg-18-5363-2021
- δ2Hn-alkane and δ18Osugar biomarker proxies from leaves and topsoils of the Bale Mountains, Ethiopia, and implications for paleoclimate reconstructions B. Lemma et al. 10.1007/s10533-021-00773-z
- Summer paleohydrology during the Late Glacial and Early Holocene based on δ2H and δ18O from Bichlersee, Bavaria M. Prochnow et al. 10.1038/s41598-023-45754-4
- Quantitative reconstruction of the relative humidity by a coupled δ18O-δ2H approach during the Younger Dryas in central China Y. Yang et al. 10.1016/j.quascirev.2022.107879
- Rapid flood intensification and environmental response of the Lower Meuse during the Allerød-Younger Dryas climate transition F. Peng et al. 10.1016/j.geomorph.2020.107469
- Climate changes during the Late Glacial in southern Europe: new insights based on pollen and brGDGTs of Lake Matese in Italy M. Robles et al. 10.5194/cp-19-493-2023
- The hydrogen isotopic compositions of sedimentary mid-chain n-alkanes record ecological change at a Portuguese paleowetland A. Taylor et al. 10.1016/j.quaint.2019.09.009
- Evaluation of bacterial glycerol dialkyl glycerol tetraether and <sup>2</sup>H–<sup>18</sup>O biomarker proxies along a central European topsoil transect J. Hepp et al. 10.5194/bg-17-741-2020
- Reconstructing Late Quaternary precipitation and its source on the southern Cape coast of South Africa: A multi-proxy paleoenvironmental record from Vankervelsvlei P. Strobel et al. 10.1016/j.quascirev.2022.107467
- Holocene landscape evolution, palaeoclimate and human impact in the Fotsch Valley, Stubai Alps, Austria: Interrogating biomarkers, stable isotopes, macrofossils and palynological indicators from a subalpine mire archive M. Lerch et al. 10.1177/09596836231176485
- Holocene fire dynamics and their climatic controls on the southern Cape coast of South Africa - A 7.2 ka multi-proxy record from the peatland Vankervelsvlei P. Strobel et al. 10.1016/j.quascirev.2023.108464
Latest update: 01 Nov 2024