Articles | Volume 69, issue 1
https://doi.org/10.5194/egqsj-69-61-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/egqsj-69-61-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Revisiting Late Pleistocene glacier dynamics north-west of the Feldberg, southern Black Forest, Germany
Felix Martin Hofmann
CORRESPONDING AUTHOR
Institute of Earth and Environmental Sciences, University of Freiburg, 79104 Freiburg, Germany
Florian Rauscher
Institute of Earth and Environmental Sciences, University of Freiburg, 79104 Freiburg, Germany
William McCreary
Institute of Earth and Environmental Sciences, University of Freiburg, 79104 Freiburg, Germany
Jan-Paul Bischoff
Institute of Earth and Environmental Sciences, University of Freiburg, 79104 Freiburg, Germany
Frank Preusser
Institute of Earth and Environmental Sciences, University of Freiburg, 79104 Freiburg, Germany
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Felix Martin Hofmann and Frank Preusser
E&G Quaternary Sci. J., 74, 1–35, https://doi.org/10.5194/egqsj-74-1-2025, https://doi.org/10.5194/egqsj-74-1-2025, 2025
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Previous reconstructions conclude that the southern Black Forest, south-west Germany, temporarily hosted four ice caps during the Late Pleistocene (129 000–11 700 years before present). This work reviews existing studies on glacial landforms north-east of its highest summit, Feldberg (1493 m above sea level), in the light of new observations. Whilst this study largely confirms previous work, we reject and newly describe several glacial landforms.
Alexander Fülling, Hans Rudolf Graf, Felix Martin Hofmann, Daniela Mueller, and Frank Preusser
E&G Quaternary Sci. J., 73, 203–216, https://doi.org/10.5194/egqsj-73-203-2024, https://doi.org/10.5194/egqsj-73-203-2024, 2024
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The Mühlbach series has been given as evidence for a Late Pliocene/Early Pleistocene Aare–Rhine fluvial system in northern Switzerland and southwest Germany. We show that these deposits represent a variety of different units. At the type location, luminescence dating indicates an age of 55 ka, and we interpret the deposits as slope reworking. Beside methodological implications, our studies recommend caution regarding the interpretation of stratigraphic units for which limited data are available.
Felix Martin Hofmann, Claire Rambeau, Lukas Gegg, Melanie Schulz, Martin Steiner, Alexander Fülling, Laëtitia Léanni, Frank Preusser, and ASTER Team
Geochronology, 6, 147–174, https://doi.org/10.5194/gchron-6-147-2024, https://doi.org/10.5194/gchron-6-147-2024, 2024
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We determined 10Be concentrations in moraine boulder surfaces in the southern Black Forest, SW Germany. We applied three independent dating methods to younger lake sediments. With the aid of independent age datasets, we calculated the growth of 10Be concentrations in moraine boulder surfaces.
Felix Martin Hofmann
E&G Quaternary Sci. J., 72, 235–237, https://doi.org/10.5194/egqsj-72-235-2023, https://doi.org/10.5194/egqsj-72-235-2023, 2023
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This study aims to reconstruct the last glaciation of the southern Black Forest. Ice-marginal positions in this region were, for the first time, directly dated. Glacier retreat from the last glaciation maximum position was probably underway no later than 21 ka. Re-advances and/or standstills of glaciers (no later than 17–16 ka, 15–14 ka and 13 ka) punctuated the subsequent trend towards ice-free conditions.
Felix Martin Hofmann
Geochronology, 4, 691–712, https://doi.org/10.5194/gchron-4-691-2022, https://doi.org/10.5194/gchron-4-691-2022, 2022
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If topographical obstructions are present in the surroundings of sampling sites, exposure ages of rock surfaces need to be corrected. A toolbox for the ESRI ArcGIS software allows for quantifying topographic shielding with a digital elevation model, but it has only been validated with few field data. In this study, the output of the toolbox is evaluated with a more extensive dataset. If suitable elevation data are chosen, the toolbox provides a sound approach to determine topographic shielding.
Charlotte E. Engelmann, Frank Preusser, Alexander Fülling, Jakob Wilk, Elisabeth Eiche, Dennis Quandt, Stefan Hergarten, and Jan H. Blöthe
E&G Quaternary Sci. J., 74, 235–262, https://doi.org/10.5194/egqsj-74-235-2025, https://doi.org/10.5194/egqsj-74-235-2025, 2025
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It is unclear since when and how meso-scale central European river systems have been dominated by human instead of natural influences. Here, the floodplain sediments of the Kinzig River, southwestern Germany, were studied as they recorded natural and human landscape changes. Sediment deposition phases were found, the modern phase of which coincides with increased deposition and heavy metal contaminations that correlate with mining records, indicating that the river system has shifted intensely over 1000 years.
Madhurima Marik, Elena Serra, Gilles Rixhon, and Frank Preusser
E&G Quaternary Sci. J., 74, 169–192, https://doi.org/10.5194/egqsj-74-169-2025, https://doi.org/10.5194/egqsj-74-169-2025, 2025
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This study examines the evolution of the lower Bruche River valley in north-eastern France through its fluvial terraces, reflecting past river dynamics and environmental changes. Terrace formations are dated using luminescence to ~ 12–14 ka, ~ 27–35 ka, and at least 200 ka. Methodological improvements over conventional luminescence dating techniques are also discussed and refined in this study.
Felix Martin Hofmann and Frank Preusser
E&G Quaternary Sci. J., 74, 1–35, https://doi.org/10.5194/egqsj-74-1-2025, https://doi.org/10.5194/egqsj-74-1-2025, 2025
Short summary
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Previous reconstructions conclude that the southern Black Forest, south-west Germany, temporarily hosted four ice caps during the Late Pleistocene (129 000–11 700 years before present). This work reviews existing studies on glacial landforms north-east of its highest summit, Feldberg (1493 m above sea level), in the light of new observations. Whilst this study largely confirms previous work, we reject and newly describe several glacial landforms.
Alexander Fülling, Hans Rudolf Graf, Felix Martin Hofmann, Daniela Mueller, and Frank Preusser
E&G Quaternary Sci. J., 73, 203–216, https://doi.org/10.5194/egqsj-73-203-2024, https://doi.org/10.5194/egqsj-73-203-2024, 2024
Short summary
Short summary
The Mühlbach series has been given as evidence for a Late Pliocene/Early Pleistocene Aare–Rhine fluvial system in northern Switzerland and southwest Germany. We show that these deposits represent a variety of different units. At the type location, luminescence dating indicates an age of 55 ka, and we interpret the deposits as slope reworking. Beside methodological implications, our studies recommend caution regarding the interpretation of stratigraphic units for which limited data are available.
Bennet Schuster, Lukas Gegg, Sebastian Schaller, Marius W. Buechi, David C. Tanner, Ulrike Wielandt-Schuster, Flavio S. Anselmetti, and Frank Preusser
Sci. Dril., 33, 191–206, https://doi.org/10.5194/sd-33-191-2024, https://doi.org/10.5194/sd-33-191-2024, 2024
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The Tannwald Basin, explored by drilling and formed by repeated advances of the Rhine Glacier, reveals key geological insights. Ice-contact sediments and evidence of deformation highlight gravitational and glaciotectonic processes. ICDP DOVE 5068_1_C core data define lithofacies associations, reflecting basin infill cycles, marking at least three distinct glacial advances. Integrating these findings aids understanding the broader glacial evolution of the Lake Constance amphitheater.
Felix Martin Hofmann, Claire Rambeau, Lukas Gegg, Melanie Schulz, Martin Steiner, Alexander Fülling, Laëtitia Léanni, Frank Preusser, and ASTER Team
Geochronology, 6, 147–174, https://doi.org/10.5194/gchron-6-147-2024, https://doi.org/10.5194/gchron-6-147-2024, 2024
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We determined 10Be concentrations in moraine boulder surfaces in the southern Black Forest, SW Germany. We applied three independent dating methods to younger lake sediments. With the aid of independent age datasets, we calculated the growth of 10Be concentrations in moraine boulder surfaces.
Felix Martin Hofmann
E&G Quaternary Sci. J., 72, 235–237, https://doi.org/10.5194/egqsj-72-235-2023, https://doi.org/10.5194/egqsj-72-235-2023, 2023
Short summary
Short summary
This study aims to reconstruct the last glaciation of the southern Black Forest. Ice-marginal positions in this region were, for the first time, directly dated. Glacier retreat from the last glaciation maximum position was probably underway no later than 21 ka. Re-advances and/or standstills of glaciers (no later than 17–16 ka, 15–14 ka and 13 ka) punctuated the subsequent trend towards ice-free conditions.
Lea Schwahn, Tabea Schulze, Alexander Fülling, Christian Zeeden, Frank Preusser, and Tobias Sprafke
E&G Quaternary Sci. J., 72, 1–21, https://doi.org/10.5194/egqsj-72-1-2023, https://doi.org/10.5194/egqsj-72-1-2023, 2023
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The loess sequence of Köndringen, Upper Rhine Graben, comprises several glacial–interglacial cycles. It has been investigated using a multi-method approach including the measurement of colour, grain size, organic matter, and carbonate content. The analyses reveal that the sequence comprises several fossil soils and layers of reworked soil material. According to luminescence dating, it reaches back more than 500 000 years.
Lukas Gegg and Frank Preusser
E&G Quaternary Sci. J., 72, 23–36, https://doi.org/10.5194/egqsj-72-23-2023, https://doi.org/10.5194/egqsj-72-23-2023, 2023
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Erosion processes below glacier ice have carved large and deep basins in the landscapes surrounding mountain ranges as well as polar regions. With our comparison, we show that these two groups of basins are very similar in their shapes and sizes. However, open questions still remain especially regarding the sediments that later fill up these basins. We aim to stimulate future research and promote exchange between researchers working around the Alps and the northern central European lowlands.
Felix Martin Hofmann
Geochronology, 4, 691–712, https://doi.org/10.5194/gchron-4-691-2022, https://doi.org/10.5194/gchron-4-691-2022, 2022
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If topographical obstructions are present in the surroundings of sampling sites, exposure ages of rock surfaces need to be corrected. A toolbox for the ESRI ArcGIS software allows for quantifying topographic shielding with a digital elevation model, but it has only been validated with few field data. In this study, the output of the toolbox is evaluated with a more extensive dataset. If suitable elevation data are chosen, the toolbox provides a sound approach to determine topographic shielding.
Flavio S. Anselmetti, Milos Bavec, Christian Crouzet, Markus Fiebig, Gerald Gabriel, Frank Preusser, Cesare Ravazzi, and DOVE scientific team
Sci. Dril., 31, 51–70, https://doi.org/10.5194/sd-31-51-2022, https://doi.org/10.5194/sd-31-51-2022, 2022
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Previous glaciations eroded below the ice deep valleys in the Alpine foreland, which, with their sedimentary fillings, witness the timing and extent of these glacial advance–retreat cycles. Drilling such sedimentary sequences will thus provide well-needed evidence in order to reconstruct the (a)synchronicity of past ice advances in a trans-Alpine perspective. Eventually these data will document how the Alpine foreland was shaped and how the paleoclimate patterns varied along and across the Alps.
Mubarak Abdulkarim, Stoil Chapkanski, Damien Ertlen, Haider Mahmood, Edward Obioha, Frank Preusser, Claire Rambeau, Ferréol Salomon, Marco Schiemann, and Laurent Schmitt
E&G Quaternary Sci. J., 71, 191–212, https://doi.org/10.5194/egqsj-71-191-2022, https://doi.org/10.5194/egqsj-71-191-2022, 2022
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We used a combination of remote sensing, field investigations, and laboratory analysis to map and characterize abandoned river channels within the French Upper Rhine alluvial plain. Our results show five major paleochannel groups with significant differences in their pattern, morphological characteristics, and sediment filling. The formation of these paleochannel groups is attributed to significant changes in environmental processes in the area during the last ~ 11 700 years.
Tabea Schulze, Lea Schwahn, Alexander Fülling, Christian Zeeden, Frank Preusser, and Tobias Sprafke
E&G Quaternary Sci. J., 71, 145–162, https://doi.org/10.5194/egqsj-71-145-2022, https://doi.org/10.5194/egqsj-71-145-2022, 2022
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A loess sequence in SW Germany was investigated using a high-resolution multi-method approach. It dates to 34–27 ka and comprises layers of initial soil formation. Drier conditions and a different atmospheric circulation pattern during the time of deposition are expected as the soil layers are less strongly developed compared to similar horizons further north. Dust accumulation predates the last advance of Alpine glaciers, and no loess deposition is recorded for the time of maximum ice extent.
Frank Preusser, Markus Fuchs, and Christine Thiel
E&G Quaternary Sci. J., 70, 201–203, https://doi.org/10.5194/egqsj-70-201-2021, https://doi.org/10.5194/egqsj-70-201-2021, 2021
Frank Preusser, Markus Fuchs, and Christine Thiel
DEUQUA Spec. Pub., 3, 1–3, https://doi.org/10.5194/deuquasp-3-1-2021, https://doi.org/10.5194/deuquasp-3-1-2021, 2021
Felicia Linke, Oliver Olsson, Frank Preusser, Klaus Kümmerer, Lena Schnarr, Marcus Bork, and Jens Lange
Hydrol. Earth Syst. Sci., 25, 4495–4512, https://doi.org/10.5194/hess-25-4495-2021, https://doi.org/10.5194/hess-25-4495-2021, 2021
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We used a two-step approach with limited sampling effort in existing storm water infrastructure to illustrate the risk of biocide emission in a 2 ha urban area 13 years after construction had ended. First samples at a swale confirmed the overall relevance of biocide pollution. Then we identified sources where biocides were used for film protection and pathways where transformation products were formed. Our results suggest that biocide pollution is a also continuous risk in aging urban areas.
Cited articles
Balco, G.: Glacier Change and Paleoclimate Applications of
Cosmogenic-Nuclide Exposure Dating, Annual Rev. Earth Pl. Sc., 48, 21–48,
https://doi.org/10.1146/annurev-earth-081619-052609, 2020.
Bangert, V., Schreiner, A., and Etzold, A.: Geologische Karte von
Baden-Württemberg 1:25000, Blatt 8115 Lenzkirch, Landesvermessungsamt
Baden-Württemberg, Stuttgart, 1992.
Barr, I. D. and Lovell, H.: A review of topographic controls on moraine
distribution, Geomorphology, 226, 44–64,
https://doi.org/10.1016/j.geomorph.2014.07.030, 2014.
Boston, C. M. and Lukas, S.: Topographic controls on plateau icefield
recession: insights from the Younger Dryas Monadhliath Icefield, Scotland,
J. Quaternary Sci., 34, 433–451, https://doi.org/10.1002/jqs.3111, 2019.
Boston, C. M., Lukas, S., and Carr, S. J.: A Younger Dryas plateau icefield
in the Monadhliath, Scotland, and implications for regional palaeoclimate,
Quaternary Sci. Rev., 108, 139–162,
https://doi.org/10.1016/j.quascirev.2014.11.020, 2015.
Boxleitner, M., Ivy-Ochs, S., Brandova, D., Christl, M., Egli, M., and Maisch, M.: Piecing together the Lateglacial advance phases of the Reussgletscher (central Swiss Alps), Geogr. Helv., 73, 241–252, https://doi.org/10.5194/gh-73-241-2018, 2018.
Bronk Ramsey, C.: Bayesian Analysis of Radiocarbon Dates, Radiocarbon, 51,
337–360, https://doi.org/10.1017/S0033822200033865, 2009.
Chandler, B. M. P., Lovell, H., Boston, C. M., Lukas, S., Barr, I. D.,
Benediktsson, Í. Ö., Benn, D. I., Clark, C. D., Darvill, C. M.,
Evans, D. J. A., Ewertowski, M. W., Loibl, D., Margold, M., Otto, J.-C.,
Roberts, D. H., Stokes, C. R., Storrar, R. D., and Stroeven, A. P.: Glacial
geomorphological mapping: A review of approaches and frameworks for best
practice, Earth-Science Rev., 185, 806–846,
https://doi.org/10.1016/j.earscirev.2018.07.015, 2018.
Duprat-Oualid, F., Rius, D., Bégeot, C., Magny, M., Millet, L., Wulf,
S., and Appelt, O.: Vegetation response to abrupt climate changes in Western
Europe from 45 to 14.7k cal a BP: the Bergsee lacustrine record (Black
Forest, Germany), J. Quaternary Sci., 32, 1008–1021,
https://doi.org/10.1002/jqs.2972, 2017.
Duprat-Oualid, F., Peyron, O., Bégeot, C., Magny, M., Millet, L., and
Rius, D.: Pollen-inferred quantification of the climate variability of the
last 50 ka from the Bergsee record (Black Forest, Germany), Quaternary Sci.
Rev., in press., 2020.
Erb, L.: Die Geologie des Feldbergs, in: Der Feldberg im Schwarzwald, edited
by: Müller, K., L. Bielefelds Verlag KG, Freiburg i. Br., 22–96, 1948.
Florineth, D. and Schlüchter, C.: Alpine Evidence for Atmospheric
Circulation Patterns in Europe during the Last Glacial Maximum, Quaternary
Res., 54, 295–308, https://doi.org/10.1006/qres.2000.2169, 2000.
Friedmann, A.: Pollenanalytische Untersuchungen zur holozänen
Vegetations- und Landschaftsgeschichte des westlichen Hochschwarzwalds, Ber.
Naturf. Ges. Freiburg i. Br., 88/89, 57–84, 1998/1999.
Giermann, G.: Die würmeiszeitliche Vergletscherung des Schauinsland
Trubelsmattkopf-Massivs (westlicher Südschwarzwald) Diploma thesis,
University of Freiburg, Freiburg, 56 pp., 1959.
Giermann, G.: Die würmeiszeitliche Vergletscherung des
Schauinsland-Trubelsmattkopf-Knöpflesbrunnen-Massivs (südlicher
Schwarzwald), Ber. Naturf. Ges. Freiburg i. Br., 54, 197–208, 1964.
Hann, H. P., Schreiner, A., and Zedler, H.: Geologische Karte von
Baden-Württemberg 1:25 000, Blatt 8113 Todtnau, Landesamt für
Geologie, Rohstoffe und Bergbau, Freiburg i. Br., 2011.
Heiri, O., Koinig, K. A., Spötl, C., Barrett, S., Brauer, A.,
Drescher-Schneider, R., Gaar, D., Ivy-Ochs, S., Kerschner, H., Luetscher,
M., Moran, A., Nicolussi, K., Preusser, F., Schmidt, R., Schoeneich, P.,
Schwörer, C., Sprafke, T., Terhorst, B., and Tinner, W.: Palaeoclimate
records 60–8 ka in the Austrian and Swiss Alps and their forelands,
Quaternary Sci. Rev., 106, 186–205,
https://doi.org/10.1016/j.quascirev.2014.05.021, 2014.
Hemmerle, H., May, J.-H., and Preusser, F.: Übersicht über die
pleistozänen Vergletscherungen des Schwarzwaldes, Ber. Naturf. Ges.
Freiburg i. Br., 106, 31–67, 2016.
Hofmann, F. M., Alexanderson, H., Schoeneich, P., Mertes, J. R., Léanni,
L., and ASTER Team: Post-Last Glacial Maximum glacier fluctuations in the
southern Écrins massif (westernmost Alps): insights from 10Be
cosmic ray exposure dating, Boreas, 48, 1019–1041,
https://doi.org/10.1111/bor.12405, 2019.
Hüttner, R.: Das Quartär, in: Geologische Karte von
Baden-Württemberg 1:25 000, Erläuterungen zu Blatt 8013
Freiburg-Südost, edited by: Geologisches Landesamt
Baden-Württemberg, Landesvermessungsamt Baden-Württemberg,
Stuttgart, 69–105, 1967.
Ivy-Ochs, S., Schlüchter, C., Kubik, P. W., Synal, H.-A., Beer, J., and
Kerschner, H.: The exposure age of an Egesen moraine at Julier Pass,
Switzerland, measured with the cosmogenic radionuclides 10Be, 26Al
and 36Cl, Eclogae Geol. Helv., 89, 1049–1063, 1996.
Ivy-Ochs, S., Kerschner, H., Kubik, P. W., and Schlüchter, C.: Glacier
response in the European Alps to Heinrich Event 1 cooling: the Gschnitz
stadial, J. Quaternary Sci., 21, 115–130, https://doi.org/10.1002/jqs.955,
2006.
Ivy-Ochs, S.: Glacier variations in the European Alps at the end of the last
glaciation, Cuadernos de Investigación Geográfica, 41, 219–315,
https://doi.org/10.18172/cig.2750, 2015.
Kerschner, H. and Ivy-Ochs, S.: Palaeoclimate from glaciers: Examples from
the Eastern Alps during the Alpine Lateglacial and early Holocene, Global
Planet. Change, 60, 58–71, https://doi.org/10.1016/j.gloplacha.2006.07.034,
2008.
Klute, F.: Die Schneereste des Schwarzwaldes im Frühsommer und die
Beziehungen ihrer Lage zu den Stellen ehemaliger Vergletscherung, Ber.
Naturf. Ges. Freiburg i. Br., 19, 61–116, 1911.
Kuhlemann, J., Rohling, E. J., Krumrei, I., Kubik, P., Ivy-Ochs, S., and
Kucera, M.: Regional Synthesis of Mediterranean Atmospheric Circulation
During the Last Glacial Maximum, J. Science, 321, 1338–1340,
https://doi.org/10.1126/science.1157638, 2008.
Lang, G.: Seen und Moore des Schwarzwaldes als Zeugen spätglazialen und
holozänen Vegetationswandels. Stratigraphische, pollenanalytische und
großrestanalytische Untersuchungen, Andrias, edited by: Staatliches
Museum für Naturkunde Karlsruhe, Karlsruhe, 160 pp., 2005.
Lang, G.: Late-glacial fluctuations of timberline in the Black Forest (SW
Germany), Veg. Hist. and Archaeobot., 15, 373–375,
https://doi.org/10.1007/s00334-006-0048-8, 2006.
Lang, G., Merkt, J., and Streif, H.: Spätglazialer Gletscherrückzug
und See- und Moorentwicklung im Südschwarzwald, Südwestdeutschland,
Diss. Bot., 72 (Festschrift Max Welten), 213–234, 1984.
Leser, H. and Metz, B.: Vergletscherungen im Hochschwarzwald, Berliner
Geogr. Abh., 47, 155–175, 1988.
Liehl, E.: Landschaftsgeschichte des Feldberggebietes, in: Der Feldberg im
Schwarzwald: subalpine Insel im Mittelgebirge, edited by: Landesanstalt
für Umweltschutz Baden-Württemberg Institut für Ökologie und
Naturschutz, Karlsruhe, 1982.
LUBW: St. Wilhelm-Katzensteig,
available at: http://www2.lubw.baden-wuerttemberg.de/public/abt2/dokablage/oac_77/558.htm (last access: 13 June 2020), 2009.
LUBW: Heibeermoos,
http://www2.lubw.baden-wuerttemberg.de/public/abt2/dokablage/oac_77/559.htm (last access: 13 June 2020), 2010.
Luetscher, M., Boch, R., Sodemann, H., Spötl, C., Cheng, H., Edwards, R.
L., Frisia, S., Hof, F., and Müller, W.: North Atlantic storm track
changes during the Last Glacial Maximum recorded by Alpine speleothems, Nat.
Commun., 6, 6344, https://doi.org/10.1038/ncomms7344, 2015.
Lukas, S.: Early-Holocene glacier fluctuations in Krundalen, south central
Norway: palaeoglacier dynamics and palaeoclimate, Holocene, 17, 585–598,
https://doi.org/10.1177/0959683607078983, 2007.
Lukas, S.: A test of the englacial thrusting hypothesis of `hummocky'
moraine formation: case studies from the northwest Highlands, Scotland,
Boreas, 34, 287–307, https://doi.org/10.1111/j.1502-3885.2005.tb01102.x,
2005.
Lukas, S. and Benn, D. I.: Retreat dynamics of Younger Dryas glaciers in
the far NW Scottish Highlands reconstructed from moraine sequences, Scot.
Geogr. J., 122, 308–325, https://doi.org/10.1080/14702540701235142, 2006.
Lukas, S. and Rother, H.: Moränen versus Till: Empfehlungen für die Beschreibung, Interpretation und Klassifikation glazialer Landformen und Sedimente, E&G Quaternary Sci. J., 65, 95–112, https://doi.org/10.3285/eg.65.2.01, 2016.
Lukas, S., Graf, A., Coray, S., and Schlüchter, C.: Genesis, stability
and preservation potential of large lateral moraines of Alpine valley
glaciers – towards a unifying theory based on Findelengletscher,
Switzerland, Quaternary Sci. Rev., 38, 27–48,
https://doi.org/10.1016/j.quascirev.2012.01.022, 2012a.
Lukas, S., Preusser, F., Anselmetti, F. S., and Tinner, W.: Testing the
potential of luminescence dating of high-alpine lake sediments, Quat.
Geochronol., 8, 23–32, https://doi.org/10.1016/j.quageo.2011.11.007, 2012b.
Lüthgens, C. and Böse, M.: From morphostratigraphy to geochronology
– on the dating of ice marginal positions, Quaternary Sci. Rev., 44,
26–36, https://doi.org/10.1016/j.quascirev.2010.10.009, 2012.
Mackintosh, A. N., Anderson, B. M., and Pierrehumbert, R. T.: Reconstructing
Climate from Glaciers, Annual Rev. Earth Pl. Sc., 45, 649–680,
https://doi.org/10.1146/annurev-earth-063016-020643, 2017.
Meinig, R.: Die würmeiszeitliche Vergletscherung im Gebiet
Breitnau-Hinterzarten-Neustadt (Schwarzwald), PhD thesis, University of
Freiburg, Freiburg, 166 pp., 1966.
Meinig, R.: Halte und Eisrandbildungen des würmzeitlichen
Bärental-Gletschers, Südschwarzwald, Late- and postglacial
oscillations of glaciers: glacial and periglacial landforms, Trier, 1980,
257–282, 1980.
Merkt, J.: Exkursionspunkt: “Feldsee”. Bohrung Feldsee-Mitte, in: 22.
wissenschaftliche Tagung in Freiburg i. Br. September 1985.
Exkursionsführer 1. Südschwarzwald, Oberschwaben/Bodensee,
südliches Oberrheingebiet, edited by: Schreiner, A. and Metz, B.,
Deutsche Quartärvereinigung, Hannover, 39–41, 1985.
Metz, B.: Geomorphologische Karte 1:25 000 der Bundesrepublik Deutschland.
GMK 25 Blatt 21. 8114 Feldberg, GMK-Schwerpunktprogramm der Deutschen
Forschungsgemeinschaft (DFG), Berlin, 1985a.
Metz, B.: Erläuterungen zur Geomorphologischen Karte 1:25 000 der
Bundesrepublik Deutschland, GMK 25 Blatt 21, 8114 Feldberg, GMK
Schwerpunktprogramm. Geomorphologische Detailkartierung in der
Bundesrepublik Deutschland, edited by: Barsch, D., Fränzle, O., Leser,
H., Liedtke, H., and Stäblein, G., Geo Center, Stuttgart, 1985b.
Metz, B.: Glaziale Formen und Formungsprozesse im Schwarzwald, in:
Schwarzwald und Oberrheintiefland, edited by: Mäckel, R., and Metz, B.,
Freiburger Geographische Hefte, 36, Institut für Physische Geographie
der Albert-Ludwigs-Universität Freiburg i. B, Freiburg i. Br., 51–74,
1997.
Metz, B. and Saurer, H.: Geomorphologie und Landschaftsentwicklung, in: Der
Feldberg: subalpine Insel im Schwarzwald, edited by: Regierungspräsidium
Freiburg, Jan Thorbecke Verlag der Schwabenverlag AG, Ostfildern, 14–62,
2012.
Monegato, G., Scardia, G., Hajdas, I., Rizzini, F., and Piccin, A.: The
Alpine LGM in the boreal ice-sheets game, Sci. Rep.-UK, 7, 2078,
https://doi.org/10.1038/s41598-017-02148-7, 2017.
Moran, A. P., Ivy-Ochs, S., Schuh, M., Christl, M., and Kerschner, H.:
Evidence of central Alpine glacier advances during the Younger Dryas–early
Holocene transition period, Boreas, 45, 398–410,
https://doi.org/10.1111/bor.12170, 2016.
Pearce, D. M., Ely, J. C., Barr, I. D., and Boston, C. M.: Glacier
reconstruction, in: Geomorphological Techniques, edited by: Cook, S.,
Clarke, L., and Nield, J., British Society for Geomorphology, London, 2017.
Pellitero, R., Rea, B. R., Spagnolo, M., Bakke, J., Ivy-Ochs, S., Frew, C.
R., Hughes, P., Ribolini, A., Lukas, S., and Renssen, H.: GlaRe, a GIS tool
to reconstruct the 3D surface of palaeoglaciers, Comput. Geosci., 94, 77–85,
https://doi.org/10.1016/j.cageo.2016.06.008, 2016.
Piotrowska, N., Blaauw, M., Mauquoy, D., and Chambers, F. M.: Constructing
deposition chronologies for peat deposits using radiocarbon dating, Mires
Peat, 7, 10, 2011.
Protin, M., Schimmelpfennig, I., Mugnier, J.-L., Ravanel, L., Le Roy, M.,
Deline, P., Favier, V., Buoncristiani, J.-F., Aumaître, G.,
Bourlès, D. L., and Keddadouche, K.: Climatic reconstruction for the
Younger Dryas/Early Holocene transition and the Little Ice Age based on
paleo-extents of Argentière glacier (French Alps), Quaternary Sci. Rev.,
221, 105863, https://doi.org/10.1016/j.quascirev.2019.105863, 2019.
Rades, E. F., Sohbati, R., Lüthgens, C., Jain, M., and Murray, A. S.:
First luminescence-depth profiles from boulders from moraine deposits:
Insights into glaciation chronology and transport dynamics in Malta valley,
Austria, Rad. Meas., 120, 281–289,
https://doi.org/10.1016/j.radmeas.2018.08.011, 2018.
Rahm, G.: Die Vergletscherung des Belchengebietes (Südschwarzwald) zur Würmeiszeit, E&G Quaternary Sci. J., 37, 31–40, https://doi.org/10.3285/eg.37.1.03, 1987.
Ramsay, A. C.: On the Glacial Origin of certain Lakes in Switzerland, the
Black Forest, Great Britain, Sweden, North America, and elsewhere, Quaterly
Journal of the Geological Society of London, 18, 185–204, 1862.
Reimer, P. J., Bard, E., Bayliss, A., Beck, J. W., Blackwell, P. G., Ramsey,
C. B., Buck, C. E., Cheng, H., Edwards, R. L., Friedrich, M., Grootes, P.
M., Guilderson, T. P., Haflidason, H., Hajdas, I., Hatté, C., Heaton, T.
J., Hoffmann, D. L., Hogg, A. G., Hughen, K. A., Kaiser, K. F., Kromer, B.,
Manning, S. W., Niu, M., Reimer, R. W., Richards, D. A., Scott, E. M.,
Southon, J. R., Staff, R. A., Turney, C. S. M., and van der Plicht, J.:
IntCal13 and Marine13 Radiocarbon Age Calibration Curves 0–50,000 Years cal
BP, Radiocarbon, 55, 1869–1887, https://doi.org/10.2458/azu_js_rc.55.16947, 2013.
Reznichenko, N. V., Davies, T. R. H., and Winkler, S.: Revised
palaeoclimatic significance of Mueller Glacier moraines, Southern Alps, New
Zealand, Earth Surf. Process. Landforms, 41, 196–207,
https://doi.org/10.1002/esp.3848, 2016.
Rixhon, G., Briant, R. M., Cordier, S., Duval, M., Jones, A., and Scholz,
D.: Revealing the pace of river landscape evolution during the Quaternary:
recent developments in numerical dating methods, Quaternary Sci. Rev., 166,
91–113, https://doi.org/10.1016/j.quascirev.2016.08.016, 2017.
Sawatzki, G.: Geologische Karte 1:25 000 von Baden-Württemberg.
Erläuterungen zu Blatt 8124 St. Blasien, Landesvermessungsamt
Baden-Württemberg, Stuttgart, 146 pp., 1992.
Schoeneich, P.: Comparaison des systèmes de légende français,
allemand et suisse, in: Cartographie géomorphologique – Cartographie des
risques. Actes de la Réunion annuelle de la Société Suisse de
Géomorphologie, 19 au 21 juin 1992 aux Diablerets et à Randa, edited
by: Schoeneich, P. and Reynard, E., Travaux et recherches, 9, Institut de
Géographie Lausanne, Lausanne, 15–24, 1993.
Schreiner, A.: Geologische Karte von Freiburg i. Br. und Umgebung 1:50 000,
1st edn., Geologisches Landesamt Baden-Württemberg, Freiburg i. Br.,
1977a.
Schreiner, A.: Quartär, in: Erläuterungen zur Geologischen Karte von
Freiburg i. Br. und Umgebung 1:50 000, 1st edn., edited by: Geologisches
Landesamt Baden-Württemberg, Landesvermessungsamt Baden-Württemberg,
Stuttgart, 174–198, 1977b.
Schreiner, A.: Quartär, in: Geologische Karte von Baden-Württemberg
1:25 000. Erläuterungen zu Blatt 8114 Feldberg, 1st edn., edited by:
Geologisches Landesamt Baden-Württemberg, Landesvermessungsamt
Baden-Württemberg, Stuttgart, 67–95, 1981a.
Schreiner, A.: Quartär, in: Erläuterungen zur Geologischen Karte von
Freiburg im Breisgau und Umgebung 1:50 000, 2nd edn., edited by: Geologisches
Landesamt Baden-Württemberg, Landesvermessungsamt Baden-Württemberg,
Stuttgart, 174–199, 1981b.
Schreiner, A.: Quartär, in: Geologische Karte 1:25 000 von
Baden-Württemberg. Erläuterungen zu Blatt 8114 Feldberg, 2nd edn.,
edited by: Geologisches Landesamt Baden-Württemberg,
Landesvermessungsamt Baden-Württemberg, Stuttgart, 67–95, 1990.
Schreiner, A.: Quartär, in: Geologische Karte von Baden-Württemberg
1:50 000. Freiburg i. Br. und Umgebung. Erläuterungen, 3rd edn.,
Geologisches Landesamt Baden-Württemberg, Freiburg i. Br., 174–199,
1996a.
Schreiner, A.: Geologische Karte von Baden-Württemberg 1:50 000.
Freiburg i. Br. und Umgebung, 3rd edn., Geologisches Landesamt
Baden-Württemberg, Freiburg i. Br., 1996b.
Schreiner, A.: Quartär, in: Geologische Karte von Baden-Württemberg
1:25 000. Erläuterungen zum Blatt 8014 Hinterzarten, edited by:
Wimmenauer, W. and Schreiner, A., Landesvermessungsamt
Baden-Württemberg, Stuttgart, 97–141, 1999.
Schreiner, A.: Quartär, in: Geologische Karte von Baden-Württemberg
1:25 000. Erläuterungen zu Blatt 8113 Todtnau, edited by: Landesamt
für Geologie, Rohstoffe und Bergbau (LGRB), Freiburg i. Br., 42–92,
2011.
Schreiner, A. and Wimmenauer, W.: Geologische Karte von
Baden-Württemberg 1:25 000. Blatt 8014 Hinterzarten, Landesamt für
Geologie, Rohstoffe und Bergbau, Freiburg i. Br., 1999.
Schrepfer, H.: Zur Kenntnis der Eiszeit im Wutachgebiet, Mitteilungen des
Bad. Landesvereins für Naturkunde und Naturschutz in Freiburg i. Br., 1,
469–473, 1925.
Schrepfer, H.: Glazialprobleme im westlichen Hochschwarzwald, Ber. Naturf.
Ges. Freiburg i. Br., 31, 161–210, 1931.
Steinmann, G.: Die Spuren der letzten Eiszeit im hohen Schwarzwalde, in:
Freiburger Universitätsprogramm zum siebzigsten Geburtstag seiner kgl.
Hoheit des Großherzogs Friedrich, Akademische Verlagsbuchhandlung von J. C. B. Mohr (Paul Siebeck), Freiburg and Leipzig, 188–226, 1896.
Steinmann, G.: Die Bildungen der letzten Eiszeit im Bereiche des alten
Wutachgebiets, Ber. d. Oberrhein. Geol. Ver., 35, 1–8, 1902.
Steinmann, G.: Die Eiszeit und der vorgeschichtliche Mensch, Aus Natur und
Geisteswelt, 302, B. G. Teubner, Leipzig, 1910.
Stokes, C. R., Tarasov, L., Blomdin, R., Cronin, T. M., Fisher, T. G.,
Gyllencreutz, R., Hättestrand, C., Heyman, J., Hindmarsh, R. C. A.,
Hughes, A. L. C., Jakobsson, M., Kirchner, N., Livingstone, S. J., Margold,
M., Murton, J. B., Noormets, R., Peltier, W. R., Peteet, D. M., Piper, D. J.
W., Preusser, F., Renssen, H., Roberts, D. H., Roche, D. M., Saint-Ange, F.,
Stroeven, A. P., and Teller, J. T.: On the reconstruction of palaeo-ice
sheets: Recent advances and future challenges, Quaternary Sci. Rev., 125,
15–49, https://doi.org/10.1016/j.quascirev.2015.07.016, 2015.
Telford, R. J., Heegaard, E., and Birks, H. J. B.: The intercept is a poor
estimate of a calibrated radiocarbon age, Holocene, 14, 296–298,
https://doi.org/10.1191/0959683604hl707fa, 2004.
Törnqvist, T. E., de Jong, A. F. M., Oosterbaan, W. A., and Van Der
Borg, K.: Accurate Dating of Organic Deposits by AMS 14C Measurement of
Macrofossils, Radiocarbon, 34, 566–577,
https://doi.org/10.1017/S0033822200063840, 1992.
van den Bogaard, P. and Schmincke, H.-U.: Laacher See Tephra: A widespread
isochronous late Quaternary tephra layer in central and northern Europe, GSA
Bulletin, 96, 1554–1571, https://doi.org/10.1130/0016-7606(1985)96<1554:LSTAWI>2.0.CO;2, 1985.
Wagner, K.: Geographic Information Systems and Glacial Environments, in:
Past Glacial Environments (Second Edition), edited by: Menzies, J. and van
der Meer, J. J. M., Elsevier, 503–536, 2018.
Westoby, M. J., Brasington, J., Glasser, N. F., Hambrey, M. J., and
Reynolds, J. M.: “Structure-from-Motion” photogrammetry: A low-cost,
effective tool for geoscience applications, Geomorphology, 179, 300–314,
https://doi.org/10.1016/j.geomorph.2012.08.021, 2012.
Wimmenauer, W. and Hüttner, R.: Geologische Karte von
Baden-Württemberg 1:25 000. Blatt 8013 Freiburg, Landesvermessungsamt
Baden-Württemberg, Stuttgart, 1968.
Wimmenauer, W., Liehl, E., and Schreiner, A.: Geologische Karte von
Baden-Württemberg 1:25 000. Blatt 8114 Feldberg, 2nd edn.,
Landesvermessungsamt Baden-Württemberg, Stuttgart, 1990.
Winkler, S.: Investigating Holocene mountain glaciations: a plea for the
supremacy of glacial geomorphology when reconstructing glacier chronologies,
Erdkunde, 72, 215–234, https://www.doi.org/10.3112/erdkunde.2018.03.04,
2018.
Winkler, S. and Hagedorn, H.: Lateralmoränen – Morphologie, Genese und
Beziehung zu Gletscherstandsschwankungen (Beispiele aus Ostalpen und
West-/Zentralnorwegen), Z. Geomorph. Supp., 113, 69–84, 1999.
Zienert, A.: Die Würm-Vereisung und ihre Rückzugsstadien im Westteil
des Hochschwarzwaldes, Z. Geomorphol., 17, 359–366, 1973.
Short summary
The Black Forest was covered by a 1000 km2 large ice cap during the last glaciation. Glacial landforms in the area north-west of the highest summit of the Black Forest, the Feldberg (1493 m above sea level), were investigated to select suitable sampling sites for dating glacial landforms in future studies. Some of the terminal moraines described in this study are mapped for the first time. The application of dating methods will provide insights into the chronology of the last glaciation.
The Black Forest was covered by a 1000 km2 large ice cap during the last glaciation. Glacial...