Data


Found 44 datasets

Datasets Project Group Resources

Geodata of continuous and discontinuous permafrost during the last glacial maximum in Europe SFB806 doi Spatial Temporal

This geodata contains shapefiles of continous and discontinous permafrost during the last glacial maximum in Europe as published in Lehmkuhl et al. (accepted). The data is based on published maps (Andrieux et al., 2016; Ruszkiczay-Rüdiger and Kern, 2016; Vandenberghe et al., 2014). Further methodological information can be found in Lehmkuhl et al. (in press). A layer package file is included that can be used to obtain the same visual appearance as published. References Andrieux, E., Bertran, P.,...
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Geodata of paleochannels on dry continental shelves in Europe during the last glacial maximum SFB806 doi Spatial Temporal

To investigate potential source areas of loess during the last glacial maximum, dry continental shelfs and their paleochannels were mapped for Europe (Lehmkuhl et al., accepted). The shapefile of dry continental shelf after Willmes (2015) was modified, as it did not include areas covered by ice. The shapefile was expanded using the LGM glaciation (Ehlers et al., 2011). Additionally, it was aligned to fit the used country shapefile (www.naturalearthdata.com) of the loess map. A layer package file can be used...
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Geodata of northern timberline in Europe during the last glacial maximum SFB806 doi Spatial Temporal

This geodataset includes the northern timberline in Europe during the last glacial maximum as published in Lehmkuhl et al. (in press). It is based on Grichuk, 1992, but was modified. A layer package file can be used to obtain the same visual appearance as published. See further details in the publication. References Grichuk, V.P., 1992. Main types of vegetation (ecosystems) for the maximum cooling of the last glaciation., in: In: Frenzel, B., Pecsi, B. Velichko, A.A. (Eds.): Atlas of Palaeoclimates and...
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Geodata of European loess domains SFB806 doi Spatial Temporal

We present a new map of the distribution of aeolian sediments (mainly loess) and major potential source areas for Europe in Lehmkuhl et al. (in press). The map was compiled combining geodata of different mapping approaches. Most of the used geodata stems from accurate national maps of 27 different countries. Problematic aspects such as different nomenclatures across administrative borders were carefully investigated and revised. The result is a seamless map, which comprises pedological, geological, and...
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Geodata of alluvial fill and fluvial deposits in Europe during the last glacial maximum SFB806 doi Spatial Temporal

For the investigation of potential source areas of loess in Europe, alluvial fill and fluvial deposits were mapped. The mapping is based on different national and pan-European datasets. The methodological approach is reported in Lehmkuhl et al. (in press). This geodataset contains a shapefiles of "alluvial fill and fluvial deposits" according to the European loess map published by Lehmkuhl et al. (in press). A layer package file can be used to obtain the same visual appearance as published. ...
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Geodata of European loess, sandy loess and aeolian sand SFB806 doi Spatial Temporal

We present a new map of the distribution of aeolian sediments (mainly loess) and major potential source areas for Europe. The map was compiled combining geodata of different mapping approaches. Most of the used geodata stems from accurate national maps of 27 different countries. Problematic aspects such as different nomenclatures across administrative borders were carefully investigated and revised. The result is a seamless map, which comprises pedological, geological, and geomorphological data and can be...
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OSL data of the Balta Alba Kurgan loess-paleosol sequence, Romania SFB806 doi Spatial Temporal

This is the DRAC file (cf. Durcan et al., 2015) used for age calculation of the optically stimulated luminescence (OSL) dating data from the Balta Alba Kurgan loess-paleosol sequence in Romania. This dataset corresponds to the luminescence age data published in Scheidt et al. (2020). The sample names in the first column are encoded as follows: Profile-number_sample-number_protocol. So for example sample BAK1_1_IR50 gives the results of conventional IRSL at 50°C measurements for sample no. 1 in profile BAK1....
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Stable organic carbon and nitrogen isotope data for two loess-palaeosol sequences in the Carpathian Basin SFB806 doi Spatial

This proxy dataset corresponds to the article Pötter et al. (2020) and comprises geochemical data (stable organic carbon and nitrogen isotope ratios) of the loess-palaeosol sequences of Irig (Serbia) and Semlac (Romania) in the southern Carpathian Basin Reference Pötter, S., Schmitz, A., Lücke, A., Schulte, P., Obreht, I., Zech, M., Wissel, H., Zech, M., Marković, S.B. and Lehmkuhl F. (accepted). Middle to Late Pleistocene environments based on stable organic carbon and nitrogen isotopes of...
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Geodata of 'Loess distribution and related Quaternary sediments in the Carpathian Basin' SFB806 doi Spatial

This set of data depicts the distribution of loess and related Quaternary sediments in the Carpathian Basin. Using a Geographic Information System (GIS), we compiled a map showing the distribution of loess and related Quaternary sediments in the Carpathian Basin, with unprecedented detail. We vectorized and analyzed existing data (mainly from geological maps) and combined and transferred these into a common (loess) sediment classification system. This cross-border map shows the distribution of eolian...
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Paleoclimatic proxy data from the MIS3/2 transition recorded at the Bodrogkeresztúr loess-paleosol sequence in Northeast Hungary SFB806 doi Spatial

This proxy dataset corresponds to the published article Bösken et al. (2017) and comprises grain size, geochemical, geomagnetic and luminescence data of the Bodrogkeresztúr loess-paleosol sequence in northeastern Hungary. Reference Bösken, J., Obreht, I., Zeeden, C., Klasen, N., Hambach, U., Sümegi, P., and Lehmkuhl, F. (in press). High-resolution paleoclimatic proxy data from the MIS3/2 transition recorded in northeastern Hungarian loess. Quaternary International.
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Three climatic cycles recorded in a loess-paleosol sequence at Semlac (Romania) – implications for dust accumulation in south-eastern Europe doi Spatial

Recent investigations of the Semlac loess section in the south-eastern Carpathian Basin, which is situated at an undercut slope position on the right bank of the Mureş River in its lower reaches (Banat region, western Romanian), are presented and discussed. Dating back to marine isotope stage (MIS) 10, the more than 10 m thick loess sequence includes four fossil soil-complexes developed in homogenous and relatively fine silty loess. Because of the good preservation of the sediment, Semlac is regarded as a...
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The Crvenka loess-paleosol sequence (Vojvodina, Northern Serbia)- a record of continuous domination of the Late Pleistocene grasslands Spatial

In this study we present a comparison of two independent paleo-environmental evidences: novel n-alkane biomarkers and traditional land snails assemblages, associated with widely used proxy records such as the low field magnetic susceptibility, grain size and various isotopic and geochemical indices. These paleo-environmental proxy records provide evidence for the continued predominance of the different grassland vegetation types during the entire Late Pleistocene. The results presented in this study...
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