Data


Found 7 datasets

Datasets Project Group Resources

Potential raw material sources for the production of lithic artefacts in western Central Europe - GIS-data for the Rhineland, Westphalia, and the Benelux countries doi

Since July 2013, the project D4 of the Collaborative Research Centre 806 at the University of Cologne has dealt with the Mesolithic in western Germany. During the first phase of this research, the primary tasks were to establish a regional chronology for the Middle Stone Age on the one hand, and the mapping of all known sites in the Rhineland and Westphalia regarding the different Mesolithic phases on the other. Since July 2017, the project has focused on mobility, cultural exchange, and human-environment...
d4 url PDF

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.,...
b1 d1 7z file

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...
b1 d1 7z

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...
b1 d1 7z file

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...
b1 d1 7z file

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. ...
b1 d1 7z file

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...
b1 d1 file