Data

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...

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...

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...

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. ...

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...

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....

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...

Luminescence age estimates and additional information about equivalen dose estimation and dosimetry. Optically stimulated luminescence and post infrared infrared stimulated luminescence applied to coarse-grained quartz and feldspar as well as polymineral fine grains from loess.

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...

The Carpathian Basin contains some of the best preserved loess deposits in Europe, including some of the continent's longest and best resolved climate records. Large areas of the basin have been intensively investigated in recent years, although deposits in the east remain largely unstudied, despite considerable regional variation in climate records. Here we discuss the sedimentary record exposed in the Orlovat brickyard using detailed litho- and pedo-stratigraphic, enviromagnetic parameters and...

The Paleolithic sites Romanesti and Cosava, situated at the foothills of the Banat Mountains in Romania, provide an important testament of life of the first European modern humans (Homo sapiens sapiens) during the Middle Pleniglacial. Even though these sites have been extensively excavated, little is known about the site formation of related loess-like sediments and soils. First luminescence data at the two investigated sections confirm sediments from the penultimate glacial period to the Holocene. ...

The Belontinac loess section is one of the southernmost loess-paleosol environmental archives for the Late Quaternary in Serbia. The climate at this site is intermediate between the continental and the Mediterranean realms, which makes this loess archive potentially highly sensitive to past climatic changes. This paper presents new insights into the paleoenvironmental history during the last glacial period in southern Serbia using grain size and isotope proxy data. The grain size parameters from the...