Data


Found 60 datasets

Datasets Project Group Resources

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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Luminescence dating results (unpublished data) project F2 and A3

Luminescence age estimates and additional information about equivalent dose estimation and dosimetry. Post infrared infrared stimulated luminescence dating applied to polymineral fine grains from lake sediments.
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Luminescence dating results (unpublished data) project F2 and B2

Luminescence age estimates and additional information about equivalent dose estimation and dosimetry. Post infrared infrared stimulated luminescence dating applied to polymineral fine grains from lake sediments.
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Luminescence dating results 2013-2017 (published and unpublished data) of project F2 and B1

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.
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Luminescence dating results 2013-2017 (published and unpublished data) of project F2 and C1

Luminescence age estimates and additional information about equivalent dose estimation and dosimetry. Optically stimulated luminescence and post infrared infrared stimulated luminescence applied to coarse-grained quartz and feldspar from cave and rock shelter deposits.
Keywords: GQT2 LRQ12
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Luminescence dating results 2013-2017 (published and unpublished data) of project F2 and C2

Luminescence age estimates and additional information about equivalent dose estimation and dosimetry. Optically stimulated luminescence and post infrared infrared stimulated luminescence applied to coarse-grained quartz and feldspar from fluvial deposits and cave sediments was measured.
Keywords: GQT2 LRQ12
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Luminescence dating results 2013-2017 (published and unpublished data) of project F2 and D1

Luminescence age estimates and additional information about equivalent 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 was measured.
Keywords: GQT2 LRQ12
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LumReader R package

A series of functions to estimate the detection windows of a luminescence reader based on the filters and the photomultiplier (PMT) selected. These functions also allow to simulate a luminescence experiment based on the thermoluminesce (TL) or the optically stimulated luminescence (OSL) properties of a material.
Keywords: LRQ1
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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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Three climatic cycles recorded in a loess-palaeosol sequence at Semlac (Romania) – implications for dust accumulation in the Carpathian Basin and the northern Hemisphere Spatial

Semlac is regarded as a key section for the Carpathian Basin because of the good preservation of the fine silt. The site is situated at the Mureş River in its lower reaches (Banat region, western Romanian). The more than 10 m thick loess sequence includes four fossil sol-complexes developed in homogenous relatively fine silty loess and dates back to marine isotope stage (MIS) 10. This setting offers possibilities to a) improve the understanding of the type and composition of the lowland loess sequences in...
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Erosion or age overestimation? – the Urluia loess-palaeosol sequence

Aeolian deposits, such as loess, are considered the ideal material for luminescence dating. However, recent studies have revealed problematic discrepancies between different grain size fractions of quartz (e.g., Timar-Gabor, 2015). Nevertheless, the emergence of the pIRIR protocol (e.g., Thiel et al. 2011) gives us another useful tool for the investigation of loess-paleosol sequences, especially in higher dose ranges. This poster presents the luminescence investigation of 13 fine grain samples from the...
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Comparison of fine grain quartz OSL and polymineral pIRIR measurements in the high dose range – examples from the Stalac loess-palaeosol sequence (Serbia)

The Stalać loess-palaeosol sequence (LPS) is located in the interior of the Central Balkan region, south of the typical loess distribution, in a zone of palaeoclimatic shifts between continental and Mediterranean climate regimes. Due to the scarcity of other LPS in this area, it is of interest for palaeoenvironmental studies and as such the geochronology is of uppermost importance. Six fine grain (4-11µm) samples of the section were investigated. Preheat plateau and dose recovery tests for one quartz...
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