Geochemical data from loess records at the archaeological site Kammern-Grubgraben, Lower Austria

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Hauptverfasser: Reiss, Lilian, Stüwe, Christian, Einwögerer, Thomas, Händel, Marc, Maier, Andreas, Meng, Stefan, Pasda, Kerstin, Simon, Ulrich, Zolitschka, Bernd, Mayr, Christoph
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Sprache:en
Veröffentlicht: PANGAEA 2022
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author Reiss, Lilian
Stüwe, Christian
Einwögerer, Thomas
Händel, Marc
Maier, Andreas
Meng, Stefan
Pasda, Kerstin
Simon, Ulrich
Zolitschka, Bernd
Mayr, Christoph
author_facet Reiss, Lilian
Stüwe, Christian
Einwögerer, Thomas
Händel, Marc
Maier, Andreas
Meng, Stefan
Pasda, Kerstin
Simon, Ulrich
Zolitschka, Bernd
Mayr, Christoph
collection Datos científicos de ciencias marinas y ambientales
contents Two loess sections from the Upper Palaeolithic site of Kammern-Grubgraben (Lower Austria) were analysed to test geochemical proxies, as well as radiocarbon data of different components for their reliability and consistency in an archaeological context. Only a reliable basal age (28.9  27.8 ka cal BP) was obtained from charcoal fragments derived from a tundra gley underlying the archaeological horizons and assigned to Greenland Interstadials 3 or 4. Grain size, organic and inorganic geochemistry, and stable isotopes of the fine organic fraction (13Corg) and of rhizoconcretions (13C, 18O) were analysed to provide information on palaeoenvironmental conditions. Low-resolution geochemical and sedimentological analyses document a humidity-related variability, while 13Corg values indicate a predominant C3 vegetation. High-resolution elemental variations derived from X-ray fluorescence scanning exhibit increasing Ca and decreasing Fe and Ti values indicating drier conditions towards the top. Secondary pedogenic carbonate concretions provide post-sedimentary (Holocene) ages and are not suitable for assessing climate and environmental changes for the Palaeolithic.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_943245
institution PANGAEA
language en
publishDate 2022
publisher PANGAEA
record_format pangaea
spellingShingle Geochemical data from loess records at the archaeological site Kammern-Grubgraben, Lower Austria
Reiss, Lilian
Stüwe, Christian
Einwögerer, Thomas
Händel, Marc
Maier, Andreas
Meng, Stefan
Pasda, Kerstin
Simon, Ulrich
Zolitschka, Bernd
Mayr, Christoph
14C dating; Last Glacial Maximum; secondary carbonates; Stable isotopes; Upper Palaeolithic; XRF-core scanning
Two loess sections from the Upper Palaeolithic site of Kammern-Grubgraben (Lower Austria) were analysed to test geochemical proxies, as well as radiocarbon data of different components for their reliability and consistency in an archaeological context. Only a reliable basal age (28.9  27.8 ka cal BP) was obtained from charcoal fragments derived from a tundra gley underlying the archaeological horizons and assigned to Greenland Interstadials 3 or 4. Grain size, organic and inorganic geochemistry, and stable isotopes of the fine organic fraction (13Corg) and of rhizoconcretions (13C, 18O) were analysed to provide information on palaeoenvironmental conditions. Low-resolution geochemical and sedimentological analyses document a humidity-related variability, while 13Corg values indicate a predominant C3 vegetation. High-resolution elemental variations derived from X-ray fluorescence scanning exhibit increasing Ca and decreasing Fe and Ti values indicating drier conditions towards the top. Secondary pedogenic carbonate concretions provide post-sedimentary (Holocene) ages and are not suitable for assessing climate and environmental changes for the Palaeolithic.
title Geochemical data from loess records at the archaeological site Kammern-Grubgraben, Lower Austria
topic 14C dating; Last Glacial Maximum; secondary carbonates; Stable isotopes; Upper Palaeolithic; XRF-core scanning
url https://doi.org/10.1594/PANGAEA.943245