Human and livestock faecal biomarkers at the prehistorical encampment site of Ullafelsen in the Fotsch Valley, Stubai Alps, Austria – potential and limitations
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Published:2022-02-23
Issue:4
Volume:19
Page:1135-1150
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ISSN:1726-4189
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Container-title:Biogeosciences
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language:en
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Short-container-title:Biogeosciences
Author:
Lerch Marcel, Bromm TobiasORCID, Geitner Clemens, Haas Jean Nicolas, Schäfer Dieter, Glaser Bruno, Zech Michael
Abstract
Abstract. The Ullafelsen at 1869 m above sea level (a.s.l.) in the Tyrolean Stubai
Alps next to Innsbruck is an important (geo)archeological reference site
for the Mesolithic period. Buried fireplaces on the Ullafelsen plateau were
dated at 10.9 to 9.5 ka cal BP and demonstrate together with thousands of
flint stone artifacts the presence of hunter-gatherers during the Early
Holocene. Grazing livestock has been a predominant anthropozoological impact
in the Fotsch Valley presumably since the Bronze Age (4.2–2.8 ka). In
order to study the human and/or livestock faeces input on the Ullafelsen, we
carried out steroid analyses on 2 modern ruminant faeces samples from cattle
and sheep, 37 soil samples from seven archeological soil profiles, and 9
soil samples from five non-archeological soil profiles from the Fotsch
Valley used as reference sites. The dominance of 5β-stigmastanol and
deoxycholic acid in modern cattle and sheep faeces can be used as markers
for the input of ruminant faeces in soils. The OAh horizons, which have
accumulated and developed since the Mesolithic, revealed high contents of
steroids (sterols, stanols, stanones and bile acids); the eluvial light layer (E (LL)) horizon
coinciding with the Mesolithic living floor is characterized by medium
contents of steroids. By contrast, the subsoil horizons Bh, Bs and BvCv
contain low contents of faecal biomarkers, indicating that leaching of
steroids into the podsolic subsoils is not an important factor. High content
of 5β-stigmastanol and deoxycholic acid in all soil samples gives
evidence for faeces input of ruminants. The steroid patterns and ratios
indicate a negligible input of human faeces on the Ullafelsen. In
conclusion, our results reflect a strong faeces input by livestock, rather
than by humans as found for other Anthrosols such as Amazonian dark earths.
Further studies need to focus on the question of the exact timing of faeces
deposition.
Funder
Deutsche Forschungsgemeinschaft
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics
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