Abstract

The Ullafelsen at 1869 m a.s.l. in the Tyrolean Stubai Alps next to Innsbruck is an important (geo-)archaeological reference site for the Mesolithic period. Buried fireplaces on the Ullafelsen plateau were dated at 10.9–9.5 cal. kyrs BP and demonstrate together with thousands of flint stone artifacts the presence of hunter-gatherers during the Early Holocene. Most recently, we demonstrated the great potential of n-alkane and black carbon biomarkers for contributing to a better understanding of pedogenesis and landscape evolution. In order to study the importance of human and/or animals for occupation of this relevant geoarchaeological site, we carried out steroid and bile acid analyses on two modern faeces samples from cattle and sheep and on 37 soil samples from seven soil profiles at the Ullafelsen. The modern animal faeces show a dominance of 5β-stigmastanol and deoxycholic acid for ruminants (cattle and sheep), which is in agreement with literature data. The OAh horizons, which have accumulated and developed since the Mesolithic, revealed high contents of steroids and bile acids; the E (LL) horizon coinciding with the Mesolithic living floor is characterized by medium contents of steroids and bile acids. By contrast, the subsoil horizons Bh, Bs and BvCv contain low contents of faecal biomarkers indicating that leaching of steroids and bile acids into the podsolic subsoils is not an important factor. Deoxycholic acid is the most abundant bile acid in all soil samples and gives evidence for strong faeces input of ruminants. The steroid and bile acid patterns and ratios indicate a negligible input of human faeces on the Ullafelsen. β-Sitosterol as plant-derived steroid has also a strong influence on the faecal biomarker pattern in our soils. Root input into the subsoils is likely reflected by β-sitosterol contents. In conclusion, our results reflect a strong faecal 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.

Highlights

  • 35 Archaeological research in high mountain regions received increasing attention during the last decades

  • This study presents the first results of faecal biomarker analyses carried out on the prehistorical encampment site of Ullafelsen, 370 Fotsch Valley, Austria

  • Steroid and bile acid patterns of contemporary ruminants showed a dominance of 5β-stigmastanol, whereas epi-5β-stigmastanol as degradation product of 5β-stigmastanol has to be considered for sheep

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Summary

Introduction

35 Archaeological research in high mountain regions received increasing attention during the last decades. Concerning the Tyrolean Alps, the Mesolithic site of Ullafelsen (1869 m a.s.l.) in the Fotsch Valley was discovered by the archaeologist Dieter Schäfer in 1994 and became an important archaeological reference site (Schäfer, 2011a, 2011b) (Figs. and 2). At this site, thousands of archaeological artifacts and many buried fireplaces were found. Previous archaeological 45 research demonstrates that the Ullafelsen was used as a summer camp by Mesolithic hunter-gatherers during the Preboreal and Boreal from around 10.9 to 9.5 kyrs BP (Schäfer, 2011a)

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