Cloth cultures in prehistoric Europe: the Bronze Age evidence from Hallstatt

Cloth cultures in prehistoric Europe is a post-doctoral fellowship project awarded to Susanna Harris by the British Academy from 2008-2011. The aim of the project is to bring together and examine evidence for textiles and animal skins in prehistoric Europe from the Neolithic and Bronze Age. A number of case studies are being examined as part of this project, including the Bronze Age Hallstatt salt mines. Here researchers working on these materials look at some of the similarities and difference between the techniques applied in their production and use in the mines as a way to understand their relationship in the past

Large‐scale mass movements recorded in the sediments of Lake Hallstatt (Austria)–evidence for recurrent natural hazards at a UNESCO World Heritage site

The Bronze to Iron Age underground salt mining complex of Hallstatt (Austria) is widely recognised for its cultural importance and wealth of archaeological artefacts. However, while the daily life in the salt mines is archaeologically well documented and environmental effects of the mining activity have been investigated recently, the impact of natural hazards on the prehistoric mining community is still poorly understood. For instance, while it is well established that the prehistoric underground mines have repeatedly been destroyed by large-scale mass movements, only little is known about the characteristics and extent of these events as well as about mass-movement recurrence during more recent times. To shed light on past mass-movement activity in the vicinity of the Hallstatt salt mines, we investigated sediment cores from adjacent Lake Hallstatt. Within the regular lake sediments we identified three large-scale event deposits, which are interpreted to originate from spontaneous or seismically induced mass movements in the mid-19th and late 9th century ce and the mid-4th century bce. While the age of the latter event is in good agreement with the abandonment of the famous Iron Age cemetery at Hallstatt, the younger events indicate that large-scale mass movements also occurred repeatedly during the Common Era

Hallstatt miners consumed blue cheese and beer during the Iron Age and retained a non-Westernized gut microbiome until the Baroque period

21openInternationalInternational coauthor/editorWe subjected human paleofeces dating from the Bronze Age to the Baroque period (18th century AD) to in-depth microscopic, metagenomic, and proteomic analyses. The paleofeces were preserved in the underground salt mines of the UNESCO World Heritage site of Hallstatt in Austria. This allowed us to reconstruct the diet of the former population and gain insights into their ancient gut microbiome composition. Our dietary survey identified bran and glumes of different cereals as some of the most prevalent plant fragments. This highly fibrous, carbohydrate-rich diet was supplemented with proteins from broad beans and occasionally with fruits, nuts, or animal food products. Due to these traditional dietary habits, all ancient miners up to the Baroque period have gut microbiome structures akin to modern non-Westernized individuals whose diets are also mainly composed of unprocessed foods and fresh fruits and vegetables. This may indicate a shift in the gut community composition of modern Westernized populations due to quite recent dietary and lifestyle changes. When we extended our microbial survey to fungi present in the paleofeces, in one of the Iron Age samples, we observed a high abundance of Penicillium roqueforti and Saccharomyces cerevisiae DNA. Genome-wide analysis indicates that both fungi were involved in food fermentation and provides the first molecular evidence for blue cheese and beer consumption in Iron Age Europe.openMaixner, Frank; Sarhan, Mohamed S; Huang, Kun D; Tett, Adrian; Schoenafinger, Alexander; Zingale, Stefania; Blanco-Míguez, Aitor; Manghi, Paolo; Cemper-Kiesslich, Jan; Rosendahl, Wilfried; Kusebauch, Ulrike; Morrone, Seamus R; Hoopmann, Michael R; Rota-Stabelli, Omar; Rattei, Thomas; Moritz, Robert L; Oeggl, Klaus; Segata, Nicola; Zink, Albert; Reschreiter, Hans; Kowarik, KerstinMaixner, F.; Sarhan, M.S.; Huang, K.D.; Tett, A.; Schoenafinger, A.; Zingale, S.; Blanco-Míguez, A.; Manghi, P.; Cemper-Kiesslich, J.; Rosendahl, W.; Kusebauch, U.; Morrone, S.R.; Hoopmann, M.R.; Rota-Stabelli, O.; Rattei, T.; Moritz, R.L.; Oeggl, K.; Segata, N.; Zink, A.; Reschreiter, H.; Kowarik, K

Hyperoxemia and excess oxygen use in early acute respiratory distress syndrome : Insights from the LUNG SAFE study

Publisher Copyright: © 2020 The Author(s). Copyright: Copyright 2020 Elsevier B.V., All rights reserved.Background: Concerns exist regarding the prevalence and impact of unnecessary oxygen use in patients with acute respiratory distress syndrome (ARDS). We examined this issue in patients with ARDS enrolled in the Large observational study to UNderstand the Global impact of Severe Acute respiratory FailurE (LUNG SAFE) study. Methods: In this secondary analysis of the LUNG SAFE study, we wished to determine the prevalence and the outcomes associated with hyperoxemia on day 1, sustained hyperoxemia, and excessive oxygen use in patients with early ARDS. Patients who fulfilled criteria of ARDS on day 1 and day 2 of acute hypoxemic respiratory failure were categorized based on the presence of hyperoxemia (PaO2 > 100 mmHg) on day 1, sustained (i.e., present on day 1 and day 2) hyperoxemia, or excessive oxygen use (FIO2 ≥ 0.60 during hyperoxemia). Results: Of 2005 patients that met the inclusion criteria, 131 (6.5%) were hypoxemic (PaO2 < 55 mmHg), 607 (30%) had hyperoxemia on day 1, and 250 (12%) had sustained hyperoxemia. Excess FIO2 use occurred in 400 (66%) out of 607 patients with hyperoxemia. Excess FIO2 use decreased from day 1 to day 2 of ARDS, with most hyperoxemic patients on day 2 receiving relatively low FIO2. Multivariate analyses found no independent relationship between day 1 hyperoxemia, sustained hyperoxemia, or excess FIO2 use and adverse clinical outcomes. Mortality was 42% in patients with excess FIO2 use, compared to 39% in a propensity-matched sample of normoxemic (PaO2 55-100 mmHg) patients (P = 0.47). Conclusions: Hyperoxemia and excess oxygen use are both prevalent in early ARDS but are most often non-sustained. No relationship was found between hyperoxemia or excessive oxygen use and patient outcome in this cohort. Trial registration: LUNG-SAFE is registered with ClinicalTrials.gov, NCT02010073publishersversionPeer reviewe

Anthropogene Einflüsse auf die Hochgebirgsumwelt im Holozän: Einblicke aus einer alpinen Bergbaulandschaft

Menschliche Begehung und Nutzung des Gebirgs- und Hochgebirgsraums reicht weit in die Vergangenheit zurück. Sedimentarchive, archäologische Quellen und Schriftzeugnisse dokumentieren die lange und vielfältige Beziehungsgeschichte zwischen menschlichen Gesellschaften und diesen Landschaften. In besonderer Detailgenauigkeit lassen sich diese Prozesse in der historischen Landschaft des österreichischen Salzkammerguts nachvollziehen. Doch die enge Verzahnung zwischen Mensch und Umwelt bzw. eng aufeinander abgestimmte sozioökologische Systeme treten uns überall dort in Gebirgsregionen entgegen, wo Menschen über einen längeren Zeitraum gesiedelt und gewirtschaftet haben. In Anbetracht des oft steigenden Drucks auf diese Landschaften ist die Integration einer historischen und interdisziplinären Perspektive für die Entwicklung nachhaltiger Nutzungskonzepte von fundamentaler Bedeutung. Anthropogenic influences on the high mountain environment in the Holocene: Human activity in mountain regions reaches back far into the past. Sediment archives, archaeological sources and written records document the long and varied history of human-environment relations in these landscapes. These processes can be traced back in particular detail in the landscape of the Austrian Salzkammergut. However, the close interrelationship between humans and the environment or closely integrated socio-ecological systems can be studied everywhere in mountainous regions where human communities were present for a long time. In view of the often increasing pressure on these landscapes, a historically informed and interdisciplinary framework for the development of sustainable landuse concepts is urgently neede

Biodeterioration Risk Threatens the 3100 Year Old Staircase of Hallstatt (Austria): Possible Involvement of Halophilic Microorganisms.

BACKGROUND:The prosperity of Hallstatt (Salzkammergut region, Austria) is based on the richness of salt in the surrounding mountains and salt mining, which is documented as far back as 1500 years B.C. Substantial archaeological evidence of Bronze and Iron Age salt mining has been discovered, with a wooden staircase (1108 B.C.) being one of the most impressive and well preserved finds. However, after its discovery, fungal mycelia have been observed on the surface of the staircase, most probably due to airborne contamination after its find. OBJECTIVE:As a basis for the further preservation of this valuable object, the active micro-flora was examined to investigate the presence of potentially biodegradative microorganisms. RESULTS:Most of the strains isolated from the staircase showed to be halotolerant and halophilic microorganisms, due to the saline environment of the mine. Results derived from culture-dependent assays revealed a high fungal diversity, including both halotolerant and halophilic fungi, the most dominant strains being members of the genus Phialosimplex (synonym: Aspergillus). Additionally, some typical cellulose degraders, namely Stachybotrys sp. and Cladosporium sp. were detected. Numerous bacterial strains were isolated and identified as members of 12 different genera, most of them being moderately halophilic species. The most dominant isolates affiliated with species of the genera Halovibrio and Marinococcus. Halophilic archaea were also isolated and identified as species of the genera Halococcus and Halorubrum. Molecular analyses complemented the cultivation assays, enabling the identification of some uncultivable archaea of the genera Halolamina, Haloplanus and Halobacterium. Results derived from fungi and bacteria supported those obtained by cultivation methods, exhibiting the same dominant members in the communities. CONCLUSION:The results clearly showed the presence of some cellulose degraders that may become active if the requirements for growth and the environmental conditions turn suitable; therefore, these microorganisms must be regarded as a threat to the wood

Linen twills from the Hallstatt salt mine re-dated

The unusual linen twill fragments found in the Hallstatt salt mine in Austria, previously assumed to date to the Bronze Age were radiocarbon dated to the Medieval period. Then new dating and reassessment of the possible find context of the two linen twills from Hallstatt has important implications for textile research as \u2013 up to now \u2013 these textiles have been counted among the oldest of their kind. They must now be excluded from the list of prehistoric finds

Large‐scale mass movements recorded in the sediments of Lake Hallstatt (Austria)–evidence for recurrent natural hazards at a UNESCO World Heritage site

The Bronze to Iron Age underground salt mining complex of Hallstatt (Austria) is widely recognised for its cultural importance and wealth of archaeological artefacts. However, while the daily life in the salt mines is archaeologically well documented and environmental effects of the mining activity have been investigated recently, the impact of natural hazards on the prehistoric mining community is still poorly understood. For instance, while it is well established that the prehistoric underground mines have repeatedly been destroyed by large‐scale mass movements, only little is known about the characteristics and extent of these events as well as about mass‐movement recurrence during more recent times. To shed light on past mass‐movement activity in the vicinity of the Hallstatt salt mines, we investigated sediment cores from adjacent Lake Hallstatt. Within the regular lake sediments we identified three large‐scale event deposits, which are interpreted to originate from spontaneous or seismically induced mass movements in the mid‐19th and late 9th century ce and the mid‐4th century bce. While the age of the latter event is in good agreement with the abandonment of the famous Iron Age cemetery at Hallstatt, the younger events indicate that large‐scale mass movements also occurred repeatedly during the Common Era.Freunde des Naturhistorisches Museums WienAustrian Science Fund http://dx.doi.org/10.13039/501100002428Austrian Academy of SciencesGerman Archaeological Institut

First molecular data on the human roundworm Ascaris lumbricoides species complex from the Bronze and Iron Age in Hallstatt, Austria

Abstract Palaeoparasitological studies can provide valuable information on the emergence, distribution, and elimination of parasites during a particular time in the past. In the prehistoric salt mines of Hallstatt, located in the Austrian Alps, human faeces have been conserved in salt. The aim of this study was to recover ancient DNA of intestinal parasites from these coprolites. Altogether, 35 coprolites from the Hallstatt salt mines, dating back to the Bronze Age mining phase (1158–1063 BCE) and the Iron Age mining phase (750–662 BCE), respectively, were analysed by microscopy and molecular methods. In 91% of the coprolite samples, eggs of soil-transmitted helminths (STH), namely of Trichuris and/or Ascaris were detected by light microscopy. The Ascaris eggs were exceptionally well preserved. For further analysis, DNA was extracted from the palaeofaecal samples and species-specific primers targeting different genes were designed. While amplification of Trichuris DNA remained unsuccessful, sequence data of A. lumbricoides species complex were successfully obtained from 16 coprolites from three different genes, the mitochondrial cytochrome c oxidase subunit 1 gene (cox1), the mitochondrial cytochrome B gene (cytB) and the mitochondrial NADH dehydrogenase subunit 1 gene (nadh1). Importantly, these included two Ascaris sequences from a coprolite from the Bronze Age, which to the best of our knowledge are the first molecular data of this genus from this period