WissKI is a free and open source virtual research environment based on the free and open source content management system Drupal. It features everything that the content management system provides while using a triplestore for authorative data storage. Thus changes can be made in the triplestore and they are directly reflected by the system. Furthermore WissKI provides all features that are necessary for a full Linked Open Data Semantic Web platform.

Hedeby was the largest town in the Viking North. Investigations have identified imports at the site from central and northern Scandinavia revealing long-distance connections. The chronology of this trade, however, is unclear. Here, the authors use a typological-biomolecular approach to examine connections during the early Viking Age. The application of ZooMS to an assemblage of antler combs, stylistically dated to the ninth century AD, reveals nearly all were made of reindeer antler. As most craft production waste from Hedeby comprises red deer antler, it is argued that these combs were manufactured elsewhere, perhaps hundreds of kilometres further north. The results have implications for understanding of production and regional connectivity in early medieval Scandinavia.

AbstractMany museums deal with socio‐scientific issues—meaning topics with multiple perspectives and ongoing research, such as climate change, vaccinations, or livestock farming. As important and trusted sources of science education, museums can play a critical role in raising awareness about such issues. They tend to highlight the various perspectives on the topic and thereby are able to provide a balanced and impartial information presentation. Visitors are therefore confronted both with views that correspond to their own beliefs and with views that contradict their beliefs and are supported in developing an informed opinion on the respective topic. In our study, we used an experimental exhibition on the topic “animal husbandry” to investigate the extent to which, first, an exhibition visit in general and, second, how different picture captions affect knowledge acquisition and interest. We chose a between‐subjects design with the factor conflict framing through picture captions. Whereas one group visited an exhibition in which the picture captions were formulated neutrally, another group read picture captions that emphasized the existing conflict. A control group, which did not visit the exhibition at all, allowed us to examine the general effect of the exhibition. As dependent variables, we chose interest and knowledge acquisition as common instruments of educational visitor research. However, we went one step further and used an innovative instrument: visitors' argument repertoire. We found that visiting the exhibition led to higher interest, knowledge acquisition, and a more balanced argument repertoire. Varying the captions had no significant effect. Implications and limitations are discussed.

Over the last glacial period, the climate of the Northern Hemisphere experienced numerous abrupt variations on millennial to centennial timescales known as Dansgaard-Oeschger events. These events, characterised by rapid warming at the beginning of interstadials and gradual cooling back to stadial conditions are best documented in Greenland ice cores and North Atlantic marine records, while their propagation onto the continents and potential feedbacks are less well documented. In this context, loess palaeosol sequences in central Europe are valuable archives, often recording these climatic changes in the form of brown soils and tundra gley horizons - indicating milder interstadial conditions - intercalated with primary loess deposits reflecting cold stadial conditions.To reconstruct palaeoclimate changes at high resolution we use singular material from loess sediments: fossil earthworm calcite granules (ECG). ECGs, composed of aggregated sparite crystals formed in the calciferous earthworm glands, are secreted daily at the soil surfacemostly by Lumbricus species and experience limited vertical mixing within the loess sedimentary column. ECGs are thus an excellent terrestrial material for palaeoclimate reconstructions using stable isotopic geochemistry and radiocarbon dating. ECGs have been collected from two temporally overlapping loess-palaeosol sequences along an NNW-SSE transect in the Rhine River valley of western Germany. We present warm-season land-surface temperature and precipitation estimates at millennial timescales spanning ~ 45-22 cal kBP (late OIS 3 - OIS 2).  We demonstrate that OIS 3-2 climate in the Rhine Valley was significantly cooler during the warm season and overall drier with annual precipitation reduced by up to 70%, compared to the present day. Interstadials were only slightly warmer (1-4°C) than stadial indicating strong attenuation compared to Greenland records. In combination with mesoscale wind and moisture transport modelling we can show that this region was dominated by westerlies and thereby inextricably linked to North Atlantic climate forcing.The approach combining high-resolution age-depth modelling and geochemical proxy-based climate reconstruction can be readily adopted at other loess palaeosol sequences. We envisage a widespread application of this approach that would improve our understanding of regional variability over the European continent in response to North Atlantic climate changes over millennial to centennial timescales.

AbstractThis paper represents a study of archaeological fish remains retrieved from the excavations conducted by C. S. Phillips between 1993 and 2001 at Kalbāʾ 4 (Emirate of Sharjah, UAE). Kalbāʾ 4 is a major coastal site that was continuously occupied from the Umm an‐Nar period to the Iron Age (c. 2700–600 BCE). The site is of particular interest regarding monumental architecture, pottery studies and exchange networks across Arabia and its neighbouring regions from the Bronze Age onwards. A corpus of about 5500 fish remains provides information on fishing economies during the entire occupation of the site. Data regarding fish complement results previously obtained from the study of other fauna including marine molluscs, sea turtles, terrestrial and marine mammals. They allow us to document a fishing‐based economy at Kalbāʾ 4. The results highlight the exploitation of a quite limited range of fish taxa associated mostly with reef areas (groupers, trevallies, snappers, spangled emperors, King soldierbreams), brackish waters (mullets) and the open sea (scombrids). The techniques seem to have mainly involved the use of baited lines from boats, fishing nets and possibly cage traps. The discussion includes comparisons with the other main fish studies conducted for the Bronze Age and the Iron Age in Eastern Arabia.

Abstract Widespread permafrost thaw is underway as arctic regions warm at twice the rate of the global average. Greenhouse gases (methane and carbon dioxide) released from thawing organic-rich permafrost soils contribute to a positive feedback loop that further accelerates global warming. There is an urgent need to understand the relationship between past permafrost conditions and palaeoclimatic change, to better predict present permafrost response to ongoing and future climate change. Through sulfur isotope analysis (δ34S) of radiocarbon-dated bone collagen samples spanning the last 50,000 years, we have identified what we term a high-magnitude Late Pleniglacial Sulfur Excursion (LPSE) in Eurasia. This anomaly is geographically widespread and several orders of magnitude higher than the sulfur isotope variation previously attributed to changing animal origin or diet alone. We show that a major change in the terrestrial sulfur cycle related to continental-scale environmental processes are, in this context, representing changing permafrost conditions. Sulfur isotope analysis of faunal samples offer an unrivalled prospect of developing high-resolution, tightly chronologically-constrained records of past permafrost change in relation to global climate changes. This would inform on the sensitivity of permafrost to past climate change, enabling constraints to be put on modelled responses of present‐day permafrost to future climate change. More broadly, our findings indicate animal δ34S values may reflect local environmental conditions, complicating the use of δ34S values as a tool for food origin, animal migration, and archaeological palaeodiet and mobility research.

Nitrogen isotope ratio analysis (δ15N) of animal tissue is widely used in archaeology and palaeoecology to investigate diet and ecological niche. Data interpretations require an understanding of nitrogen isotope compositions at the base of the food web (baseline δ15N). Significant variation in animal δ15N has been recognised at various spatiotemporal scales and related to changes both in baseline δ15N, linked to environmental and climatic influence on the terrestrial nitrogen cycle, and animal ecology. Isoscapes (models of isotope spatial variation) have proved a useful tool for investigating spatial variability in biogeochemical cycles in present-day marine and terrestrial ecosystems, but so far, their application to palaeo-data has been more limited. Here, we present time-sliced nitrogen isoscapes for late Pleistocene and early Holocene Europe (c. 50,000 to 10,000 years BP) using herbivore collagen δ15N data. This period covers the Last Glacial-Interglacial Transition, during which significant variation in the terrestrial nitrogen cycle occurred. We use generalized linear mixed modelling approaches for interpolation and test models which both include and exclude climate covariate data. Our results show clear changes in spatial gradients of δ15N through time. Prediction of the lowest faunal δ15N values in northern latitudes after, rather than during, the Last Glacial Maximum is consistent with the Late Glacial Nitrogen Excursion (LGNE). We find that including climatic covariate data does not significantly improve model performance. These findings have implications for investigating the drivers of the LGNE, which has been linked to increased landscape moisture and permafrost thaw, and for understanding changing isotopic baselines, which are fundamental for studies investigating diets, niche partitioning, and migration of higher trophic level animals.