Brandbestattungen von der mittleren Donau bis zur Ägäis zwischen 1300 und 750 v. Chr.

In these conference proceedings particular attention is paid to the performance of burials and burial rites between 1300 and 750 BC. A change in burial customs took place in large parts of central Europe during the 13th century BC. The dead were no longer buried in inhumation graves – as was customary until then – but were burned and laid to rest in urns. This transformation of burial customs is probably connected to far reaching changes in society and religious beliefs

Bioinduced precipitation of barite and celestite in dolomite microbialites Examples from Miocene lacustrine sequences in the Madrid and Duero Basins, Spain

This paper provides an ancient analogue for biologically mediated celestite and barite formation in dolomite precipitating microbial mats developed in lacustrine environments during the Miocene. Barite and celestite occurrences were studied in three temporally and spatially separated sedimentary successions: S1 and S2 in the Madrid Basin and S3 in the Duero Basin. In S1, macrocrystalline selenite gypsum occurs as laterally continuous beds; in the two other successions (S2 and S3), calcite pseudomorphs of lenticular gypsum aggregates are hosted in dolomite beds as evidence for the former presence of this evaporite. In S1, only celestite is associated with dolomite. Celestite crystals occur as both intergrown clusters, concentrated in pockets likely created by the dissolution of intrasedimentary anhydrite precursors, and as single precipitates associated with dolomite masses that replace selenite gypsum. Celestite crystals are nucleated commonly on organic substances that are pervasively associated with them. In S2 and S3, scarce single celestite crystals are restricted to calcite pseudomorphs after gypsum, whereas barite is the sulphate precipitated in the pseudomorphs' surroundings. Barite is commonly present as patchy poikilotopic crystals which include microbial structures and is embedded in organic matter. Additionally, barite is found as a secondary precipitate within Ba-bearing feldspars. Feldspar weathering is, thus, envisaged as amajor source of barium at these sites. Petrographical, isotopic and compositional observations point out that the barite and celestite formation was not caused by abiological processes only. Rather, the patchy distribution of the sulphates, close links to organic matter with biogenic isotope signatures, and inclusion of microbial structures, such as biologically mediated dolomite, provides evidence for the involvement of microbes in the formation of the sulphates. The coprecipitation of barite and celestite with dolomite entails complex interactions between different microorganisms and reinforces the biological formation of dolomite in saline lakes

The Hoard of the Rings. "Odd" annular bread-like objects as a case study for cereal-product diversity at the Late Bronze Age hillfort site of Stillfried (Lower Austria)

Cereals, in addition to being a major ingredient in daily meals, also play a role in the preparation of foodstuffs for ritual purposes. This paper deals with finds that may correspond to such ritual preparations retrieved from the hillfort site of Stillfried an der March. The site, spreading across an area of ca. 23 ha, held a very important position among settlements of Late Urnfield period (particularly during the 10th– 9 th c. BCE), acting as a central place where large scale storage of grain as well as textile and metal production took place under the control of local elites. Three incomplete ring-shaped charred organic objects, found together with 14 rings and ring frag- ments made of clay were discovered in a secondary filled silo pit, excavated among a total of about 100 pits of this kind at the site. The overall good state of preservati on of the organic ring fragments suggests that they were deposited intact on the bottom of the pit and covered well so that no re-deposition or damage occurred. This could be indicate their intentional placement in this position. Light and scanning electron microscop y revealed that the charred organic rings are cereal products containing hulled barley and a wheat species. Indications that the objects were shaped from a wet cereal mixture and had been subsequently dried without baking are discussed, as well as the possible significance of the find assemblage. The annular objects are put in context with the contemporary cereal spectrum as well as other cereal preparation s from Stillfried, outlining their different chaıˆnes opératoires for handling cereal food