Biological Characterisation of Haliclona (?gellius) sp.: Sponge and Associated Microorganisms

We have characterised the northern Pacific undescribed sponge Haliclona (?gellius) sp. based on rDNA of the sponge and its associated microorganisms. The sponge is closely related to Amphimedon queenslandica from the Great Barrier Reef as the near-complete 18S rDNA sequences of both sponges were identical. The microbial fingerprint of three specimens harvested at different times and of a transplanted specimen was compared to identify stably associated microorganisms. Most bacterial phyla were detected in each sample, but only a few bacterial species were determined to be stably associated with the sponge. A sponge-specific β- and γ-Proteobacterium were abundant clones and both of them were present in three of the four specimens analysed. In addition, a Planctomycete and a Crenarchaea were detected in all sponge individuals. Both were closely related to operational taxonomic units that have been found in other sponges, but not exclusively in sponges. Interestingly, also a number of clones that are closely related to intracellular symbionts from insects and amoeba were detected

Palaeoenvironmental control on distribution of crinoids in the Bathonian (Middle Jurassic) of England and France

Bulk sampling of a number of different marine and marginal marine lithofacies in the British Bathonian has allowed us to assess the palaeoenvironmental distribution of crinoids for the first time. Although remains are largely fragmentary, many species have been identified by comparison with articulated specimens from elsewhere, whilst the large and unbiased sample sizes allowed assessment of relative proportions of different taxa. Results indicate that distribution of crinoids well corresponds to particular facies. Ossicles of Chariocrinus and Balanocrinus dominate in deeper-water and lower-energy facies,with the former extending further into shallower-water facies than the latter. Isocrinus dominates in shallower water carbonate facies, accompanied by rarer comatulids, and was also present in the more marine parts of lagoons. Pentacrinites remains are abundant in very high-energy oolite shoal lithofacies. The presence of millericrinids within one, partly allochthonous lithofacies suggests the presence of an otherwise unknown hard substrate from which they have been transported. These results are compared to crinoid assemblages from other Mesozoic localities, and it is evident that the same morphological ad-aptations are present within crinoids from similar lithofacies throughout the Jurassic and Early Cretaceous

Saturated with meaning: peatlands, heritage and folklore

YesPeatlands have often been represented in cultural material as being dangerous and inhospitable places, partly based on post-medieval influences, but also partly based on elements of folklore which emphasise the ‘other-worldly’ and liminal nature of these environments. Using Ilkley Moor, West Yorkshire, as a case study, the role of heritage, folklore and cultural media in guiding perceptions of the landscape is explored. Contemporary society is more diversified than historic situations, and our review indicates that perceptions of heritage landscapes reflect this complexity. The use of the peatland by different groups is explored, before addressing the interconnected roles of folklore and archaeology in past, present and future engagement with this landscape.JP-ICH under Grant number AH/S006427/1

The English medieval first-floor hall: part 2 – The evidence from the eleventh to early thirteenth century

The concept of the first-floor hall was introduced in 1935, but Blair’s paper of 1993 cast doubt on many of those buildings which had been identified as such. Following the recognition of Scolland’s Hall, Richmond Castle as an example of a hall at first-floor level, the evidence for buildings of this type is reviewed (excluding town houses and halls in the great towers of castles, where other issues apply). While undoubtedly a number of buildings have been mistakenly identified as halls, there is a significant group of structures which there are very strong grounds to classify as first-floor halls. The growth of masonry architecture in elite secular buildings, particularly after the Norman Conquest, allowed halls to be constructed on the first floor. The key features of these are identified and the reasons for constructing the hall at this level – prestige and security – are recognized. The study of these buildings allows two further modifications to the Blair thesis: in some houses, halls and chambers were integrated in a single block at an early date, and the basic idea of the medieval domestic plan was already present by the late eleventh century