Lower Ordovician trilobites from the Septembersø formation,North-East Greenland

McCobb, L.M.E., Boyce, W.D., Knight, I. & Stouge, S., 2014. Lower Ordovician trilobites from the Septembersø formation, North-East Greenland. Alcheringa 38, 575–598. ISSN 0311-5518.

The informally named Septembersø formation is a 76 m thick succession of microbial and peritidal shelf carbonates deposited on the North-East Greenland shelf of Laurentia. The formation, assigned to the lower part of the Cape Weber Formation in all previous studies, lies disconformably upon the Skullrockian Antiklinalbugt Formation (revised) and conformably below the Tulean to Blackhillsian Cape Weber Formation (revised) in the Fimbulfjeld Group. With the exception of Randaynia, the modest trilobite fauna recovered from the Septembersø formation consists exclusively of bathyurids, and all represent new species. Both Chapmanopyge knudseni sp. nov. and Punka adamsi sp. nov. are represented by sufficient material to merit specific names. The remaining taxa, belonging to Bolbocephalus, Peltabellia, Randaynia and Chapmanopyge are left in open nomenclature. The trilobite genera present suggest that the Septembersø formation is referable to the Tulean Stage of the Ibexian Series, latest Tremadocian/earliest Floian in Global Standard terms.

Lucy M. E. McCobb [lucy.mccobb@museumwales.ac.uk], Department of Natural Sciences, National Museum of Wales, Cathays Park, Cardiff CF10 3NP, UK; W. Douglas Boyce [dougboyce@gov.nl.ca] and Ian Knight [ianknight@gov.nl.ca], Geological Survey, Newfoundland and Labrador Department of Natural Resources, PO Box 8700, St. John’s, NL, Canada A1B 4J6; Svend Stouge [svends@snm.ku.dk], Natural History Museum of Denmark (Geological Museum), Øster Voldgade 5–7, DK-1350 Copenhagen K, Denmark.     

Changing Notions of Authenticity: Presenting a Castle Over Four Centuries

Bolsover Castle is a 17th‐century mock‐medieval castle built for the Cavendish family. First impressions suggest that its Pillar Parlour has survived with little alteration for nearly four centuries. In reality, there have been minor but telling changes to its fabric. The 18‐century Cavendishes venerated the castle as a shrine to their ancestors. Bolsover’s 19th‐century tenants recreated a romantic Olden Time appearance. The public bodies responsible for the castle in the 20th century used archaeology to reconstruct its 17th‐century form. In each case, these custodians aimed to present the site ‘authentically’, but their work reveals their own contemporary readings of the castle’s history. This evidence, gathered for a Conservation Plan, allowed English Heritage’s re‐display of the castle (1996–2001) to take a more reflective and positive approach to creating new meanings. This use of history to create local important meanings should give good cheer to those managing similar small but significant sites across the world.     

Dendrochemical analysis of a tree-ring growth anomaly associated with the Late Bronze Age eruption of Thera

The most marked tree-ring growth anomaly in the Aegean dendrochronological record over the last 9000 years occurs in the mid 17th century BC, and has been speculatively correlated with the impact of the Late Bronze Age eruption of Thera (Santorini). If such a connection could be proved it would be of major interdisciplinary significance. It would open up the possibility of a precise date for a key archaeological, geological and environmental marker horizon, and offer a direct tie between tree-ring and ice-core records some 3600 years ago. A volcanic explanation for the anomaly is highly plausible, yet, in the absence of a scientifically proven causal connection, the value of the proposed correlation is limited. In order to test the hypothesis, dendrochemical analysis via Synchrotron Radiation Scanning X-ray Fluorescence Microscopy (SXFM), Inductively Coupled Plasma Atomic Emission Spectroscopy (ICP-AES) and Inductively Coupled Plasma Mass Spectroscopy (ICP-MS) was carried out on growth-ring series from four trees displaying the anomaly. Increases of sulfur, calcium, and rare earth elements following the onset of altered growth, plus concentration spikes of zinc and hafnium in the first affected growth-ring provide promising new evidence in support of a volcanic causal factor. Although a volcanic association is implied, the new data are not sufficient to prove a link to the exact eruption source.     

A Feminist Network in an Artists’ Home: Mary and George Watts,George Meredith,and Josephine Butler

This interdisciplinary, historicist-feminist paper (combining literary and art historical perspectives as well as an awareness of historical context and an application of recent feminist theory) explores the feminist affiliations of the Victorian artists Mary and George Watts, focusing specifically on their close friendships with the writer and women’s suffrage supporter George Meredith and the women’s rights worker Josephine Butler. It introduces the Wattses’ own anti-patriarchal conjugal creative partnership before investigating their relationships with Meredith and Butler through a reading of Mary Watts’s unpublished and hitherto untranscribed diaries (which record their interactions) as well as a discussion of George Watts’s paintings (particularly his portraits of Meredith and Butler in his ‘Hall of Fame’). This paper thus offers an unprecedented insight into the Wattses’ personal and professional relationships as well as their progressive socio-political positions, reclaiming them as early feminists who were part of a wider emergent feminist community. This paper’s discussion of the Wattses, Meredith, and Butler provides new perspectives on the connections, works, and views of these public literary, artistic, and feminist figures as well as the ways in which they supported and promoted the women’s rights movement that escalated over the course of the second half of the nineteenth century. It thus offers a fuller understanding of these figures as well as of the rise of early feminism in the Victorian period.     

Reconstruction of the Late Glacial and Early Holocene landscape and human presence in Lubrza,Western Poland,on the basis of multidisciplinary analyses

This paper presents the results of a multidisciplinary study that combines archaeological and palaeoenvironmental research to examine the relationship between environment and human activities in Western Poland during the Late Glacial and Early Holocene. The study area lying within the young moraine landscape produced several Late Palaeolithic and Early Mesolithic sites, varied in terms of size and function. Analyses of pollen, plant macro-remains and molluscs accompanied by geomorphological investigations and supported by series of radiocarbon dates have enabled a detailed reconstruction of environment. It has shown that despite climatic fluctuations during the Allerød and Younger Dryas, the studied area provided favourable conditions for hunter-gatherer occupation. The presence of micro- and macroscopic charcoal, charred particles of herbaceous plants and charred mosses in peat deposits of former water bodies evidence various activities carried out by Federmesser and Swiderian groups, for example setting up camp-fires and deliberate burning of the local marsh vegetation. Usewear analyses of flint implements have revealed further traces of diversified human activities undertaken at examined sites. Most importantly, this article focuses on plant-based craft activities undertaken by hunter-gatherers, about which little has hitherto been known.