Notes,Documents, and Bibliographies

The New Propaganda boom; Philip M. Taylor     

Palaeolimnological impacts of early prehistoric farming at Lough Dargan,County Sligo,Ireland

This study provides a unique method of inquiry for archaeological investigation with an aim to assess the intensity and effects of Neolithic and Bronze Age farming practices at Lough Dargan, northwest Ireland, through a multi-proxy analysis of a lake sediment core. Chironomid (non-biting midge fly) subfossils and lake sediment geochemistry (δ¹³C, δ¹⁵N and C:N ratios) were used to assess changes in limnological conditions through time. The limnological data were compared with macroscopic charcoal concentration and pollen data to examine the potential influence that early farmers had on a freshwater lake system within a prehistorically active catchment. Results from the chironomid analysis show that the first substantial period of agricultural activity in the early Neolithic (c. 3730–3190 BC) resulted in a temporary shift to more eutrophic lake conditions. There is evidence of animal husbandry with substantial levels of animal waste reaching the lake, leaving an imprint in the geochemical record of increased δ¹⁵N values and decreased δ¹³C values and C:N ratios during this time. The chironomid community reverted back to its pre-impacted state c. 3190 BC in response to a period of reduced farming (c. 3390–3000 BC) which eventually led to a distinct lull in activity, with possible cessation of farming from 3000 to 2700 BC. A return to eutrophic conditions coincided with the gradual return of agriculture, with more permanently altered lake conditions dominating from 2400 BC, even during a 250-year period of reduced human activity commencing at c. 1440 BC. Increased sedimentation rate, along with increases in δ¹³C, δ¹⁵N and C:N, the presence of chironomid taxa indicative of erosion, more eutrophic lake conditions and high concentrations of macroscopic charcoal all point to more intensive land use practices during the Bronze Age. Palaeolimnological data exhibited an immediate response to intensified farming during this time, and were especially responsive to pastoral farming due either to scale of activity or proximity to the lakeside. The success of this study demonstrates the effectiveness of palaeolimnological analysis in the investigation of prehistoric farming. This approach will help inform Neolithic and Bronze Age land-use practice and human–environment relations in the region, and highlights the potential for chironomid-based archaeological research.     

A short-snouted trematosauroid (Tetrapoda,Temnospondyli) from the Early Triassic of Australia: the oldest known trematosaurine

The trematosauroid temnospondyl Tirraturhinus smisseni gen. et sp. nov. from the Arcadia Formation of central Queensland, Australia, is described on the basis of its rostrum. This is the first trematosaurine (short-snouted) trematosauroid from Australia, and is considered to be most closely related to Tertrema acuta from Spitzbergen. Tirraturhinus smisseni occurs alongside lonchorhynchine (long-snouted) trematosauroids in the Arcadia Formation; the co-occurrence of both trematosauroid morphotypes in that fauna is repeated in a number of non-marine Early Triassic faunas elsewhere in Pangaea. The Arcadia Formation is probably Griesbachian (earliest Triassic), so that T. smisseni is the oldest known trematosaurine.     

Eilert Sundt. A founding father of the social sciences in Norway

The cult of St Nicholas spread in Scandinavia and northern Rus' in approximately the same period, namely in the last decades of the 11th and the first decades of the 12th centuries. In spite of such a correspondence, the dissemination of the cult in the two adjacent regions has been treated as two separate phenomena. Consequently, the growing popularity of the cult in Scandinavia has traditionally been dealt with as an immanent part of the transmission of the Catholic tradition, and a similar phenomenon in northern Rus' has been discussed with reference to the establishment of Orthodox Christianity. By contrast, the evidence analysed in this article shows that the establishment of the cult of St Nicholas in the two regions was an intertwined process, in which the difference between Latin Christendom and Greek Orthodoxy played a minor role. The early spread of this particular cult thus suggests that, as far as some aspects of the cult of saints are concerned, the division between Catholicism and Orthodox Christianity in Northern Europe was less abrupt in the 11th and 12th centuries than has been traditionally assumed. This was due to the fact that the medieval cult of saints was not limited to the liturgy of saints, but was a wider social phenomenon in which political and dynastic links and cultural and trading contacts across Northern Europe often mattered more than confessional differences. When we leave the liturgy aside and turn to kings, princes, traders and other folk interacting across the early Christian North, then the confessional borders are less useful for our understanding of how some aspects of Christian culture were communicated across Northern Europe in the first two centuries after conversion.     

Marcusodictyon Bassler from the Lower Ordovician of Estonia: not the earliest bryozoan but a phosphatic problematicum

Marcusodictyon priscum (Bassler 1911) from the Tremadocian Ungulite Sandstone (A2) of Jegelecht Falls, Estonia, is redescribed following SEM study of type and other specimens. The fossil consists of a polygonal network of low ridges known to exist only on the exterior surfaces of valves of the inarticulate brachiopod Obolus. Electron microprobe analysis demonstrates that, like its host substratum, Marcusodictyon is composed of calcium phosphate. This, together with the detailed morphology and dimensions of the ridge system, is used to negate Bassler's assignment of the genus to the ctenostome Bryozoa. Instead Marcusodictyon resembles the Silurian problematicum Gochtia Eisenack. The inferred growth pattern of Marcusodictyon suggests that it may have been a symbiont of a living brachiopod.