Roger,Bishop of salisbury,Chancellor and Justiciar of England,1102-113

Abstract

The discovery of several sections of a trefoiled arcade of 14th-century date at Coverham abbey is a major addition to sculpture from the English Premonstratensian houses. Discovered in a robber trench whilst resurfacing a courtyard, they can be linked to a panel reused in the gable of the Georgian house. When reconstructed, they show a trefoiled arcade with sculpted spandrels in the form of human figures. Positive identification of the figures is difficult, and they could be of Christ or apostles. While the arcade looks to have been part of a cloister arcade, there is the possibility that it formed part of the abbey laver, flanking the refectory doorway.     

The Earthworks of Brinklow,Lilbourne, and Earl’s Barton

Fyfield Hall, a timber-framed aisled hall in Essex, has been tree-ring dated to 1167–85. It was built with passing braces, notched lap joints and curved arcade braces, and underwent major repairs between 1391 and 1416, when the central arcade posts, arcade plates and braces were replaced, but, curiously, in a late twelfth-century style with passing braces. To repair the building in the archaic style might seem surprising, but tree-ring dating shows that such developments were not unusual. This study examines the building in detail and looks at later developments on the site.     

Excavations on Brightstone and Bowcombe Downs,Isle of Weight,Made in August 1854

Abstract

Not a single English Romanesque great cloister arcade survives in situ. Despite this, the existence of a number of 11th- and 12th-century rear walls, and the discovery of quantities of stonework likely to have originated in cloister arcades, make it possible to recover something of the likely appearance and character of the cloister in Anglo-Norman England. The following paper considers that evidence, and assesses how our understanding of the underlying topography and archaeology of Anglo-Norman cloisters might enable us to reconstruct their lost walks. It concludes with an appraisal of the chronology of English cloister building.     

A Carved Romanesque Springer with Voussoirs in Church House,Gloucester Cathedral

A Romanesque double-springer and five voussoirs, decorated with foliate carving and pellet, have been reused as a door-head in the ground floor of Church House, Gloucester Cathedral. The carved stones are illustrated, together with a reconstruction of the original double arch, which may have come from an early 12th- century pulpitum screen or the arcade of the first Norman cloister.     

Marble Pieces in the Romanesque Portal of Glory of the Santiago de Compostela Cathedral. New Data through a Multi-Analytical Approach

ABSTRACT

Probably the most important Romanesque artwork in Spain, the Portal of Glory of Santiago de Compostela is essentially made in granite, the most abundant stone in the NW of Iberia, with the only exception of five marble pieces. Different hypothesis on the origin of these marbles have previously been proposed based on visual assessment or by directly assuming a local source. To shed light on their quarry provenance, a multi-analytical study was performed combining polarized-light optical microscopy, cathodoluminescence microscopy, XRPD, SEM-EDS and stable C and O isotopes. The comparison of the results with the available databases reveals the use of marbles from the Estremoz Anticline (Portugal) in the three exquisitely carved columns strategically placed in the central arcade, whereas the other two pieces are local marbles, illustrating a more complex consumption of this noble material than that initially expected.     

Compton Castle

Abstract

One of the perennial problems in the study of medieval architectural sculpture is the lack of identifiable patrons. At the church of St Michael, Horwood (North Devon), however, the north aisle and chapel of c. 1400 can be firmly associated with the patronage of the Pollard family, in particular John Pollard and his wife Emma. This includes the north arcade of five bays with its four freestanding and two engaged columns, all of which bear carved capitals. It is likely that the building of this extension was intended to establish the Pollard family at Horwood as well as to commemorate the patrons. Thus the work carries a funereal/monumental air that is reflected in the choice of sculptural imagery which includes a skull, angels and hybrid monsters. This context provides new insight into the ways in which architectural images were perceived and used in the later Middle Ages, particularly with regards to the image of the mermaid.     

On some Anomalies Observable in the Earlier Styles of English Architecture

Excavations in the south range of the cloister of Bordesley Abbey have produced an unusual sequence. The construction scheme of the buildings to the south of the cloister arcade—centring on the refectory and kitchen—was piecemeal and took over two hundred years, from the later twelfth to early sixteenth centuries. At an early stage the range included timber (which may have been part of the original temporary structures) and stone buildings. In the fifteenth century there was a major change of use: the refectory became a workshop and dumping area while the kitchen was used for non-ferrous metalworking: these activities probably continued to the Dissolution. The implications of the excavations are considered in the context of the development of the cloister and then the precinct. The important evidence for adaptation and innovation is discussed in the light of work elsewhere in order to argue that the results have a relevance for other Cistercian houses and monasteries in general.     

The prediction of physique from the skeleton

This paper attempts to define the relation between (1) human skeletal measurements and (2) height, weight and physique indices. Admitted to the study were 686 men and women from five ethnic groups (White, Inuit, Gurkha, Bantu and San). In addition to height and weight, subjects had defined cranial and postcranial measurements taken using methods derived from clinical examination techniques. Measurements were checked for reliability. Skinfold callipers were used to allow for the thickness of soft‐tissues overlying bone widths. Adjustment factors were derived from radiological gold standards. Radiological measurements, adjusted for magnification, of the lumbar vertebrae from 42 subjects were also done. A correlation matrix was constructed for the complete study population and all variables to allow a preliminary assessment of useful predictive independent variables. Discriminant scores for classification by gender were calculated. Regression computations, using least square regression, were calculated for six defined reference populations. The regression residuals were examined to confirm fulfilment of assumptions. The results indicated that skull and dental arcade variables yield little information about the size and physique of an individual but have some relevance for group comparisons. Long bone widths are moderately and equally correlated with height and weight. Lower limb bone widths are better correlated with body weight than those of the upper limb. The best predictive variables for body weight are the minimal ‘area’ of the lumbar vertebrae (L1–L4) and regressions involving various bone widths. It is confirmed that height correlates well with the lengths of long bones, but the prediction is improved by the addition of a width from the same bone as a second independent variable. Lower limb long bones are not better predictors of height than upper limb ones. The body mass index is best predicted from the available measurements by a regression with the minimal ‘area’ of L1 and the tibial length as independent variables. A lumbar vertebra, particularly L1, yields important information about height, weight and the body mass index. The patella width is, in part, a marker for mesomorphy. Reconstruction of the ankle to enable the width across the malleoli to be measured would yield useful estimates of weight and height. The findings have been applied to the Paviland femur. A provisional male attribution has been made. The derived height is similar to that of tall modern White men. The physique was probably mesomorphic and ectopenic, the physique of strength rather than mobility, but the confidence intervals are very wide. To enable this sort of assessment to be made more confidently, the study requires replication substituting the precision of magnetic resonance imaging for the relative imprecision of skeletal measurements taken directly from the intact body. Copyright © 1999 John Wiley & Sons, Ltd.     

Stable carbon and nitrogen isotope variations in tooth dentine serial sections from Wharram Percy

Here we report δ¹³C and δ¹⁵N measurements of serial sections of human deciduous and permanent tooth dentine from archaeological samples taken from the medieval village site of Wharram Percy, Yorkshire, UK. We found a pattern of enrichment, for both δ¹³C and δ¹⁵N, where the tooth crown was greater than the cervical part of the root, which in turn was greater than the apical portion of the root and the associated rib collagen values. This pattern reflects a decrease in the consumption of isotopically enriched breast milk and the introduction of less enriched weaning foods in the diet. The (mean±SD) difference between the deciduous second molar crowns and corresponding rib samples from the same individuals after 2 years of age was 1.2±0.4‰ for δ¹³C and 3.2±0.8‰ for δ¹⁵N. The δ¹⁵N values are as predicted, but as there were no C₄plants at Wharram Percy, this 1.2‰ enrichment in δ¹³C represents clear evidence of a carbon trophic level effect in collagen from breastfeeding infants. Carbon and nitrogen results also show that the infant diet among those who died in infancy did not differ from those who survived into childhood. This study demonstrates the promise of using dentine serial sections to study the temporal relationships of breastfeeding, weaning, and dietary patterns of single individuals.     

Quantitative analysis of COH fluids synthesized at HP–HT conditions: an optimized methodology to measure volatiles in experimental capsules

The quantitative assessment of COH fluids is crucial in modeling geological processes. The composition of fluids, and in particular their H₂O/CO₂ ratio, can influence the melting temperatures, the location of hydration or carbonation reactions, and the solute transport capability in several rock systems. In the scientific literature, COH fluids speciation has been generally assumed on the basis of thermodynamic calculations using equations of state of simple H₂O–nonpolar gas systems (e.g., H₂O–CO₂–CH₄). Only few authors dealt with the experimental determination of high‐pressure COH fluid species at different conditions, using diverse experimental and analytical approaches (e.g., piston cylinder + capsule piercing + gas chromatography/mass spectrometry; cold seal + silica glass capsules + Raman). In this contribution, we present a new methodology for the synthesis and the analysis of COH fluids in experimental capsules, which allows the quantitative determination of volatiles in the fluid by means of a capsule‐piercing device connected to a quadrupole mass spectrometer. COH fluids are synthesized starting from oxalic acid dihydrate at P = amb and T = 250°C in single capsules heated in a furnace, and at P = 1 GPa and T = 800°C using a piston‐cylinder apparatus and the double‐capsule technique to control the redox conditions employing the rhenium–rhenium oxide oxygen buffer. A quantitative analysis of H₂O, CO₂, CH₄, CO, H₂, O₂, and N₂ along with associated statistical errors is obtained by linear regression of the m/z data of the sample and of standard gas mixtures of known composition. The estimated uncertainties are typically <1% for H₂O and CO₂, and <5% for CO. Our results suggest that the COH fluid speciation is preserved during and after quench, as the experimental data closely mimic the thermodynamic model both in terms of bulk composition and fluid speciation.     

Late Precambrian algal megafossils Chuaria and Tawuia in some areas of eastern China

Chuaria is widespread in Late Precambrian deposits throughout the world. In China it has been found in the Jingeryu Formation of Jixian County, Tianjin, and in its equivalents in eastern China including the Nanfen Formation of Liaoning and Jilin Provinces, and the Liulaobei Formation of Anhui Province. In the latter, Chuaria is associated with the genus Tawuia which Hofmann (in Hofmann & Aitken, 1979) described as algae of undertermined affinity and which is based on material from Canada. The glauconitic sandstone directly resting upon Chuaria-bearing greyish-green shale of the Jingeryu Formation in Jixian County has a K-Ar age of 0.899 Ga. This paper describes C. circularis Walcott, T. dalensis Hofmann and T. sinensis n. sp., and discusses the morphology, biological and taxonomic affinities, and age and geographic distribution of Chuaria. Because of the association of Chuaria and Tawuia in the Mackenzie Mountains, Canada, and also in the area of Shouxian County, Anhui Province, China, it is considered that Chuaria and Tawuia probably have close affinities. According to their general morphology and occurrence, both may be marine planktonic multicellular algae.     

Metaceratodus kaopen comb. nov. and M. wichmanni comb. nov., two Late Cretaceous South American species of an austral lungfish genus (Dipnoi)

Cione, A.L. & Gouiric-Cavalli, S., June 2012. Metaceratodus kaopen comb. nov. and M. wichmanni comb. nov., two Late Cretaceous South American species of an austral lungfish genus (Dipnoi). Alcheringa 36, 203–216. ISSN 0311-5518.

Metaceratodus wollastoni, an Australian species, was reported from Upper Cretaceous beds of Patagonia in 1997. Later, three new species (Ceratodus wichmanni, Ptychoceratodus kaopen and Ptychoceratodus cionei), based on scarce material, were described from the same region. Two of these species were later referred to Ferganoceratodus. After examining much more abundant and better-preserved material, we conclude that neither the occurrence of Metaceratodus wollastoni nor those of Ptychoceratodus and Ferganoceratodus in the Cretaceous of South America are supported. We consider that C. wichmanni and P. cionei are synonyms and we reassign the three putative species to Metaceratodus under two new combinations: M. kaopen comb. nov. and M. wichmanni comb. nov. Both differ from the other species of the genus in having pits over most of the occlusal surface and a different occlusal profile of the tooth plate, and most have four ridges in the lower and upper tooth plates. Metaceratodus wichmanni differs from M. kaopen in oclussal profile, inner angle, and symphysis development among other features. Metaceratodus kaopen is known from the upper Santonian–lower Campanian Anacleto Formation of Río Negro province and M. wichmanni from upper Campanian–lower Maastrichtian units of Chubut, Río Negro, Neuquén and Mendoza provinces, Argentina. The occurrence of Metaceratodus in southern South America corroborates a close biogeographical relationship with Australia in the latest Cretaceous.

Alberto Luis Cione [acione@museo.fcnym.unlp.edu.ar] and Soledad Gouiric-Cavalli [sgouiric@museo.fcnym.unlp.edu.ar], División Paleontología Vertebrados, Museo de La Plata, Paseo del Bosque s/n, W1900FWA La Plata, Argentina. Received 23.11.2010, revised 11.7.2011, accepted 7.8.2011.

     

New light on early caprine herding strategies from isotope analysis: a case study from Neolithic Anatolia

The measurement of stable carbon (δ¹³C) and nitrogen (δ¹⁵N) isotopes of caprine bone collagen from the Neolithic sites of Çatalhöyük and Aşıklı Höyük in south-central Anatolia have allowed examination of exploitation and herding practices of sheep and goats. The isotope values from protodomestic caprines at Aşıklı Höyük suggests that these animals were consuming very similar foods to each other and were all confined to the same or similar environments with no access to C₄ plants. At Çatalhöyük, the results show how the caprine management strategy develops from the strategy seen at Aşıklı Höyük into a more varied practice at an early stage as the site grows with an increasing dietary contribution obtained from C₄ plants. No change in diet is isotopically discernible at Aşıklı Höyük. Interestingly, no distinction could be made between the diets of sheep and goats at either site. Therefore, such studies are a useful method of examining the development of early herding or management strategies of caprines in the Near East.     

Stable oxygen (δO) and hydrogen (δD) isotopes in ovicaprid dentinal collagen record seasonal variation

Understanding paleoenvironmental conditions, including the frequency and amplitude of seasonal variation, is crucial to understanding a wide array of human behaviors in prehistory. In vertebrate calcified tissue, inorganic oxygen isotopes derived from apatite have been widely used as a proxy for paleoenvironment and seasonality in the archaeological record. However, organic sources of δ¹⁸O and δD in mineralized tissue have remained largely unexplored. Here we measure the oxygen (δ¹⁸O) and hydrogen (δD) composition of dentin collagen sequentially sampled from the lower cheek teeth of four modern ovicaprids from the Baga Gazar'in Chuluu (BGC) region of the Gobi Desert of Mongolia. A significant correlation between trends in hydrogen and oxygen isotope values within individual teeth was identified. The amplitude of isotopic variation observed in sampled tooth dentin is similar to the yearly range of hydrogen and oxygen isotopic variation observed in meteoric precipitation for the region. These data indicate that dentin collagen δ¹⁸O and δD isotopic values reflect seasonal variation in the organic oxygen and hydrogen isotopic composition of diet and ingested water. We argue that paired measurements of dentin collagen δ¹⁸O and δD appear to be reliable seasonal climatic indicators.     

Establishing the Public Sphere and Abolishing the Private Domain: The Rise of a Doctrine and Its Social Significance in the Spring and Autumn Period

The dominant views regarding the concepts of “the public” (gong) and “the private” (si) took shape in the Spring and Autumn period and matured in the succeeding years of the Warring States period. This paper is an attempt to trace both the growth of the vocabulary containing “gong” and “si” and the development of philosophical views regarding issues that center on the relation between the individual and the larger social/communal/political body, of which that individual is a member; it also touches on issues related to the proper handling of public affairs and the relation between state, sovereign, and the individual. The era is often characterized as “The Contention of the Hundred Schools of Thought,” notwithstanding it ended with but one view that is universally accepted by thinkers of diverse persuasion, namely, si is the source of all social evil and, therefore, should be condemned. This is the doctrine known as ligong miesi (abolishing si so gong may be established), which contributed to the orthodox for that era and the millennium to come. By extolling gong and condemning si, it painted a portrait of the pair as two irreconcilable norms or forces in social and political life; it provided a justification for the then emerging new social arrangement and ways of distribution of power and resources, and it also led to acute conflicts between the sovereign and the state, the ruled and the ruler, the state and the subject, as well as the public sphere and the private domain. Translated from Nankai Journal, Vols. 4, 5, 2004     

Opposing peace: English political pamphlets against the Treaty of Madrid in 1630

ABSTRACT

In November 1630 the Treaty of Madrid was signed between Philip IV, king of Spain, and Charles I, king of England. During the peace negotiations several pamphlets critical of the pro-Spanish policy of Charles I were printed in England. These publications contributed to the development of an increasing criticism of Charles I, by identifying his neutral European policy with pro-Spanish policies. The anti-Spanish and anti-Catholic rhetoric, which formed the basis of this criticism, was used to promote an aggressive foreign policy and consequently an active opposition to the king. The following pamphlets are discussed in this paper: Considerations T ouching a W arre with Spaine; The M erchandises of Popish P riests; The English Spanish Pilgrim; Further O bservations of the English Spanish Pilgrim; The P ractise of P rinces; The P resent E state of Spayne; and Three S everall T reatises C oncerning the T ruce.     

Dating the Ramat Saharonim Late Neolithic desert cult site

The Ramat Saharonim site, located in the central Negev desert, Israel, consists of four shrines in a shallow valley and 30 tumuli, aligned on two cuesta cliffs on the valley's sides. Previous assessments based on site surveys suggested a general chronological span from Late Neolithic period (ca. 5000–5500 BC) through the Early Bronze Age (third millennium BC). Excavations in one shrine and three tumuli revealed a well-constructed double wall at the shrine and seven primary adult burials in the three tumuli. Quartz from sediment samples post-dating the construction of the burials and shrine was dated by optically stimulated luminescence (OSL) using the single aliquot regenerative dose (SAR) protocol, and charcoal and leather samples were dated by ¹⁴C. The OSL results for a burial in one tumulus are 7500 ± 700 to 6000 ± 600 years. In a second tumulus, OSL ages of 2000 ± 200–1800 ± 170 years and a ¹⁴C age on leather of 390–200 BC (2340–2150 cal BP) imply that this burial is Nabatean and that the site was used also in the Hellenistic period. Two ¹⁴C ages on charcoal from the shrine give an age between 5280 and 4710 BC (7230–6660 cal BP). OSL single aliquot ages for sediment from the shrine are highly scattered and far too old (60,000 to 12,000 years). The unlikely old ages are due to insufficient resetting of the OSL signal of some of the quartz grains when sand was blown onto the site. Indeed, single grain measurements for six samples of sediment postdating the shrine show a very large range of grain ages, but with a distinct young population in all samples. Ages calculated from these young populations average 5400 ± 800, in better consistence with the ¹⁴C dates and confirming our supposition that only some of the transported grains were reset at the time of deposition. The combined OSL and ¹⁴C dating shows that the shrines and tumuli are contemporaneous and attributes the complex to the Late Neolithic. This has clear ramifications for our understanding of the period and the rise of desert pastoral societies.     

Late Silurian pentameride brachiopods from Yass and Molong,New South Wales

The five known species of pentameride brachiopods from the Yass Syncline Ludlow (LateSilurian) succession, belonging to the superfamilies Pentameroidea, Gypiduloidea and Clorindoidea, are fully revised; no new species are recognised. The pentameroids Conchidium sp. cf. hospes and Aliconchidium yassi are confined to the Bowspring Limestone Member (Silverdale Formation). The gypiduloid Ascanigypa glabra and externally homeomorphic clorindoids Barrandina wilkinsoni and Clorinda minor replace them in the overlying Barrandella Shale Member, the last two extending into the Yarwood Siltstone Member (Black Bog Shale). Clorinda minor is also possibly present in the Rainbow Hill Member (Rosebank Shale). All except C. minor are uncommon to rare components of the Yass brachiopod fauna. Clorinda molongensis, a species of uncertain mid- to late Silurian age from the Molong Limestone, is also revised. Aliconchidium and Barrandina are known only from Yass, whereas Clorinda is cosmopolitan. Conchidium alsois widespread, but C. hospes is a species from the Prague Basin probably also known from the Urals and the Tien Shan. Ascanigypa is another Prague Basin taxon, recently recognised in Arctic Canada.     

Early Carboniferous Siphonodella (Conodonta) faunas from eastern Australia

Early to Middle Tournaisian conodont faunas with Siphonodella from ten sections in eastern Australia, between Gloucester in New South Wales and Rockhampton in Queensland, may be referred to the following ‘standard’ zones; 1 sulcata, 2 upper duplicata, 3 sandbergi, 4 lower crenulata and 5 isosticha-upper crenulata, in ascending order. In eastern Australia the first occurrences of Gnathodus cuneiformis, G. delicatus, G. typicus and Protognathodus cordiformis, near the base of the lower crenulata zone, are significantly earlier than in Europe and North America. Consequently the base of the isosticha-upper crenulata zone in eastern Australia is defined by the first appearance of G. punctatus rather than that of G. delicatus. On the present evidence it is difficult to reconcile some brachiopod and conodont occurrences in the Early-Middle Tournaisian of eastern Australia.

Seventeen discrete conodont species are discussed, four of which are described informally: Dinodus sp. nov. A, Dinodus sp. nov. B, Pinacognathus sp. nov. A, and a species of Siphonodella transitional between S. cooperi and S. crenulata.     

Roman blue-green bottle glass: chemical–optical analysis and high temperature viscosity modelling

Chemical analysis, optical absorption spectroscopy and mathematical modelling of high temperature viscosity have been carried out on five 1st–2nd century AD Roman blue-green bottle glass fragments from Coppergate, York. Modelled viscosities indicate remarkable consistency within the sample set studied and support the suggestion that temperatures of ∼1000–1150 °C were required to remelt these glasses and to provide suitable viscosities for forming articles. Iron redox ratios (Fe²⁺/ΣFe), analysed SO₃ contents and the absence of characteristic Fe³⁺–S²⁻ amber absorption bands suggest that melting conditions for all studied glasses were mildly, rather than strongly, reducing (estimated pO₂ ≈ 10⁻¹–10⁻⁶ bar). These furnace conditions are consistent with the effects of combustion gases and carbonaceous matter contained in the raw materials.