The craniology and relationships of four species of Bos II. Basic craniology: Bos taurus L. Proportions and angles

This paper is the second of a series on the craniology of four species of Bos. It is a further study of the skulls of British domestic cattle which are used in an attempt to establish a basic craniology for the genus. Part 1 (Grigson, 1974) dealt with nomenclature, material, history, age assessment and absolute size. This paper deals first with cranial proportions and then with cranial angles.The results show that the proportions of the skull depend on its size and, to a lesser extent, on its sex, cows having relatively narrow skulls, with short horncores, but sometimes longer horns than bulls. Cranial angles seem to be independent of size or sex, but are influenced slightly by age, and also, in some cases, strongly by breed.     

The biological and archaeological implications of the beetle Aglenus brunneus (Gyllenhal) in ancient faunas

The distribution and ecology, as far as they are known, of the Colydiid beetle Aglenus brunneus (Gyll.) are summarized and the significance of its records from archaeological sites considered. The supposition that A. brunneus originated in North America (Peyerimhoff, 1945) is questioned in the light of the ancient records. The species is used to illustrate some of the general principles and problems involved in the theoretical reconstruction of past environments from ancient faunas.     

The craniology and relationships of four species of Bos 3. Basic craniology: Bos taurus L. Sagittal profiles and other non-measurable characters

This paper is the third in a series on the craniology of four species of Bos and it is the last of the three papers in which the skulls of British domestic cattle are used in an attempt to establish a basic craniology for the genus. Part 1 (Grigson, 1974) dealt with nomenclature, material, history, age assessment and absolute size. Part 2 (Grigson, 1975) dealt with cranial proportions and angles. This paper deals first with sagittal profiles and then with other non-measurable characters.Sagittal profiles may be rounded or pointed with some intermediate forms. The rounded shape (an infantile character) persists throughout life in some breeds and is unaffected by age, sex or size. The pointed form develops with age in some breeds and is probably more marked in older and larger animals. Seventeen other minor characters are examined for the effects of age, sex, breed and size.     

Micromorphology of Pech-de-l'Azé II sediments

A micromorphological study of the sediments from the cave of Pech-de-l'Azé II using the terminology of Brewer (1964) was undertaken in order to describe them, to compare the results and their palaeoclimatic interpretations (e.g., Laville, 1973) with those of classical sedimentological analyses and to evaluate the role of micromorphology in the analysis of cave and rock-shelter deposits.The soil skeleton is composed of quartz sand and silt resulting principally from the decay of bedrock with local reworking by solifluction and ruissellement. Lithorelicts consist of bedrock fragments of cryoclastic origin and detrital phosphate grains which can be identified as being large carnivore (bear or hyaena?) coprolites. The plasma is composed of mostly iron rich clay and although it was most abundant in reddish layers of previously recognized soils, no micromorphological evidence for clay illuvation was found. The latter might have been caused by post-depositional destruction by freeze and thaw which produced the generally well developed banded fabrics in many of the beds. Free grain argillans occur sporadically but are particularly well developed on phosphate grains. Secondary calcite, occurring either in dispersed zones or as void calcitans and neocalcitans occurs throughout but is more marked in the upper layers and bed 6.Micromorphologically based palaeoclimatic interpretations agreed on the whole with those obtained by classical sedimentology although several questions were raised which should make us more cautious in interpreting “classical” data: such as the origin of the clay, especially in “soil” horizons. The advantages of micromorphology in delineating sequence of events were indicated.     

Food markets and shops in Manchester 1770–1870

It is one of the minor oddities of the recent “boom” in urban history that we know so little about so central an activity as how the people living in nineteenth-century towns bought their food. Of course, there are always a great number of subjects that we would like to know that little bit more about, but after all, the purchase of food did represent a half to two-thirds of working-class budgets for much of the nineteenth century. And we are a nation of shopkeepers! Yet until recently, the subject of food distribution within nineteenth-century industrial towns was a long way down the agenda of research topics. ^[2] We would like to think that this was not through lack of interest but was due to the authoritative nature of one major work on the subject, J. B. Jeffery's Retail trading in Britain, 1850–1950.     

Some aspects of change in flaked stone industries of the mesolithic and neolithic in Southern Britain

In a recent article, one of the writers suggested that the traditional bipartite division of the British Mesolithic, based on consideration of microlith types, was reflected in the shape of waste flakes (Pitts, 1978a). Four early assemblages were dominated by narrow flakes, in contrast to three later ones with a higher representation of broader flakes. In this paper, the originally tentative conclusions are explored in greater detail, and the next major boundary, the start of the Neolithic, is investigated. Related changes in the tool components are also examined and the outlines of an explanatory framework are proposed.     

The composition of the copper alloys used by the Greek,etruscan and Roman civilisations: 2. The Archaic,Classical and Hellenistic Greeks

This paper is the second dealing with the composition of copper alloys used by the Greeks. About 500 analyses of Archaic, Classical and Hellenistic objects are published here pp. 117–123 together with comments upon the alloys used. The data are arranged chronologically within broad limits and further subdivided typologically. The techniques of sampling and analysis are discussed in depth in the first part of this project (Craddock, 1976).The development of casting technology is one of the principal features of bronze-working during this period. Our knowledge of Greek casting technology comes both from archaeological excavation and from a careful examination of the castings themselves. Evidence from these sources has been brought together here for the first time together with the comments of medieval, renaissance, and modern technical authors to attempt a coherent picture of the way the superb Greek bronzes were produced and adorned.It was during this period that the Greeks started using mercury gilding on copper and bronze; and the techniques and range of gilded metal are discussed.     

The building cycle and the urban fringe in Victorian cities: another comment

In a recent debate in this Journal, Daunton and Whitehand engaged forces on the issue of building cycles and the urban fringe in Victorian cities.^[1] While eschewing detailed involvement in their discussion, certain points emerged which in the context of new evidence on the Scottish building cycle it may be useful to consider further.     

The social structure reflected in the Yuanjunmiao cemetery

This paper attempts an analysis of the burials of the Yuanjunmiao¹ cemetery in Shansi Province, China, where the author was in charge of archaeological excavation from 1958 to 1959, in terms of the social structure of the inhabitants at that time (Fig. 1).     

The corporate group as an archaeological unit

Although corporate groups have featured in the anthropological literature for a century, and have more recently been proposed as a potentially useful unit for archaeological analysis (L. Freeman, 1968, In Man the hunter, edited by R. Lee and I. De Vore, pp. 262–267. Aldine, Chicago), application of the concept in archaeology has largely remained hypothetical, and little theoretical modeling has been attempted. In spite of this neglect, it is argued here that the corporate group is potentially one of the most useful and important aspects of the archaeological record that can be dealt with. This conclusion is derived from a detailed ethnoar-chaeological analysis of over 150 households in the Maya Highlands, in which it became apparent that social, economic, and demographic characteristics of households were only loosely associated with a wide variety of material culture expressions. In contrast, such inferences seemed to be much more reliable when households were grouped into “hypothetical corporate groups” and group averages were compared. In addition, theoretical considerations based on economics and on interactions also indicate that the analysis of corporate groups shold be more rewarding and potentially more accurate than the analysis of individual households. Archaeologically, corporate groups can be defined where residential coherency and internal hierarchies are demonstrable. Because corporate groups can be viewed as signaling major changes in the structuring of society, and in the evolution of social and political complexity, the investigation of conditions under which corporate groups emerge should be of major theoretical significance to the entire discipline of archaeology. Moreover, because of the close logical links to material culture and the environment, theoretical modeling should be particularly amenable to archaeological testing. In sum, corporate groups provide an unusually fertile problem area which archaeologists can hope to attack with at least a promising degree of success.     

The Hungarian and Slovak sources of archaeological obsidian: an interim report on further fieldwork,with a note on tektites

This report describes the results of fieldwork carried out in the Zemplén Mountain area of north-eastern Hungary in 1975. The aim of this work was to locate and sample geological sources of obsidian which may have been used by prehistoric man. These sources are of increased importance since the work of Nandris (1975) showed that the Romanian “sources” do not produce workable obsidian. During the fieldwork three sources in Hungary were visited and sampled; one of these was the previously unlocated source of Csepegö Forräs. A number of other possible localities for geological obsidian are mentioned in 19th and 20th century geological and archaeological literature, and the present state of knowledge with regard to these is summarized. Further sources exist in central and in south-eastern Slovakia. These sources were not visited but material has been obtained from both areas. The central Slovak sources do not produce workable obsidian and are not therefore relevant to archaeological studies. Obsidian from three localities in south-eastern Slovakia is of good glassy quality and further fieldwork is now needed to check the validity of these localities as geological sources. Reference is made to obsidian sources in the western U.S.S.R., and the problem of the use of tektites in archaeological sites is discussed.The obsidian samples obtained during this work are currently being analyzed using neutron activation, in order to characterize the sources on the basis of their trace element analysis and thus to relate them to archaeological obsidian from central and eastern Europe.     

Palaeoenvironmental implications of the giant crocodylian Mourasuchus (Alligatoridae,Caimaninae) in the Yecua Formation (late Miocene) of Bolivia

Tineo, D.E., Bona, P., Pérez, L.M., Vergani, G.D., González, G., Poiré, D.G., Gasparini, Z.N. & Legarreta, P., 1.10.2014. Palaeoenvironmental implications of the giant crocodylian Mourasuchus (Alligatoridae, Caimaninae) in the Yecua Formation (late Miocene) of Bolivia. Alcheringa 39, xxx–xxx. ISSN 0311-5518

Outcrops of the Yecua Formation (late Miocene) are exposed for approximately 230 m along the La Angostura section of the Piraí River (50 km southwest of Santa Cruz de la Sierra). These reveal massive (argillic palaeosols) and laminated (quiet-water lacustrine and marsh settings) mudstones interbedded with thin sandstones containing microfossils, molluscs and vertebrate remains. Significantly, the succession hosts a giant crocodylian, Mourasuchus (Alligatoridae, Caimaninae), which is represented by both skull and postcranial fragments found in association with freshwater turtles and fishes. Mourasuchus was distributed widely from the middle Miocene of Colombia to upper Miocene of Venezuela, Brazil and Argentina, suggesting connections between major fluvial systems and an active mechanism for dispersal of South American freshwater vertebrates during the Miocene.

David Eric Tineo [tineo.d.e@gmail.com] and Daniel Gustavo Poiré [dgpoire@yahoo.com.ar], CONICET—Centro de Investigaciones Geológicas, Universidad Nacional de La Plata. Calle 1 (644), B1900FWA, La Plata, Argentina; Paula Bona [paulabona26@gmail.com] and Zulma Gasparini [zgaspari@fcnym.unlp.edu.ar], CONICET—División Paleontología Vertebrados, Museo de La Plata. Paseo del Bosque s/n, B1900FWA, La Plata, Argentina; Leandro Martín Pérez [pilosaperez@gmail.com] CONICET—División Paleozoología Invertebrados, Museo de La Plata. Paseo del Bosque s/n, B1900FWA, La Plata, Argentina; Gustavo Dardo Vergani [gvergani@pluspetrol.net]—Pluspetrol S.A. Lima (339), C1073AAG, Ciudad Autónoma de Buenos Aires, Argentina; Gloria González Rigas [ggonzalez@pluspetrol.net]—Pluspetrol Bolivia Corporation SA, Av. Grigotá esq. Las Palmas, Santa Cruz de la Sierra, Bolivia; Pablo Legarreta [plegarreta@pluspetrol.net]—Pluspetrol S.A. Lima (339), C1073AAG, Ciudad Autónoma de Buenos Aires, Argentina.     

E. B. Tylor and the Problem of Primitive Culture

Edward Burnett Tylor’s (1832–1917) theory of survivals, or elements of the “primitive” or archaic past that continued to play an active part in the beliefs of the present day, hallmarks the Victorian effort to isolate and display what were thought to be the most developed features of the contemporary world. However, in focusing on what was outmoded in society, the theory of survivals brought primitive beliefs into an uncomfortable relationship with the beliefs of the present, threatening to disrupt the harmony of this conception. The resulting problems of recognition and understanding in the theory of survivals led Tylor finally to affirm a static and mechanical view of the continuity of cultures, in opposition to the radical, dynamic view with which he had been working until the publication in 1871 Tylor, E. B. 1871. Primitive Culture: Researches into the Development of Mythology, Philosophy, Religion, Art, and Custom, Vol. 2, London: John Murray.  [Google Scholar] of Primitive Culture.     

The mandible and dentition of the Early Cretaceous monotreme Teinolophos trusleri

Rich, T.H., Hopson, J.A., Gill, P.G., Trusler, P., Rogers-Davidson, S., Morton, S., Cifelli, R.L., Pickering, D., Kool, L., Siu, K., Burgmann, F.A., Senden, T., Evans, A.R., Wagstaff, B.E., Seegets-Villiers, D., Corfe, I.J., Flannery, T.F., Walker, K., Musser, A.M., Archer, M., Pian, R. & Vickers-Rich, P., June 2016. The mandible and dentition of the Early Cretaceous monotreme Teinolophos trusleri. Alcheringa 40, xx–xx. ISSN 0311-5518.

The monotreme Teinolophos trusleri Rich, Vickers-Rich, Constantine, Flannery, Kool & van Klaveren, 1999 Rich, T.H., Vickers-Rich, P., Constantine, A., Flannery, T.F., Kool, L. & van Klaveren, N., 1999. Early Cretaceous mammals from Flat Rocks, Victoria, Australia. Records of the Queen Victoria Museum and Art Gallery 106, 1–34. [Google Scholar] from the Early Cretaceous of Australia is redescribed and reinterpreted here in light of additional specimens of that species and compared with the exquisitely preserved Early Cretaceous mammals from Liaoning Province, China. Together, this material indicates that although T. trusleri lacked a rod of postdentary bones contacting the dentary, as occurs in non-mammalian cynodonts and basal mammaliaforms, it did not share the condition present in all living mammals, including monotremes, of having the three auditory ossicles, which directly connect the tympanic membrane to the fenestra ovalis, being freely suspended within the middle ear cavity. Rather, T. trusleri appears to have had an intermediate condition, present in some Early Cretaceous mammals from Liaoning, in which the postdentary bones cum ear ossicles retained a connection to a persisting Meckel’s cartilage although not to the dentary. Teinolophos thus indicates that the condition of freely suspended auditory ossicles was acquired independently in monotremes and therian mammals. Much of the anterior region of the lower jaw of Teinolophos is now known, along with an isolated upper ultimate premolar. The previously unknown anterior region of the jaw is elongated and delicate as in extant monotremes, but differs in having at least seven antemolar teeth, which are separated by distinct diastemata. The dental formula of the lower jaw of Teinolophos trusleri as now known is i2 c1 p4 m5. Both the deep lower jaw and the long-rooted upper premolar indicate that Teinolophos, unlike undoubted ornithorhynchids (including the extinct Obdurodon), lacked a bill.

Thomas H. Rich [trich@museum.vic.gov.au], Sally Rogers-Davidson [srogers@museum.vic.gov.au], David Pickering [dpick@museum.vic.gov.au], Timothy F. Flannery [tim.flannery@textpublishing.com.au], Ken Walker [kwalker@museum.vic.gov.au], Museum Victoria, PO Box 666, Melbourne, Victoria 3001, Australia; James A. Hopson [jhopson@uchicago.edu], Department of Organismal Biology & Anatomy, University of Chicago,1025 East 57th Street, Chicago, IL 60637, USA; Pamela G. Gill [pam.gill@bristol.ac.uk], School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, U.K. and Earth Science Department, The Natural History Museum, Cromwell Road, London SW7 5BD, UK; Peter Trusler [peter@petertrusler.com.au], Lesley Kool [koollesley@gmail.com], Doris Seegets-Villiers [doris.seegets-villiers@monash.edu], Patricia Vickers-Rich [pat.rich@monash.edu], School of Earth, Atmosphere and Environment, Monash University, Victoria 3800, Australia; Steve Morton [steve.morton@monash.edu], Karen Siu [karen.siu@monash.edu], School of Physics and Astronomy, Monash University, Victoria 3800, Australia; Richard L. Cifelli [rlc@ou.edu] Sam Noble Oklahoma Museum of Natural History, University of Oklahoma, Norman, OK 73072, USA; Flame A. Burgmann [flame.burgmann@monash.edu], Monash Centre for Electron Microscopy, 10 Innovation Walk, Monash University, Clayton, Victoria 3800, Australia; Tim Senden [Tim.Senden@anu.edu.au], Department of Applied Mathematics, Research School of Physical Sciences and Engineering, The Australian National University, Canberra, Australian Capital Territory 0200, Australia; Alistair R. Evans [alistair.evans@monash.edu], School of Biological Sciences, Monash University, Victoria 3800, Australia; Barbara E. Wagstaff [wagstaff@unimelb.edu.au], School of Earth Sciences, The University of Melbourne, Victoria 3010, Australia; Ian J. Corfe [ian.corfe@helsinki.fi], Institute of Biotechnology, Viikinkaari 9, 00014, University of Helsinki, Finland; Anne M. Musser [anne.musser@austmus.gov.au], Australian Museum, 1 College Street, Sydney NSW 2010 Australia; Michael Archer [m.archer@unsw.edu.au], School of Biological, Earth, and Environmental Sciences, University of New South Wales, Sydney, NSW 2052, Australia; Rebecca Pian [rpian@amnh.org], Division of Paleontology, American Museum of Natural History, Central Park West at 79th Street, New York, NY 10024-5192, USA. Received 7.4.2016; accepted 14.4.2016.     

Estimating Core Number in Assemblages: Core Movement and Mobility During the Holocene of the Fayum,Egypt

The utility of the cortex ratio first developed by Dibble et al. (American Antiquity, 70(3), 545–560, 2005) and extended by Douglass et al. (American Antiquity, 73(3), 513–526, 2008) is examined in contexts where cores rather than flakes may be transported. The cortex ratio is used to demonstrate the movement of artifacts by quantifying missing surface area, typically where it is the flakes that were removed and the cores that were left behind. In such situations, the removal of flakes with small volumes will result in the removal of relatively large cortical surface areas resulting in a low cortex ratio. However, when it is the cores that were removed, assemblages will lose greater proportions of artifact volume relative to the loss of artifact surface area. Here, we propose methods to investigate the effects of high-volume artifact removal from archeological assemblages as a proxy for human movement in addition to the cortex ratio. We apply the methods to stone artifact assemblages from the Fayum, Egypt, where changes in mid-Holocene mobility are closely linked to food production.     

A new damsel-dragonfly (Odonata: Anisozygoptera: Campterophlebiidae) from the earliest Jurassic of the Junggar Basin,northwestern China

Zheng, D., Wang, H., Nel, A., Dou, L., Dai, Z., Wang, B. & Zhang, H. 27 June 2019. A new damsel-dragonfly (Odonata: Anisozygoptera: Campterophlebiidae) from the earliest Jurassic of the Junggar Basin, northwestern China. Alcheringa XX, X–X. ISSN 0311-5518.

A new genus and species of campterophlebiid damsel-dragonfly, Jurassophlebia xinjiangensis gen. et sp. nov., is described from the Lower Jurassic Badaowan Formation in the Junggar Basin, northwestern China. Jurassophlebia differs from all other campterophlebiid genera in having PsA in the same orientation as the distal branch of AA, and in its uniquely open subdiscoidal cell with very acute apical angle in the hind wing. The new discovery adds to the Asian diversity of damsel-dragonflies in the earliest Jurassic.

Daran Zheng* [dranzheng@gmail.com], He Wang [hwang@nigpas.ac.cn], Bo Wang [bowang@nigpas.ac.cn], and Haichun Zhang [hczhang@nigpas.ac.cn], State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, 39 East Beijing Road, Nanjing 210008, PR China; André Nel [anel@mnhn.fr], Institut de Systématique, Évolution, Biodiversité, ISYEB-UMR 7205-CNRS, MNHN, UPMC, EPHE, Muséum national d’Histoire naturelle, Sorbonne Universités, 57 rue Cuvier, CP 50, Entomologie, F-75005, Paris, France; Longhui Dou [345317122@qq.com], Comprehensive Geology Exploration Team, Xinjiang Coalfield Geology Bureau, West Mountain Road, Ürümqi 830000, PR China; Zhenlong Dai [286321388@qq.com], No.9 Geological Team, Xinjiang Bureau of Geology and Mineral Resources, Ürümqi 830011, PR China; Daran Zheng also affiliated with Department of Earth Sciences, The University of Hong Kong, Hong Kong Special Administrative Region, PR China.     

Ceramic Production and Interaction in the Northern Range of Trinidad

Regional syntheses based on data recovered mostly from outside of the Northern Range have characterized the mountainous region in northern Trinidad as a boundary between two distinct interaction spheres during the Early Ceramic Age (ca. AD 350–650/800) (Boomert 2000 Boomert, A. 2000. Trinidad, Tobago and the Lower Orinoco interaction Sphere: An Archaeological/Ethnohistorical Study. Alkmaar: Cairi Publications. [Google Scholar]). Changes occurring on Trinidad, other islands of the southern Lesser Antilles, and the South American mainland resulted in the disintegration of these earlier style zones during the final centuries of the Early Ceramic (Boomert 2000 Boomert, A. 2000. Trinidad, Tobago and the Lower Orinoco interaction Sphere: An Archaeological/Ethnohistorical Study. Alkmaar: Cairi Publications. [Google Scholar], 2010). This period of Late Ceramic cultural realignment was characterized by climate change, the renegotiation of political and social networks, and demographic transformations. We consider newly recovered ceramic evidence from the central Northern Range in order to evaluate the characterization of the region as a boundary and the region's role in broader Caribbean trends. We examine participation in interaction spheres to provide a more nuanced understanding of regional dynamics as they were expressed locally. Ceramic data indicate that occupants of the central Northern Range interpreted regional styles using locally derived materials, thus simultaneously engaging regional traditions and constructing local patterns of resource exploitation.