The Foramina Transversaria of The Sunghir 2 and 3 Cervical Vertebrae

The Mid Upper Paleolithic immature Sunghir 2 and 3 skeletal remains exhibit non-closure and doubling of several of their cervical vertebral foramina transversaria. Both exhibit non-closure of the atlas (C1) foramina. Sunghir 3 also exhibits foraminal non-closure in her C4 to C5. Sunghir 2 has doubling of the foramen on C4 and C6, whereas Sunghir 3 has it on C4 to C6. The anatomical distribution of these variants places Sunghir 2 and 3 at the limits of recent human cervical vertebral morphological variation. The correspondence between these variants and vascular pathways is unclear, and therefore their implications remain uncertain.     

The Sunghir 3 Upper Paleolithic Juvenile: Pathology versus Persistence in the Paleolithic

The Mid Upper Paleolithic Sunghir 3 late juvenile early modern human, from the most elaborate burial in the Pleistocene, had pathologically foreshortened and anteriorly bowed femora and, based on her dental enamel hypoplasias and transverse lines, sustained severe and persistent systemic stress throughout her decade of life. Her modest femoral and tibial asymmetry and her femoral bicondylar angles indicate non‐pathological patterns of posture and locomotion. The levels of rigidity for her weight‐bearing tibiae and the non‐dominant left arm reflect normal weight‐bearing and manipulation. These indicators are combined with an elevated level of right humeral strength, leading to pronounced humeral diaphyseal asymmetry, combined with elevated muscular insertion asymmetry. In combination with marked upper limb muscle markings and normal levels of bone formation, these reflections of her robustness indicate that she was fully mobile and participated actively in the tasks of her social group. There is no indication of the skeletal hypotrophy/atrophy that would be associated with less than full participation in the mobility and subsistence of her social group. As such, Sunghir 3 joins a growing list of developmentally or degeneratively pathological Late Pleistocene humans who nonetheless remained mobile and active. Copyright © 2012 John Wiley & Sons, Ltd.     

Anatomical evidence for the antiquity of human footwear: Tianyuan and Sunghir

Trinkaus [Trinkaus, E., 2005. Anatomical evidence for the antiquity of human footwear use. J. Archaeol. Sci. 32, 1515–1526] provided a comparative biomechanical analysis of the proximal pedal phalanges of western Eurasian Middle Paleolithic and Middle Upper Paleolithic humans, in the context of those of variably shod recent humans. The anatomical evidence indicated that supportive footwear was rare in the Middle Paleolithic but became frequent by the Middle Upper Paleolithic. Based on that analysis, additional data are provided for the Middle Upper Paleolithic (∼27,500 cal BP) Sunghir 1 and the earlier (∼40,000 cal BP) Tianyuan 1 modern humans. Both specimens exhibit relatively gracile middle proximal phalanges in the context of otherwise robust lower limbs. The former specimen reinforces the association of footwear with pedal phalangeal gracility in the Middle Upper Paleolithic. Tianyuan 1 indicates a greater antiquity for the habitual use of footwear than previously inferred, predating the emergence of the Middle Upper Paleolithic.     

The death and burial of sunghir 1

The Mid Upper Paleolithic Sunghir 1 burial of an older adult male is one of the most elaborate burials known, with red ochre, thousands of mammoth ivory beads, and other body ornaments. Reanalysis and cleaning of the skeletal remains revealed a perimortem incision in the ventral–lateral first thoracic vertebra (T1) body, most likely from a sharp blade or point and the probable cause of death. Context indicates that the trauma was most likely from a hunting accident or social altercation. The unusual cause of death may be correlated with the exceptional burial elaboration of Sunghir 1, adding to the high frequency of unusual individuals in the ‘red ochre’ burials of the Mid Upper Paleolithic. Copyright © 2010 John Wiley & Sons, Ltd.     

Age of closure of the foramen of Huschke: an osteological study

The foramen of Huschke is a dehiscence in the antero‐inferior surface of the tympanic plate, which forms during the normal post‐natal development of the temporal bone. Closure of the foramen is generally reported to take place by 5 years of age, although a persistent foramen has been observed in 0–67% of adult crania depending on the population. A persistent foramen of Huschke in adult life may be involved in abnormalities of the external auditory canal and related structures, which can lead to otological complications. This paper examines age‐related changes in the development of the tympanic plate from the perinatal to the adult condition using two osteological samples from Britain, and is the first systematic evaluation beyond the age of six years. The results suggest that the widely cited chronology for the closure of the foramen of Huschke is erroneous. Earlier stages of formation may be used for narrowing age estimation in fragmentary remains of juveniles in a skeletal collection of unknown age or in a forensic or clinical context. Copyright © 2005 John Wiley & Sons, Ltd.     

Nutritional and disease stress of juveniles from the Dakhleh Oasis,Egypt

Bioarchaeologists use skeletal health indicators to measure how ancient populations adapted to their physical, cultural and biological environments. Skeletons of infants and children are rarely included in these kinds of analyses because of factors such as poor preservation, small sample size, incomplete recovery or research design. In this study, skeletal remains of juveniles aged from foetal to 15 years (N = 238) from Kellis 2, a Romano‐Byzantine cemetery in the Dakhleh Oasis, Egypt, are analysed to shed light on how infants and children were affected by Roman policies during the early years of the Christianisation of Egypt. Non‐specific indicators of physiological stress (cribra orbitalia, enamel hypoplasia and osteoperiostitis) are analysed for post‐natal individuals and interpreted in the context of the physical, cultural and biological landscapes. Results from these analyses suggest moderate levels of skeletal and dental stress with a marked improvement in general health from pre‐Roman times. This study contributes to a better understanding of juvenile paleoepidemiology and mortuary practices in Egypt during the Romano‐Byzantine period. Copyright © 2010 John Wiley & Sons, Ltd.     

The Upper Paleolithic of Northern Asia: Achievements,problems, and perspectives. II. Central and Eastern Siberia

Earlier scholars believed that the Upper Paleolithic of Central and Eastern Siberia appeared very late. However, modern research has shown that not only was there a local Middle Paleolithic, but also there was a very early series of sites in Central Siberia which show both Middle and early Upper Paleolithic traits. These are called the Makarovo horizon and may be 70,000–50,000 years old; features derived from this horizon can be dated to about 30,000 B.P. and can be seen in the early D'uktai culture. The true early Upper Paleolithic is relatively homogeneous in Central and Eastern Siberia and includes artwork. The local Upper Paleolithic reached its florescence in the culture of Mal'ta and Bur'et', which developed out of local antecedents and which is here reinterpreted in light of recent research (including the artwork, structures, and burials). The final stages of the Upper Paleolithic show considerable variability, perhaps including some exotic traits.     

The Middle Paleolithic from Mujina Pećina,Dalmatia, Croatia

Abstract

Mujina Pe?ina in Dalmatia, Croatia is the only systematically excavated and well-dated Middle Paleolithic cave site in the eastern Adriatic. Its stratigraphic sequence covers the period between 45 and 39 uncalibrated years ka. Results of sedimentological, lithic, faunal, and paleobotanical analyses of the upper levels (Levels B, C, D1, and D2) show that this was a hunting site only sporadically visited by humans. During these occupation episodes humans processed animal remains (mostly large bovids, cervids, and caprids) and produced tools from locally available raw material. Carnivore use of the cave is also indicated. This work contributes to our understanding of lifestyles and mobility patterns of the Middle Paleolithic inhabitants of this region.     

Childhood Cranial Trauma from a Late Roman and Merovingian Context from Michelet,Lisieux, France

The Michelet necropolis in Lisieux, France, dating to the late Roman and Merovingian period, comprises of a large number of well‐preserved subadult remains offering a unique opportunity to better understand childhood trauma in the past. The focus of this study was to determine the amount, type and mechanisms of trauma evidenced in subadults from the 4th–8th century AD, and explore potential circumstances surrounding the trauma. The remains of 109 subadults from the Michelet necropolis were examined for the presence of cranial and post‐cranial trauma. Three individuals exhibited perimortem trauma, one individual had an antemortem cranial injury, and no cases of post‐cranial trauma were identified. Cranial trauma affected 4.1% of children with observable cranial remains (N  = 4/97). The children affected were young (2–7 years old), making it unlikely that they would have participated in militaristic activities. Based on the location, morphology and mechanism of injury identified, it is likely that the perimortem injuries sustained by three children were not accidental. The presence of a number of cranial injuries from this site may be related to increased stress in the community related to the decline of the Roman Empire in Gaul, possible raiding barbarian groups during the 4th–5th centuries, or stresses related to the Gallic aristocracy solidifying political powers in northern Gaul during the 5th–7th centuries AD. The consideration and inclusion of childhood trauma in bioarchaeological analyses allows for a more detailed and in‐depth understanding of violence and childhood in the past. Copyright © 2017 John Wiley & Sons, Ltd.     

The Middle-Upper Paleolithic transition in Southeastern Central Europe (Czechoslovakia and Hungary)

Southeastern Central Europe is quite rich in finds of progressive Neandertals from Middle Paleolithic contexts and early modern humans associated with evolved Upper Paleolithic (Aurignacian and Pavlovian). There are no human fossils that can be related to the transitional Middle-Upper Paleolithic units (the Bohunician and the Szeletian); thus, from anthropology we know only that the transitional period began with Neandertals and ended with modern humans. The archaeological record is more complex. The Jankovichian industries of Hungary differ from the mostly non-Levallois Middle Paleolithic of Central Europe in the presence of some Levallois; they seem to be technologically related to the Levallois-Leptolithic Bohunician industries of Moravia, dated to 43,000–38,000 B.P., which are the first transitional Upper Paleolithic unit. The appearance of the Szeletian before 42,000 B.P. in Hungary and at about 39,000 in Moravia represents a technological variation of the transition, although retaining marked local Middle Paleolithic elements. The date of the appearance of the typical Aurignacian, the first culture clearly related to modern humans, is unclear, but it certainly developed after 36,000 B.P. and has several dates between 35,000 and 30,000 B.P.     

“I found the truth in Foot Locker”: London 2011, Urban Culture,and the Post‐Political City

The article begins with an overview of what is implied in the notion of the “post‐political” before looking closely at post‐political interpretations of the 2011 London riots. It presents a critique of the restricted sense of political subjectivity in such accounts. It demonstrates how participation in the riots and their aftermath may be seen as indicative of an embryonic form of urban politics that works with and against the post‐political city. This discussion is illuminated by an analysis of the discursive space of London hip‐hop which reveals an ironic, complex and reflexive dialogue about identity, justice and politics that is far removed from the caricature offered by “strong” interpretations of the post‐political subject. This is then linked to readings of the post‐political city that place a welcome stress not only on the evacuation of the political dimension from the city, but also on the opportunities for the re‐emergence of the proto‐political.     

History,Chronology and Techno-Typology of the Upper Paleolithic Sequence in the Shuidonggou Area,Northern China

The timing and behavioral markers of the Upper Paleolithic in different parts of the world are of great importance to research on modern human dispersals. The pattern of behavioral developments in the Upper Paleolithic in northern China differs in important ways from the patterns observed in West Eurasia, Africa, and South Asia. Shuidonggou (SDG), a cluster of Paleolithic sites in northern China, contains several of the most important Upper Paleolithic sites in the region. Various localities yield evidence of three major cultural components dated by ¹⁴C, uranium-series, and optically stimulated luminescence (OSL) methods to between roughly 46 ka and 10 ka. The oldest component, blade assemblages with western Eurasian early Upper Paleolithic characteristics, appears to be intrusive from Siberia and/or Mongolia, beginning at least 41 ka (e.g., SDG 1 and SDG 9). Advanced core and flake assemblages may mark the appearance of an indigenous Late Paleolithic of North China beginning at around 33 ka (e.g., SDG 2 and SDG 8). Finally, around 10.5 ka, microblade technology arrived in the area (SDG 12), although we are not sure of its origins at present. Other typical Upper Paleolithic cultural remains, such as bone tools and body decorations, have been found at various localities in the SDG area as well (e.g., ostrich eggshell beads from SDG 2, 7, and 8). Information from this cluster of occupations increases our understanding of cultural variability, adaptation, and demographic dynamics of modern humans in Late Pleistocene northern Asia.

     

Temporal change in groundwater level following the 1999 (Mw = 7.5) Chi-Chi earthquake, Taiwan

We examine the post‐seismic change in the groundwater level following the 1999 (M_w = 7.5) Chi‐Chi earthquake in central Taiwan, as recorded by a network of 70 evenly distributed hydrological stations over a large alluvial fan near the epicenter. Four types of post‐seismic responses may be distinguished. In type 1, the groundwater level declined exponentially with time following a coseismic rise. This was the most common response in the study area and occurred in unconsolidated sediments on the Choshui River fan. In type 2, the groundwater level rose exponentially with time following a coseismic fall. This occurred in the deformed and fractured sedimentary rocks in the foothills near the Chelungpu fault that ruptured in the Chi‐Chi earthquake. In type 3, the groundwater level continued to decline with time following a coseismic fall. This also occurred in the deformed and fractured sedimentary rocks near the ruptured fault. Finally, in type 4, the groundwater level, following a coseismic rise, stayed at the same level or even rose with time before it eventually declined. This occurred mostly in unconsolidated sediments along the coast of central Taiwan and along the Peikang Stream. We analyze these post‐seismic responses by using a one‐dimensional model. Together with the results from well test, the analysis show that the type 1 response may be explained by an aquifer model with coseismic recharge and post‐seismic subhorizontal discharge across a length of 500–5000 m; the type 2 response may be explained by a model of coseismic discharge and post‐seismic recharge from surface water; the type 3 response may be explained by a model of coseismic discharge and post‐seismic subhorizontal discharge across a length of 500–5000 m; and the type 4 response may be explained by a model of coseismic recharge and sustained post‐seismic recharge from surface water. The characteristic time for the post‐seismic changes is similar to that for the groundwater‐level decline during dry seasons before the earthquake, suggesting that there was no earthquake‐induced changes in the aquifer properties (i.e. hydraulic conductivity), confirming the earlier results from recession analyses of the post‐seismic streamflow elsewhere after several earthquakes.     

Occipitalization of the Atlas in Two Female Skeletons from Apollonia Pontica,Bulgaria

Occipitalization of the atlas was observed in two adult female skeletons from the Greek colonial site of Apollonia Pontica (5^th to 3^rd centuries BC), located on the Bulgarian Black Sea coast. Representing a rare congenital anomaly of the atlanto‐occipital junction, this condition has been documented in very few skeletal remains from Classical antiquity. Postmortem damage to one of the specimens prevented an evaluation of its clinical significance. The dimensions of the second specimen, however, suggest that the affected individual may have experienced some neurological symptoms associated with her condition. The burial of the two females in close proximity to one another raises the possibility that they may have been biologically related. Copyright © 2012 John Wiley & Sons, Ltd.     

New Archaeological Books and Journals

Abstract

As part of a research program aimed at clarifying the date of the Middle Paleolithic in Greece and its relationship with contemporary industries in the Balkans, a survey of the Larisa area of Thessaly for Paleolithic remains was undertaken in 1987. The results of this survey are reported, along with a reinterpretation of the available evidence in Greece for the date of the Middle Paleolithic. The banks and terrace system of the Peneios River were systematically searched along with those parts of Thessaly with deposits old enough to contain prehistoric artifacts. In 1987, we discovered 32 find spots and collected211 lithic artifacts. The lithic artifacts are Middle and Upper Paleolithic types, and are dated by their association with the fluviatile deposits exposed by downcutting of the river. Radiometric dates for the fluviatile deposits indicate an age of 45–27 KYA (thousands of years ago) for the Paleolithic finds. Other dates for the Middle Paleolithic in Greece are on the same order. The Thessalian Paleolithic industry is a Levallois-Mousterian facies with bifacial leafpoints, side Scrapers, Mousterian points, denticulates, andAurignacian-type end scrapers, burins, retouched Blades, and bifacial leafpoints with rounded bases. The Thessalian industry with its mixture of Middle and Upper Paleolithic types, is similar to other assemblages in Greece. The Greek Levallois-Mousterian resembles the Szeletian of Hungary and is of approximately the same age. It was perhaps produced by late Neanderthals in contact with an anatomically-modern human population. Late Upper Paleolithic Epigravettian and Mesolithic industries were not identified in Thessaly and are rare in Greece. Some areas may have been uninhabited or little used until 9 KYA when the first Neolithic settlements appear in Thessaly.     

The Pleistocene Peopling of the North: Paleolithic Milestones and Thresholds Horizons in Northern Eurasia: Part I: Lower Paleolithic Antecedents

Human occupation of northern Eurasia high latitudes entailed coping with severe bioclimatic circumstances and Ice Age cycle fluctuations. Resolving this “adaptability paradox” required depending on cultural, rather than biological means. Paleolithic evidence indicates culture historical developments of considerable time depth, long-term adaptive stages, and thresholds in the “peopling of the North.” It began with Lower Paleolithic populations expanding into temperate and continental Eurasia, becoming fully actualized during the Middle and Upper Paleolithic. The Middle Paleolithic formative stage constituted a human biogeographic realm overlapping significantly with the Mammoth-Steppe Biome faunal complex. Part I identifies issues, time perspectivism, culture, foraging adaptation, and human biogeography concepts. Lower Paleolithic occurrences, initial occupation episodes are surveyed and discussed.     

The Story of Koula: music and nationhood in Greece

The Story of Koula, one of the Marshall Plan films, was made in Greece in 1951. It neatly exemplifies the capacity of Europe to ‘talk back’ to the USA within the framework of cultural aid programmes. And as such it can introduce a little‐explored topic: the politics of the avant‐garde in Greece in the post‐Civil War years and in particular the role of US cultural aid. This post‐war perspective throws light on the better‐known National School associated above all with Manolis Kalomiris, who dominated Greek music and musical life in the interwar period. The second part of this paper scrutinises the agenda and achievements of the Kalomiris circle, and that in turn enables useful generalisations about romantic nationalism in music. The third part of the paper reflects on the pre‐World War I achievements of Heptanesian traditions, again caught between singularities and dependencies.     

Epipaleolithic/early Neolithic settlements at Qinghai Lake,western China

Transitions from terminal Pleistocene Upper Paleolithic foraging to Holocene Neolithic farming and pastoralist economic orientations in the northern Tibetan Plateau are examined from the perspective of Epipaleolithic sites located near Qinghai Lake, Qinghai Province, western China. Jiangxigou 2 is an artifact-rich, multicomponent midden site with the main period of occupation dating ca. 9000–5000 cal yr BP, containing abundant flaked stone artifacts including a substantial proportion of microlithic tools, abundant faunal remains including gazelle, deer, and sheep, and a small number of ceramics, including the oldest known on the Tibetan Plateau. Heimahe 3, on the other hand, is a brief hunter's camp dating ca. 8450 cal yr BP, with evident affinities to late Upper Paleolithic camps in the same region that date several thousand years older. The two distinctively different sites are probably nodes within a single Epipaleolithic foraging system that developed on the margins of the high Tibetan Plateau during the early Holocene, and that served as a basis for colonization of the high-altitude Plateau at that time. Jiangxigou 2 appears to be connected to early Neolithic agricultural settlements along the upper Yellow River (Huang He) drainage during the middle Holocene, and may provide insights into forager–agriculturalist interactions that lead to the development of pastoralist systems in the region.     

Fracture sealing and fluid overpressures in limestones of the Jabal Akhdar dome,Oman mountains

Fractures are important conduits for fluid flow in the Earth's crust. To better understand the spatial and temporal relations among fracturing, fracture sealing, and fluid flow, we have studied fractures, faults, and veins in a large dome (Jabal Akhdar) in the Oman mountains. Our work combines the results of meso‐ and microstructural analyses and stable isotope analyses. Seven generations of fractures and veins have been identified in the carbonate‐dominated dome. The earliest generations of veins developed during extension and subsidence of the Mesozoic basin. These veins formed in the inclined segments of bedding‐parallel stylolites and in extensional fractures that are perpendicular to bedding (#1 and #2, respectively). These extension‐related veins are truncated by bedding‐parallel veins (#4) that formed during top‐to‐north bedding‐parallel shear of both the northern and southern limbs of the dome. These veins are consistent with a change in stress regime and may be related to an earlier generation of strongly deformed pinch‐and‐swell veins (#3) that are exposed locally on the southern limb of the dome. Normal faults contain a set of en‐echelon tension gashes (#5) and veins emplaced in dilational jogs along the fault planes (#6). In the northern part of the dome, veins (#7) associated with thrusts post‐date the normal faults. Samples of veins and their host rocks were analyzed to provide information on fluid‐rock interaction in the dome and the scale(s) of fluid movement. Oxygen isotope values range from +16.2 to +29.3‰; carbon isotope values range from 0 to +3.6‰. The results of the structural and isotopic analyses are consistent with the early veins (#2–#5) having precipitated from overpressured fluid in a isotopically rock‐buffered system. During normal faulting (#5 and #6), a more open system allowed external fluid to infiltrate the dome at drained conditions and precipitate the youngest sets of veins (#6 and #7).     

Two sides of the same coin—rocks, bones and site function of Picareiro Cave, central Portugal

The issue of site function rarely has been a main focus in the study of Portuguese Upper Paleolithic. This fact may be related to a lack of interest in this research area. More likely, however, it is due to the fact that there are relatively few Paleolithic sites with data that allow a serious study of site function. At Picareiro Cave, central Portugal, there are various data sets from level F/G dated to the latter Magdalenian that are adequate for this type of research. These are habitat structures, lithic artifacts, macro- and mesofauna, as well as 3D location of all artifacts and fauna larger than 1 cm. Based on the interpretation of the analytical results of each data set, it is possible to reconstruct site function of this particular level of Picareiro Cave. The morphology of one of the hearths, being very large in size, with the base prepared and a pavement surrounding it, as well as the condition and diversity of fauna, indicates that it was used for processing the meat of rabbits, red deer, and wild boar, probably through smoking and grilling. All of the evidence from the different types of data (lithic artifacts, habitat structures, use of space, and fauna) indicate that Layers F/G of Picareiro Cave are the result of a specific task, that of processing animal carcasses of rabbits, red deer, and wild boar.