Age changes in bone microstructure: do they occur uniformly?

Age estimations based on conventional multifactorial methods were compared with trends observed in the internal morphology of bones obtained from high‐resolution µCT. Specifically, average trabecular thickness and number of trabeculae/mm transect were determined in the non‐load‐bearing capitate (hand) and the load‐bearing navicular (foot). The µCT findings reveal age‐related trends but—surprisingly—these correspond only loosely with the ages assigned by conventional ageing methods, and are also not in accordance with what would be predicted from biomechanical considerations: trabeculae tend to be thinner in the (habitually) load‐bearing navicular than in the (habitually) non‐load‐bearing capitate. While the statistically significant correlation between trabecular thickness and number of trabeculae would suggest a compensatory mechanism between these two aspects of microanatomy, they are not correlated with the assigned ages and, importantly, may differ between sexes. Only in females is there an unequivocal trend towards trabecular thickness increase with age. These findings, although unexpected, can be reconciled with recent histological evidence and assumed average activity levels in historical populations. Conversely, changes in trabecular number are less clear‐cut and may be due to the lack of very old individuals in the sample. Nevertheless, the trends observed for trabecular thickness, as well as for trabecular number, seem to imply that the higher incidence of osteoporosis in women could be explained from a structural point of view alone. Copyright © 2005 John Wiley & Sons, Ltd.     

The variation in δ13C values in bone collagen for two wild herbivore populations: Implications for palaeodiet studies

The δ¹³C values for un-defatted bone gelatin of individual members of wild populations of mule deer (Odocoileus hemionus hemionus) and field vole (Microtus townsendii) have been measured to determine the variability within each population. Means and standard deviations for the mule deer sample (N=55) and vole sample (N=22) are −20·6±0·5‰ and −23·2±0·6‰, respectively. The distributions of δ¹³C values for each of these populations are normal and we observed no correlation in δ¹³C values with age or sex.     

Evaluation of carnivory in inland Jomon hunter–gatherers based on nitrogen isotopic compositions of individual amino acids in bone collagen

Archaeological studies including stable carbon and nitrogen isotope analyses of bone collagen from human remains have suggested their heavy dependence on terrestrial foods during the Jomon period in the inland central region in Japan. However, it is not easy to quantitatively evaluate the extent of carnivory for archaeological human remains based on the bulk collagen chemistry, because of variable ¹⁵N-enrichment factor along the trophic step and background isotopic variations in ecosystems. In order to overcome these problems and more precisely evaluate diets of prehistoric humans who strongly adapted to terrestrial environment, in this study we applied nitrogen isotope analysis of individual amino acids in bone collagen to two inland human populations in the Jomon period. Our results suggest that the two populations were predominantly dependent on the C₃-plant-based terrestrial ecosystem and consumed little aquatic resources. Furthermore, their mean trophic positions (2.7 for both cases) are closer to that of the fox (2.8–3.0) rather than those of pure herbivores (2.0–2.2), and show little change over time. These results are the first evidence that inland Jomon populations may have had more carnivorous diets than is traditionally considered.     

Avian resource depression or intertaxonomic variation in bone density? A test with San Francisco Bay avifaunas

Previous analyses of the Emeryville Shellmound fauna suggested that ever-expanding late Holocene human populations of the San Francisco Bay area depressed a wide range of vertebrate taxa, including cormorants (Phalacrocorax), geese (Anserinae), and large shorebirds (e.g., Numenius, Limosa). Far-reaching implications for prehistoric human behavior, historical ecology, and modern conservation biology have resulted from that work. We test the generality of the bird-based conclusions here by documenting temporal trends in avifaunal abundances from five additional sites located on the San Francisco Peninsula. Analyses of these data reveal patterns identical to those found at Emeryville, showing significant declines through time in the relative abundances of both geese and cormorants between about 2000 and 700 B.P. New photon absorptiometric-based density data for cormorants, geese, and ducks (Anatinae) are used to determine if the declines through time in the relative abundances of geese and cormorants are correlated with variation in the extent of density-mediated attrition observed in these faunas. The data and analyses presented here suggest that while density-mediated attrition played a role in structuring element abundances in these avifaunas, there is no evidence that it varied systematically through time to produce the revealed patterns in taxonomic abundances. Resource depression thus remains a viable hypothesis for the declining abundances of large-sized waterbirds during the late Holocene of the San Francisco Bay region. The new bone density data we present should be useful to analyses of archaeological and paleontological avifaunas wherever these or related taxa are found around the world.     

Re-investigating fish consumption in Greek antiquity: results from δC and δN analysis from fish bone collagen

One of the frequently encountered issues in ancient Greek dietary reconstructions through isotope analyses has been the apparent unimportance of fish protein in human diets. The significance of this observation is amplified by the abundant ichthyofaunal remains, iconographic evidence and literary information on fish and fishing, pertaining to almost all sites and time periods of Greek antiquity. In this project, we measured for the first time isotopes from a large number of fish bones from Greek sites dating from the Mesolithic to the Classical times, aiming to investigate whether this absence is an artefact of the methodology or whether it reflects a reality of restricted fish consumption. Results show that regional trends are stronger that temporal ones in fish isotope values. The range of values overlaps with terrestrial resources, making it difficult or impossible to reject fish consumption based on isotope data alone. This variability proposes a reconsideration of the amount of fish in ancient Greek diets specifically for each site and amplifies the importance of interdisciplinary studies, especially for regions with variable ecological resources.     

Geographic variation in bone carbonate and water δO values in Mendoza,Argentina and their relationship to prehistoric economy and settlement

Questions of mobility, settlement pattern, and their relation to economic organization and resource use are central to ongoing work in central-western Argentina. Here we analyze geographic patterns in the distribution of 178 human bone carbonate δ¹⁸O samples, 46 human tooth enamel carbonate δ¹⁸O samples, and 48 water δ¹⁸O samples from throughout the Andean Cordillera and Monte Desert and evaluate their implications for prehistoric mobility and economy. We confirm and refine previous generalizations regarding a highland/lowland dichotomy in water δ¹⁸O values and show that the range of human carbonate δ¹⁸O values generally reflect available water sources. While there is little within-lifetime change in patterns of water use, we show that most individuals have stable isotope signatures consistent with water use from multiple areas or areas other than where they were ultimately interred. These data indicate high levels of residential mobility, and we conclude by discussing their implications for our understanding of regional prehistory.     

Ottawa's Byward Market: a festive bone of contention?

This paper considers recent developments in the revitalization of the Byward Market, with reference to applicable concepts of the 'tourist-historic city' and the 'convivial city. The central objective is to assess its convergence, in specific detail, with the festival marketplace model. Convergence on most dimensions is demonstrated, but shown to be limited by alternative management philosophies and the fractured complexity of a 'real world' setting. The Market's growing real-world centrality is shown to give rise to a range of stakeholder contest beyond a festival marketplace, as specifically defined. It is suggested that this will prove more generally true of evolved traditional markets.     

Burning wood or burning bone? A reconsideration of flotation evidence from Upper Palaeolithic (Gravettian) sites in the Moravian Corridor

This paper compares archaeobotanical and other data from new excavations at two Upper Palaeolithic sites — Dolní V?stonice II and P?edmostí I — in the Moravian Corridor, Czech Republic. Both contain the traces of broadly contemporary ‘Gravettian’ occupations during the warmer episodes of the Pleistocene which preceded the last glacial maximum. Yet their archaeobotanical remains show striking differences — those from Dolní V?stonice II being dominated by large quantities of conifer wood charcoal, while those from P?edmostí I are much more scanty and dominated by vitrified plant remains, in association with large quantities of burnt bone. We argue that these differences between these two datasets arise from different uses of fuel at either site: bone at P?edmostí I and wood at Dolní V?stonice II. Subsequently, we explore the possible reasons for this difference and argue that once likely taphonomic distinctions are accounted for, these data on fuel use offer fresh insights into the functions and durations of these Upper Palaeolithic occupations of the Moravian corridor and some possible implications for how archaeobotanical data from such sites should be interpreted.     

Intentional or incidental thermal modification? Analysing site occupation via burned bone

Although there has been extensive experimental research on the thermal modification of bone, the results have rarely been applied to interpret zooarchaeological assemblages. The faunal assemblage from Wanderer's Cave, Australia was analysed to investigate the origins, timing and context in which faunal specimens became burned during the mid–late Holocene occupation of the site. Statistical analyses of uniformity of burning, burning over fracture surfaces and epiphyses, frequency of carbonisation by prey taxa, and thermal modification of canid modified specimens indicate that the majority of faunal specimens were unintentionally modified when on the surface of the deposit or while buried in sediment when fires were lit at subsequent site occupation events. Thermal modification at the site does not reflect intentional cooking activities. Significant preservation biases were identified from the lower acidic levels of the site, preventing knowledge of the early fire history at Wanderer's Cave.     

Diet uniformity at an early farming community in northwest Anatolia (Turkey): carbon and nitrogen isotope studies of bone collagen at Aktopraklık

Aktoprakl?k is a settlement site composed of three areas (A–C) in the Marmara region of northwest Anatolia, with phases of occupation that date to the Late Neolithic and Early Chalcolithic periods, mid-seventh to mid-sixth millennium bc (ca. 6400–5600 cal. bc). Here, we present 54 human and fauna bone collagen stable isotope results from the site, alongside five modern fish bone collagen isotope results, to examine the nature of human diet. The stable isotope analysis shows that human diet comprised the consumption of select C₃ terrestrial resources, with a preference for domestic animal proteins over plant proteins. The evidence to date suggests that animal husbandry was at the forefront of Late Neolithic and Early Chalcolithic subsistence practices. No isotopic difference in humans is observed between biological sex or between areas B and C at the settlement.     

What makes bones shiny? Investigating trampling as a cause of bone abrasion

Taphonomic modifications on animal bones have the potential to provide a wealth of information on the depositional histories of faunal assemblages. However, certain modifications have received little attention and their interpretation remains complex due to their varied or uncertain aetiology. This has hindered progress in approaches to taphonomic research and it remains relatively rare that a comprehensive suite of modifications is recorded during zooarchaeological analysis. Abrasion, defined as a shine or polish on bone, is one such modification, with a plethora of processes having been cited as a potential cause. Relatively little holistic analysis of archaeological specimens has been carried out and consequently the interpretative potential of the modification is yet to be realised. This paper examines the degree to which the process of trampling causes bone abrasion. Trampling causes multiple, sub-parallel, linear striations on bones and has been suggested by some researchers as a cause of abrasion (see Andrews and Cook, Man 20:675–691, 1985; Behrensmeyer et al., Palaeogeogr Palaeocol 63:183–199, 1986; Fiorillo, Univ Wyoming Contrib Geol 26:57–97, 1989; Myers et al., Am Antiquity 45:483–490, 1980; Nielsen, Am Antiquity 56:483–503, 1991; Olsen and Shipman, J Archaeol Sci 15:535–553, 1988). Research presented here involves statistical analysis of a large and diverse faunal dataset from seven British sites. Results from both correlation and logistic regression analysis demonstrate the very close relationship between the two modifications, although this is not the case at every site. These findings strongly suggest that trampling is a major cause of abrasion in a British context. Once the relationship is established at a specific site, the modification can be more reliably used for reconstructing the taphonomic trajectory of an assemblage.     

Metacarpal radiogrammetry: a useful indicator of bone loss throughout the skeleton?

Metacarpal radiogrammetry has received increasing interest in recent studies of archaeological human bone in facilitating the identification of age-related cortical bone loss and osteoporosis risk in the past. The technique is relatively simple and non-destructive, and existing comparative clinical data is an advantage in its application to archaeological samples. In order for metacarpal radiogrammetry to be useful in identifying individuals that could have been at risk of fracture in the past, cortical bone loss as measured at the second metacarpal is assumed to be reflective of bone loss occurring throughout the skeleton and across the metabolically different cortical and trabecular bone. Archaeological studies have frequently relied on literature reviews of clinical data to justify the technique as valid and useful. However, the present study has examined whether cortical bone loss measured in the second metacarpal is similar to bone loss measured at specific skeletal sites that are more frequently affected by osteoporosis-related fracture. Skeletons from two post-medieval collections from London, UK, Redcross Way and Farringdon Street (lower burial ground of St. Bride's Church) were studied. The results of the present study demonstrate that the second metacarpal is useful in identifying age-related bone loss at sites that are predilected to osteoporotic fracture, most notably the distal radius, which is prone to Colles' fractures. Metacarpal radiogrammetry also correlates well with bone loss in skeletal sites that are primarily composed of trabecular bone, including the fourth lumbar vertebra (a site of compression fractures) and the iliac crest (the location for clinical biopsies). The present study also confirms previous findings of significant differences between the pattern of cortical bone loss between the metacarpal and the femur. The poor relationship between these two areas is most likely attributable to mechanical loading.     

Sino-American Cooperation in Geological Survey in Tibet

TheHimalayasandtheQinghai-TibetPlateau,plusareasundertheirimpact,makeupone-thirdoftheChineseterritory.Thisyoungpartoftheworid,withanaver-ageelevationof4,500meters,isstillrising.WarmandhumidcurrentsfromtheIndianOceaninthesouthareblockedbytheHimalayas,causi…     

Leaders in Thinking,Laggards in Attention? Bureaucratic Engagement in International Arenas

Frameworks that examine policy subsystems, networks, and coalitions view bureaucracies as part of the mix of policy actors that advocate policy positions in both domestic and international arenas. However, few examine bureaucracies as independent actors and how they exercise influence distinct from other pressure groups. The ways in which domestic bureaucracies engage in the international environment is woefully under examined, with only a few studies examining how domestic bureaucrats affect decision making in the international arena. However, it is not unreasonable to posit that bureaucratic engagement in the international arena may have political implications in the domestic sphere. Building on examinations of bureaucratic autonomy, this research queries the ways in which domestic bureaucracies can interact in the international arena to "change agendas and preferences" of domestic political actors. While it finds that attention to developing an international reputation can enhance political leverage at home, it may do so at a cost to domestic programs if insufficient attention is given to domestic aspects of the organization's mission. Nevertheless, as attention lurches from one arena to another, policy change is facilitated by the politically powerful resources of an international reputation in expertise, active engagement in the international policy community, and broadly based support for programmatic change.     

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