青海喇家遗址人类遗骸的锶同位素比值分析

喇家遗址位于青海省民和县,主体为齐家文化的遗存,距今大约3900~4300年。喇家遗址古代人类迁移活动的研究,对于探索黄河上游古代文明,推动该地区齐家文化研究,有着积极的学术意义。本文首先采用电感耦合等离子体质谱技术对喇家遗址出土的22个个体的44份牙釉质和骨骼样品进行了元素分析,根据检测结果排除了受到污染的2份骨骼样品。其次,通过热电离质谱分析方法对喇家遗址出土22个个体的42份牙釉质和骨骼样品及8个猪牙釉质样品的锶同位素比值进行了测定。检测数据表明,猪牙釉质的锶同位素比值的标准偏差远小于其他动物,可以推断猪由当地饲养的可能性是最大的,因此其牙釉质锶同位素比值可以代表当地的锶同位素水平。经过计算得到8个猪牙釉质的锶同位素比值的平均值为0.710930,将该平均值加或减2倍标准偏差可以得到喇家遗址当地的锶同位素比值范围在0.711058~0.710802之间。以此为前提可以推测,本次检测的22个个体中,有17个个体牙釉质的锶同位素比值在遗址当地的锶同位素比值范围内,可能为本地出生。还有2个个体牙釉质在当地的锶同位素比值范围上下限附近,姑且存疑;仅有3个个体牙釉质的锶同位素比值在遗址当地的锶同位素比值范围以外,表明这些个体可能在其他地区出生,去世后埋葬在遗址中。此外,数据分析还显示,本地出生人群牙釉质的锶同位素比值平均值与骨骼的锶同位素比值平均值比较接近,暗示喇家遗址当地古人类生活方式可能比较统一。     

Cremated human and animal remains of the Roman period--microscopic method of analysis (Sepkovcica, Croatia)

Human and animal cremated osteological remains from twelve graves of Roman Period from archaeological site Sepkovcica near Velika Gorica (Turopolje region, NW Croatia) were analysed. Beside the content of urns and grave pits, fillings of grave vessels like bowls, pots and amphoras from twentytwo grave samples were included in this study. The preservation of osteological and dental remains of human and animal origin was very poor, majority of fragments hardly reach lengths of 10 mm. Weight of each specimen barely exceeds 100 g per person. Apart from traditional macroscopic methods of analysing cremated remains, microscopic method for determination of age at death was also tested. Fragments of femoral bone diaphysis of eighteen persons whose remains had been found on the site were analysed. Person's age at death was presented in the range of five or ten years, and the long bone fragments of a child (infants) were detected. Taxonomic position for each analysed specimen was determined by microscopic analysis of animal cremated bones. Analysis results confirm validity of microscopic method in determination of age at death for human remains and taxonomic qualification of cremated animal remains from archaeological sites.     

关于锶同位素考古研究的几个问题

本文讨论了锶同位素考古研究所涉及的几个重要理论方法问题。首先是岩石、土壤和河流的锶同位素组成以及生物锶的来源问题。然后是锶同位素方法的四点局限性,即骨骼和牙本质样本的成岩污染问题、不同地区的锶同位素重叠现象、牙齿和骨骼的锶同位素混合效应和不能识别移民后代的问题。最后讨论了锶同位素方法应用于人类迁移研究的两个重难点,一是如何分辨一个遗址或墓地中的外来人口,二是如何找到外来人口的来源地。     

Trans‐Atlantic slavery: Isotopic evidence for forced migration to Barbados

The question of the ultimate origin of African slaves is one of the most perplexing in the history of trans‐Atlantic slavery. Here we present the results of a small, preliminary isotopic study that was conducted in order to determine the geographical origin of 25 enslaved Africans who were buried at the Newton plantation, Barbados, sometime between the late 17th and early 19th century. In order to gain a more nuanced understanding of the slaves' origin, we used a combination of carbon, nitrogen, oxygen, and strontium isotope analyses. Carbon and nitrogen isotope ratios were determined in bone and dentinal collagen; oxygen and strontium isotopes were measured in tooth enamel. Results suggest that the majority of individuals were born on the island, if not the estate itself. Seven individuals, however, yielded enamel oxygen and strontium ratios that are inconsistent with a Barbadian origin, which strongly suggests that we are dealing with first‐generation captives who were brought to the island with the slave trade. This idea is also supported by the fact that their carbon and nitrogen stable isotope values differ markedly between their teeth and bones. These intra‐skeletal shifts reflect major dietary changes that probably coincided with their enslavement and forced migration to Barbados. While it is impossible to determine their exact origins, the results clearly demonstrate that the slaves did not all grow up in the same part of Africa. Instead, the data seem to suggest that they originated from at least three different areas, possibly including the Gold Coast and the Senegambia. Am J Phys Anthropol, 2009. © 2009 Wiley‐Liss, Inc.     

The Ice Man's diet as reflected by the stable nitrogen and carbon isotopic composition of his hair.

Establishing the diets of ancient human populations is an integral component of most archaeological studies. Stable isotope analysis of well-preserved bone collagen is the most direct approach for a general assessment of paleodiet. However, this method has been limited by the scarcity of well-preserved skeletal materials for this type of destructive analysis. Hair is preserved in many burials, but is often overlooked as an alternative material for isotopic analysis. Here we report that the stable carbon and nitrogen isotope values for the hair of the 5200 year-old Ice Man indicates a primarily vegetarian diet, in agreement with his dental wear pattern. Whereas previous investigations have focused on bone collagen, the stable isotope composition of hair may prove to be a more reliable proxy for paleodiet reconstruction, particularly when skeletal remains are not well preserved and additional archaeological artifacts are unavailable.     

Technical note: interpreting stable carbon isotopes in human tooth enamel: an examination of tissue spacings from South Africa

Stable isotope analysis of skeletal tissues is widely used in archeology and paleoanthropology to reconstruct diet. In material that is poorly preserved or very old, the tissue of choice is frequently tooth enamel, since this is less susceptible to diagenesis. The relationships between carbon isotope ratios in tooth enamel (δ(13) C(enamel) ), bone collagen (δ(13) C(collagen) ), and bone apatite (δ(13) C(bone apatite) ) are, however, not well understood. To elucidate these, we have measured all three indicators in archeological humans from the western and southern Cape coastal regions of South Africa. The correlation between δ(13) C(enamel) and δ(13) C(collagen) is good (R(2) = 0.71 if two outliers are excluded, n = 79). The correlation between δ(13) C(enamel) and δ(13) C(bone apatite) is weaker (R(2) = 0.37, n = 33) possibly due to bone diagenesis. No systematic offset between δ(13) C(bone apatite) and δ(13) C(enamel) was observed in this sample of archeological humans. Intertooth comparisons of δ(13) C(enamel) in three individuals showed little variation, despite the different ages of crown formation. Carbon isotope ratios in both enamel and bone collagen are good proxies for δ(13) C(diet) .     

Genetic analysis of modern and historical burned human remains

Burning of corpses is a well-known funeral procedure that has been performed for a long time in many cultures. Nowadays more and more corpses are burned in crematories and buried in urns, often for practical and financial reasons. In some scientific, criminal or civil cases even after cremation there is the need of genetic investigations for identification or paternity testing. Furthermore, burned remains are the only remains left in North Europe from 1200 BC to 500 AD. This makes genetic investigation of those materials interesting for anthropological reasons. We present on one hand a systematic investigation of 10 corpses before and after the cremation and on the other hand the analysis of seven historical remains representing the bronze age. We chose the ground bone powder and the less destroyed bone parts respectively and employed a slightly modified commercially available DNA extraction method. The presence of human nuclear and mitochondrial DNA was tested by a simple but highly sensitive Duplex-PCR. DNA quantification was done using real time PCR, and genetic typing was tried out using the AmpFISTR Identifiler Multiplex Kit, followed by an automatic analysis on an AbiPrism310.     

A study of cremated human remains from an urn field dating to the final phase of the Bronze Age, found at “Le Caprine” (Guidonia, Rome, Italy 10th-9th century B.C.)

In this paper cremated human remains from an urn field dating from the final phase of the Bronze age (Guidonia, Rome, Central Italy) were studied. The aim of this study was to identify the minimal number of individuals for grave and cremation patterns. The results show as the ways in which the cremations were carried out were archaic in all the elements that made them up.     

Early African Diaspora in colonial Campeche, Mexico: strontium isotopic evidence

Construction activities around Campeche's central park led to the discovery of an early colonial church and an associated burial ground, in use from the mid-16th century AD to the late 17th century. Remains of some individuals revealed dental mutilations characteristic of West Africa. Analyses of strontium isotopes of dental enamel from these individuals yielded unusually high (87)Sr/(86)Sr ratios, inconsistent with an origin in Mesoamerica, but consistent with an origin in West Africa in terrain underlain by the West Africa Craton, perhaps near the port of Elmina, a principal source of slaves for the New World during the 16th century. These individuals likely represent some of the earliest representatives of the African Diaspora in the Americas.     

Changing patterns of mobility as a response to climatic deterioration and aridification in the middle Holocene southern Sahara

The African Humid Period witnessed a rapid human re‐occupation of the Sahara as numerous lakes formed during the Holocene climatic optimum circa 10‐5 kya. Permanent waters attracted a variety of aquatic and terrestrial fauna allowing for long‐term occupation of specific paleolake basins. The Gobero paleolake in central Niger was one such location that preserves a unique mortuary record from the southern Sahara. Here, we use radiogenic strontium isotope analysis to investigate how human communities adapted to aridification throughout the Holocene. In particular, we examine the effects of increasing climate instability on patterns of human mobility. Results of radiogenic strontium isotope analysis of enamel and bone samples from Middle Holocene burials (～7.2–4.9 kya) indicate predominantly local values with no evidence for sex‐based variation. Comparisons of radiogenic strontium isotope data with previously published (Stojanowski and Knudson: Am J Phys Anthropol 146 (2011) 49–61) Early Holocene burials (～9.7–8.3 kya) indicate significant differences in both enamel and bone values. Middle Holocene individuals demonstrate a predominantly non‐local signature for enamel values and a predominantly local signature for bone values. Those individuals with non‐local bone values always demonstrated non‐local enamel values; however, the opposite was not the case. This suggests a divergence of mobility strategies during the Middle Holocene with a minority of individuals maintaining a more mobile existence throughout their life and others maintaining a similar strategy as Early Holocene hunter–gatherers that was tied to the paleolake basin. The more mobile individuals likely lived during the terminal phase of the lake's occupation. One response to aridification by Saharan peoples, then, was increasing mobility. Am J Phys Anthropol 154:79–93, 2014. © 2014 Wiley Periodicals, Inc.     

Fire and bones: Bronze Age III in the North-Eastern Iberian Peninsula

Between the third millennium BP and the fifth century AD, there are numerous necropolises that house urns in the Iberian Peninsula. One example is the "Pi de la Lliura" (Vidreres, Girona). However, there is a dearth of research concerning these structures. The "Pi de la Lliura" housed 43 structures, which contained a total of 47 vessels with human remains. Of these 43 structures, 22 were totally or partially excavated at the laboratory. The evidence from the fragments indicates cremation at a temperature of 650-700 degrees C. Part of the cremated corpse was then deposited in an urn. One of the most unique characteristics of the necropolis is the high frequency of individuals younger than 20 years old. The mortality of sub-adults is high in any prehistoric necropolis, but it is even higher in a cremation necropolis. "Pi de la Lliura" is a very small necropolis, where corpses were treated similarly over a short period.     

Isotopic tracing of the impact of mobility on infectious disease: The origin of people with treponematosis buried in hull,England, in the late medieval period

Treponematosis has been one of the most studied and debated infectious diseases in paleopathology, particularly from the standpoint of its origin, evolution, and transmission. This study links evidence for treponematosis in skeletons from the 14th–16th century AD cemetery of the Augustinian friary of Hull Magistrates Court, England, with data from stable isotope analysis to test the hypothesis that the people with treponemal disease buried at this site were not locally born and raised. The objective is to explore the potential of using stable isotope data to track the place of origin and extent of mobility of individuals with an infectious disease. Dental enamel samples of 12 skeletons were selected for strontium (⁸⁷Sr/⁸⁶Sr ratio) and oxygen (δ¹⁸O) stable isotope analysis based on the presence (six ‐ diseased) or absence (six ‐ controls) of bone changes associated with treponemal disease. The oxygen isotope ratios of all but three individuals (1047, 1121, 823) overlapped at two standard deviations with the inferred local precipitation range, and only one individual (1216) had a strontium isotope ratio outside the regional range. Two of the four had probable/possible treponemal bone changes. Those with treponemal bone changes were not demonstrably more likely to be migrants than those without such lesions. However, because of extensive documentary evidence for trade with the Baltic Sea area, and for merchants from towns such as Stralsund, Danzig and Elbing being in Hull, it is very plausible that the four migrants came from the Baltic area or even southern Sweden. Am J Phys Anthropol, 2013. © 2012 Wiley Periodicals, Inc.     

Lateral angle: a method for sexing using the petrous bone

We report on the results of applying the so-called lateral angle method for sex determination on skeletal remains. The lateral angle denotes the angle of the internal auditory canal in relation to the medial surface of the petrous part of the temporal bone. The method involves making a small cast of the proximal part of the internal acoustic canal and determining the angle at which the canal opens up to the surface of the petrous bone. The method has the great advantage of utilizing one of the sturdiest bone elements of the human skeleton, and may thus be especially suited for analyses of very fragmented skeletal remains or cremated bones, where the petrous bone may still be readily recognizable. The method was tested using a forensic sample of 113 petrous bones with known sex. Intra- and interobserver testing was also performed. We found a statistically significant difference in angle size between males and females (mean angle size of males, 39.3 degrees ; mean angle size of females, 48.2 degrees ; P < 0.001). There was no bilateral difference in angle size. In blind trials, 83.2% of petrous bones were assigned to the correct sex. We also tested the lateral angle method against an archaeological skeletal sample. True sex was not known for this sample; instead, sexing had been carried out by assessing pelvic and cranial morphology in independent trials. We found a higher concordance between the lateral angle and "pelvic" sex than for lateral angle and "cranial" sex. Finally, we note that subadult sexing may also be possible with this method.     

Utility of multiple chemical techniques in archaeological residential mobility studies: case studies from Tiwanaku- and Chiribaya-affiliated sites in the Andes

In the south central Andes, archaeologists have long debated the extent of Tiwanaku colonization during the Middle Horizon (AD 500-1000). We tested the hypotheses regarding the nature of Tiwanaku influence using strontium isotope, trace element concentration, and oxygen isotope data from archaeological human tooth enamel and bone from Tiwanaku- and Chiribaya-affiliated sites in the south central Andes. Strontium isotope analysis of 25 individuals buried at the Tiwanaku-affiliated Moquegua Valley site of Chen Chen demonstrates that it was likely a Tiwanaku colony. In contrast, no immigrants from the Lake Titicaca Basin were present in 27 individuals analyzed from the San Pedro de Atacama cemeteries of Coyo Oriental, Coyo-3, and Solcor-3; it is likely that these sites represent economic and religious alliances, but not colonies. However, strontium isotope analysis alone cannot distinguish movement between the Tiwanaku- and Chiribaya-affiliated sites in the Moquegua and Ilo Valleys of southern Peru. Analyzing oxygen isotope and trace element concentration data and comparing it with strontium isotope data from the same individuals provides a more detailed picture of residential mobility in the Tiwanaku and Chiribaya polities. In addition to monitoring diagenetic contamination, trace element concentration data identified movement during adulthood for certain individuals. However, these data could not distinguish movement between the Moquegua and Ilo Valleys. While oxygen isotope data could clearly distinguish the high-altitude sites from others, more data is needed to characterize the local oxygen isotope ratios of these regions. These data demonstrate the potential for archaeological reconstruction of residential mobility through multiple lines of evidence.     

山西陶寺遗址出土人骨的病理和创伤

本文对陶寺文化中晚期部分墓葬和灰坑中出土的人骨的牙齿病理和头骨创伤进行了观察。病理观察项目包括龋齿、牙周病、牙齿釉质发育不全三个指标, 还对稳定同位素15N数据进行了再分析。研究结果指出, 牙齿的龋齿率处于较低水平, 其原因可能有两个方面, 一是调查人群的平均年龄相当低; 二是与陶寺人群的饮食中有一定比例的肉食量有关。这一认识得到陶寺早期人群牙齿磨耗速率的研究和对稳定同位素δ15N数据的再分析的支持。另外, 牙周病的调查结果显示墓葬和灰坑人骨半数以上个体都有牙周病。牙齿釉质发育不全的调查显示, 约三分之一的陶寺人群在其儿童生长发育过程中受到机体代谢压力的影响, 如常患感染性疾病、发烧或营养失调等。灰坑再现的乱骨现象以及头骨片上多见的创缘和裂缝反映出人群之间的暴力色彩, 折射出陶寺社会矛盾的激化和动荡。     

Apotropaic Practices and the Undead: A Biogeochemical Assessment of Deviant Burials in Post-Medieval Poland

Apotropaic observances-traditional practices intended to prevent evil-were not uncommon in post-medieval Poland, and included specific treatment of the dead for those considered at risk for becoming vampires. Excavations at the Drawsko 1 cemetery (17^th–18^th c. AD) have revealed multiple examples (n = 6) of such deviant burials amidst hundreds of normative interments. While historic records describe the many potential reasons why some were more susceptible to vampirism than others, no study has attempted to discern differences in social identity between individuals within standard and deviant burials using biogeochemical analyses of human skeletal remains. The hypothesis that the individuals selected for apotropaic burial rites were non-local immigrants whose geographic origins differed from the local community was tested using radiogenic strontium isotope ratios from archaeological dental enamel. ⁸⁷Sr/⁸⁶Sr ratios ( = 0.7112±0.0006, 1σ) from the permanent molars of 60 individuals reflect a predominantly local population, with all individuals interred as potential vampires exhibiting local strontium isotope ratios. These data indicate that those targeted for apotropaic practices were not migrants to the region, but instead, represented local individuals whose social identity or manner of death marked them with suspicion in some other way. Cholera epidemics that swept across much of Eastern Europe during the 17^th century may provide one alternate explanation as to the reason behind these apotropaic mortuary customs, as the first person to die from an infectious disease outbreak was presumed more likely to return from the dead as a vampire.     

Is the Sr isotope ratio of mosses a good indicator for Asian dust (Kosa)?

The need for monitoring Asian dust is increasing owing to concerns about its harmful effects on ecosystems and human health. Strontium isotope ratios of mosses can be used to monitor Asian dust because of the traceability of these ratios and nutrient uptake by mosses from atmospheric deposition. Hence, the present study examined the suitability of strontium isotope ratios of mosses for monitoring Asian dust. Given the higher strontium isotope ratios of Asian dust than those of domestic origins, these ratios of mosses would be higher in areas with Asian dust. Moss samples were collected from 13 sites across Japan. The strontium isotope ratios of mosses in all study sites were lower than those of Asian dust. Although western Japan is more strongly influenced by Asian dust than eastern Japan, there were no significant differences in the strontium isotope ratios between these regions. Notably, the strontium isotope ratios of mosses significantly and positively correlated with those of the local soil across the study sites. These results indicate that strontium in mosses was derived from the local soil, and this uptake pattern may be attributed to a considerable supply of soil-derived strontium. In conclusion, the strontium isotope ratio of mosses is not a suitable indicator for the influence of Asian dust in Japan. Future studies should investigate whether these results could be applied to epiphytic mosses as potential indicators for Asian dust because epiphytes are less influenced by soil-derived minerals than terrestrial mosses.

     

Earliest Evidence for Social Endogamy in the 9,000-Year-Old-Population of Basta,Jordan

The transition from mobile to sedentary life was one of the greatest social challenges of the human past. Yet little is known about the impact of this fundamental change on social interactions amongst early Neolithic communities, which are best recorded in the Near East. The importance of social processes associated with these economic and ecological changes has long been underestimated. However, ethnographic observations demonstrate that generalized reciprocity – such as open access to resources and land – had to be reduced to a circumscribed group before regular farming and herding could be successfully established. Our aim was thus to investigate the role of familial relationships as one possible factor within this process of segregation as recorded directly in the skeletal remains, rather than based on hypothetical correlations such as house types and social units. Here we present the revealing results of the systematically recorded epigenetic characteristics of teeth and skulls of the late Pre-Pottery Neolithic community of Basta in Southern Jordan (Figure S1). Additionally, mobility was reconstructed via a systematic strontium (Sr) isotope analysis of tooth enamel of the Basta individuals. The frequency of congenitally missing maxillary lateral incisors in the 9,000-year-old community of Basta is exceptionally high (35.7%). Genetic studies and a worldwide comparison of the general rate of this dental anomaly in modern and historic populations show that the enhanced frequency can only be explained by close familial relationships akin to endogamy. This is supported by strontium isotope analyses of teeth, indicating a local origin of almost all investigated individuals. Yet, the accompanying archaeological finds document far-reaching economic exchange with neighboring groups and a population density hitherto unparalleled. We thus conclude that endogamy in the early Neolithic village of Basta was not due to geographic isolation or a lack of exogamous mating partners but a socio-cultural choice.     

Structural studies of human alkaline phosphatase in complex with strontium: implication for its secondary effect in bones

Strontium is used in the treatment of osteoporosis as a ranelate compound, and in the treatment of painful scattered bone metastases as isotope. At very high doses and in certain conditions, it can lead to osteomalacia characterized by impairment of bone mineralization. The osteomalacia symptoms resemble those of hypophosphatasia, a rare inherited disorder associated with mutations in the gene encoding for tissue-nonspecific alkaline phosphatase (TNAP). Human alkaline phosphatases have four metal binding sites--two for zinc, one for magnesium, and one for calcium ion--that can be substituted by strontium. Here we present the crystal structure of strontium-substituted human placental alkaline phosphatase (PLAP), a related isozyme of TNAP, in which such replacement can have important physiological implications. The structure shows that strontium substitutes the calcium ion with concomitant modification of the metal coordination. The use of the flexible and polarizable force-field TCPEp (topological and classical polarization effects for proteins) predicts that calcium or strontium has similar interaction energies at the calcium-binding site of PLAP. Since calcium helps stabilize a large area that includes loops 210-228 and 250-297, its substitution by strontium could affect the stability of this region. Energy calculations suggest that only at high doses of strontium, comparable to those found for calcium, can strontium substitute for calcium. Since osteomalacia is observed after ingestion of high doses of strontium, alkaline phosphatase is likely to be one of the targets of strontium, and thus this enzyme might be involved in this disease.     

Health status of the Neolithic population of Alepotrypa Cave, Greece

During the Neolithic, human health and lifestyle changed following the adoption of domesticated plants and animals and sedentism. This paper presents a study on human osteological remains from Alepotrypa Cave, an important and very well-preserved Late and Final Greek Neolithic site occupied from 5000-3200 BC. The Alepotrypa sample comes from primary and secondary burials as well as scattered bone, and consists of a minimum number of 161 individuals. It includes equal proportions of adults and subadults and males and females, is characterized by high child mortality, and falls within the range of other Neolithic sites in terms of age profiles and stature. The most frequent pathological conditions observed in this population are: 1) anemic conditions (cribra orbitalia and porotic hyperostosis), mild or healed in manifestation, most probably of nutritional origin, resulting from a poor diet focused on terrestrial resources such as domesticated cereals; 2) osteoarthritis and musculoskeletal stress markers, indicative of increased physical activity and heavy workloads; and 3) elevated prevalence of healed, depressed cranial fractures, serving as evidence of violent, nonlethal confrontations. Teeth exhibit a low prevalence of dental carries and linear enamel hypoplasia. The overall demographic, pathological, and behavioral results are consistent with observations of Neolithic populations elsewhere in Greece and the Mediterranean.