Temporal and spatial variation of dental pattern in the voles, Microtus arvalis, of the Orkney Islands

A sample of first lower molars of Microtus arvalis of Neolithic age from the Orkney island of Westray was compared with respect to size and shape with other Neolithic and Recent samples of the species. The results show (1) a decline in size since the Neolithic on Westray (as on Orkney Mainland) and (2) divergence in shape between populations from Westray and Orkney Mainland since the Neolithic. Comparisons were also made with continental samples, and explanations of the origin and large size of the Orkney voles are reviewed.     

福建漳平奇和洞发现的新石器时代早期人类头骨

2011年在福建漳平奇和洞发现的距今1万年左右的新石器时代早期人类遗骸"奇和洞III号",是迄今在福建地区发现的最早、最完整的古人类头骨,为探讨华南更新世晚期向全新世过渡阶段人类的体质特征及现代人群的形成与分化提供了重要的研究材料。本文对这件头骨进行了研究,奇和洞III号为35岁左右的男性个体,牙齿龋病严重,推测当时人类的经济模式主要以农耕为主。通过与更新世晚期柳江、山顶洞101号及14组新石器时代人类头骨的比较,发现奇和洞III号头骨兼有更新世晚期人类及新石器南、北方居民的混合体质特征:奇和洞III号头骨长而脑量大,似更新世晚期人类;其高而狭窄的面部、宽阔而低矮的鼻部,呈现出不同于南、北方人群的特殊体质特征。主成分分析显示,奇和洞III号与对比的新石器时代各组在头骨的测量数据上没有表现为明显的南、北地区间差异,但在头骨的测量指数或形状上存在时代和地区间的不同。本文研究为新旧石器过渡阶段人类体质特征的变异提供了进一步证据。     

Beyond the Levant: First Evidence of a Pre-Pottery Neolithic Incursion into the Nefud Desert,Saudi Arabia

Pre-Pottery Neolithic assemblages are best known from the fertile areas of the Mediterranean Levant. The archaeological site of Jebel Qattar 101 (JQ-101), at Jubbah in the southern part of the Nefud Desert of northern Saudi Arabia, contains a large collection of stone tools, adjacent to an Early Holocene palaeolake. The stone tool assemblage contains lithic types, including El-Khiam and Helwan projectile points, which are similar to those recorded in Pre-Pottery Neolithic A and Pre-Pottery Neolithic B assemblages in the Fertile Crescent. Jebel Qattar lies ∼500 kilometres outside the previously identified geographic range of Pre-Pottery Neolithic cultures. Technological analysis of the typologically diagnostic Jebel Qattar 101 projectile points indicates a unique strategy to manufacture the final forms, thereby raising the possibility of either direct migration of Levantine groups or the acculturation of mobile communities in Arabia. The discovery of the Early Holocene site of Jebel Qattar suggests that our view of the geographic distribution and character of Pre-Pottery Neolithic cultures may be in need of revision.     

Iberia: population genetics, anthropology, and linguistics.

Basques, Portuguese, Spaniards, and Algerians have been studied for HLA and mitochondrial DNA markers, and the data analysis suggests that pre-Neolithic gene flow into Iberia came from ancient white North Africans (Hamites). The Basque language has also been used to translate the Iberian-Tartesian language and also Etruscan and Minoan Linear A. Physical anthropometry of Iberian Mesolithic and Neolithic skeletons does not support the demic replacement in Iberia of preexisting Mesolithic people by Neolithic people bearing new farming technologies from Europe and the Middle East. Also, the presence of cardial impressed pottery in western Mediterranean Europe and across the Maghreb (North Africa) coasts at the beginning of the Neolithic provides good evidence of pre-Neolithic circum-Mediterranean contacts by sea. In addition, pre-dynastic Egyptian El-Badari culture (4,500 years ago) is similar to southern Iberian Neolithic settlements with regard to pottery and animal domestication. Taking the genetic, linguistic, anthropological, and archeological evidence together with the documented Saharan area desiccation starting about 10,000 years ago, we believe that it is possible that a genetic and cultural pre-Neolithic flow coming from southern Mediterranean coasts existed toward northern Mediterranean areas, including at least Iberia and some Mediterranean islands. This model would substitute for the demic diffusion model put forward to explain Neolithic innovations in Western Europe.     

Europe, the bull and the Minotaur: the biological legacy of a Neolithic love story

The European cattle was domesticated 10 000 years ago in eastern Turkey, 1000 years later pottery-associated milk fats identify cattle-based dairy activity in western Turkey. Subsequently, the Indo-European language, domesticated animals and plants travel as a Neolithic package along two major routes across Europe. A striking south-east to north-west gradient of a mutation in the current European population (lactase persistence into adulthood) documents the expansion of a Neolithic dairy culture into a Mesolithic hunter society. Using oral tradition (myths), archaeological and written historical evidence and biological data, it is asked whether highly transmissible viral diseases like measles and smallpox entered during the Neolithic from domesticated animals into the human population. The bovine origin of paramyxovirus infections is likely; smallpox comes from camels or from rodents via cattle while mycobacteria and Helicobacter infected humans already before the Neolithic. Microbes adapt constantly and quickly to changing ecological situations. The current global environmental changes will lead to another highly dynamic phase of viral transmissions into the human population.     

Dietary change and the effects of food preparation on microwear patterns in the Late Neolithic of abu Hureyra, northern Syria

Comparison of the microwear features created on the occlusal surfaces of molar teeth from different cultural horizons at abu Hureyra, northern Syria, indicates that the hardness of the food eaten changed profoundly after the introduction of domestic cereal grains at the beginning of the Neolithic (Neolithic 2A), and again after the introduction of pottery in Neolithic 2C times. Comparison with the microwear features on the teeth of human groups known to eat cooked food demonstrated the identity of the microwear on the abu Hureyra teeth from the pottery levels with those who had eaten cooked food. It is suggested that the evidence for an increase in the population in Neolithic 2C times is a direct consequence of changes in food preparation techniques.     

Pollen and phytolith evidence for rice cultivation during the Neolithic at Longqiuzhuang, eastern Jianghuai, China

Phytolith and pollen analyses were carried out at the archaeological site at Longqiuzhuang in Gaoyou, Jiangsu, southern China. The results indicate that the key morphological phytolith types associated with cultivated rice (Oryza) are common in the Neolithic cultural layers at this site. The evidence strongly suggests that cultivated rice (mainlyO. japonica) was grown locally during the Neolithic. The archaeopalynological record provides information about the impact of human activity and, in particular, farming on the natural vegetation. The evergreen and deciduous broad-leaved forest was substantially altered, and herbaceous taxa, including ruderals, expanded. Based on the results from the phytolith and pollen analyses, two distinct phases of human activity have been recognized, namely (1) phase A (7000-6300 B.P., i.e. early Neolithic) a warm and humid period when arable farming, including rice cultivation, was pursued but the variation in the size of the carbonized rice grains was low, and (2) phase B (6300-5500 B.P., late Neolithic age), a period of relatively cold and/or arid climate when cultivated rice was of major importance and was morphologically similar to present-day rice. Environment, and in particular climate change in the late Neolithic, were important factors affecting the development of rice as a cultivated crop. It was mainly during this period that artificial selection favoured the emergence of forms similar to those of today.     

New evidence for Neolithic rice cultivation and Holocene environmental change in the Fuzhou Basin,southeast China

A stratified profile of the Zhuangbianshan (ZBS) archaeological site (Fuzhou Basin, Fujian) was studied to investigate Neolithic era anthropogenic influence and associated environmental changes. Analysis of the archaeological sediments focused on phytoliths, palynomorphs and microcharcoal. Until now, a lack of direct evidence for agriculture has made it difficult to know if Neolithic cultures of this area relied on the exploitation of wild plants such as nuts and sago palm, or a combination of farming and foraging. Three types of rice phytoliths were found in ZBS archaeological deposits, providing robust evidence for rice farming as part of a broad-spectrum Neolithic subsistence economy centered on fishing and hunting. Chronologies based on AMS ¹⁴C dates and artifact typology place the earliest rice during the Tanshishan (TSS) Period (5,000–4,300 cal bp) followed by a shift to economic dependency on rice in the Huangguashan (HGS) Period (4,300–3,500 cal bp). The ZBS phytolith assemblage contains high frequencies of rice husk (peaked-shape glume cells) phytoliths, with far fewer leaf and stem types. This indicates late stage processing activities such as dehusking, implying a focus on consumption rather than rice production. High concentrations of charcoal in the Neolithic ZBS deposits indicate local human settlement and peaks in fire use. The ZBS pollen record also reflects human settlement and peaks in local forest clearance during the Neolithic. Forest cover was renewed when the site was temporarily abandoned following the Neolithic. Rapid formation of the Min River floodplain began ~2,000 cal bp in association with retreating sea level and intensifying anthropogenic influence. Prior to that, rice farming in the Fuzhou Basin was limited by the scarcity of wetlands suitable for agriculture.     

The Early Neolithic site at Hoge Vaart, Almere, the Netherlands, with particular reference to non-diffusion of crop plants, and the significance of site function and sample location

The construction of a new motorway necessitated the excavation of an Early Neolithic site in the Dutch Flevopolder near the Hoge Vaart canal. In 1994-1996, an area of ca. 1700 m² was excavated in 0.5x0.5-m squares. The excavation revealed 150 surface hearths and more than a hundred deep hearth pits. The finds, mainly flint and pottery, as well as¹⁴C dates from charcoal demonstrated that the area had been used mainly during the Early Neolithic (ca. 4900–4500 cal. B.C.). The investigation of the Early Neolithic remains included detailed botanical analyses of 182 samples and hand-sorting by the excavation team, which included archaeobotanists, of tens of thousands of samples sieved over 2-mm-mesh sieves. No remains of cultivated plants were recognised among the 87 taxa (40 identified to species level) that were preserved, mainly in carbonised form. These results are compared with other Early Neolithic sites studied in the Netherlands, such as Swifterbant S3 and Schokland P14. The possible significance of site function and sample location as important factors influencing presence/absence of cultivated plant remains at a particular site is discussed.     

Reconsidering the Early Neolithic of Anatolia. Recent recoveries,some excerpts and generalities

In the course of last decades Neolithic research has taken a new pace in Turkey, while projects in the western and the central parts of the of the country have been working mainly on the later stages of the Neolithic era, those in south-eastern Turkey had their focus on the incipient stages of neolithization. Work in the south-eastern parts, highlighted by the results attained at Göbeklitepe has been carrying out large scale excavations at several Pre-Pottery Neolithic sites, most of them having their earliest layers by the very beginning of PPNA, evidence of antecedent stages being highly debatable. Recent recoveries have been greatly elaborating our understanding on the entire span of Neolithic way of living, also displaying the differences among distinct core areas of neolithization. However, more significant is the outcome of new research taking place in the Upper Euphrates-Upper Tigris basins of south-eastern Anatolia, revealing ground breaking results so different from our conventional perceptions that redefining what is implied by the term Neolithic is now stands as an absolute necessity; inevitably some more time is necessary for the newly emerging picture on Neolithic process to sink in. However, some of the recent findings being unexpectedly different is apt to lead to speculative misconceptions, particularly when coupled with deeply rooted biases of research history. In this respect, the paper will present a conspectus on the progressive stages of Neolithic research in Anatolia, touching upon some biases in retrospect. Accordingly, the paper neither intends to cover an exclusive narrative of research history nor to bring the highlights of present research; it is targeted to surface the modalities that patterned past research so as a provide a subtle bases to future prospects.     

Human impact as registered in the pollen record: some results from the western Lake Constance region,Southern Germany

Pollen analytical results from a littoral profile taken in Lake Constance compared with pollen profiles from small kettle holes nearby form the basis for conclusions concerning human population density, the economy and environment from the Neolithic period to the Middle Ages. Early Neolithic human impact is implicated in a lime decline and also the expansion of beech. The late Neolithic lakeshore settlements caused a decline of elm, beech and lime and, by shifting cultivation, considerably changed the forest cover. The settlements were abandoned after less than 100 years. There were long periods without distinct human impact in the middle and towards the end of the late Neolithic period. Since at least the Late Bronze Age there has been permanent habitation in the region. Human impact was greatest in the High Medieval period and later, and was also substantial in the late La Tène and Roman periods. Distinct declines in human impact can be observed between the La Tène and Roman periods and in the Migration and Merovingian periods. In these intervals, open land and grazed oak forest were replaced by birch and later on by beech forests. The decreases in human impact are not of the same intensity in all diagrams.     

Body size, body proportions, and mobility in the Tyrolean "Iceman"

Body mass and structural properties of the femoral and tibial midshafts of the "Iceman," a late Neolithic (5,200 BP) mummy found in the Tyrolean Alps, are determined from computed tomographic scans of his body, and compared with those of a sample of 139 males spanning the European early Upper Paleolithic through the Bronze Age. Two methods, based on femoral head breadth and estimated stature/bi-iliac (pelvic) breath, yield identical body-mass estimates of 61 kg for the Iceman. In combination with his estimated stature of 158 cm, this indicates a short but relatively wide or stocky body compared to our total sample. His femur is about average in strength compared to our late Neolithic (Eneolithic) males, but his tibia is well above average. His femur also shows adaptations for his relatively broad body (mediolateral strengthening), while his tibia shows adaptations for high mobility over rough terrain (anteroposterior strengthening). In many respects, his tibia more closely resembles those of European Mesolithic rather than Neolithic males, which may reflect a more mobile lifestyle than was characteristic of most Neolithic males, perhaps related to a pastoral subsistence strategy. There are indications that mobility in general declined between the European Mesolithic and late Neolithic, and that body size and shape may have become more variable throughout the continent following the Upper Paleolithic.     

郑州青台遗址新石器时代中晚期人群龋齿的统计与分析

本文通过对郑州青台遗址新石器时代中晚期91例个体、1913枚牙齿罹患龋齿的统计与分析可知,青台人群患龋率为71.43%,龋齿率为13.38%。其中,龋齿率女性高于男性,可能与女性孕期生理变化、食物选择及性别分工等有关。上颌龋齿率高于下颌,臼齿及咬合面为龋齿易患齿类及部位。通过对比可知青台人群显示出较高的龋齿罹患率,暗示该人群饮食中应包含较多的碳水化合物类食物,这可能与新石器时代中晚期黄河中游发达的旱作农业有关。此外,龋齿率在黄河及长江中、下游新石器时代农业人群中的区域性差异可能与龋病病因的复杂性和各地区不同的文化面貌、人群生活方式有关。     

香港壕涌遗址孢粉、植硅石组合及其环境考古

香港壕涌遗址孢粉、植硅石组合表明：自新石器时期以来该遗址周围植被以热带-亚热带蕨类植物为主;草本植物以禾本科、莎草、藜科等主为;在遗址附近的高地及山坡上生长了常绿阔叶林,其成分包括：阿丁枫香属（Altingia）、栲属（Castanopsis ）、常绿栎（evergrenn Quercus）、棕榈（Palmae）等;植被面貌是人类活动干扰的结果。新石期时期,遗址受海水影响,人类活动以采集、捕捞为主;唐宋时期,禾本科花粉及典型水稻硅酸体的大量出现,反映了稻作农业的发展及人类生存方式的改变。     

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.     

Neolithic greenstone in Umbria, from the Bellucci Collection. Petrography, provenance, interpretation

Sixty-six stone tools sampled through archaeological criteria, all but six from the Bellucci Collection in the Archaeological Museum, Perugia, are presented. Sixty-four of them are axes or chisels (two) of Neolithic typology, and save a few of them all are complete and largely polished; two are Chalcolithic shaft-holed axes. Sixty tools are made of HP-metaophiolites (33 eclogites, 26 Na-px jades, 1 serpentinite), the same lithologies dominant in Neolithic implements found in Northern Italy. Their study gives the first petrographic evidence of an important supply of these lithologies from the NW Italy production areas towards Central Italy. Three implements (including one shaft-holed axe) are made of sedimentary rocks of local origin. Three others (including one shaft-holed axe), made of lavic volcanites pertaining to the Tyrrhenian Quaternary potassic volcanism of Central — Southern Italy, provide evidence of occasional sources from the South to Umbria, lasting from the Neolithic to Chalcholitic periods.      

The chickpea, summer cropping, and a new model for pulse domestication in the ancient near east

The widely accepted models describing the emergence of domesticated grain crops from their wild type ancestors are mostly based upon selection (conscious or unconscious) of major features related either to seed dispersal (nonbrittle ear, indehiscent pod) or free germination (nondormant seeds, soft seed coat). Based on the breeding systems (self-pollination) and dominance relations between the allelomorphs of seed dispersal mode and seed dormancy, it was postulated that establishment of the domesticated forms and replacement of the wild ancestral populations occurred in the Near East within a relatively short time. Chickpea (Cicer arietinum L.), however, appears as an exception among all other "founder crops" of Old World agriculture because of its ancient conversion into a summer crop. The chickpea is also exceptional because its major domestication trait appears to be vernalization insensitivity rather than pod indehiscence or free germination. Moreover, the genetic basis of vernalization response in wild chickpea (Cicer reticulatum Ladiz.) is polygenic, suggesting that a long domestication process was imperative due to the elusive phenotype of vernalization nonresponsiveness. There is also a gap in chickpea remains in the archaeological record between the Late Prepottery Neolithic and the Early Bronze Age. Contrary to the common view that Levantine summer cropping was introduced relatively late (Early Bronze Age), we argue for an earlier (Neolithic) Levantine origin of summer cropping because chickpea, when grown as a common winter crop, was vulnerable to the devastating pathogen Didymella rabiei, the causal agent of Ascochyta blight. The ancient (Neolithic) conversion of chickpea into a summer crop required seasonal differentiation of agronomic operation from the early phases of the Neolithic revolution. This topic is difficult to deal with, as direct data on seasonality in prehistoric Old World field crop husbandry are practically nonexistent. Consequently, this issue was hardly dealt with in the literature. Information on the seasonality of ancient (Neolithic, Chalcolithic, and Early Bronze Age, calibrated 11,500 to 4,500 years before present) Near Eastern agriculture may improve our understanding of the proficiency of early farmers. This in turn may provide a better insight into Neolithic agrotechniques and scheduling. It is difficult to fully understand chickpea domestication without a Neolithic seasonal differentiation of agronomic practice because the rapid establishment of the successful Near Eastern crop package which included wheats, barley, pea, lentil, vetches, and flax, would have preempted the later domestication of this rare wild legume.     

Genomics at the origins of agriculture,part one

The causes and consequences of the Neolithic revolution represent a fundamental problem for anthropological inquiry. Traditional archeological evidence, ethnobotanical remains, artifacts, and settlement patterns have been used to infer the transition from foraging to primary food production. Recent advances in genomics (the study of the sequence, structure, and function of the genome) has enhanced our understanding of the process of plant and animal domestication, revealed the impact that adaptation to agriculture has had on human biology, and provided clues to the pathogens and parasites thought to have emerged during the Neolithic. Genomic analysis provides insights into the complexity of the process of domestication that may not be apparent from the physical remains of bones and seeds, and allows us to measure the impact that the shift to primary food production had on the human genome. Questions related to the location and the process of domestication can be answered more fully by analyzing the genomes of the plants and animals brought under human control. The spread of the agriculture package (plants, animals, and technology) by cultural diffusion or demic expansion can also be investigated through this approach. Whether dissemination by farmers or the diffusion of farming knowledge and technology was the source of the Neolithic expansion, this process should be revealed by the patterh of genetic and linguistic diversity and language found from centers of agricultural Neolithic development. In addition, a number of pathogens that were previously thought to have been transmitted from domesticated species to human now appear to have been present in foragers long before the agricultural revolution took place. Furthermore, we now have evidence that humans were the source of the transmission of some parasites to domesticated animals. For all of these reasons, data from genomic studies are providing a more complete understanding of the origins of agriculture, a critical hallmark in human evolution.     

磨盘山遗址新石器时代人骨研究

磨盘山遗址是分布在云南省楚雄彝族自治州元谋盆地的一处新石器时代聚落。本文通过对遗址出土的6例新石器时代人骨的体质人类学研究,得出以下结论:磨盘山组颅骨的形态特征可以概括为中颅型与正颅型相结合,阔额型、阔上面型、阔鼻型、中眶型并伴有颇大的面部扁平度;磨盘山组应属于亚洲蒙古人种范畴,在次级分类比较中与南亚类型在鼻眶形态和上面部形态上表现出更多的相似性;在与亚洲蒙古人种各近代组的比较中,磨盘山组与广西壮族组关系最为密切,与蒙古组关系最为疏远;在与其他新石器对比组的比较中,磨盘山组与代表"古华南类型"的甑皮岩组、鲤鱼墩组和昙石山组表现出更多的一致性,与"古中原类型"和"古华北类型"关系疏远。     

Les haches polies du site de Chastel-sur-Murat (commune de Chastel-sur-Murat,Cantal, France)

A study of 25 probably Middle Neolithic polished axes discovered at the beginning of the 20th Century in the site of Chastel-sur-Murat (Cantal, France), allowed to establish the origin of these objects. Some were shaped in rocks of the sector (basalts and fibrolites). The other ones result from regions several hundred kilometres apart: cinerite from Aveyron, flint from Berry, eclogite from the Italian Alps. This surprising variety confirms the existence of long-distance traffic currents of lithic raw materials during the Neolithic. To cite this article: A. de Goër de Herve et al., C. R. Palevol 1 (2002) 123–128.