湖北郧县直立人遗址研究新进展

郧县人Ⅰ号头骨、郧县人Ⅱ号头骨分别于1989年5月和1990年6月出土于中国湖北省郧县直立人遗址。2000年以来中法两国学者对遗址进行了深入研究,在考古学、古人类学、沉积学、微观形态学、地球化学、磁性地层学、地球年代学和孢粉学研究方面取得了一些新成果。研究成果显示遗址的年代在距今984000~780000年之间,两具头骨化石的年代在距今936000年左右,是世界上更新世早期重要的直立人化石之一;郧县人遗址石制品面貌比较古老,是中国南方典型的砾石石器文化传统。     

Provenience,age and associations of archaic Homo sapiens crania from Lake Eyasi,Tanzania

Fifty years ago, an ethnographic expedition found primitive human fossils at Lake Eyasi, Tanzania. Subsequent emphasis has centered almost exclusively on cranial morphology, neglecting the discovery site and associated finds. Fauna has been deemed “essentially modern” and racemization dates suggest a late Pleistocene age for the hominid remains; these assessments have been advanced as consistent with a “terminal Middle Stone Age” antiquity. Based on recent observations at the site and new sediment analyses, a provisional sequence is now proposed: an earlier formation, the Eyasi Beds, is distinguished from later Pleistocene deposits, the Mumba Beds, the latter being partially calibrated by uranium series and radiocarbon dates. This evidence indicates that the Eyasi Beds, the probable source of the human fossils, are older than 130,000 years, and the fauna may include seven extinct large mammal species. Documented Eyasi Beds artifacts are mostly unspecialized Middle Stone Age types; no typological or technical features suggest later MSA specializations or innovations foreshadowing Later Stone Age industries. A series of core tools from the lakeshore suggests an industry of Sangoan aspect. All lines of evidence from the locality contradict the young amino acid racemization dates; artifacts and fauna, including archaic Homo sapiens remains, are of probable Middle Pleistocene age.     

中国旧石器时代考古反思

近年来,在中国旧石器时代考古学界屡屡爆出重大新闻,亦真亦幻,令人扑朔迷离。谢飞指出：“目前,解决上述重大学术问题显得非常乏力的原因,不是旧石器考古队伍的问题,而是文物管理部门和学术权威单位关注不够、组织不力的问题”。…此话切中要害．非常值得深思。     

Shell tool use by early members of Homo erectus in Sangiran,central Java,Indonesia: cut mark evidence

Sangiran has been known as a source of fossil Homo erectus but is better known for the absence of archaeological tools. Cut mark analysis of Pleistocene mammalian fossils documents 18 cut marks inflicted by tools of thick clamshell flakes on two bovid bones created during butchery at the Pucangan Formation in Sangiran between 1.6 and 1.5 million years ago. These cut marks document the use of the first tools in Sangiran and the oldest evidence of shell tool use in the world.     

A radiocarbon chronology for the complete Middle to Upper Palaeolithic transitional sequence of Les Cottés (France)

The Middle to Upper Palaeolithic transition is the key period for our understanding of Neanderthal and modern human interactions in Europe. The site of Les Cottés in south-west France is one of the rare sites with a complete and well defined sequence covering this transition period. We undertook an extensive radiocarbon dating program on mammal bone which allows us to propose a chronological framework of five distinct phases dating from the Mousterian to the Early Aurignacian at this site. We found that the Mousterian and Châtelperronian industries are separated from the overlying Protoaurignacian by a gap of approximately 1000 calendar years. Based on a comparison with Upper Paleolithic sites in Europe we see an overlap in the ages of Châtelperronian industries and Aurignacian lithic assemblages, which are usually associated with Anatomical Modern Humans, which is consistent with an acculturation at distance model for these late Neanderthals. The Proto and Early Aurignacian appear contemporaneous indicating that this transition was rapid in this region. Anatomically Modern Humans are present at the site of Les Cottés at least at 39,500 cal BP roughly coincident with the onset of the cold phase Heinrich 4.     

ESR dating of the Donggutuo Palaeolithic site in the Nihewan Basin, northern China

The fluvio-lacustrine sequences in the Nihewan Basin, northern China, provide important terrestrial archives about Palaeolithic settlements and, therefore, about early human occupation in high northern latitude in East Asia. Here we present detailed ESR dating of the Donggutuo Palaeolithic site, located in this basin. Four levels A, B, C and E of the Donggutuo archaeological layer yield ESR ages ranging from 1060±129 ka to 1171±132 ka with a mean of 1119±132 ka. The ages are consistent with the paleomagnetic data, which show that the Donggutuo Palaeolithic site lies just below the onset of the Jaramillo normal subchron (0.99–1.07 Ma). Furthermore, our results indicate that the reliable ESR dating range of bleached quartz using Ti-Li centre can be effectively extended to 1100 ka and the Ti-Li centre was zeroed before the last deposition, which requires improvement of the understanding of the bleaching mechanism conditions.     

Palaeolithic archaeology and the evolution of mind

This paper reviews recent archaeological studies concerning the evolution of mind. It is structured around four themes: language, intelligence, symbolism, and social learning. It includes reference to recent work in other disciplines that is either having, or likely to have, considerable impact on archaeological thought. The evolution of mind is a highly contentious subject, plagued by problems of definition and lacking an explicit methodology. This paper argues that the two most positive trends of recent work have been greater attempts at interdisciplinary studies and the integration of the study of cognition with that of hominid lifestyles.     

中国北方早期智人与直立人对环境适应性比较研究——L2时期的环境变化对人类演化的影响

直立人与早期智人在石器类型上的相似性反映了它们所处的相似的地质背景为他们提供了相似的石料;而在打片技术、用火等方面的差异可能反映了它们在适应环境能力上有一定的区别;和早期智人相比,直立人采用的适应方式可能要消耗更多的资源。L2时期恶劣的气候变化可能是直立人演化为早期智人的原因之一。     

长春地区(99)发现的动物化石和旧石器

本文对所发现的九处动物化石地点 (其中包括旧石器地点一处 )、37件动物化石以及石器和骨器进行分析研究。所发现的动物种类均属于东北地区晚更新世猛犸象—披毛犀动物群成员。石制工具具有细、小石器共有的特征 ,为东北地区细、小石器的深入研究提供了重要资料。依据石、骨器的性质分析 ,其年代应属于旧石器时代的晚期之末 ;又根据动物化石种属判断 ,其生存的地质时代为晚更新世的晚期。     

Research on the Palaeolithic and Neolithic of Hadramaut and Mahra

This paper presents some of the results of exploration and excavation by the Soviet-Yemeni expedition carried out between 1983 and 1990 in Hadramaut and Mahra. Oldowan, Acheulean, Middle Palaeolithic, Upper Palaeolithic, and'Neolithic'stone tool industries are attested, providing what is probably the most detailed sequence covering these periods in the entire Arabian peninsula.     

OSL dating using quartz fine grains extracted from loess in Upper Palaeolithic sites of Nihewan Basin, northern China

Although radiocarbon (¹⁴C) dating, uranium-series dating, and optically stimulated luminescence (OSL) dating have been conducted for Upper Palaeolithic sites in the Nihewan Basin, northern China, there is room for constructing a detailed chronological framework. In this study, loess sediments collected from two Upper Palaeolithic sites, Youfang site and Hutouliang site, were dated using the single-aliquot regenerative-dose (SAR) OSL protocol. OSL measurements for palaeodoses estimation used fine-grained quartz samples extracted from loess. OSL dating results were obtained as 10–17 ka. These OSL ages were consistent with the related stratigraphy of Palaeolithic sites, archaeological evidence and independent ¹⁴C ages.     

The paleolithic site of Longwangchan in the middle Yellow River,China: chronology,paleoenvironment and implications

The Longwangchan Paleolithic site, situated on the Yellow River terraces in the Hukou area, Shaanxi province, China, was found in 2003–2004, and two areas (Localities 1 and 2) of the site were excavated in 2005–2008. Abundant stone artifacts including microliths, a grinding stone fragment and a shovel, with some animal bones and shells, were recovered from Locality 1. In this study, the cultural deposits from Locality 1 were dated using radiocarbon and optical dating techniques, and the sediment properties of the deposits were analyzed. The results show that the age of the deposits ranges from 29 to 21 ka and most of them were deposited between 25 ka and 29 ka. This indicates that corresponds to late Marine Isotope Stage (MIS) 3 and early MIS 2. During the human occupation period, the climate in this area became colder and drier. Sediments from beds where the grinding slab and the shovel were found were dated to ∼25 ka, which is the oldest among the grinding stones found in China. The microliths and the grinding stone are important evidence for an incipient socio-economic process that eventually led to the regional transition from hunting-foraging to farming.     

The chronology of Neolithic dispersal in Central and Eastern Europe

We analyze statistically representative samples of radiocarbon dates from key Early Neolithic sites in Central Europe belonging to the Linear Pottery Ceramic Culture (LBK), and of pottery-bearing cultures on East European Plain (Yelshanian, Rakushechnyi Yar, Buh-Dniestrian, Serteya and boreal East European Plain). The dates from the LBK sites form a statistically homogeneous set with the probability distribution similar to a single-date Gaussian curve. This implies that the duration of the spread of the LBK is shorter than the available temporal resolution of the radiocarbon dating; therefore, the rate of spread must be larger than 4 km/yr, in agreement with earlier estimates. The East European sites exhibit a broad probability distribution of dates. We identify in these data a spatio-temporal sequence from south-east to north-west, which implies the rate of spread of the initial pottery-making of the order of 1.6 km/yr, comparable to the average rate of spread of the Neolithic in Western and Central Europe. We argue that this spatio-temporal sequence is consistent with an idea that the tradition of the initial pottery-making on East European Plain developed under an early impulse from the Eastern Steppe.     

Particle size distribution of lithic assemblages and taphonomy of Palaeolithic sites

Lithic debris derived from knapping and used tools can be assimilated to simple sedimentary particles that may undergo size sorting when exposed to geomorphic processes such as streamflow or overland flow. Sorting can be identified by comparing the size distribution of archaeological assemblages to that of experimental core reduction sequences. A new database including different types of raw material (mainly flint and quartzite) and Palaeolithic debitage (blade, Levallois, discoid, on anvil, and shaping) has been built for this purpose. Palaeoeskimo data have also been added to illustrate microlithic industries. For all the debitages and raw materials, the particle size of knapping products >2 mm in width fits with a power-law distribution and shows only minor fluctuations, the range of which is always <15% between experiments (all steps of the chaîne opératoire included up to the final tool). A lithic assemblage derived from block/core knapping or blank/preform production will display a particle size distribution close to the experimental distributions if not subsequently modified. Modifications may originate either from sedimentary processes or from anthropogenic factors. To help distinguishing amongst these, data on the impact of both water flows on sedimentary particles or experimental assemblages, and anthropogenic processes such as importation-exportation (of core, preforms or finished tools) or uneven spatial distribution of the different steps in core reduction and tool production within a site, are reviewed. By contrast to anthropogenic modifications, sedimentary processes are generally typified by strong impoverishment in or selective accumulation of fine-grained (<10 mm) artefacts together with a low intra-site variability (spatial homogenization) or a downslope size trend. Archaeological case studies taken from French Palaeolithic site are then detailed. Evidence for lithic redistribution implies that care should be taken in archaeological site analysis since sorting may impact significantly the initial techno-typological balance of the assemblage.     

A Palaeolithic fishhook made of ivory and the earliest fishhook tradition in Europe

Prehistoric fishhooks have previously been described in northern Europe as being common since the Mesolithic. Here we present a Final Palaeolithic ivory fishhook from the site Wustermark 22 (north-eastern Germany), the raw material of which is about 19,000 years old. Five further fishhooks were discovered in situ at the same site one of which has a calibrated radiocarbon age of about 12,300 years. The tool industries of flint artefacts and bone/antler tools are associated with descendants of the Federmesser-culture and the palynological context indicates a Younger Dryas environment. Wustermark 22 represents the largest collection of Palaeolithic fishhooks so far found at a single European site. A comparison with other sites in Europe, containing Palaeolithic fishhooks suggests that the appearance and development of fishhooks may be associated with a general change in resource availability during the Greenland Interstadial 1 (Bølling/Allerød warming), which is also connected with a change from late Upper Palaeolithic to Final Palaeolithic industries in Northern Central Europe. We conclude that Mesolithic fishhook tradition has its roots in the Final Palaeolithic.     

Palaeolithic Living Sites in Upper and Middle Egypt: A Review Article

Abstract

In 2000 Leuven University Press of Leuven, Belgium published a very important volume on the prehistory of Egypt entitled Palaeolithic Living Sites in Upper and Middle Egypt. Egyptian Prehistory Monographs 2, edited by Pierre M. Vermeersch. This impressive volume presents partial results of the fieldwork of the Belgian Middle Egypt Prehistoric Project of Leuven University in the Nile Valley, between Luxor and Assiut, carried out from 1976 to 1991, and in 1994. A second publication, Palaeolithic Quarrying Sites in Upper and Middle Egypt, also edited by Pierre M. Vermeersch, appeared in 2002 as the fourth volume of the series. The 2000 volume, under review here, is a collection of detailed reports on nine excavated Paleolithic living sites, ranging in time from Acheulean to Epipaleolithic, complemented by a chapter on Quaternary geomorphology and stratigraphy of the Makhadma area, near Qena, as well as a study of chronology, subsistence, and environment of the Late Paleolithic fishing sites at Makhadma. The reviewers discuss in detail most of the sites reported and address the conclusions reached by the Belgian authors in light of their own experiences with the prehistory of the Egyptian Nile. Of particular interest are differences in views concerning late use of Levallois technology in the Nile Valley and the geomorphological history of the river.     

Defining and Characterising Clusters in Palaeolithic Sites: a Review of Methods and Constraints

Journal of Archaeological Method and Theory - Spatial analysis studies in Palaeolithic archaeology arise as indispensable research tools for understanding archaeopalaeontological sites. In general...     

Estimates of Upper Palaeolithic meta-population size in Europe from archaeological data

Three databases (2961 georeferenced archeological sites, simulated climatic variables simulating a typical “warm” phase of the isotopic stage 3 (IOS3 project), and ethnographic of hunter–gatherers (HG)) were used to estimate the size, growth rate and kinetics of the metapopulation of HG during four periods of the Upper Paleolithic in Europe. The size of the metapopulation was obtained by multiplying a demographic density (per 100 km²) by the size of the population territory of HG. Demographic density for each period was calculated by successively backprojecting a reference density obtained for the Late Glacial with inter-period growth rate of the archeological sites. From the Aurignacian to the Glacial Maximum, the metapopulation remained in a positive quasi-stationary state, with about 4400–5900 inhabitants (95% confidence interval (CI95%): 1700–37,700 inhabitants). During the Glacial Maximum, the metapopulation responded to the cold: (i) by moving the northern limits of its maximum expansion zone towards the low latitudes by 150–500 km from west to east, (ii) by concentrating in few refuge zones (mainly Périgord, Cantabria and the Ibérian coasts), (iii) by becoming perhaps distributed in smaller groups than during the pre and post Glacial Maximum. The metapopulation reached 28,800 inhabitants (CI95%: 11,300–72,600) during the mid-Late Glacial recolonisation.