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Table of Content

    15 June 2006, Volume 25 Issue 02
    A dental morphological observation on the neolithic human skeletons from Jiangjialiang, Yangyuan, Hebei Province
    LI Fajun, ZHU Hong
    2006, 25(02):  87-101. 
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    The author researched the dental morphological traits of Neolithic human skeletons from Jiangjialiang, Yangyuan in Hebei Province, China, using the method based on the Arizona State University Dental Anthropology System and multivariate analysis of Mean Measure of Divergence (MMD). The author found dental morphology of Jiangjialiang skeletons belonged to the Sinodontic type. And yet, there are some unique traits, such as the great appearance of shoveling in the UI 1 and UP 1 1root. The frequencies of occurrence of some traits such as UI 1 shoveling, UI 1 double shoveling, and LM 1 deflect wrinkle are also very high. The author found that the northeastern Asian groups have a distant morphological distance compared to southeastern Asian groups. In terms of dental morphological traits, Jiangjialiang people have a closer relationship with Miaozigou people than with the Xiawanggang people. As we have known, the Jiangjialiang and Miaozigou people also have similar skull traits, but more research needs to be conducted on dental traits to confirm this association.
    Cribra orbitalia on the bronze age skulls from Yanghai cemetery in Shanshan, Xinjiang
    ZHANG Quanchao, ZHU Hong
    2006, 25(02):  102-105. 
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    While cribra orbitalia studies have been undertaken in many parts of the world, until recently little was known about ancient human health in China. Focusing on skeletal pathologies, this paper documentsthe results of the first complete analysis of frequencies and pathogenic factors of cribra orbitalia of Bronze Age skulls from Xinjiang, China. The incidence of cribra orbitalia of 61skulls from Yanghai cemetery were observed, with the following results: 44.4% of 45 adults had cribra orbitalia; and 75% presence in the group of age 16 and under. Therewas also a marked sexual difference in the frequency of cribra orbitalia. Since the Yanghai nationality did not have enough food or lived mainly on flesh without enough iron, these results suggest that iron deficiency anemia is the major cause of cribra orbitalia.
    Paleolithic artifacts from Shirengou Site, Helong County, Yanbian City
    CHEN Quanjia, WANG Chunxue , FANG Qi, ZHAO Hailong
    2006, 25(02):  106-114. 
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    Forty stone artifacts were unearthed from the primary context of archaeological deposits at the Shirengou site, Helong county, Yanbian city of Jilin province. These objects include cores, flakes, microblades, used flakes, scrapers, burins and backed knives. Obsidian is the only raw material used for this stone assemblage. Major blanks for tools fabrication are flakes and blades. The principal flaking technique at the site is mainly direct hammer percussion, also indirect percussion. Modified tools appear to be retouched by direct hard hammer percussion, mostly soft hammer percussion, followed by pressure technique. According to the characteristics of this deposit (such as no polish on the stone artifacts, and no pottery) and the stratum yielding the stone artifacts, we suggest that the site is probably late Late Pleistocene or Late Paleolithic.
    New findings and dates of the Shibazhan Paleolithic site, Heilongjian Province
    ZHANG Xiaoling , YU Huili, GAO Xing
    2006, 25(02):  115-128. 
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    New excavations were carried out at the Shibazhan Paleolithic site in Tahe Country, Heilongjiang Province. This paper describes and analyzes 58 artifacts: 38 pieces of stone were unearthed from B and C layers, and 20 pieces of stone were collected from the ground surface nearby. Blades are important components of this assemblage, which is similar to the Shuidonggou site located at Ningxia Hui Autonomous Region. A bifacial specimen and a round-end scraper collected on the ground exhibit close resemblance to the stone tool types from some microlithic sites in northern China and the far eastern region of Russia. The absolute date of the four layers of this site were dated by optically stimulated luminescence (OSL), and two cultural stages were established, namely 25 ka BP (Level C) and 10 ka BP (Level B), respectively.
    With its location in northeastern China and on the basis of morphological characters of these stone artifacts, the Shibazhan Paleolithic site provides important data for studying northeastern Asian human migration and cultural communication during late Pleistocene and early Holocene.
    A study of Wedge-shaped cores from Hutouliang Site
    ZHU Zhiyong , GAO Xing
    2006, 25(02):  129-142. 
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    Hutouliang site is located in the Nihewan Basin near Hutouliang village of Yang Yuan County, Hebei Province in northern China. The site had been excavated from 1972 to 1974 for three successive seasons and a large number of artifacts including simple cores, discoid cores, pillar cores bipolar cores, wedge-shaped cores, choppers, scrapers, points, awls and adze-shaped tools, were collected from the site.
    In this paper , 444 wedge2shaped cores unearthed from the Hutouliang site are studied using typological and statistical analyses. On the basis of the differences of core platforms, these wedge-shaped cores can be classified into two types. The platform of Type Ⅰis edge-shaped, whereas the platform of Type Ⅱis flat. According to the ratio between height and length, Type Ⅰcan be classified into two subtypes-subtype ⅠA and ⅠB . In the ⅠA subtype, its length is twice of its height. In the ⅠB subtype, its height is twice of its length. According to different strategies of making the platform, Type Ⅱcan be classified into two subtypes: ⅡA and ⅡB. The platform of subtype ⅡA is made by longitudinal striking, whereas the platform of subtype ⅡB is made by cross2wise striking.
    The purpose of producing both types is to obtain microblades of lengths between 10—40mm, and widths of 3 —8mm. Raw materials include breccia, siliceous rhyolite, quartzite, jasper, agate, dacite, obsidian and crystal, with breccia and siliceous rock being the most important stone materials. These wedge-shaped cores made in different stages were abandoned for various reasons including reserving , exhausted and miscarriaging.
    A new study on the paleolithic materials from Liangshan site
    LU Na, HUANG Weiwen, YIN Shenping, HOU Yamei
    2006, 25(02):  143-152. 
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    This paper is about new research on the Longgangsi locality of Liangshan site. At the southern foot of the Qinling Range, the Liangshan site is located in the upper reaches of the Hanshui River in Shaanxi Province and occupies a unique position in a transitional region of dividing northern and southern China. Discovered from the third terrace of Hanshui River in the 1950s and worked in 1980s, the Liangshan Paleolithic industry is known for its assemblage of chopper-chopping tools, spheroids, handaxes, cleavers, picks, and scrapers, etc. Bearing some morphological characters of the Acheulean tradition of most heavy-duty tool types, the Liangshan culture has close relationships with that of artifacts from Yunxian Man site, Dingcun, Lantian Man site, and Sanmenxia. This assemblage is also similar to Bose, Longgupo of southern China in terms of some characters of typology and technology. Research of Liangshan Paleolithic industry can help to lead to more discussion about environmental change and human migration in the geological period from late Lower Pleistocene to Middle Pleistocene.
    Formation and stratigraphy of the Chuanfan Cave
    LI Jianjun, FAN Xuechun
    2006, 25(02):  153-160. 
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    The Chuanfan Cave is one of two Paleolithic cave sites on the Wanshouyan Hill, a limestone hill with several caves and fissures situated about 17 km northwest of Sanming City, Fujian Province. Two Paleolithic cultural levels were recovered from the cave in 1999—2000. One of the significant archaeological discoveries at the site was an artificial pebble2paved living surface from the lower cultural level. This paper presents preliminary results of studies on the formation processes of the site and it stratigraphy based on information derived during the second excavation in 2004.
    The formation processes of the Chuanfan Cave follow four stages. 11The cave functioned as a passage for drainage during the late Middle Pleistocene and deposits began to accumulate (Layers 26—22, see Table 1) . 21The accumulated deposits suffered serious breakage and new sediments rich in mammalian fossils formed new layers (Layers 21—17). 31A flood brought new materials to the cave , which became Layers 16—7. 41Ravines developed in the deposits as the result of water movement and later filled with sediments (Layers 6—1) .
    Geological strata can be divided into four parts (from bottom to top) . Unit Ⅰ, late Middle Pleistocene deposits, gravel and sandy clay, with several kinds of fossil including Vespertolionidae, Petaurista sp., Niviventer sp., and Rhizomys sp.Unit Ⅱ, of early Late Pleistocene age, red-yellow clay and grayish green sandy clay, rich in mammalian fossils, such as Macaca robustus, Canis lupus, Coun dubius, Ailuropoda melanoleuca, Ursus thibetanus, Meles suillus, Crocuta ultima, Crocuta spelaeus, Acinonyx sp. , Stegodon orientalis, Rhinoceros sinensis, Megatapirus augustus, Sus scrofa. Unit Ⅲ, late Late Pleistocene deposits , greenish gray clay with two cultural layers identified. AMS dating indicates that Layer 15 and Layer 8 were formed 37 ka BP and 29 ka BP, respectively. Unit Ⅳ, of Holocene age, with mixed deposits and yielding Song to Qing Dynasties cultural remains.
    Artiodactylia from the Jinpendong site in Wuhu, Anhui Province
    DONG Wei, JIN Changzhu, ZHENG Longting, SUN Chengkai, LUJinyan, XU Qinqi
    2006, 25(02):  161-171. 
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    The systematic study of artiodactyls from the Jinpendong Paleolithic Site, Wuhu, Anhui Province, shows six identified species: Sus lydekkeri, Cervus ( Sika) nippon, Cervus ( Sika) grayi, Cervus elaphus, Muntiacus sp. and Bison cf. palaeosinensis. By the appearance of Cervus ( Sika) nippon and Cervus elaphus, this fauna is clearly cervid or browser dominated. This fauna is of a northern region and of an age younger than that of the Longtandong fauna associated with Homo erectus from Hexian, and equivalent to that of the upper Yinshan fauna associated with Homo sapiens from Chaoxian (i. e. , late stage of the Middle Pleistocene, or equivalent to Riss Glaciation) . This fauna suggests an ecological environment of forests of short trees with some limited shrubbery and grassland, and with a climate similar to that of Inner Mongolia and Gansu of today. The coexistence of three species of Cervus in the same horizon at the site suggests that the Jinpengdong Site is a location where prehistoric peoples dealt with prey from different habitats.