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    15 September 1994, Volume 13 Issue 03
    Restudy of nine hand-axe specimens and the applicability of Movius'theory
    Lin Shenglong
    1994, 13(03):  189-208. 
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    The nine specimens which were considered as handaxes by some archaeologists (Huang, W., 1989) were restudied. The primary results are as follows:
    1. Specimen P.3468 from Pingliang (Fig.2)
    It is a heavy, pointed tool made on a cobble, with a minimum bifacial primary flaking and retouch. There is an oblique rideg on either face of the tool. The larger part of the upper face and the butt still remains the natural surface. The lenght of the edge is about 54% of the whole circumference. The butt is thick, robust and is also the most thick part of the tool. There is a prominent, flattish tip in the frontal end. Longitudinal section tends to be wedge-shaped, while cross-section is subtriangle.
    2. Specimen P.2768 lrom Sanmenxia (Fig.4)
    A sturdy, pointed implement made on a large and thick flake, with a minumum bifacial marginal retouch. There is a prominent, sharp tip in the distal end. The butt end is particularly thick with a steep retouch. The length of the edge is about 60% of the whole circumference. Longitudinal section is wedge-shaped, while cross-section approzimately subtriangle.
    3. Specimen P.0684 from Dingcun (Fig.S)
    A trihedral, pointed tool with a minimum trimming, with emphasis upon the tip. The base is flat and there is a dorsal mdeian ridge extending from point toward butt for the whole length of the tool. The tip is slightly constrained and was worked on all three faces. Longitudinal section is wedge-shaped, while cross-section is triangle. The edge is planoclinal.
    4. Specimen P.5786 from Qianxian (Fig.11,1)
    A large and sturdy tool, with a minimum bifacial primary flaking and retouch and dorsal median ridge extending from point toward butt for most of the length of the tool. The tip is absent. The length of the edge is about 60% of the whole circumference in the present state. Longitudinal section is wedge-like shaped, while cross-section is thick and irregular quadrilateral. The main functional part of the tool is the frontal end.
    5. Specimen P.8203 from Baise Basin(Fig.11,4)
    A very large and heavy tool the weight of whick is 4125g., made on a cobble, with a minmum bifacial primary flaking and retouch. The side edges are irregular. The butt is left completely unworked. The cross-section is thick. The main functional part of the tool is the frontal end which is round and blunt.
    6. Specimen P.4171 from Liangshan, Hanshui Valley (Fig.11,2)
    A pointed implement made on a cobble, with a minimum bifacial primary flaking and trimming. The cortex still remains on the whole butt. There is a prominent and sharp tip at the frontal end. It is similar to the "untrimmed butt" pick defined by Kleindienst(1962).
    7. Specimen from Shanugou (original specimen P.1889 from Dingcun) (Fig. 9)
    This specimen is a biface-like implement identified by Professor Pei et al. (1958). The problem is that it was collected on the ground surface of Shanugou, 5km east of Dingcun, with no accurate level and reliable age. Particularly the archaeologists had found a stone tool factory at the Dagudui mountain 2km east of Shanugou. The age of the Dagudai mountain culture is estimated between the end of the Paleolithic and the early period of the Neolithic. So I think, it is difficult to regard this specimen as an artifact of Dingcun Industry, and we should call it as "Biface-like implement from Shanugou", with a note of "original specimen P.1889 from Dingcun".
    8. Specimen P.1844 from Dingcun (Fig.10)
    Collected from the heap of the gravel-sand whick was digged by the local farmers in the past, this specimen was identified to a multi-edged chopper by Professor Pei et a1.(1958). It was made on a chunk, wiith a bifacial alternating flaking, and with the chopping edges around much of the circumference (nearly 83%). Cross-section is thick in relation to the size. There is a broken plan at one end. Longitudinal section is wedge-shaped.
    9. Specimen from Laozhihe (Fig. 11,3)
    Collected from the ground surface of Laozhihe, the original researchers did not described it in detail, and also did not provided the longitudinal section and cross-section. I don't see the specimen and can not ascribe it to the accurate type.
    Table 1 is the compilation of some data of nine specimens.
    Based on above descriptions, the present author considers that the opinions of original researchers about some specimens should be maintained, i.e., specimens of Pingliang P.3468, Sanmenzia P.2768 and Liangshan P.4171 are picks, specimen P.0684 from Dingcun is a trihedral pick, specimen from Shanugou (Original specimen P.1889 from Dingcun) is a biface-like implement, specimen P.1844 from Dingcun is a multi-edged chopper. The author tends to consider the specimens P.5786 from Qianzian and P.8203 from Baise Basin as the core-axes. The accurate type of specimen from Laozhihe can not be determined for the present.
    So no typical hand axes with the accurate level, reliable dating and associated artifacts had been collected from the formal excavation in the specimens in consideration. This may suggest that there are very few true hand axes or hand axe-like implements, even through not completely absent, in the Chinese Palaeolithic. The, author thinks, so far as Chinese materials are concerned, Movius' theory about the two cultural traditions between the Orient and the West is still applicable.
    A study on the stone artifacts from 54:90 site in Dingcun Region
    Zhang Senshui
    1994, 13(03):  209-285. 
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    One hundred and seventy one pieces of stone artifacts which were unearthed from the sand-gravel layer of 54:90 site near Dingcun village in 1954 have been studied here.
    A. The general characters of the artifacts
    The details of the observation, classification, measurements and statistics of the stone artifacts are shown in the text and tables 1-4. The general characters of the artifacts could be recognized as follows:
    1. Most artifacts are large in size. On the basis of the measurements of the undamaged flakes, the large flakes make up 64.79% of the total and small tools are very rare (only 6.67% of total tools).
    2. The flakes were mainly produced by direct percussion, occasionally by other flaking methods, such as throwing method, colliding anvil process etc. Though the cores were not prepared before producing the flakes, more flakes were regular in shape. It indicates that the "craftsman" who applied the primitive technique for getting flakes was more proficient.
    3. The used flakes without retouch are more common and make up 17.71% of the total flakes.
    4. Blanks of the tools have several kinds. The flakes constitute 76.66% of the total blanks. Tools made on the core are of less number (23.34%) (details sce table 4).
    5. The tool type is simple and the tools include scrapers, chopping tools and pointed tools. The tools with two and more edges have higher percentage (70%) and the single edge tools are not so much (30%).
    6. Tools were trimmed by direct percussion. The complex mode is the main way for retouching tools. Most of them were irregular in shape and the edges usually were blunt.
    B. Industrial comparison
    Because the artifacts from other sites in Dingcun region, except those from 54:100 site have not been studied in detail, the present author limited himself in comparing the component from 54:90 site with that from 54:100 site near Dingcun. The stone artifacts from these two sites have similarities and obvious differences. The similarities are: 1) The direct percussion is the most important method for producing flakes; 2) Though the cores are not prepared before chipping the flakes, most flakes are more regular in shape; 3) The tools are usually made by trimming the flakes (80.82% in 54:90 site and 71.8% in 54:100 site); 4) To trim tools is by direct percussion without exception. Retouching on the dorsal surface is the important mode for making tools.
    The most important differences between the stone artifacts from the two sites are: 1) Most artifacts from 54:90 site are large; In 54:100 site the small stone artifacts have higher percentage: the small stone flakes make up 64.28% of the total flakes and the small tools make up 40.02%; 2) The used flakes from 54:90 site (17.71%) appear much more frequent than those from 54:100 site (8.46%); 3) The tools of two sites are obviously different in type and mode of manufacturing. In 54:90 site the chopping tools occupy higher proportion (36.67%), while no chopping tools were found in 54:100 site. The tools manufactured by complex mode hold large part in the component from 54:90 site while the tools trimmed on the dorsal surface occupy higher proportion (48.7%) in 54:100 site.
    Besides, the tools found in two sites also exist other less important differences: 1) No graver were found in 54:90 site; 2) The pointed tools of B type are not only more in number but also better trimmed than that (just only one) from 54:100 site; 3) The tools with two and more edges from 54:90 site constitute the great majority (70%) and the single edge tools only make up smaller percentage (30%), while in 54:100 site they are 38.46% and 61.51% respectively.
    Judging from the above mentioned similarities the assemblages from 54:90 site and 54:100 site should belong to a same culture tradition, but due to existing several differences of the artifacts from these two sites, we consider that they could represent different groups.
    Banshan Paleolithic Site from the Lower Pleistocene in the Nihewan Basin in Northern China
    Wei Qi
    1994, 13(03):  223-238. 
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    Banshan Paleolithic site discovered in the Nihewan Formation in a Lower Pleistocene context in 1990 is located northwest of the Donggutuo site in the Nihewan Basin in northern China. The site is situated over 70 meters below the Donggutuo site and located in the hanging wall of a normal fault named the Brown Fault where the vertical displacement is about 75 meters. The cultural assemblage includes 95 stone artifacts and some fossil bone fragments with cut marks. The artifacts are excavated from a 2 square meter trench and are found in silty and sandy gravel 70 cm thick. The field survey suggests that the cultural Horizon at the Banshan site would be stratigraphically equivalent to the layer A of the Donggutuo horizon formed within the Matuyama Reversed Chron below the Jaramillo Subchron. So the Banshan site may extend back to the late Early Pleistocene as well, that is about 1 million years ago.
    Tentative excavation of the Zangshan Site of Yingkou County,Liaoning Province
    Cui Dewen, Li Yousheng
    1994, 13(03):  239-287. 
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    This paper reports the results of the tentative excavation of Zangshan Paleolithic cave site. It was found in the early 1986 and was tentatively excavated in September of the same year. The Paleolithic cave site is located in a hill about 30km northeast of Yingkou county at N.40°30′01″, E.122°30′35″.It is about 20m above the local ground surface and 110m above the sea level. The entrance of the cave is facing the east.
    The excavation was undertaken in two parts: at entrance part and in central part of the cave. The deposits were divided into two parts: The upper part and lower part. In the upper part we found 8 kinds of the mammalian fossils such as Gulo sp., Myspalax aspalax (see table 4), but no stone artifacts were found. Thirteen kinds of the mammalien fossils including Macaca robustus, Equus sanmeniensis, Crocuta ultima as well as 13 stone artifacts including 2 broken artifacts, 2 bipolar cores, 1 bipolar flake, 1 half flake, 1 single side convex scraper, 1 end scraper, 2 single side straight scrapers and 1 graver were found in the lower part. They were mainly retouched on the dorsal surface and crudely trimmed by direct hammer percussion.
    According to the deposits, artifacts characters, mammmalien fossils and paleomagnetic dating, the age of the lower part of the cave deposits could be compared to that from Loc. C of the Jinniushan sites and was dated to be of the upper stage of Middle Pleistocene and the upper part of Zangshan site to Upper Pleistocene in age.
    Re-examination of the chronological position of Chaoxian Man
    Shen Guanjun, Fang Yingsan, Jin Linhong
    1994, 13(03):  249-256. 
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    The chronological position of the paleoanthropological site of Yinshan in Anhui Province, East China, was re-examined by applying U-series dating to stalagmitic carbonate and fossil bone samples. Judging by the result of a stalagmitic sample taken from a travertin layer above the hominid fossil containing 2nd layer, Chaoxian Man should be older than 310 ka. It seems therefore possible to re-arrange it into the category of late "Homo erectus" instead of formerly accepted classification of early "Homo sapians". The reliability of the U-series age of stalagmitic carbonate has been discussed. The results of two fossil bones taken from the lower strata of the site, assigned to Early Pleistocene by the existence of several Tertiary survivals, may be cited as an evidence that consistancy between the results of two U-series methods does not necessarily guarantee its validity.
    Thermoluminescence dating of Jinniushan Archaeological Site
    Zheng Gongwang, Kang Yongzhu
    1994, 13(03):  257-259. 
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    Section A at Jinniushan Archaeological Site was divided into eight layers. In i984, some fossil human bones were found at bottom of Layer VII .According to TL dating, the lower part of Layer YI is 188.4±15.1 ka, the upper part of Layer VII( is 197.0±7.0 ka, the lower part of Layer VII is 194.6±3.4 ka and the upper part of Layer VIII is 388.7±50.7 ka. The order of these figures is identical with the stratigraphic sequence. TL ages of the strata are concordant with mammalian fossils found in corresponding layers. It showed that accumulation was quickly and continually from Layer VI to Layer VII. However, between Layer VII and Layer VIII, there was a clear gap in accumulation. About 200 ka ago, the cave might be stable when Jinniushan Man lived.
    The study of chemical element in the human bones from Chongtang Neolithic Site, Chongzuo County, Guangzi
    Wei Boyuan, Zhu Wen, Zhong Ershun, Chen Wen
    1994, 13(03):  260-264. 
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    Trace elements and heavy elements in three individual bones from Chongtang neolithic site Guangai were investigated with AAS. The main results are as follows.
    The high content (124.64 ppm) of Sr and the observed ratio (0.368) imply that the foods of Chongtang neolithic people were mainly from vegetable. Considering a lot of shell fossils in the site we think that the cause of high content of Zn in the bones relates with shells which are the main protein food for the neolithic people.
    The low content of Cd and Pb indicates that the neolithic people lived in primitive natural environment.
    Affinities of Asian populations
    Liu Wu, Motoharu Suzuki
    1994, 13(03):  265-279. 
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    The somatometric data of 25 Asian populations were analyzed with multivariate statistic methods. Two big population branches can be identified according to their different physical characters. NE Asian populations of China, Korea and Japan form one branch; all SE Asians belong to the other. The South Asian peoples of India, Sri Lanka and Nepal have closer relationship with SE Asians but still show their own distinctiveness. The populations in Japanese archipelago have two physical types. The main islanders have closer affinity with NE Asians while all the isolated populations including Ainu and Ryukyu islanders possess the similar physical characters as SE Asians. The aboriginals of Taiwan also show closer relationship with SE Asians. The authors believe the results of present study support the opinions on population relationship of Asia offered by Brace and Turner. Also some of their theories were discussed here.