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    15 September 1983, Volume 2 Issue 03
    Variability in tooth size of Gigantopithecus blacki and the dietary hypothesis for australopithecines
    Zhang Yinyun
    1983, 2(03):  205-217. 
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    The isolated teeth of Gigantopithecus blacki kept in our laboratory ate measured and statistically tested. The heterogeneity of Liucheng sample can be shown by a comparison of the teeth from locus C with those from non-C loci in the Gigantopithecus cave. A re_x001F_view of geological literature suggests that some teeth from non-C loci, which may be of later rage, are responsible for. this heterogeneity.
    The teeth of G. blacki can be divided into early and late groups on 'temporal grounds; The late G. blacki is significantly larger than the early G. blacki in cheek teeth, but there are no significant differences in front tooth size between these two groups; It means that there is a differences in proportionate size of the canines to the cheek teeth between early and late G. blacki. The difference is like that seen between gracile and robust of South African australopithecines. The fauna and tooth chipping indicate that the difference in tooth size between eatly and late G. blacki can hardly be attributed to different dietary resources. TKe evdlutionary. trerfd in tooth size of G. blacki implies that :a mote reasonable explanation of the difference between gracile and robust type of South African australopithecines might not be due to diets as suggested by Robinson.
    On some problems of the upper palaeolithic culture in southern China
    Zhang Senshui
    1983, 2(03):  218-230. 
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    The palaeolithic research of southern China has been done for a long time. Some archaeologists and palaeontologists made efforts in the survey of the prehistoric materials. In 1913, J. Edgar began to gather stone tools in Hubei and Sichuan Provinces. In 1930s, Prof. Pei and others worked in Sichuan and other provinces such as Guangxi and Yunnan in the field of Cainozoic research and they paid attention to the palaeolithic artifacts and found prehistoric materials in this region. Dr. G. Bowles had studied prehistoric materials too.
    After the founding of the People's Republic of China, discoveries made in the extensi_x001F_ve field in southern China led to a clearer understanding of the upper palaeolithic conditions of this region. Therefere, a brief review of the materials of the upper palaeolithic in southern China is made by the author and some questions are raised about it in this paper.
    1. Main results
    About 60 sites bearing the materials of the upper palaeolithic or human fossils (Ho_x001f_mo sapiens) in southern China have been reported. The sites spreaded in a wide area from 100°一122° E. to 22°—33°N. (Fig. 1). The interesting industries in this region are found from Fulin, Tonglian, Maomaodong and Chaungdong sites etc., and altogether over 10,000 pieces of artifacts have been found. Some bone took, several antler implements and the remains of used fire as well as some human fossils have also been collected in this region (Table 1).
    2. General characters of the industry
    (1) The flakes are produced by four flaking methods which are all direct percussion, so most of flakes and cores are various in shape. So far blades, micro-blades and microcores made by punch and pressure have not been found.
    (2) The stone tools made from the flakes are more than those from the cores. The assemblage consists of three main types: scraper, point and chopper. In addition, a few pieces of the gravers have been collected and most of them are atypical. Among them the chopper has a larger numbers in proportion compared with contemporaneous industries of northern China.
    (3) The stone tools are retouched by direqt percussion, therefore, most of them are rather rough. Up till now, no specimens trimmed by pressure have been observed.
    (4) Some bone and antler tools worked by scraping and polishing have been gathered in this region.
    The characters mentioned above indicate particularity, succession and development in the palaeolithic culture known in China.
    3. The problem concerning the local culture
    In view of typology and technology, there are several local cultures such as Fulin Culture, Tonglian Culture and Maomaodong Culture. Besides, the artifacts picked up from Guangxi and Yunnan may also represent several local cultures. Its distribution is limited in certain region.
    4. Industrial developmental tendency and cultural relation among different sites
    Generally speaking, the fragmentary materials found from some sites in Yunnan are similar to those of the Tonglian Culture according to type and technique, while the artifa_x001f_cts from the cave sites in Guangxi can be compared with those of the Maomaodong Culture. Besides, the assemblage in which small tools are more than large ones spreds in an extensive area of southern China and this industry is more close to the tradition in northern China.
    According to the materials of the upper palaeolithic found in Guizhou recently, the stone tools may be from small to large in size, and the bone tools and antler implements are gradually increasing in quantity from early stage to late stage of the upper palaeolithic age. At the present time this question can not yet be answered whether these tendencies of the cultural development are applied to all conditions of the upper palaeolithic in southern China.
    Discovery of a new palaeolithic site on the bank of the yellow river, in northwest Shanxi province
    Wen Benheng, Wei Qi, Chen Zheying, Li Yiucheng
    1983, 2(03):  231-305. 
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    Some palaeolithic artifacts noted in this paper were found in the basal gravel (bearing Lamprotula) of the Reddish Clay in Hequ County, Shanxi Province, in 1979. The artifacts include five cores and five flakes and a single edge scraper (made of small flat pebble). The age may be late Middle Pleistocene based on geomorphological and stratigraphical evi_x001F_dences.
    The excavation of Qingciyao palaeolithic site in Datong
    Li Chaorong, Xie Tingqi, Tang Yunjun
    1983, 2(03):  236-308. 
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    The Qingciyao palaeolithic site is situated between Datong city and the world-famous Yungang Grottoes in the north of Shanxi Province. It is about 5 km to the east of the Yungang Grottoes and about 8.5 km to the west of Datong city (40°6'N, 113°11'E). The site was discovered in construction of highway in the spring of 1975. This is the first pa_x001F_laeolithic site discovered in Datong area. A joint team of IVPP, Datong Museum and Datong Cultural Bureau excavated the site in 1976 and 1977, and discovered 8 species of mammalian fossils and about 1000 pieces of artifacts in the sand layer of the hind margin of the second terrace.
    The mammalian fossils associated with stone artifacts belong to Cams lupus, Palaeolo- xodon sp., Coelodonta antiquitatis, Equus cf. sammeniensis, Gazella sp., Spirocerus sp. A and B. Bovinae indet.
    Most of the artifacts were made of quartzite and vein quartz, the rest were made of flint and volcanic rock. The raw materials mainly came from Jurassic stratum nearby, and some were collected from gravel layer of the second terrace on the Shili River.
    There are 135 cores which can be divided into two types: single platform and polyplatform cores. 375 pieces of flakes were divided into two types: flakes produced by the direct method with a stone hammer and bipolar flakes. In addition, a hammerstone and anvil were also found.
    138 stone tools were affirmed. They are 110 scrapers (79.71%) 15 points (10.87%) and chopper tools 13 (9.42%), The utilization ratio of the cores was rather low. The cortex can be found on the cores and flakes. The stone tools were retouched simply and roughly and half of them retained cortex in varying degree.
    The form and technique of Qingciyao assemblage are similar to those of early palaeolithic sites in North China.
    Judging from the evidence of stratigraphy and fauna, it can be tentatively regarded [hat the age of Qingciyao site is the late stage of the early palaeolithic or the late Middle Pleistocene.
    Observation on interparietals among the Chinese
    Luo Shudong, Hou Shizhan, Fu Chengjun, Zhou Zhichun
    1983, 2(03):  247-306. 
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    1600 skulls were observed. The appearance rate of interparietals is 2.94%. All the in- terparietals appear above the superior nuchal line, and 27.6% of them cross over the highest nuchal line. The upper parts of occipital squama of 60 fetal skulls of 7—38 weeks were studied, ossifications were developing around two centers in the form of endomembranous. The author holds that the formation of interparietals resulted from the failure of the transverse occipital fissure to fuse together and the forming of the abnormal ossified center. The author also suggests that the fusion between the superior region and the inferior region of the occipital squama occurs above the superior nuchal line. Both the superior and the highest nuchal line should not be considered as the fusing line o£ the two regions.
    Estimation of stature from skull, clavicle, scapula and os coxa of male adult of southern Chinese
    Peng Shulin, Zhu Fangwu
    1983, 2(03):  253-259. 
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    The horizontal circumference of skull, maximum length of clavicle and os coxa and the morphological breadth of scapula of 70 male adult human skeletons from South China were measured and the coefficients of correlation between the average length of the right, left and both sides of these items and the stature were calculated. The coefficients range from 0.298 to 0.616. The significance tests denote that all of these coefficients are significant (p V 0.01). Hence, 10 regression formulae were computed. All of these equations were checked on 70 Chinese skeletons. It shows that the estimating stature from the equation of the os coxa appears more reliable than from the scapula, the skull and the clavicle.
    Physical characters of Zhuang nationality in Guangxi
    Zhang Zhenbiao, Zhang Jianjun
    1983, 2(03):  260-271. 
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    A somatological survey on 245 males and 61 females of Zhuang nationality living in Guangxi was carried out by the authors in January, 1980.
    The results of the studies are summarized as follows:
    The physical characters of Zhuang nationality
    The hair is straight in form and black in color in most cases. The form of the head belongs to short-wide type and cephalic index mostly belongs to Brachycephaly.
    Brown eye color is commonly represented in both sexes. There are not Mongolian folds in most cases. Double eye-lids are observed in high percentage. The palpebral opening is o£ the wide type and its direction is of horizontal type.
    The profile view of the nasal bridge is mainly of wavy type. The nasal index belongs to Mesorrhiny. The facial form in most cases is of ovoid type. According to the component classification of the morphological facial height and facial breadth, most of them belong to low-wide type. The morphological facial index belongs to Euryprosopy.
    The relationship between Zhuang and other nationalities
    In comparison with other minority nationalities in "Rm" value, Zhuang nationality is closer to Li, Buyi and Yi nationalities. As to the relationship with Han nationality living in different provinces, Zhuang nationality is by "Rm" value, closer to Han nationality living in Guangxi, Guangdong, Fujian and Hunan provinces. Zhuang nationality is basically similar to the other inhabitances living in South China in physical1 characters.
    Zhuang nationality is different 任om Han living in Guangxi mainly in the fact that they have lower morphological facial height, lower height of nose and that of head.
    According to these analyses we consider that Zhuang nationality belongs to South China pattern in physical characters, like other inhabitances living in South China, and may originate from a common ancestor.
    A dermatoglyph1c study of the hands of 300 people of Han nationality in the Zhejiang region
    Chen Yanglei
    1983, 2(03):  272-281. 
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    This paper presents a detailed dermatoglyphic study of the normal hands of Han nationality which comprises 150 males and 150 females.
    1. Frequencies of finger print patterns W, Lu, Lr, >A are 51.67%, 43.4%, 2.83% and 2.1% respectively. The male whorls are more abundant than female, while the arches appear with a greater frequency in females than in males (p < 0.01).
    2. -Mean t% is 17.7%. Mean atd angle is 40.28°. The existence of two separate axial criradii (tm) amounts to 18 hands with a frequency of 3%.
    3. The ab ridge count is 39.09 with a higher number in males than in females (p < 0.01). The mean value between a and b triradii is 2.21 cm. The normal values for ad ridge count and ad distance are 87.55 and 5.1cm respectively. The ratio of ab distance- to ab ridge count is 0.057cm.
    4. No a and b triradii absence, while the frequency of absence of c or d triradii is 10.3%. The interdigital triradii (I2, L, I4) total up to 6.33%.
    5. The A line terminates in 9.33% of the 600 hands at the thenar area with the right hands having much less frequency (2.33%) than the left (16.33%). If the hypothenar area is divided artificially into proximal and distal halves, the A line to the distal half is much more frequent at the right hands (55%) than that at the left (12.33%). Right hands in group comparison with left show a greater degree of transversality of configuration.
    6. Frequency of true patterns in palmar thenar area (T/L) is 11.3%, that in palmar hypothenar area、2O,5%. Frequencies of bilateral pattern in I<. are 1%, 4.67% and 57% separately.
    7. The distribution of different patterns of the palmar crease is the normal pattern, 88.2%; the simian line pattern, 2%; the, transitional'I pattern, 4.2%; the transitional1 II pattern, 3.5% and the pattern of Sydney, line, 3.2%.