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    15 March 1983, Volume 2 Issue 01
    Morphological features of ramapithecus and sivapithecus and their phylogenetic relationships——morphology and comparison of the crania
    Wu Rukang (Woo Ju-kang), Xu Qinghua, Lu Qingwu
    1983, 2(01):  1-112. 
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    Since 1975 a late Miocene site at Shihuiba, Lufeng County, Yunnan Province has revealed a great number of fossil hominoids and other fossil animals. The hominoid specimens include Ramapithecus and Sivapithecu.
    Ramapithecus: three crania, fo* mandibles, twenty pieces of fragments of crania and jaw bones, twenty dental rows and 278 isolated teeth ;
    Sivcpithecus: two crania, five mandibles, 22 pieces of fragments of crania and jaw bones, seven dental rows and 290 isolated teeth.
    In addition there are a few extremity bones of hominoids.
    The major characters of the crania of Sivapithecus are as follows:
    The face is short and wide, with both zygomatic archs spreaded outwards. Viewed laterally the mid-facial contour is concave from the supraorbital ridges to the naso_x001F_alveolar clivus, but the anterior region of the maxilla is markedly raised upwards. This feature is quite similar to orang-utan and GSP 15000 skull from Pakistan, and different from that of the gorilla and chimpanzee.
    The temporal ridges are well developed. They start from both lateral segments of supra-orbital ridges, contact and parallel with them, and then turned strongly backward to form a median sagittal crest at the middle part of the vault.
    The supra-orbital ridges are not continuous from side to side of the forehead. This is also an important feature of the Lufeng crania, which resembles that of orang-utan and GSP 15000 skull from Pakistan, but differs from gorilla and chimpanzee.
    A specific character of the Lufeng crania is the wide concave glabella that is different from those of all living apes and GSP 15000 skull.
    The orbits have a sub-rounded contour. The interorbital region is quite broad and concave.
    The positions of the infraorbital rims are located slightly below the superior margin of the nasal aperture.
    The nasal aperture is specially narrow, and its lateral borders are bounded inferiorly by prominent canine juga. The concave-rounded naso-alveolar clivus is short and smallr with slight anterior naso-spinale. The canine fossae are very deep. The canines on botli sides diverge laterally downward into a reversed V-shape. This feature is also sttongly similar to that of orang-utan and GSP 15000, and different from- gorilla and chimpanzee.
    The central incisor roots are very curved, thus exist the pronounced central incisor juga and a deep central incisor sulcus as in orang-utan and GSP 15000.
    The dental arcade of the maxilla is sub-U-shaped, and is slightly diverged posteriorly.
    A prominent feature of the central incisors is the particularly great labio-lingual breadth of their crown. The breadth-length indices of some teeth are even more than 100. This is different from all recent apes and GSP 15000 skull.
    The lateral incisors are very small, only about one half size of the central incisors. The canines are relatively big. The crowns and cusps of the buccal teeth (premolars and molars) are of median height. They have thick enamel and crenated complex wrinkles on the occlusal surface of the crown, and no cingulum on the molars.
    The PA 677 cranium is considered as a typical one of the Ramapithccus from Lu- feng. Its main morphological characteristics are basiccally concordant with those of Sivapithecus (PA 644), except relatively smaller in size, and is gracile in morphology.
    The study of the crania of Ramapithecus and Sivapithecu^ from Lufeng shows that they are sexual dimorphism. They have many features similar to those of orang-utan, but different from gorilla and chimpanzee. It is suggested that they are the early ancestor of orang-utan. The branch of orang-utan seems to be divergent from the hominoid main stock at about 12 Myr B. P.
    Description of carnivora fossils from Lufeng
    Qi Guoqin
    1983, 2(01):  11-115. 
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    Partial collections of Carnivora excavated by the Lufeng team in 1975 and 1976 are described in this paper. They are:
    Proputorius lufengensis sp. nov.
    Sivaonyx bathygnaihus
    Lutra sp
    Ictitherium gaudryi
    Epimacluiirodus fires sp. nov.
    Pseudaeilurus sp.
    Of them Proputorius lufengensis and Epima ch air o dus fires are two new species. Pro_x001F_putorius lufengensis differs from P. mimnum Zdansky 1924 by P2 with single tooth root, smaller tooth row of P2-4 and P4 with metastylid. As compared with P. yaogouensis and P. s(misaniensisf P. lufengensis has a lower jaw, more developing premolars and related small Mi. So it is considered to be a new species. Epimachairodus fires, another new species, is characterized by especially huge size of upper canine and reduced P3 and P4.
    A new species of lophochoerus from Lufeng
    Han Defen
    1983, 2(01):  22-26. 
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    The specimen of Lophochoerus described here was collected at Sivapithecus (Ba- mapithecus) site., Lufeng county, Yunnan Province in 1981. It includes almost all left lower cheek teeth, except the first lower molar, and a fragment of the anterior part of right mandibule with P1 and a lower canine. Judging from the characters of the molars it belongs to the Lophochoerus.
    This pig is of small size. The premolars possess high main cusps, and P4 is not coni_x001F_cal. On the contrary, its width is comparatively narrow and the posterior ridge of main cusps of P3 and P4 separates into two branches. The talonid tapers anteriorly and blocks the medium valley of P3. The outside branch connects with talonid of P4. Pi, P2, P3 and the front part of P4 have no contact facets. This may be due to the existence of little diastema between each of them. The cusps of molars are comparatively simple. M: is absent, M2 is broken, but it seems to be slightly longer than P4'. Lingual cusps of M(3 are conical, separated down to the basal part of the crown. Labial cusps are somewhat V shaped, the anterior arms of which extend to the anterior cingulum and the first transverse eresting respectively. A slightly longer anterior ridge runs from the talonid to the second transverse cresting.
    From the characters of the pig described above, it is quite obvious that the Lufeng form {Lophochoerus lufengen^is sp. nov.) differs from that species of Lophochoerus of Siwalik in: 1) ra.ther larger in size; 2) M2 slightly longer than P4; 3) posterior structure of P3 and P4 and 4) the structure of talonid of M3.
    Lophochoerus is a pig which occurred in Lower and Middle Siwalik in India, But now it is also found in lignite beds of Miocene in Yunnan Province. Whether that species of India is in fact ancestral to Lophochoerus lu.fengensis sp. nov. remains to be seen.
    Distinguishing first from second molars of Gigantopithecus by multivariate analyses
    Wang Linghong
    1983, 2(01):  27-39. 
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    In is difficult to distinguish Ml from M2 of Gigantopithecus through any single trait such as crown length and breadth, as showed by their distributions.
    The present paper applies the method of principal component analysis to distinguish first upper molars from second ones, and the variables used are crown length, crown breadth and protocone length index (newly defined). The results show the existence of two categories in M1,2. A reasonable explanation for this is that they represent M* and Ma respectively. *The role played by protocone length (mesiodistal diameter) to discriminate between M1 and M2 of Gigantopithecus becomes clear due to the principal component analysis. This trait is likely to be of significance for other high primates in the same aspect.
    The distinguishing of lower molars is based on the observation of the three Gigantopithecus mandibles with teeth as well as the over 100 isolated teeth. Two series of ellipses in the coordinate chart of crown length and breadth represent the ranges of different sample distribution probabilities of Mi and M2, respectively, and disesiminatory lines are drawn between and M2.
    Discussion on the age of “Yuanmou man”
    Liu Tungsheng, Ding Menglin
    1983, 2(01):  40-48. 
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    Biostratigraphical, lithostratigraphical and magneto?tratigraphical restudies of Yuan- niou formation (in broad sense) show that the boundary between the Shagon formation of Pliocene and Yuanmou formation (in narrow sense) of lower Pleistocene is situated at the limit of Matuyama/Gauss Epoch about 2.48 m.y, (B.P.) and the boundary bet> ween the latter and the Shangnabang formation of middle Pleistocene is situated at the limit of Brunhes/Matuyama Epoch about 0.73 m.y. (B.P.).
    According to a reexamination of the paleomagnetic polarity of Yuanmou section? it is easily to find that there is an evident polarity reverse in the 13th layer of the 2nd member up to the 23rd layer of the 3rd member of the section ,that covers in a thickness about 300 m. Then, it follows more than 100 m in thickness of the 4th member with normal polarity, i.e., the Shangnabang formation. So, it might be appropriate to correlate this normal polarity member as the Brunhes Epoch but not to a certain normal polarity event of the Matuyama Epoch. If so? a fully different explanation on the magnetostratigraphy of Yuanmou formation could be reached that the layer which yielded the fossils of uYuanmou man?, is magnetostragraphically situated at the base of the Brunhes Epoch and the age of "Yuanmou manM might be not older than 0.73 m.y. (B.P.), possibly 0.5—0.6m.y. (B.P.), but not 1.3一1.7 m.y. (B.P.).
    Excavation report on a mesolithic site at Layihai, upper yellow river
    Gai Pei, Wang Kuodao
    1983, 2(01):  49-116. 
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    The site, reported here, excavated in 1980, is the first Mesolithic site fonnd in West China. The site is located in the region of Layihai, some 200 km southwest of Xining, the capital of Qinghai province.
    The cultural remains were found in the sediments of the second terrace of Yellow River. A radiocarbon date of 6745±85 BP has been obtained for this site. No pottery or polished stone tools were found at this site. The excavation has yielded 1478 specimens including cores, flakes, microblade cores, choppers, end-scrapers, side-scrapers, burins, grinding tools, bone needles and awls, and one stone bead.
    There is a brief description of the artifacts in this paper. While examining them, the senior author first recognised a specific technology of microblade cores present at the site, and the name of Layihai technique wars given to this technological pattern. The reconstruction of Layihai technology is illustrated in Fig. 6.
    The assemblage of artifacts and the animal remains suggest that the Layihai site is of Mesolithic age, or that it represents the Mesolithic level of cultural development of the stone age.
    Anthropological survey on Dawuer tribe, Heilongjiang province
    Shi Quande, Hu Junqing, Yang Hongyou
    1983, 2(01):  60-71. 
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    An anthropological study was made in September 1980 on Dawuer tribe including 144 males and 83 females.
    Tre results of the survey can be summarized breifly as follows:
    The mean value of the stature of males is 164.77 cm and belongs to '' Mittelgross'' but tends to 4 4 Untermittelgross, ? type, while that of females is 153.53 em and belongs to “Mittelgross". The cephalic index is of brachycephalic type in both sexes. The facial form is leptoprosory type in males and females. The facial index belongs to leptorrhiny type in both sexes.
    In addition, both males and females mostly have Mongolian folds (70%). The eye aperture is sloping upward laterally, and the breadth of eye aperture is of narrow type in most cases. The thickness of red lips is of thin type in most cases.
    Compared with the surrounding groups, Dawure tribe is most closely related to Han nationality living in North China and Chaoxian nationality, while it is remotely related to Li and Miao nationalities.
    The relationship between the construction of maxillary first molar and age
    Wei Boyuan, Feng Jiajun, Fang Zhonghu
    1983, 2(01):  72-79. 
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    97 maxillary first permanent molars of Southern Chinese were investigated in this report.
    The method of study is as follows: the teeth investigated were ground into 0.5 mm thick slies through the central part of the buccolingual sides of the molar. The height and width of the pulp chamber and the dentine of the slice were measured with the micrometer through microscope. The pulp-dentine index was calculated according to the following formula:
    Pulp-dentine index =(height + width of pulp chamber)/(height + width of dentine)*100. We found that there is a negative correlation between the pulp-dentine index and the age of all teeth examined. The regression formula to estmate age is: g=( —1.01) )s+ 82.82 (where: t/=pulp-dentine index, a:^estimated age).
    Estimation of stature by long bones of chinese male adults in south China
    Mo Shitai
    1983, 2(01):  80-85. 
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    Based on the materials of 50 Han male adult cadavers collected in South China in recent years, we have calculated the constants (a) and the regression coefficients (b) for estimating the stature by long bones as well as the coefficients of correlation (r) between the length of long bones and the stature. The value of the correlation coefficients varies within 0.516.913. This indicates that the degree of correlation is high. On this basis we have also calculated ten regression formulae by which the stature can be estimated. The correction value 0.6 mmX (age—30) is used to correct the error caused by age.
    The results of the calculation by humerus and fibula, humerus plus radius and femur plus tibia are better than those by other bones. The regression formulae made in the present article can be used to estimate the stature of South Chinese.
    The larynx pouch of presbytis francoisi
    Zhang Yi, Yang Jignang, Wu Qijun
    1983, 2(01):  86-89. 
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    Larynx pouches of four individuals of Presbytis francoisi are reported. It was found anteriorly at the left side of the neck. Anatomically it was located with museuli platysma anteriorly, museuli sternohyoid-eus posteriorly, museuli sternoeleidomastoideus- posterolaterally and museuli mylohyoideus superiorly.
    Uranium series dating of "Ordos man" and "Sjara-osso-gol culture"
    Yuan Sixun, Chen Tiemei, Gao Shijun
    1983, 2(01):  90-94. 
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    Some fossilized mammalian teeth and antlers collected from various stratigraphical position of primary Sjara-osso-gol sediment are dated by both 230Th and 231 Pa methods.
    The results are:
    1) The lower Sjara-osso-gol formation (lacustrine deposition) was accumulated between 30—50 thousand years B.P. The "Ordos man'' and "Sjara-osso-gol Culture,, are located in this formation.
    2) The upper Sjara-osso-gol formation (alluvial deposition) is dated no more than 30 thousand years B.P.