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Table of Content

    15 September 2011, Volume 30 Issue 03
    Sex and age of Homo erectus skull 3 from Zhoukoudian: enlightenment from Nanjing Homo erectus skull
    ZHANG Yin-yun; XING Song
    2011, 30(03):  241-249. 
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    Davidson Black initially identified the third skull (Skull E) from the 1929 excavations of Zhoukoudian as an adolescent or early adult female. Later, after preparation that revealed additional details of the bones, Black modified his opinion suggesting the Skull E was an early adolescent male, equivalent in age to a modem twelve-year-old. Weidenreich agreed with Black, but assigned a slightly younger age of eight to nine years to the specimen. He based this conclusion on four points, including the presence of: a cleft in the tympanic bone, a lacrimal groove, small frontal torus, and small glenoid fossa. Since then, many paleoanthropologists have been puzzled by the identification of the Skull E.
    In this paper, this skull is compared with other Homo erectus skulls, especially the skull from Nanjing, an adult female. The comparison shows that Skull E shares features in common with the Nanjing skull, including smaller cranial dimensions, relatively small supraorbital torus, and faint muscle makings. Meanwhile, the cleft in llie tympanic bone, lacrimal groove, glenoid fossa, frontal sinus and thickness of cranial wall are not indictors that show the skull to be immature ormale. It is noteworthy that the Skull 12 from Zhoukoudian, a mature one, exhibits open sutures without any hint of closure, as the state of the sutures of kull 3.In view of the above considerations, this skull represents an adult female.
    Morphological evidence of the formation and diversification of modern Chinese: analysis of cranial non-metric traits in Chinese, African and European populations
    LIU Wu; WU Xiu-jie; XING Song; Victoria GIBBON; Ronald CLARKE
    2011, 30(03):  250-264. 
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    The formation and diversification of modern human populations brought about the emergence of current human populations ( or races ) living in various geographical regions. Physical differences and biological affinities are an important component of studying the formation and diversification of modern human populations. In the present study, the frequency and expression patterns of 21 cranial non-metric traits were analyzed in 330 crania from three main human groups of recent-modern Chinese, modern African and European populations. Our result and some impressions are as follow:
    1. Crania of modern Chinese were characterized by gracile morphology with features of robusticity ( e.g., supraorbital structure, angular torus, zygomatic trigone and zygomaxillary tuberosity) much less developed compared to African and European populations. Modern Chinese crania differed from African and European populations in terms of their sharp infero-lateral margin, flat intraglabellar notch, round cranial later profile, flat obelionic and lambdoid region, deeply arc-shaped lower zygomaxillary margin and different frontonasal and frontomaxillary sutures.
    2. In terms of non-metric cranial features and population affinities, our results showed different frequency and patterns in most of the features among the three populations with some anatomical traits having significant inter-populational differences. The value of differentiating populations with only one feature is very limited, so in order to explore populational relationships of these non-metric cranial features, discriminant analysis was used to distinguish the three main population groups. Using this approach, between 67 and 79.5 percent of the specimens could be correctly classified (70.4% -82.9% of the Chinese specimens were correctly classified). In the discrimination plots of individual specimens, the African crania were scattered widely, while Chinese and European crania were closely concentrated, suggesting that Chinese and European populations were more derived.
    3. Recent studies of non-metric cranial features have begun to analyze the functional or biomechanical morphology of these features, relating them to cranial robusticity, or how robust the crania are in structure. Cranial robusticity is also related to cranial size and thickness, but also expressed by a series of morphological features (referred to as cranial superstructures) including the uplifting ridge, torus and tubercles on the cranial surface. The expression of these robust features is influenced by both genetic and environmental factors and can be very different among populations. Although the evolution of modern Homo sapiens is characterized by skeletal gracilization, a number of robust features still occur in some fossils of early modern humans, as well as recent and modern human skeletons.
    This analysis of 21 cranial non-metric features in Chinese, African and European modern human populations indicates that most of the examined features show interpopulation differences related to cranial robusticity, and therefore these types of features must have played a significant role in the formation and diversifications of modern Chinese populations.
    Paleopathological lesions and osteological wounds of human bone from the Taosi site, Shanxi Province
    ZHANG Ya-jun; HE Nu; YIN Xing-zhe
    2011, 30(03):  265-273. 
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    This study describes the dental pathology and wounds of human bones unearthed from tombs and ash pits dating to the middle to late periods of the Taosi culture. The pathologies include dental caries,periodontal disease and enamel hypoplasia.This research shows that there might be two causes for the lower ratio of dental caries, either from the low average age of the analyzed bones or based on the proportion of meat in the diet. This result is confirmed by studies of dental abrasion rates as well as the re-analysis of stable isotope 15N data. In addition, this work reveals that more than half of the tomb bones had periodontal disease and about a third of the Taosi people were affected by metabolic stresses such as infectious diseases, fever and malnutrition during development from childhood. These bone disorders and crevices often seen on the skull fragments also suggest violent tendencies of the Taosi people, possibly from turbulent and conflict-intense periods in Taosi history.
    A preliminary study on the stone artifacts excavated from locality 74093 of the Xujiayao site in 1977
    MA Ning; PEI Shu-wen; GAO Xing
    2011, 30(03):  275-288. 
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    Xujiayao(40°06'02.8''N;113°58'41.4''E; ca.970 m above sea level) is an open-air site discovered in 1973 during field reconnaissance by members of the Institute of Vertebrate Paleontology and Paleoanthropology(IVPP), Chinese Academy of Sciences. The site is located on the right bank of the Liyi River and is named after the local village. Scientists from the IVPP excavated Xujiayao in 1976, 1977, and 1979. Xujiayao is represented by two localities(74093 and 73113), with evidence for archaic Homo sapiens, and the majority of the artifactual and vertebrate materials recovered from Locality 74093. The present paper is a preliminary report on the stone artifacts from Locality 74093 excavated in 1977. The Xujiayao site comprises fluviolacustrine deposits, with a stratigraphic profile consisting of a series of erosional surfaces intercalated with eight sandy clay and silty clay depositional layers. Five stratigraphic layers of the 3rd terrace were identified, with a total thickness of more than 15—20 m. Archaeological materials were unearthed mainly from the 3rd layer consisting of grayish green to brown clay(4 m thick). Dating shows that the human activities at this locality most probably took place in the early Late Pleistocene.
    A total of 1765 stone artifacts were unearthed from the spit U3 of the excavation in 1977. The stone assemblage includes cores(N=140), retouched pieces(132), flakes(399), flake fragments(427), chunks(667), and stone hammers(2). Lithic materials were locally available from ancient riverbeds with quartzite and vein quartz as the predominant raw material(accounting for 82.6%). The principal flaking technique was direct hammer percussion without prepared striking platforms, together with bipolar technique. Most stone artifacts were small in size,and most blanks for tool fabrication were flakes and flake fragments. More than 10 retouched types were identified, with scrapers and spheroids the most dominant, followed by notches, denticulates, points, burins, scraper-notches, borers, and choppers. Modified pieces were retouched by direct hammer percussion with mostly unifacial retouch on the distal end and lateral margins of the blanks.
    The lithic assemblage of this locality shows a close affiliation with the "Small Tool Tradition" in North China.It should be noted that the emergence of spheroids in the lithic assemblage is unique in Chinese Paleolithic studies.
    The age, lithics and paleoenvironmental study of the Sumiaoyuantou locality, Gansu Province
    ZHANG Dong-ju; CHEN Fa-hu; JI Du-xue; L Barton; pj Brantingham; WANG Hui
    2011, 30(03):  289-298. 
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    The Sumiaoyuantou locality in Gansu Province was discovered during archaeological survey. Thousands of lithics are distributed in a lens of 1.3m long and 0.13m thick in the Malan loess on the first terrace of the Zhangma River. An assemblage of 2318 fragments of artifacts was obtained by collecting from the profile(2166) and surface(48) in 2002 and 2004, only 2214 of which are reported here. This assemblage is dominated by flakes, shatters and debitage with a few cores and tools. The stone tool technology employed in this locality is mainly bipolar percussion,plus little edge percussion. The main raw material is quartz cobbles from the modern riverbed or the bottom gravel layer. Radiocarbon dates and paleoenvironmental reconstruction shows that the climate changed much during the period 30-15ka BP in the study region. From 30ka to 24ka BP,the climate was warm and humid due to a strong summer monsoon. From 24ka to 18ka BP, it became dry and cold with a decrease in the summer monsoon and an increase in the winter monsoon. From 18ka to 15ka BP, the climate ameliorated a little with the slightly recovered summer monsoons. Sumiaoyuantou represents the late Paleolithic culture in this region, with human activity occurring at the coldest and driest time, the Last Glacial Maximum, 24-18ka BP, which may suggest the high adaptative ability of humans.
    A late Paleolithic site discovered at Shenhu Bay, Jinjiang City, Fujian Province
    FAN Xue-chun; WU Jin-peng; HUANG Yun-ming; ZUO Zi-juan
    2011, 30(03):  299-306. 
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    A Paleolithic site buried from the tides of Shenhu Bay was discovered in January 2009 by several tourists. The same year, archaeologists from the Fujian Museum and Jinjiang Museum launched an investigation and test excavation of this new site.The site located at the coast of southeastern of Jinjiang City, Fujian Province, with geographic coordinates of 24°38'16.2''N, 118°38'49.4''E. Together with evidence for ancient forests and ancient oysters, this Paleolithic site shows a peculiar landscape. A total of 87 stone artifacts and several mammalian fossils including Elephurus maximus, Bubalus sp.and Cervidea were collected. The stone assemblage includes cores, flakes, chunks, scrapers, choppers and points. Only three kinds of raw materials including quartzite, crystal and quartz were indentified. Direct hammer percussion and bipolar percussion techniques were used. Most of flakes were flat platform type, and the size of the artifacts was mainly medium(30-100mm), which was different from the Pebble Tool Industry(Main Industry) in South China.Rough retouch and variability of tool shapes suggests tools being used in an expedient fashion. With evidence from Quaternary geology, geomorphology, mammalian fossils and chronology from an adjacent area, we infer the age of the cultural layer may be 10-15ka BP.
    Palaeolithic artifacts from the Baifeng site at Baise, South China
    HUANG Sheng-min; LIU Yang; GUO Yao-zhen; HUANG Ming-yang; LIU Kang-ti; HUANG Lin-zhen
    2011, 30(03):  307-312. 
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    Baifeng Paleolithic site was discovered at Tianyang County,Guangxi in 2009. It is located on the fourth terrace of the right side of the Youjiang River; its geographical position is 23° 45.399'N, 106° 43.636'E. During the survey, 27 stone artifacts were gathered from the surface, including cores(N=3), flakes(N=2), picks(N=14), choppers(N=5) and scrapers(N=3). Lithic raw materials were locally available from ancient riverbeds including quartzite(33%), argillite(22%), quartz(19%), farina sandstone(19%) and breccia(18.82%). Tool blanks were mostly pebbles as only two pick blanks were flakes. Most of the stone artifacts were large or medium in size, and modified by direct hammer percussion. According to typological analysis of these stone artifacts along with comparison to geomorphological and chronological details with other sites of the Baise Basin, we suggest that this site should date to the early Middle Pleistocene.
    Cultural modifications on the animal bones from the Lingjing site, Henan Province
    ZHANG Shuang-quan; LI Zhan-yang; ZHANG Yue; GAO Xing
    2011, 30(03):  313-326. 
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    A cluster of early modern human(EMH) skull fragments, dated between 100—80 ka was recovered along with a large quality of mammalian fossil remains and artifacts during recent excavations at the Lingjing site near Xuchang, Henan Province. The present study was based on the animal bones unearthed from this site in 2005 and 2006. About 13% of the bones bore clear evidence of cut marks with cut-marked midshaft specimens numbering 98.45%. With respect to the total number of cut-marked long bone fragments, upper and intermediate limb bones showed a greater representation of cut-marked specimens(34% and 41%) than did lower(25%) limbs. Evidence of percussion marks, burning marks and use-wear accounted for 4.2%, 1% and 1.32%, respectively. As well, the large number of fragmented bones at the site may be related to marrow-extracting behaviors of these ancient people. Through careful observation, statistical analyses, and comparison to experimental samples and other archaeological sites, we are confident that early humans were the agent most probably responsible for the accumulation of these animal remains.
    U-series dating of Huanglong Cave, a Paleolithic site at Yunxi, Hubei Province
    TU Hua; SHEN Guan-jun; WU Xian-zhu
    2011, 30(03):  327-333. 
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    Huanglong Cave is located at Yunxi County, Hubei Province in central China. Three excavations between 2004 and 2006 lead to the discovery of seven human teeth,dozens of stone and bone artifacts and other evidence of hominin activities. The mammalian fossils represent the Middle-Late Pleistocene "Ailuropoda-Stegodon" fauna commonly found in southern China. Judging by morphological and metric features, the human teeth should be classified as modern Homo sapiens.The deposits inside the cave are divided into five layers. All of the hominin teeth and artifacts, and most of the mammalian fossils were unearthed from the deposits of Layer 3 at Region 1 located ca.100m from the cave entrance and intercalated by flowstone layers, from which four relatively pure and dense calcite samples were taken. Here we report the results of U-series dating of these samples with conventional α spectrometry. A small stalagmite that developed on a flowstone layer beneath Layer 3 gives an age of ~100ka BP. A thin flowstone layer intercalated in the upper part of the deposits dates to ~77ka BP. Two calcite samples taken from the capping flowstone indicate its formation between 57—27ka BP. This paper reports also the U-series dates on four rhinoceros teeth that fall within the range 35—72ka BP, which is consistent with dates on speleothem samples. The excavators claimed that the deposits inside the cave exhibit a relatively simple and consistent stratigraphic sequence. If so, the human teeth and stone artifacts, recovered from the lowest section of Layer 3, should be bracketed in the range of 100 and 77ka BP. This conclusion is in support of a much earlier presence of modern H.sapiens in Asia than previously thought, in particular before the Younger Toba eruption at 74ka BP. Even considering the fact that the samples for dating were not collected during the excavations and that generally the stratigraphy of cave deposits tends to be quite complicated, the human fossils from Huanglong Cave should be emplaced before the formation of capping flowstone at 57ka BP, much older than the fossils from Tianyuan Cave at Zhoukoudian, which is widely accepted as the oldest representative of modern H.sapiens in China.The results of this paper indicate that humans lived in China in the so-called "temporal gap" of 100—40ka BP.
    A dermatoglyphic study of the Truku aboriginal population of Taiwan
    CHEN Yao-fong; ZHANG Hai-guo; SHEN Chien-fu
    2011, 30(03):  334-342. 
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    In this study, we collected and analyzed the dermatoglyphics of 200 individuals of the Truku people in Taiwan.Research method is ADA standard-CDA edition. Study item is CDA-standard of Ⅱ class model swatch. We report a wide range of dermatoglyphics variables including two class model swatch, atd angle, axial triradius percent distance, and simian line. This study is the first comprehensive dermatoglyphics research of Truku people of two class model swatch,and its dermatoglyphics data will be useful for future research in anthropology, genetics and medicine.
    Dermatoglyphs is a biological trait of humans. It is a product of both genetic and environmental factors. Dermatoglyphs are different among individuals and stable for whole life, so they are useful for identifying individuals. They also have specificity for populations or ethnic groups. Population dermatoglyphics present the stable variation within a population and also the variation among populations. Also, population dermatoglyphics can find markers that may help to trace the origin of populations or ethnic groups.