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    15 September 2016, Volume 35 Issue 03
    Putaoyuan Paleolithic site from the Lower Pleistocene of the Nihewan Basin
    WEI Qi, PEI Shuwen, AO Hong, MA Ning, JIA Zhenxiu
    2016, 35(03):  321-330. 
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    Seventy-nine stone artifacts were discovered from a Lower Pleistocene context at the Putaoyuan site, Nihewan Basin (or Sangganhe Basin). The stone artifacts include cores, flakes, modified pieces and chunks. Bone and tooth fragments of mammalian fossils, including elephants, equids, and rhinocerids were also collected. Judging from the magnetostratigraphic context, the cultural horizon is close to the Olduvai subchron, which indicates early human occupation probably took place about 1.5-1.6 million years ago.
    Stone artifacts from the newly discovered site of Nanshanbian, Nihewan Basin
    WANG Fagang
    2016, 35(03):  331-342. 
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    The Nanshanbian site was discovered on the eastern fringe of the Nihewan Basin and the northern fringe of the Datianwa Plateau in 2013. In a test excavation, 38 stone artifacts and 3 fragmentary bones were unearthed. The stone artifacts included cores, flakes, scrapers, and incomplete flakes and chunks, all attributed to the main industry of the Paleolithic tradition in North China. The artifacts were from the middle to lower part of the Nihewan Bed. According to geomorphological and chronological comparison, the stratigraphic profile of the Nanshanbian site is equal to the Dachangliang, Xiaochangliang, Zhaopo, and Putaoyuan sites, more than one million years ago.
    A preliminary report on the excavations at Madigou E6 and E7 sites in the Nihewan Basin
    JIA Zhenxiu, PEI Shuwen, MA Ning, ZHANG Xinglong
    2016, 35(03):  343-358. 
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    The Nihewan Basin, covering the northwest of Hebei Province and northeast of Shanxi Province, is located in the transition zone between the North China Plain and the Inner Mongolian Plateau with an area of roughly 150-200 km2. Bearing the earliest and centralized evidence on the human dispersal to Northeast Asia from Africa, the basin is considered as the key region on the study of the relationship between early hominin evolution and adaptive behavior in North China. This paper will give a preliminary report on a newly discovered Early Pleistocene Paleolithic site complex named Madigou (MDG), but with particular emphasis on the two sites (MDG-E6 and MDG-E7) of the MDG site complex. Madigou site complex is situated in the concentrated area of Early Paleolithic sites on the Cenjiawan Platform of the eastern part of the Nihewan basin. MDG-E6 and MDG-E7 sites were discovered in 2007 and were excavated in 2012 and 2013 field seasons by the staff from Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences (IVPP). Archaeological occurrences were buried in the fluvio-lacustrine deposits of Nihewan beds of fine sands, silt and clay, with grey, yellow, brown, and green in color. Geomorphological and stratigraphic comparisons as well as preliminary magnetostratigraphic dating results indicate that early hominins occupied the site before ca. 1.07 Ma. The excavation of MDG-E6 exposed an area of 30m2. In total, it unearthed 127 lithic artifacts, 9 animal fossils and 48 pebbles and cobbles. Archaeological materials were mainly from the altitude of 933-932m, and the feature of archaeological layers is the typical lacustrine sediment of fine sand and silt. Lithic assemblage can be classified into debitage(n=82; 64.57%), cores (n=44; 34.64%) and retouched pieces(n=1; 0.79%). Lithic raw materials derive from local sources, including chert(n=48; 37.80%), dolomite(n=35; 27.56%), breccia(n=12; 9.45%), and some volcanic rocks (andesite, basalt, and tuff). The stages of weathering and abrasion of the stone artifacts are dominated by slightly and moderate stages (1 and 2). Most artifacts are medium in size without size lesser than 2cm. The technique of lithic artifact manufacturing is only direct hard hammer percussion. The cores include unifacial chopper cores, bifacial chopper cores, heavy-duty scrapers, polyhedrons, discoids and causal cores. The technological breakdown of complete flakes was dominated by Type V and Type II. The animal fossils are too fragmentized to identify species. The excavation of MDG-E7 exposed an area of 20m2, unearthed 92 lithic artifacts, 35 animal fossils and 47 pebbles and cobbles, while 29 archaeological materials were collected from screening. The attitude of 933.5-932.5m and 935-934m are the main archaeological layers, and also show lacustrine sediment feature of fine silt and clay. The lithic assemblage includes debitage(n=85; 92.39%), cores (n=5; 5.43%) and retouched pieces (n=2; 2.17%). The use of raw materials and the main stages of weathering and abrasion of the stone artifacts resemble the feature of MDG-E6 to some extent. Most artifacts are small and medium in size. Flaking technique is also direct hard hammer percussion. Cores consist of bifacial chopper cores, heavyduty scrapers, causal cores and subspheroid. The technological breakdown of complete flakes is dominated by Type V. As too fragmented condition, the animal fossils cannot be identified either. In conclusion, the weathering and abrasion stages, technological composition, and the characteristics of archaeological layers indicate that the MDG-E6 and MDG-E7 sites were formed in the lake margin contexts and were disturbed by relatively gentle energy of lamellar flow from lake shore. As dominated by Oldowan-type core forms and debitage, the stone artifact assemblages of MDG-E6 and MDG-E7 may be considered to Oldowan-like (Mode1, core and flake technology) Industry. The unearthed archaeological remains from the two sites not only enrich the discoveries of Early Pleistocene sites but also will provide valuable clues for the research on the evolution, dispersal and technical development mode of early hominins in the Nihewan Basin, North China.
    The excavation of the Shuanghe Paleolithic Locality 1 in the Danjiangkou Reservoir Region
    CHEN Changfu ZHANG Juzhong YANG Xiaoyong
    2016, 35(03):  359-370. 
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    The Shuanghe Paleolithic locality 1 buried in the third terrace of the left bank of the Danjiang River, and located in the Shuanghe town, Xichuan County, Henan Province. The locality was excavated from 2010 by the Department of history of Science & Scientific Archaeology of University of Science & Technology of China, as a salvageable archaeological project due to the construction of the Danjiang Reservoir dam at a higher latitude. The excavation exposed an area of 400m2. A total of 225 stone artifacts were unearthed. The stone assemblage includes cores, flakes, retouched tools, chunks and split and so on. Human mainly used quartz cobbles to flake and retouch tools. The principal flaking technique was direct hammer percussion. Most stone artifacts were small or medium in size. Pebble retouched tools were dominated, especially choppers. Most tools were retouched in one end of the pebble. The characteristics contained South China Paleolithic industry elements, as well the flake tools were in appearance. The Stratigraphic and topographic comparison with other site showed that the site likely formed in the Middle Pleistocene.
    A preliminary report on the excavation in 1996 of the Huihe Dam Microlithic Site, Inner Mongolia
    YUE Gouming, CHEN Hong, FANG Mengxia, ZHEN Ziming
    2016, 35(03):  371-384. 
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    The Huihe Dam Microlithic site is located in Hulun Buir area. The site was discovered in 1975, and an area of 150m2 was excavated in 1996 by Inner Mongolia Institute of Archaeology. Eight stratigraphic layers were identified at the site, and archaeological materials were mainly unearthed from the 4-8 layers. It can be inferred from the excavation that the Huihe Dam site shows close relationship with the Hake Culture on basis of the sediment. More than 4000 stone artifacts were excavated and collected from the site. According to the "hierarchical dynamic typology”, the 2654 pieces of stone artifacts excavated from 6-8 layers were classified into three groups: manufacture, usage and discard, including flakes, blades, cores and various kinds of tools. General features of these artifacts are summarized as follows: 1) Lithic raw materials were dolomite mainly, which were procured locally from riverbeds. 2) Most cores were intentionally prepared, since lots microblade cores in wedge-shape and core trimming flakes were found. 3) In this assemblage, microblade technology was applied, as well as flake technology. Some artifacts similar to geometric microliths remain further analysis. 4) Various tools appeared small size dominantly, and composite tools were found. 5) Most tools were retouched unifically at edges. Bifacial thinning and backed techniques were applied. 6) Several artifacts were modified by grinding technique at edge partially. 7) Broken artifacts were unearthed and dominated by scrapers.
    A preliminary research on the bone, antler and tooth artifacts from the Haminmangha site in Inner Mongolia
    CHEN Quanjia, CHEN Jun, JI Ping, WANG Chunxue
    2016, 35(03):  385-396. 
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    Haminmangha Neolithic site is located at Horqin Left Wulat Middle Banner of the Inner Mongolia Autonomous Region. According to the dating result of C14, it dated to 5500-5000 BP. More than one hundred bone, antler and tooth artifacts were unearthed from Haminmangha Neolithic site. These artifacts include stone knives with bone handle, bone dart, bone arrowhead, bone needle cylinder, bone needle, bone dagger, bone awl, bone hairpin, horn, antler awl, antler borer, tooth ornaments and bone, antler materials. According to the analysis of these artifacts, we can deduce the retouching technology and manufacturing process of them, and conclude the characteristics of artifacts, deepen the understanding of the production and living conditions of human in the Haminmangha site.
    Behavioral modernity and variability of late Late Pleistocene humans in South China: A case study of Diaotonghuan in Wannian, Jiangxi Province
    WANG Youping
    2016, 35(03):  397-406. 
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    Diaotonghuan is a rock shelter located in the limestone hills of the southwestern Dayuan basin in Wannian County, Jiangxi Province. The Diaotonghuan site was excavated in 1993, 1995 and 1999. Thousands of stone artifacts that include both flake and pebble tools were found during the excavations. A large number of antler and bone tools, as well as shell knives, were also found, and fireplaces and occupation surfaces were uncovered in different cultural horizons. The diversity of the finds indicates that the rock shelter had been used by Late Pleistocene hunter-gatherers for a variety of activities, including base camps, stone workshops, animal butchery, etc. in the late Late Pleistocene. The research at Diaotonghuan is significant as it opens a new window for examining the diversity of modern human behaviour in the Late Pleistocene of South China.
    The application of lithic raw material mechanical analysis in Paleolithic archaeology
    ZHOU Zhenyu, HUAN Yong, LIU Wei, DONG Jie
    2016, 35(03):  407-417. 
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    Raw material is commonly considered as a very important element in prehistoric stone tools production. Different raw material has been proved to cause variability in lithic assemblages by influencing the knapping technique and tool types. The knapping properties of raw material have a strong correlation with rock mechanical properties which are determined by factors such as mineral composition, crystal size, density, texture, and degree of weathering, moisture content, etc. For a long time, hardness is taken as only criteria to evaluate the raw material mechanical properties based on a semi-quantitative lithic grade scale. In most cases, “easy”, “good”, are used to describe the high quality raw material by knappers’ subjective sensation. Lithology analysis and mechanical tests have been proved as quantitative approach for mechanical properties of stone raw material. In the past study, four mechanical properties, elastic response, compressive strength, tensile strength, and fracture toughness were selected for testing. Fracture toughness was supposed as the most objective measure of the knapping quality of raw materials. In this paper, the results of lithology mechanical tests have shown that compressive strength is also an objective measure of the raw material quality. Besides that, rock damage processes in compression tests include the initiation, development and nucleation of cracks that can be reflected on strain vs. stress curves. To investigate the mechanical properties of raw material, compression tests were performed using a MTS 810 material testing machine. Specimen cubes were cut out of pebbles from Paleolithic site for the tests. Force is measured by the load cell, and the deformation of the specimen is measured by a COD displacement sensor fixed between two compression plates. This deformation vs. force relationship was then transformed to a strain vs. stress curve. Six kinds of raw material, dolomite, chert, obsidian, quartz, quartzite, and granite, were involved in the compression test. In Shuidonggou site, dolomite shows higher ductility and brittleness than quartz and quartzite. This result implies that dolomite appears better flaking properties than quartz and quartzite in Shuidonggou. Archaeology remains The quartz from Beitaishanmiao site, Hubei and Xujiacheng site, Gansu present the similar lithology mechanical properties, which might be taken as one explanation for that both two sites shows similar raw material utilization and lithic assemblage. In the chert (Daerwo site, Guanyindong site, Guizhou) and obsidian (Japan) specimens we examined, since of the microfissure, both the dispersion of maximum stress and maximum strain is bigger than dolomite, quartz, sand quartzite, and granite. This suggests that, in some case, the macro-crystal rock maybe appears better flaking properties than microcrystal rock, such as chert, flint, and obsidian. In this study, mechanical properties analysis has been proved quite objective method for raw material utilization analysis. We suggest that knapping experiment should be correlated with mechanical tests. Moreover, more mechanical tests with different raw materials from different sites are necessary for the comparative examination and also significant for building a raw material mechanical properties database.
    Research on small mammals in zooarchaeology
    WU Xianzhu, Drozdov NI
    2016, 35(03):  418-430. 
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    Small mammals are an indispensable important link in the ecological chain of nature. These types of animals possess a number of unique characteristics: strong selectivity of living areas; minimal activity and migration patterns; and a relatively small scope of behavioural activities, all of which are helpful in analyzing ecological evolution including environmental sanitation of ancient sites and housing conditions of ancient residents. Zooarchaeology examines the symbiotic relationship between small mammals and humans including environmental constraints, and utilization of small mammals. To conduct this type of research requires anatomical expertise and biologically based laboratory equipment. Chinese Paleolithic Age archaeology, according to small mammals remains materials, research geological age of ancient ruins, ancient human living environment, etc., has achieved fruitful results. Neolithic Age and later historical phase of small mammals archaeology, in the sample extraction methods, typical case studies and other aspects, also has made some gains. But overall observation, less professional researchers in this field, especially the Neolithic Age and later historical phase, small mammals archaeology research remains to be strengthen popularization and research depth.
    A study on the physical characteristics of Barags in China
    LI Yonglan, ZHENG Lianbin
    2016, 35(03):  431-444. 
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    The physical characteristics in Xin Barag Left Banner of Hailaer (196 males and 204 females) of Barags were investigated, compared with the physical characteristics between Barags and Chinese or foreign groups, Come to the conclusion of physical characteristics of Barags and approached a problem, that is the Barags typing position in the ethnography, analyzed the reason of formation of the physical characteristics of Barags. The results are as follows: 1) Barags with higher frequency of eyefold of the upper eyelid and he percentages of mongoloid is 40%. The nasal root height is medium-type, the height of ala nasi is medium-type, the nasal profile is lower. The nasal profile is straight type, the zygomatic projection is prominent, thickness of lips is mainly filmy. Black hair color, yellow skin color and brown eye color. Convex chin with higher frequency obviously. Barags have the physical characteristics of mongolian stock. 2) The most obvious body characteristics of Barags is large weight. The lavel of bust, waist circumference, hip circumference and thigh circumference are largest of ethnic groups in china. Its subcutaneous fat is thick and BMI far more than modern rural of Han in china. 3) The males and females of Barags are brachycephaly, hypsicephalic type and tapeinocephalic type, mesoprosopy, mesorrhiny, broad chest circumference and medium shoulder breadth. Medium distance between iliac crests, mesatiskelic type, short and fat. In addition, males are long trunk. Females are middle trunk. 4) The results of principal component analysis show Barags showed medium figure in Mongolia, and weight is bigger, head is longer and wider, crack a narrow mouth, nose high value is small, the nose wide, and with thin lips. Barags hane physical characteristics is closest to Buriats and Tuvas. 5) The physical characteristics of Barags belong to a medium tapy between the Baykal of the North Asian type of Mongoloid and the Central Asian type, which contain the European race. 6) Barags from Turkic language groups to Mongolian language groups gradually. Genetic factors is the main reason for the formation of its physical characteristics and living environment, dietary components also have important effects on formation of its physical characteristics.
    Effects of environmental factors on adolescent body surface area growth of urban Chinese
    GAO Guozhu
    2016, 35(03):  445-457. 
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    This research used Stevenson and DuBois’ formulae to calculate the average body surface area of 7-18 year-old adolescents in 30 cities throughout China, and then used factor analysis to obtain growth scores. Correlation analysis and multiple regression analysis were used to analyze the growth scores, natural environment and socio-economic environment to determine the comprehensive effects of the environmental factors on adolescents body surface area growth. The results show that the development of body surface area of urban Chinese adolescents has regional differences. Specifically, the body surface area in the top five samples were located in circum-Bohai Sea region. Growth scores had a conspicuousness positive correlation with longitude and latitude, sunshine duration, annual range of temperature, GDP per capita, disposable income per capita and number of medical technicians per 1000 people. Growth scores had a negative correlation with altitude, annual precipitation, relative humidity, Engel’s coefficients, birth rate, rate of population increase and children’s burden rate. The key factors that affected adolescent body surface area growth of urban Chinese were altitude, annual average humidity, Engel’s coefficients and children’s burden rate. Environmental factors that influenced body surface area growth come from the result of co-interaction between the natural and socioeconomic environments.
    A study of physical differences between eastern and western Han students in China
    LI Guofeng
    2016, 35(03):  458-468. 
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    The purpose of this work is to explain Han student physical differences between eastern and western China from two investigations in 1985 and 2010 dealing with student constitution and health. The results shows that students in the eastern primary school are superior and statistically significant to the ones in western China (P<0.05). Overall elementary student body shape, function and urban primary school student physical qualities shows a trend of widening, in contrast to overall rural elementary student physical quality that shows a trend of widenening. Eastern and western elementary student body shape development is expressed in a long-term trend growth with a decline in lung capacity (P<0.05) where western students are less than eastern. Eastern and western elementary students endurance running shows a decline whereas body pull-ups capabilities inclined and have statistical significance (P<0.05). Differences of physical quality between eastern and western students are obvious, with eastern primary school students showing better physical quality in terms of quantity, range and speed, but with number, size and speed lower than western students.
    Vegetation succession in response to climate changes since the LGM in the desert-loess transition zone, North China
    YANG Qing, LI Xiaoqiang, ZHOU Xinying
    2016, 35(03):  469-481. 
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    Human culture was profoundly influenced by climate change. The increasing warmth of the anathermal in the Last Deglaciation and the Megathermal Period of the Holocene are two important periods for cultural evolution. Sensitive vegetation responses to climate change can be traced by fossil pollen records. The loess-paleosol sections of Caijiagou(CJG), Yulin (38.1°N, 109.8°E) and Hanjialiang(HJL), Fugu(39.5°N, 111.1°E), located in the desert-loess transition zone, northern Loess Plateau, were selected to conduct high-resolution pollen analysis. Based on a field survey, as well as the comparison of magnetic susceptibility curves, grain size curves and the δ18O record of stalagmite from Sanbao/Hulu caves during the last 50 ka, we established a depth-age mode of these profiles. Forty-four pollen samples were palynologically identified to rebuild the vegetation succession in the region, and to explore its response to climate changes since the LGM. At least 300 pollen grains were counted for most samples. Forty-seven families and 20 genera of pollen were identified. Four to five pollen assemblage zones were divided according to the variations of major pollen percentages, pollen concentrations and modern surface pollen research for the CJG and HJL profiles, respectively. A detailed history of vegetation succession and its response to climate changes since the LGM was reconstructed. For the CJG section, the pollen assemblage consisting mainly of Artemisia seems to represent a desert steppe during the LGM. During the Last Deglaciation, the pollen assemblage mainly consisting of Rununculaceae and Poaceae might reflect the appearance of a sparse steppe environment. In the Younger Dryas, the Artemisia and Poaceae assemblage might suggest the development of a meadow steppe. During the Holocene Optimum, the meadow-steppe dominated by Artemisia appeared. For the HJL section, steppe dominated by Artemisia lasted from the LGM to the Holocene Optimum, but the pollen concentration of the Last Deglaciation and Holocene Optimum was significantly higher than that of MIS-3 and the LGM. Moreover, accompanying drought-resistant plants such as Chenopodiaceae and Taraxacum-type appeared during the LGM, but suffurticosa plants of Zygophyllaceae appeared during the Last Deglaciation due to the improvement of water availability. Our results showed that the vegetation succession of the Desert/Loess transitional zone was mainly controlled by the changes of temperature and water availability since the LGM. During the cold/dry period of the LGM, local vegetation was dominated by drought-resistant species with low vegetation coverage and monotonous community. During the anathermal of the Last Deglaciation and Megathermal Period of the Holocene, vegetation coverage increased with some magaphanerophytes. Our research provides a valuable modern analogue for the study of vegetation in response to global warming.