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    Modeling the origin of modern humans in light of new evidence
    NI Xijun
    Acta Anthropologica Sinica    2022, 41 (04): 576-592.   DOI: 10.16359/j.1000-3193/AAS.2022.0028
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    Anatomically modern human (AMH) is a term used for living and fossil humans that have globular skull, short and flat face, gracile skeleton, and a set of other osteological distinctive features different from most of the archaic humans. Researchers, who take Multiregional Evolution model (MEM) as their paradigm, use AMH as a counter part of archaic Homo sapiens, while Recent African Origin (RAO) supporters use the term for all H. sapiens. MEM was derived from continuous evolution ideology. Branching evolution was believed to be negligible during the rise of modern populations. The similarities between different local populations were regarded as the results of convergent evolution. RAO on the other hand suggests that human evolution follows the cladistic form as in the other creatures. AMHs belong to a monophyletic group and have a single origin in Africa. Non-African human populations dispersed out of Africa. Archaic human populations in Europe and Asia were replaced by the anatomically modern human during the dispersal of the latter, and there were very limited genetic exchanges between modern and archaic human populations. Recent advances in ancient DNA and proteomic researches revealed that inter-specific interbreeding did occur among H. sapiens, H. neanderthalensis and the unnamed Denisovan populations. Genomic analyses, however, indicate that regions with a high frequency of Neanderthal derived alleles in modern human genomes are mostly related to deleterious genes. Strong reproductive isolation between modern humans and Neanderthals was also detected. Instead of supporting the multiregional model, the molecular data actually reveals that modern humans, Neanderthals and Denisovans are all belong to their own species at genetic level. Debates over taxonomic assignments of some specific fossils may not be helpful for detecting the evolutionary pattern of Homo in general and the origin of H. sapiens in particular, because most of recent comparisons and analyses are at specimen or population levels, not at species level. Our recent parsimony analyses and Bayesian inferring based on large data matrix revealed that the AMHs formed a monophyletic group. Another monophyletic clade represented by Dali and Harbin skulls is the sister of this group. The divergent time between Neanderthals and AMHs is over 1 million years. This estimation is much older than previous aDNA inferring, but is consistent with the recent results based on genome-wide genealogical analyses. Biogeographic model tests also reveal that a model including multiple multi-directional dispersals among Asia, Europe and Asia statistically fits the phylogenetic tree better than the MEM and RAO.

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    Morphological diversities and evolutionary implications of the late Middle Pleistocene hominins in China
    LIU Wu, WU Xiujie
    Acta Anthropologica Sinica    2022, 41 (04): 563-575.   DOI: 10.16359/j.1000-3193/AAS.2022.0024
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    The hominin fossils have been found in more than 20 late Middle Pleistocene sites in present China. For many years, these fossils have been classified as archaic Homo sapiens, intermediate between Homo erectus and early modern humans, and the ancestors of modern humans in East Asia. However, such an opinion has never been widely accepted in paleoanthropological community. There have been debates on the evolution and taxonomy of late Middle Pleistocene hominins in China and around the world. Since 21st century, some noticeable progresses on the late Middle Pleistocene hominin evolution in China have been achieved. The discoveries and studies on the hominin fossils of Penghu, Xuchang, Hualongdong, Xiahe and Harbin greatly enriched the hominin fossil record in China. Studies on the late Middle Pleistocene hominin fossils in China revealed complicated morphological diversities indicating simply classifying all the hominins of this time period into archaic Homo sapiens cannot accurately reflect the evolutionary patterns of Middle Pleistocene hominins in China. According to the studies of the hominin fossils from Xujiayao, Xuchang, Hualongdong, Xiahe and Harbin, some new opinions on the evolutionary pattern and taxonomy of the late Middle Pleistocene hominins in China have been proposed and triggered different understandings.

    In this study, with analyzing the morphological diversities of late Middle Pleistocene hominin fossils in China, four types of the diversities were identified. Xuchang and Xujiyao are characterized with huge-sized crania and cranial capacity (1800 mL and 1700 mL respectively) with some Neanderthal features. These features occurred together in Xuchang and Xujiayao crania constitute unique morphological combinations which have not been found in all other contemporaneous hominin fossils. The other types of morphological diversities are characterized with 1) dominant common sharing features of late Middle Pleistocene hominins; 2) mainly primitive features; and 3) mainly derived or modern features. These morphological diversities suggest that not all the late Middle Pleistocene hominins in China contributed the formation of modern humans equally. Regarding the opinions that put some of the hominin fossils into different Homo members or taxa, the authors believe that at the present with no fully understanding these morphological diversities, treating the related late Middle Pleistocene hominin fossils in China with combined or mosaic morphological features as populations of unclear taxonomic status is a proper way.

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    Ancient genomes reveal the complex genetic history of Prehistoric Eurasian modern humans
    ZHANG Ming, PING Wanjing, YANG Melinda Anna, FU Qiaomei
    Acta Anthropologica Sinica    2023, 42 (03): 412-421.   DOI: 10.16359/j.1000-3193/AAS.2023.0010
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    Significant shifts in human populations occurred several times throughout history, as populations dispersed throughout Eurasia about 50 kaBP. During the Last Glacial Maximum (LGM), global temperatures dropped sharply causing environmental deterioration and population turnover in areas. After the LGM, populations increased as the natural environment stabilized and gradually developed into today’s populations. With advancements in ancient DNA extraction and sequencing technology, it is increasingly possible to directly retrieve genome-wide data from prehistoric modern human remains. The rapid emergence of new ancient genomes provides an entirely new direction for studying modern human population structure and evolutionary history. This research on Eurasian populations spanning 45~19 kaBP (pre-LGM) and 19~10 kaBP (post-LGM) summarizes the movement and interaction of prehistoric modern human populations, focusing especially on prehistoric East Eurasia, a region that has been less well-studied genetically. Of at least six distinct populations in Eurasia, three did not contribute substantial ancestry to present-day populations: Ust’-Ishim (≈45 kaBP) from northwestern Siberia; Oase 1 (≈40 kaBP) from Romania; and Zlatý kůň (over 45 kaBP) from Czechia. One population represented by three individuals (4.6~4.3 kaBP, from Bacho Kiro Cave, Bulgaria) seemed to contribute at least a partial genetic component to later some Eurasian populations. One population represented by Tianyuan man (≈40 kaBP, from East Asia) was shown to be more similar to present-day East Asians and Native Americans than to present-day or ancient Europeans. One population represented by Kostenki 14 (≈36 kaBP, from western Siberia) and Goyet Q116-1 (≈35 kaBP, from Belgium) was more closely related to Europeans than to other Eurasians. This work also summarized five representative populations after 40 kaBP and before the end of the LGM. In East Eurasia after the LGM (or since 14 kaBP), population histories played out very differently. For instance, high genetic continuity is observed in the Amur region in the last 14 kaBP, while in the Guangxi region of southern China, an ancient population that lived 10.5 kaBP carried ancestry not represented in any present-day humans. To conclude, comparison of genome-wide ancient DNA from multiple prehistoric humans have illustrated a complex genetic history of prehistoric Eurasian modern humans. In the future, additional ancient genomes will provide more evidence and details to illuminate the complex genetic history of modern humans.

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    Classification and variation of the temporal line of skulls in modern human
    YAN Yi, ZHAO Yuhao, WU Xiujie
    Acta Anthropologica Sinica    2022, 41 (05): 775-787.   DOI: 10.16359/j.1000-3193/AAS.2021.0075
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    The temporal lines are muscle attachment marks bilaterally on the surface of the skull. Their morphological variations are meaningful to study the physical features and masticatory function in human evolution. In order to know the temporal line classifications and variations in modern populations, 278 adult skulls from Asia, Africa and Europe were selected to observe and analyze. Based on the arc trend, line width, development degree, roughness and terminal position, the temporal lines are classified into various types, and their identifications are standardly defined and established. The database of various temporal line types in sides, sexes and regions were obtained, that can be used for additional studies in physical anthropology. The primary results of this study show that: 1) there is no significant differences between left and right skull; 2) there were no significant differences in arc trend types and development degree between male and female, or among different regions; 3) There are sex difference in the width and roughness types, showing males have higher percentages than females; 4) There are spatial significant differences in the width and roughness types: Super-wide striped type was only found in the specimens from Yunnan and northern China. The Europeans have a high proportion of ridged type and rough types. The Africans have a high proportion of ridged type and a low proportion of rough type; 5) The specimens of temporal line ending in the occipital bone are very few; 6) The width on the frontal and parietal bones were significantly correlated with each other, as well as with the temporal line arc type; the development degree types on the frontal and parietal bones were significantly correlated with each other, too.

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    History of experiments and debates on the identification of soft-hammer flakes
    CAO Yu, YI Mingjie
    Acta Anthropologica Sinica    2023, 42 (01): 36-45.   DOI: 10.16359/j.1000-3193/AAS.2022.0009
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    The soft-hammer technique refers to the method that removing flakes by direct percussion using indenters made of soft materials, usually involving wood, bones, antlers or soft stones. The use of soft-hammer technique is beneficial for controlling the morphology of flakes more effectively, which is considered to be an important sign of the progress of ancient human cognitive and technological level. Since the early 20th century, the principle of soft-hammer technique and the characteristics of soft-hammer flakes have been described by scholars during the observation of prehistoric lithic assemblages and knapping experiments. It was generally believed that flakes produced by soft-hammer percussion were usually with special attributes such as diffuse bulb of force and lipping, which were usually regarded as direct evidence. Due to the lack of soft hammer discovery in archaeological sites, these attributes usually act as the only evidence for the existence of soft-hammer technique. But with the development of targeted knapping experiments, the above-mentioned attributes have been proved to be the results of multiple factors during the percussion process, such as properties of raw materials, force angle, edge angle and even the style of different knappers and it is controversial to distinguish soft and hard hammer technique based on the characteristics of flakes. This paper reviews the process of recognizing of soft-hammer technique and the history of systematic experiments. It is suggested that the “attributes of soft-hammer flakes” should not be taken as the only evidence for the existence of soft-hammer technique, but need to take into account various factors involved in the whole percussion process. We call for the establishment of a database containing experimental and archaeological data to provide richer comparative materials for the lithic analysis.

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    Physical types and ethnological characteristics of Tibetans
    LI Yonglan, YU Keli, ZHANG Xinghua, BAO Jinping, LI Chong, ZHENG Lianbin
    Acta Anthropologica Sinica    2022, 41 (04): 698-711.   DOI: 10.16359/j.1000-3193/AAS.2022.0020
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    The physique types and ethnological characteristics of Tibetans have always been concerned by academia. According to the statistics of 1530 cases of Weizang Tibetan, Kham Tibetan and Amdo Tibetan measured in 2018, 2019 and 2021, it was found that Tibetan men and women were all super-medium stature, overweight, and all brachycephaly, hypsicephalic, metriocephalic, mesorrhiny, middle trunk, wide chest, wide shoulders, wide pelvis, mesatiskelic, most of them have eyefold of upper eyelid and mongoloid fold. Analysis of the average principal component of 15 Chinese ethnic measurement indicators shows that the location between Tibetans and Han ethnic group of the East Asian is closer than most of North Asian ethnic groups, and the location of Tibetans is closer to most South Asian ethnic groups. The main component analysis chart of East Asian, South Asian, North Asian and Arctic type data in Tibetan data and foreign data shows that Tibetans are the closest to East Asian-type. Research has confirmed that contemporary Tibetans have the characteristics of Mongolian East Asian-type constitution.

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    The origin, spread, and impact of agriculture
    LI Xiaoqiang
    Acta Anthropologica Sinica    2022, 41 (06): 1097-1108.   DOI: 10.16359/j.1000-3193/AAS.2022.0013
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    The origins of agriculture is one of the most significant events in human prehistory and the foundation of ancient cultures. At 10000 BP, agriculture emerged almost independently in western and eastern Asia and Central America at the same time. Mesopotamia in western Asia was thought to be the origin of wheat, barley and oats, while corn, potato, peanuts, etc. were firstly cultivated in Central America. China was featured by two independent agricultural systems, namely rice in the middle and lower reaches of the Yangtze River and millet in the Yellow River Basin. During the process of early crop development, agriculture spread widely from its origin centers to most parts of the world, building an important bridge for cultural exchange and integration in the Eurasia. After Columbus discovered the Americas at the end of the 15th century, the opening of new shipping routes and emergence of numerous trade routes accelerated the spread and integration of crops in the New and Old worlds. The origin of agriculture has changed the ability of human beings to transform or adapt to our environment, and has made an significant impact on human society and the natural environment. Agriculture not only promoted the emergence of a settled lifestyle, but also led to major changes in population structure, division of labor and commodity exchanges. Agriculture improved production efficiency, provided a stable food supply and storage, and increased the intensity and scope of human activities, largely impacting the global ecology and natural environment.

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    A study of the bone awl from the Ziyang Man site, Sichuan Province
    ZHANG Yue, WU Xiujie, ZHANG Shuangquan
    Acta Anthropologica Sinica    2023, 42 (01): 1-14.   DOI: 10.16359/j.1000-3193/AAS.2023.0002
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    Osseous artifacts manufactured with techniques specifically conceived for such materials, such as cutting, scraping, carving, grinding and polishing, is labeled as formal bone tools and commonly associated with modern human behaviour. Bone awls produced with such techniques are among the most significant components of formal bone tool assemblages uncovered from a large number of the important prehistoric sites in the Old World. In Africa, a bone awl with an age of 98.9±4.5 kaBP was discovered from the Blombos M3 phase; and such implements were also unearthed at a number of sites securely dated to between 75-60 kaBP. In Europe, the earliest age (44-40 kaBP cal) of bone awls which were from the Châtelperronian and the Uluzzian sites in France and Italy, is much younger than that in Africa. In China, the early appearance of bone awls is reported at the Longquan Cave in Henan province and the Ma’anshan Cave in Guizhou province, roughly contemporary to that in Europe.

    The Ziyang Man site in Sichuan Province is well-known for the discovery of an almost complete skull-cap of late Homo sapiens. However, an entirely modified bone awl, the unique osseous artifact from the site has received little attention after its first appearance in academic works in 1952. In this paper, we present a detailed techno-functional analysis of this bone awl.

    By comparing with modern reference collections curated at the IVPP, we conclude this artifact was most probably made from the tibia midshaft of a large-sized deer (most possibly Cervus unicolor), as some anatomical features of this bone element could still be observed on its surface.

    Technological and morphometric analyses show the dorsal aspect of this specimen was unevenly scraped, with certain parts of the original compact bone surface still preserved; the ventral aspect, on the contrary, preserved no original bone surface as its distal and medial portion was leveled off by scraping and the proximal portion with a U-shape section was shaped by the repeated gouging with a lithic scraper.

    Microscopic observation of the bone awl shows that rounding, fine transverse striations and polish are confined mostly within a limited area of both its tips. This is in full agreement with the features of ethnographic and experimental examples of awls used to piece hide and skins, as well as those of archaeological specimens of well-established functions.

    Observation of the specimen under microscope revealed the presence of red residues still adhering to the distal tip of the bone awl. Both the SEM-EDS (Scanning Electron Microscope-Energy Dispersive Spectrometer) and LIBS (Laser-Induced Breakdown Spectroscopy) analyses of the sampled red residues detect Fe-rich components, and yield spectra with peaks centered on Fe element more intense than the control samples lacking red residues. We thus suggest that the distal tip of the awl might have been stained by ochre powder when it was used for hide or skin piercing.

    Through comparative studies with the alike finds from the archaeological sites of southern China, the regional specificity as well as human behaviors embodied in this artifact were tentatively explored and it seems reasonable to argue that the bone artifact from the Ziyang Man site was an exemplary osseous tool in prehistoric China with signs of multi-functionality and clearly identified ochre residues on its functional unit.

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    The origins and destinations of the Levantine Initial Upper Paleolithic: A view from the Negev Desert, Israel
    Omry BARZILAI
    Acta Anthropologica Sinica    2023, 42 (05): 626-637.   DOI: 10.16359/j.1000-3193/AAS.2022.0035
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    The Initial Upper Paleolithic (IUP) is a chrono-cultural phase corresponding with the onset of systematic production of pointed blades in various regions in Eurasia. This phenomenon is often conceived to correlate with the MIS 3 modern human expansion. Originally defined after the site Boker Tachtit in the Negev Desert, Israel, the Levantine IUP is composed of two consecutive superimposed lithic industries. The lower, named Emiran, is characterized with bidirectional blade technology, whereas the upper industry with unidirectional blades. Until recently the chronology of Boker Tachtit was insecure but new radiometric ages have shown that the Emiran is contemporaneous with the local Late Mousterian, thus supporting the assumption of this industry being imported. Similar technological features and chronological proximities between Boker Tachtit and assemblages from the Nile Valley and southern Arabia suggest the early Boker Tachtit inhabitants may have originated from these regions. The Emiran industry developed in Boker Tachtit into a later variant, the unidirectional industry, but it also expanded northward to central Europe and north-central Asia. The later variant acted in a similar manner as it developed locally into the early Ahmarian techno-complex but also expanded into the northern Levant and the Balkans. It is proposed the IUP phase featured at least two dispersal events. The first is the expansion from the Nile Valley/Arabia to the Levant from where it expanded rapidly to central Europe and north-central Asia. The second dispersal occurred slightly later and began in the southern Levant from where it spread to the northern Levant and the Balkans.

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    Quantitative analysis of the correlation between fingerprint and age
    SONG Huanting, TANG Wei, ZHANG Limei, ZHANG Zhongliang, ZHANG Jiayu, CHEN Shitao
    Acta Anthropologica Sinica    2022, 41 (06): 1047-1057.   DOI: 10.16359/j.1000-3193/AAS.2021.0088
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    A difficult problem in the study of criminology is the determination of age and other personal characteristics of criminal suspects, especially the use of fingerprints. For a long time, many scholars noted subtle changes in fingerprints with an increase in age, but presently there is a lack of specific correlation between the characteristics of fingerprints that change with age and the age of the individual. In this work, we use the Leica M125 volumetric microscope to measure right thumb wrinkles, density of friction ridges, width of friction ridges and small furrows, fine point lines and flexion crease in 1510 samples. The correlation between feature information in the right thumb and age was analyzed with SPSS software. Variables showing high correlation were selected for multiple linear regression. We found features of wrinkles, friction ridges density, width of friction ridges and small furrows, fine point lines and flexor crease in fingerprints all correlated with age, but the goodness of fit of the multiple regression model based on these variables was not high. Then we used principal component analysis to recombine the variables and conducted multiple regression analysis again. An ideal model was still not obtained, and we believe this model cannot be applied to the practice for accurate fingerprint age analysis. For research on fingerprints and age, these anatomical features listed above can be used as for reference. Age information that is difficult to measure and express (characteristics such as edge shape of friction ridges, degree of ambiguity of fingerprint marks, and perspiration holes) may play a key role in fingerprints age analysis, therefore such researches need to be continued.

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    Fossil evidence of the emergence of modern humans and their evolution
    XING Song
    Acta Anthropologica Sinica    2022, 41 (06): 1069-1082.   DOI: 10.16359/j.1000-3193/AAS.2022.0036
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    Modern humans (or recent, late or modern Homo sapiens) are characterized by their morphology, behavior, genetics etc. The mode of modern human origins and their evolutionary route has been the focus of many multidisciplinary researches including paleoanthropology, molecular biology, Paleolithic archaeology, environment and chronology. In recent years, findings of new fossil materials and chronological dating have updated the first appearance of modern humans in different continents and to earlier times. Applications of molecular biology reveal common genetic mixing among Neandertals, Denisovans, and modern humans, leading to a complicated scenario of early modern human evolution since the Upper Paleolithic. However, controversies still exist, and in particular, there are still several unsolved issues about how modern humans originated and evolved on the East Asian mainland. This work summarizes the important fossils of modern humans and the key findings about origin mode and evolutionary routes. Pre-modern H. sapiens can be traced back to Marine Isotope Stage 9 (MIS 9) in Africa, where there is relatively continuous fossil evidence through the late Middle to Late Pleistocene. The first appearance of modern humans in Eurasia was pushed back to MIS 6, and after a hiatus of fossil evidence during MIS 5a and MIS 4, modern humans began to widely disperse across the whole Eurasian continent including islands of East Asia, the southeast and Oceania. It is this fossil evidence and chronology that indicates multiple dispersals of early modern humans out of Africa. Based on morphological and molecular evidence, the evolutionary route of Eurasian modern humans during the MIS 3 and MIS 2 is non-linear. Instead, the evolutionary dead end of certain individuals (or the population it represents) and the inter-continent population connections suggest a mode of “net with breakpoints” for the evolutionary route of early modern humans. Future studies focusing on phenomics of fossil hominins and extant modern humans, more fossil evidence and analysis of ancient DNA will shed more light on this emergence pattern and evolutionary mode of modern humans in Eurasia, especially those in the East Asian continent.

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    Head facial characteristics of Miao students in Lar Mountain area
    LI Wenqin, QIN Dabao, XIONG Jian, ZHANG Huijuan, HUANG Dayuan
    Acta Anthropologica Sinica    2022, 41 (05): 862-874.   DOI: 10.16359/j.1000-3193/AAS.2021.0062
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    Ten items of head facial characteristics of 1896 Miao primary and middle school students(919 males and 977 females)aged 6~16 in Lar mountain area were investigated by anthropometry method, and 13 cephalofacial index values were calculated by formula. The results were as follows: 1) The growth development in head and face of Miao students has following characteristics: The mean value of measuring items increased gradually with age, the mean values of head and face indicators of boys were higher than those of girls in the same age group, and there were significant difference in majority of age groups. 2) Overall, the values of length-breadth index of head, morphological facial index, morphological upper facial index, physiognomic facial index, zygomatic frontal index, physiognomic upper facial index, physiognomic upper facial height index of male students and morphological facial index, morphological upper facial index, physiognomic facial index, zygomatic mandibular index, physiognomic upper facial index of female students increased at first and then decreased with age. 3) The values of vertical cephalo-facial index of male students and length height index of head, breadth height index of head, transverse cephalo-facial index of female students increased gradually with age. 4) There were significant differences between the values of length height index of head, breadth height index of head, transverse frontoparietal index of male students and those of female students in majority of age groups. 5) Head shapes of Miao students of Lar Mountain area were characterized by mesocephaly, hypsicephalic and tapeinocephalic, and their facial types were mainly featured by euryprosopy and hypereuryen. 6) The results of the principal component showed that compared with other ethnic groups, the face type of boy was short and wide, and the head shape was long, while the face type of girl was shorter, and head type was longer and narrower of Miao ethnic group in Lar mountain. 7) The head and facial feature of Miao students in Lar Mountain is close to those of Tujia and Rongshui Miao, far away from Kazak and Han of Xinxiang.

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    A probe into the southern dispersal route of early modern humans
    LI Hao
    Acta Anthropologica Sinica    2022, 41 (04): 630-648.   DOI: 10.16359/j.1000-3193/AAS.2022.0031
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    The southern dispersal route of early modern humans has become a highly discussed topic internationally, primarily because it aids our understanding of modern humans’ migration and adaptations in the southern part of Eurasia, Island Southeast Asia and Oceania. This paper aims to review various aspects of this dispersal, including its timing, possible routes, and current debates.

    Presently, increasing evidence indicates that early modern humans equipped with Middle Paleolithic technologies migrated out of Africa and arrived in the Arabia peninsular and South Asia during MIS 5 stage, and they may also have reached Australia by at least 65 ka. Paleoenvironmental and GIS-based analyses indicate that both coastal and inland routes were likely taken during the dispersal, and current dispersal debates are concerned with establishing the range of its geographic expansion, in addition to assessing how influential it was in facilitating the occupation of early modern humans in different regions.

    After ca. 50 ka, early modern humans on the Southern Dispersal Route begin to show similar behavioral characteristics with contemporaneous modern humans in Africa and in the northern part of Eurasia, such as the use of ochres, personal ornamentation, and cave art. At the same time, these modern humans also developed regional adaptations independently, for instance, the exploitation of rainforest environments and marine resources, the production of water craft, amongst others. Regarding lithic technology, archaeological evidence in South Asia shows the appearance of advanced microlithic technology (microblade, backed tools and etc.) by 50-30 ka, whereas in Southeast Asia and the Oceania, lithic technology trends towards miniaturization, expediency, and an emphasis on micro-flake production. The application of use-wear and residue analyses also indicates that some micro-flakes were used to make organic tools or to form part of composite tools, implying the existence of complex technological behaviors.

    South China is adjacent to Southeast Asia and the Indian Peninsular and therefore can be included in research on the Southern Dispersal Route, from both geographical and environmental perspectives. However, such a study has rarely been done in South China. To explore the emergence and evolution of early modern humans in South China, quantitative and inter-regional technological-based comparisons and analyses are needed on both the Middle Paleolithic assemblages and those micro-flake-based Late Paleolithic assemblages found in South China, along with robust use wear and residue studies.

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    The study progress of the morphological variation of human orolabial region
    LI Haijun, WENG Minjie, DUAN Wanqi, LIU Liming
    Acta Anthropologica Sinica    2023, 42 (01): 137-148.   DOI: 10.16359/j.1000-3193/AAS.2022.0016
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    The orolabial region is one of the most important anatomical structures of the human face, closely connected to the skin around the oral cavity, and has important physiological functions. The lips protect the oral cavity from the penetration of external substances, and maintain the humidity and temperature inside the oral cavity, and aid to chew. At the same time, the orolabial region is also one of the main parts of cosmetic surgery, and lip wrinkles have an important identification value in forensic physical evidence research. In addition, the orolabial region is one of the main objects of study in the fields of archaeology, anthropology, and medicine. In the field of anthropology, both the skeletal and soft tissue morphology of the orolabial region are important materials for the study of the characteristics of different ethnic groups. In the field of medicine, the study of orolabial morphology can provide a more accurate basis for the treatment of orolabial diseases and the individualization of plastic surgery. With the development of science and technology, research on orolabial morphology in different fields at home and abroad has used a variety of research techniques and methods and involved multiple aspects, forming a diverse range of research results, providing a basis for the establishment of a quantitative database on the orolabial region of the population in the future. Current research on orolabial morphology includes the following aspects: 1) The manifest characteristics of sex differences in orolabial morphological variation, and their association with nasal width; 2) Age differences in morphological variation of the orolabial region, and their age-related sex comparisons; 3) Ethnic differences in morphological variation of the orolabial region; 4) Factors influencing the morphological variation of the orolabial region, including genetics, dietary structure, tooth and jaw morphology, and breathing patterns; 5) Applications related to the study of the morphology of the orolabial region, including medical aspects such as cheilopalatognathus, orthodontics, lip plastic surgery, etc., personal identification through lip prints and lip shapes, and applications in the field of forensic criminal investigation such as reconstruction of the deceased’s appearance. There are relatively few studies on the morphology of the orolabial region in China, especially the lack of more systematic studies on the growth and development of the morphology and variation of the orolabial region. In this paper, we examined the research results on orolabial morphology at home and abroad, sorted out and summarized the research data and conclusions in the related literature, gave a brief overview of the research on orolabial morphology according to certain research directions, and made a brief review and outlook on the research on orolabial growth and development and morphological variation in China.

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    A review of Paleolithic raw material exploitation studies in China
    SHEN Xuke, LI Ting, ZHANG Dongju
    Acta Anthropologica Sinica    2023, 42 (02): 161-176.   DOI: 10.16359/j.1000-3193/AAS.2023.0014
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    As an important part of the lithic artifact manufacturing system, lithic raw materials exploitation reflects several attributes of prehistoric humans, including environmental cognition, resource exploitation, mobility patterns, and cultural exchanges. However, there were differences in these attributes between Africa and Western Eurasia: In the former, high-quality flint and obsidian are relatively abundant, whereas in East Asia the Paleolithic hunter-gatherers mainly exploited the locally ubiquitous vein quartz, quartzite, and ordinary chert to produce stone artifacts. This has resulted in a relatively small number of Paleolithic raw materials exploitation studies in East Asia. To better understand what is known about the lithic raw material exploitation strategies of the Paleolithic hunter-gatherers in China, here we review and summarize all previous related studies. We found that from the Lower Paleolithic to Upper Paleolithic periods, raw materials composition, source selection and exploitation methods changed substantially. During the Lower Paleolithic period, hunter-gatherers mainly exploited local vein quartz, quartzite and flint from riverbeds, bedrock outcrops and weathered outcrops near residential or camp sites. The quality of these raw materials was usually unexceptional, and the exploitation distances were generally within 10 km. During the Middle Paleolithic period, lithic raw material types increased in number and they varied between regions. Although the quality of these raw materials was also generally unexceptional, high-quality flint began to appear at some sites, albeit not in dominant proportions. Local procurement within 10 km still dominated during this period, while long-distance procurement occurred occasionally. The hunter-gatherers during this period clearly had an improved ability to recognize and utilize local raw materials, and they relied increasingly on high-quality raw materials. During the Upper Paleolithic period, the types of lithic raw materials increased greatly, and there was a marked decrease in the proportion of vein quartz and quartzite, and a significant increase in the proportion of high-quality raw materials, like flint, chalcedony, siliceous rock and volcanic tuff, and there was also the first appearance of obsidian. Long-distance procurement of high-quality raw materials in northern China became more common, but in southern China local procurement from riverbeds still dominated. The emergence of specialized raw material exploitation and lithic production workshop sites is another distinctive feature of this period. These temporal and spatial changes in Paleolithic raw material exploitation strategies in China were likely the result of multiple factors, including the mobility patterns of hunter-gatherers, advances in stone tool production technologies, and climate changes. In summary, the study of Paleolithic raw material exploitation strategy is critical for understanding human behavior, population interactions and migrations. Therefore, more intensive and systematic studies of Paleolithic raw materials exploitation in China are needed in the future.

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    Early position of the Daur language branch in the Mongolian language group
    SHAREN Gaowa, CHENG Huizhen, WEI Lanhai
    Acta Anthropologica Sinica    2022, 41 (06): 1037-1046.   DOI: 10.16359/j.1000-3193/AAS.2022.0006
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    According to previous linguistic work, the Daur language was categorized as a separate language or cluster in nearly all classifications of the larger Mongolic language group. Previous studies showed that many elements of the ancient Mongolic language in the 13th century are found in the modern Daur language. Here, based on evidence from genetics, history, ethnology, and linguistics, we explored the evolutionary history of the ancestral group of Mongol-speaking populations and provided an accurate timeframe for the early differentiation of Mongolic languages and the emergence of the Daur language as a separate branch. Y-chromosome lineage M401 is one of the paternal founding lineages of all Mongolic-speaking populations. The dominant paternal lineage of Daur, F5483, was one of the oldest sub-branches of M401, while most of the M401 individuals from other Mongolic-speaking populations belong to another lineage, the F3796 or other major sub-branch of M401. These two sub-branches differentiated at about 2,900 years ago. Studies of history, ethnology, and linguistics also revealed a permanent separation between Mongolic tribes who dispersed across the eastern Eurasian steppe and their relatives who remained as hunter-gatherers in the forest since the 9th century. In terms of demographic history, Daur is indeed the oldest branch of all Mongolic-speaking populations. We suggested that the multidisciplinary evidence, especially that of biological anthropology, supports the early branching of the Daur language from the Mongolic language group.

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    Antler fossil of Sinomegaceros ordosianus from Nanbaishan site of Late Pleistocene age in Yüxian, Hebei Province
    MEI Huijie, ZHANG Bei, LEI Huarui, TONG Haowen
    Acta Anthropologica Sinica    2023, 42 (02): 225-237.   DOI: 10.16359/j.1000-3193/AAS.2023.0001
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    Giant deer is among the most common animals of Mid-Late Pleistocene sites in northern China, and was one of the representative icons of the Pleistocene fauna in northern China, while the fossil materials are fairly poor and very few complete antlers were ever recovered, except those from Zhoukoudian site; on the other hand, the knowledge about the age-related changes of the antlers is absolutely insufficient. Therefore, the previous taxonomic work based only on the antler features is open to questions.

    In 2018, a quite complete antler of giant deer was recovered from the Nanbaishan site of Middle Paleolithic period in Yüxian County, Hebei Province. The antler is quite big; brow tine and the palmation of beam are thin and fan-like, without palm tines; the brow tine and the palmation of beam run along two nearly parallel planes, but are not exactly parallel; the shaft of the beam bends at the basal part, but the sigmoid form is not prominent. In general morphology, the new antler is very close to that of Sinomegaceros ordosianus. The new specimen represents the most complete antler of S. ordosianus ever recovered. The dimensions (L: length & W: width) of the palmate is 670×526.8 mm; the dimensions (L& W) of the brow tine is 510×480 mm, the length and circumference of the beam are 270 and 193 mm respectively, the circumference of the burr is 310 mm. The first phalanx is robust, its greatest length is 77.7 mm; proximal width is 29.2 mm, transverse and antero-posterior diameters are 24.0 and 26.0 mm respectively.

    In China, quite a number of megalocerine taxa had been named at the species and subspecies levels, namely Sinomegaceros pachyosteus, S. ordosianus, S. flabellatus, S. konwanlinensis, S. youngi, S. luochuanensis, S. sangganhoensis, S. o. mentougouensis and S. baotouensis, among which S. ordosianus is the most widely distributed species and has the richest fossil records. On the contrary, S. baotouensis is the least known species which only represented by one shed antler and one metatarsal bone. With only a few exceptions, e.g. Tangshan near Nanjing, Zhoushan island in Zhejiang and Hualong Cave in Anhui, all the other megalocerine fossil sites in China occur north of the Yangtze River, and most of them are located in northern China. The fossils of S. ordosianus were frequently appeared in the prehistoric site, which indicates that the giant deer was very probably among the food sources of early humans. The OSL age of the Nanbaishan site is around 110 kaBP, which falls into the range of the Middle Paleolithic period.

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    The northern dispersal route: New evidence of Upper Paleolithic human behavior from the Tsagaan Turuut River Valley, central Mongolia
    Tsedendorj BOLORBAT, Dashzeveg BAZARGUR, Guunii LKHUNDEV, Batsuuri ANKHBAYAR, Adyasuren ALTANBAGANA, Tsend AMGALANTUGS, Gonchig BATBOLD, CAO Jian’en, SONG Guodong, CAO Peng, CAI Xi
    Acta Anthropologica Sinica    2023, 42 (04): 488-502.   DOI: 10.16359/j.1000-3193/AAS.2022.0007
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    Mongolia’s unique geographical location between northern China and the Siberian Plateau of Russia has facilitated its role as a corridor of regional cultural connection since the Pleistocene. It is evident that the Early Upper Paleolithic of Mongolia dates to 33-27 kaBP from the archaeological studies of those Upper Paleolithic sites at Tsagaan Agui and Chikhen Agui in Bayankhongor Province (Southwest Mongolia). Here, we present the results of archaeological analysis of Paleolithic remains from the six sites in the Tsagaan Turuut River Valley located in Galuut district, northern Bayankhongor Province. These newly discovered sites significantly expand our knowledge of the prehistory of central Mongolia and most of Central Asian region. The knapping technology at these sites is based on radial cores and unidirectional prismatic cores. By analyzing the lithic artifacts from these six sites, we believe that these cultures have continuity from early to late stages of the Early Upper Paleolithic. Special tools such as points and large bifaces were recovered. The 14C dating results of a bone sample from the lower layer of a test pit indicate that the Tsagaan Baast Valley sites are no later than 43500 BP cal (β-TSTC1).

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    A report on the 2019-2020 paleolithic survey in Yuxian Basin
    NIU Dongwei, YAN Xiaomeng, MA Dongdong, XU Zhe, PEI Shuwen
    Acta Anthropologica Sinica    2022, 41 (05): 936-944.   DOI: 10.16359/j.1000-3193/AAS.2021.0067
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    Yuxian basin, located in the southeast part of the Nihewan basin (senso lato) in Hebei Province, is an important area occupied by early hominins during Pleistocene. This report presents some preliminary results of the new Paleolithic survey conducted by the staff from the Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences and Hebei Normal University from 2019 to 2020 in Yuxian basin. A total of 18 Pleistocene localities including 16 Paleolithic localities and 2 mammalian fossil localities, were newly discovered and confirmed, and 35 stone artifacts and a few mammalian fossil fragments were collected. The Paleolithic and fossil remains are buried in the Nihewan lacustrine sediments and loess. Typologically, the stone artifacts collected from these Paleolithic localities include hammerstone, cores (including microblade cores), debitage (whole flakes, flake fragments and chunks) and tools. The raw materials for stone knapping are dominated by volcanic rocks, followed by cherts and quartzite. The principal flaking and retouching technique were hard hammer percussion, while soft hammer had probably also been used when modifying bifacial preforms of wedge-shaped microblade cores. Based on the technological and typological characteristics of these stone artifacts, two different assemblages of lithic artifacts have been identified, one is a core-flake assemblage characterized by simple cores, flakes, lightly-retouched tools etc.; the other is a microblade assemblage characterized by wedge-shaped microblade cores. Based on the geomorphological and stratigraphic comparison in the Nihewan basin and the technological traits of lithic assemblage, it can be inferred that these new 18 discovered localities may be assigned to the Middle Pleistocene (n=4) and the Late Pleistocene (n=14). Furthermore, the two microlithic localities are more likely formed during the late Upper Pleistocene based on the comparison with the similar finds (Youfang site and Ma’anshan site) in the Nihewan basin of Yangyuan county.

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    Human tooth and diet from a bioarcheological perspective
    LEI Shuai, GUO Yi
    Acta Anthropologica Sinica    2022, 41 (03): 501-513.   DOI: 10.16359/j.1000-3193/AAS.2021.0057
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    Diet plays an important role in the origin and evolution of human culture. As the main carrier of dietary information, teeth provide the possibility to reconstruct the dietary lineage of ancient human from different perspectives. As a direct reflection of human chewing behavior, dietary structure and living pattern, the physical anthropological analysis of oral diseases and microscopic traces on the surface of teeth is particularly important. The detection of trace elements and stable isotopes in teeth plays an immeasurable role in revealing the migration and flow of ancient human beings, the feeding behavior and nutritional status in different stages of life, and the origin and development of agriculture. In this paper, based on the review of the importance of human teeth unearthed from archaeological sites and the diversity of research methods, combined with the characteristics of tooth growth and development, we draw the human age map of the dentin growth sequence matched by different dentin positions. Based on this map, we proposed a new method of dentin continuous section sampling. This paper proposes that from the angle of physical anthropology and stable isotope analysis of carbon and nitrogen, using continuous sections of dentin, limb bones, ribs and other human tissues as related materials, on the basis of exploring the individual life history of ancient human beings, the research of “intergenerational archaeology” is prospected.

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