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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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    Periodic climate change and human adaptation
    LYU Houyuan
    Acta Anthropologica Sinica    2022, 41 (04): 731-748.   DOI: 10.16359/j.1000-3193/AAS.2022.0029
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    Since ancient times, climate change, especially periodic oscillation, has profoundly affected the transformation and development of human society. Periodic climate change left its imprints in the origins and migration of humans in the Paleolithic Age, the evolution of culture and civilization in the Neolithic Age, the rise and fall of dynasties in historical periods, the socio-economic turmoils in the era of industrialization, and all other anthropological issues. On the basis of new evidence and progresses in paleoclimatology, paleoanthropology, and environmental archaeology in recent years, this paper examines climatic characteristics at various development stages and key nodes of human society from the perspective of periodic climate change. Using typical study cases, it introduces and analyzes the complex interaction between periodic climate change and human activities at different temporal and spatial scales in the Paleolithic, Neolithic and historical periods, involving the link of periodic climate change to human evolution and migration during the Paleolithic Age, the association of periodic climate change with cultural succession as well as the origin and development of agriculture during the Neolithic Age, complex relationship between periodic climate change and human activities since the historical period, and new viewpoints on the mechanisms of periodic climate change and human social adaptability; it also discusses the similarities and differences between natural and social sciences in understanding the mechanisms underlying the relationship of climate change to human activities, and expounds a new paradigm to study of the relationship between climate change and human activities under the background of interdisciplinary research.

    This new research paradigm involves progresses and breakthroughs in theories, methods, technologies, and applications of climate change and social-cultural development. The following aspects thus must be considered in future studies: 1) transforming the traditional and scattered evidence of qualitative description into continuous temporal-spatial sequences of quantitative parameters (e,g., rate of change, speed, amplitude, threshold) and, and taking into account the multi-source, multi-scale, high-dimensional and complex spatio-temporal dependence of data; 2) merging the case study into the statistical test of big data, and distinguishing the climate-culture phenomena and nodes associated with periodic changes and event superpositions at different time scales through statistical methods such as Bayesian probability and probability inference; 3) carrying out systematical studies on the representative signs of cultures and their quantitative methods in different scenes of history and prehistoric periods, and establishing linear-nonlinear relationships models among human activities, cultural changes, and variations of temperature, precipitation and ecological environment; and 4) having a clear understanding that the studies of paleoclimate changes are providing evidence of multi-layered interaction for the study of earth system science together with the studies of archaeological culture instead of just serving for interpreting past human activities.

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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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    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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    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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    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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    Upper Paleolithic human dispersals and cultural diffusions in Eastern Eurasia
    KATO Shinji
    Acta Anthropologica Sinica    2023, 42 (06): 842-856.   DOI: 10.16359/j.1000-3193/AAS.2022.0012
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    First, trends in the Upper Paleolithic (UP) industries on the eastern China, Korean Peninsula, and Japan Archipelago in Far Eastern Eurasia (FE Eurasia) are outlined. Next, developments in the UP industries in those regions are analyzed from the perspectives of relocation diffusion and expansion diffusion (contact diffusion). As a result, it is possible to gain an understanding of the following events. At the beginning of the UP (before 40 kaBP cal), southern human groups bearing a pebble and flake tool industry moved north and diffused in the southern part of eastern China. In the early stage of the UP (40-28 kaBP cal), regional groups formed, and they contacted each other. As a result, UP techno-cultural elements were diffused between those regional groups. In the late stage of the UP (after 28 kaBP cal), human groups with the microblade industries moved and spread widely in FE Eurasia, and as a result of contact between those groups, microblade industries widely diffused in this area. A glimpse of several entering of western or northern human groups (e.g., the human group with Initial Upper Paleolithic industry) into the FE Eurasia and its neighborhoods were able to catch, all of these, however, proved to be local and temporary ones. From the analysis on Paleolithic industries in this paper, it can be said that the movement of human groups with UP industries as generally consistent with the movements of East Asian ancestral populations that revealed by genomic analysis.

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    Philosophical issues in the study of human origins
    Ni Xijun
    Acta Anthropologica Sinica    2023, 42 (06): 709-720.   DOI: 10.16359/j.1000-3193/AAS.2023.0072
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    The question of human origins is one of the ultimate questions of human existence, and the study of human origins touches on many philosophical issues. Based on recent advances in paleoanthropology and biology, this paper briefly reviews the history of human origins and evolution, and discusses philosophical issues such as the nature of being, the purpose and meaning of human existence, divine creation and evolution, the driving force of human origins and evolution, the nature and role of labor, and contingency and necessity. Counting from the origin of primates, human evolution has a history of at least 56 million years, or 7-8 million years if we count from the human-ape divergence in the sense of evolutionary biology. As a class of biological organisms and the bearer of the subjective world, the nature of being has always been a very complex subject, and it is even impossible for most people to have a recognized answer. From a biological point of view, human existence is essentially the existence of nature. Human beings are a part of the nature and greatly influence the existence of the nature. The characteristics of human beings that distinguish them from primates are the essential characteristics of human beings in the biological sense. In the study of human origins, the question of the nature of being should be examined from different angles of the various sub-disciplines of biology. The purpose and meaning of human existence at the philosophical level are not scientific questions, and the test standards of scientific research can not be applied to it. If human existence has a purpose and meaning, then that purpose and meaning is “existence”. Although traditional creationism is no longer a major part of the human knowledge system, the ideas represented by intelligent design still attempt to answer the questions of whether or not supernatural forces and intelligent things exist, and why they exist. As a living creature, the origin and development of human beings are not fundamentally different from those of other living creatures, and the driving force of human evolution is the result of a combination of intrinsic genetic factors and extrinsic environmental factors. There have been heated discussions about the role of “labor” in the origin and evolution of human beings, but from the empirical evidence of modern paleontology, archaeology, zoology, behavior, ecology, and other disciplines, it is impossible to give an accurate definition of “labor”. It can be argued that human labor itself is a state of behavior exhibited by humans in the process of survival and reproduction. The accumulation of contingent events is recorded, that is, the process of obtaining a quantitative change, and when the quantitative change accumulates to a level where order and hierarchy can be recognized, the change can be defined as qualitative change. Qualitative change in human evolution also occurs when the accumulation of countless contingent changes reaches a definable level. Self-awareness and thinking are not unique to humans. The development of complex systems in the universe with the ability to think is a necessity of material development, but the exact form in which it appears in things is controlled by chance.

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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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    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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    Significance of modern human exploration of ochre in its evolution
    YANG Shixia, XU Jingwen, HUAN Faxiang
    Acta Anthropologica Sinica    2022, 41 (04): 649-658.   DOI: 10.16359/j.1000-3193/AAS.2022.0030
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    The ochre using has been long featured centrally in debates about the origins of symbolic and cognitively modern human behavior. In this paper, we reviewed the ochre using archaeological evidence internationally to clarify its origin, developmental process and its relationship with modern human evolution. Though the ochre using could be dated back to the Middle Pleistocene and also could happened to some archaic hominins, such as Neanderthals, it is deeply related to the origin and dispersal of modern human. We also reviewed the current archaeological evidence related to the ochre exploration in China. It is quite evident that the ochre using behaviors were clear recorded 40,000 years ago, at the time window modern human arrived at North China indicated by fossil and DNA evidence.

    Exploitation of ochre, happened between 300 ka and 500 ka in Africa, is a part of technique innovations or behavioral shifts recorded in Middle Pleistocene, and contemporaneous with the raise of more hominin species (including our own species). Afterwards, around 200 ka, more ochre using evidence were recorded in Africa, Europe and Western Asia. Until around 100 ka, the clear ochre processing evidence and application of ochre on body decoration, cave paintings and even as adhesive. The "ochre using" emerged in large numbers during this period, could be related the dispersal of modern human and the increasing of some archaic hominins. Until around 40 ka, when the modern human widely distributed, diverse ochre applications appeared worldwide. When reviewing the archaeological evidence from China, within this time window, the ochre processing of Xiamabei was occurred, and shows that new adaptations were taking place as modern humans entered the region roughly 40,000 years ago. Afterwards, more archaeological evidence appeared in North and South China, such as the well-known finding in Zhoukoudian Upper Cave, and recently published rock paintings at Tiger Leaping Gorge. Although residue analysis indicated that the presence of ochre within the incised lines in Lingjing site can be dated back to around 100 ka BP, this may illustrate the possibility of ochre exploration of other Late Pleistocene hominins. We should not rule out the possibility that much older ochre exploration evidence would be identified in the future archaeological studies.

    We augured that the behavior adaptation and evolution should be a process, not an event. For our own species, the so called ‘behavioral modernity’ could be rooted in the evolutionary history of some late archaic hominins. The ochre using widespread after the modern human occupied most of the world, and it is a key element of the package of behavioral modernity, but it is not an event of invention of Homo sapiens.

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    Discussion on several issues of Sr isotopic archaeology
    WU Xiaotong, ZHANG Xingxiang
    Acta Anthropologica Sinica    2022, 41 (03): 535-550.   DOI: 10.16359/j.1000-3193/AAS.2021.0053
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    This paper introduces several important theoretical and methodological issues involved with the strontium isotope archaeological research. The first is the variation pattern of strontium isotope ratios in the lithosphere and its influence on the study about human migration. Secondly, four restrictions of the strontium isotope method are addressed, the diagenetic contamination of bone and dentin samples, the overlapping effect of strontium isotope in different regions, the mixed effect of strontium isotope in teeth and bones, and the inability to identify migrant descendants. Finally, two major difficulties in the application of strontium isotope to the study of human migration are investigated. One is how to distinguish the migrant population in a site or cemetery, and the other is how to find the origin of the migrant population.

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    Paleolithic typology and relevant practice in archaeological research in China
    GAO Xing
    Acta Anthropologica Sinica    2022, 41 (04): 618-629.   DOI: 10.16359/j.1000-3193/AAS.2022.0034
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    This paper made a critical review on the development of stone artifact classification and typological research in paleolithic archaeological field. It traced back the origin of this approach in France and subsequent development in Africa, Southeast Asia and China. Its roles in paleolithic studies as well as the limitation and controversies surrounding it were accessed and analyzed.

    Classification on lithic materials and typological analysis are basic academic practice in paleolithic research. F. Bordes’ typological framework came into being in the 1950s and 1960s made profound influence in this subject, other scholars also made contributions to this scheme by adding regional typological variants. Throughout its development, the exercise of lithic classification and typological investigation have been questioned and criticized for its subjective matters and the lack of commonly accepted criteria, and efforts of amendment and improvement have been continued. Today, lithic typological system has largely become a tool-kit for organizing, categorizing, simplifying and describing information of unearthed materials from certain sites. Its function as a descriptive tool is important; it can provide vital information on the content of certain archaeological collection, the nature and formation of the site, lithic technology, stone tool function, cultural tradition and development, etc. However, compared to studies on lithic technology, tool function, raw material exploitation, subsistent pattern, adaptation strategy and landscape utility, which are more closely related to human behavior and cognitive capacity, typological inquiry is becoming less indispensable and more and more marginal in the whole research enterprise. Lithic typology in China is a good example of the general trend of development of this research field; it is an admixture and integration of key western typological elements and terms and innovation with regional characteristics. To better understand the current debates and concerns regarding the status and function of lithic typology, we need to clarify the nature, principle, function and limitation of traditional typology, and to move forward from a basic classification and description tradition to in-depth research into human behavior and adaption. A techno-typological approach guided by the conception of Chaîne opératoire and aided by digital technology might be the solution toward this direction.

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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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    Body indexes of the Chinese population
    LI Yonglan, ZHENG Lianbin
    Acta Anthropologica Sinica    2022, 41 (05): 848-861.   DOI: 10.16359/j.1000-3193/AAS.2021.0059
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    This paper is based on the statistical analysis of 12 indices of the human body of 63452 Chinese people aged from 18 to 97 years old, and the morphological characteristics of Chinese people at present were obtained. Studies have found that overall body type of Chinese people are generally long torso, mid-shoulder, mid-pelvic, and mid-leg type. Men have a mid-chest shape, and women have a wide-chested shape. As their age increase, the upper body of Chinese appears shorter, the ratio of upper body to lower body is smaller, the chest becomes wider, the lower part of torso appears wider, and the legs appear longer. Compared with the southern ethnic groups, the Mongolian and Turkic ethnic groups have a stronger body, a thicker chest, a taller upper body, shorter upper limbs, and a relatively narrower upper part of the torso (shoulder), and a wider lower part of torso (pelvis). The ratio of the length of the upper limbs to the length of the lower limbs is smaller. The study also found that compared with women of the same height, men’s upper limb length and lower limb length are generally smaller than women, and women have a greater sitting height value than men. Compared with the length of the torso, women do have shorter legs than men. Compared with Chinese men and women the same lower body length, the sitting height of women is larger than that of men. In the case of the same height, the sitting height of the Chinese is larger than that of the Eurasian and African races. That is, they have a higher upper body height.

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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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    Reliability and upper age limit of luminescence dating for the Paleolithic and paleoanthropological sites
    ZHANG Jiafu
    Acta Anthropologica Sinica    2022, 41 (04): 712-730.   DOI: 10.16359/j.1000-3193/AAS.2022.0032
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    The development of the luminescence dating technique has made it one of the important dating tools for c onstructing the chronological framework of Paleolithic and palaeoanthropological sites, especially those related to modern humans. It has provided the earliest evidence for the appearance of modern humans in Africa, Asia, and Australia. Therefore, this dating method has attracted extensive attention from Paleolithic archaeologists and paleoanthropologists, especially on the reliability and upper age limit for this dating technique. Luminescence dating materials are ubiquitous quartz or potassium feldspar grains within archaeological deposits, which makes it to date any archaeological sites. In this paper, the basic principle of luminescence dating is briefly introduced, and its reliability and upper age limit, as well as their influencing factors, are reviewed. Literature data show that the precision (e.g., the relative standard error) of luminescence age is mainly related to the physical properties of dated samples and dose rates. The relative standard error(σ) of luminescence age is generally 5%-10%, but it could be <5% under some ideal conditions and sometimes >10% for some samples. A large number of studies have shown that luminescence ages are consistent with independent ages obtained from other dating methods, indicating that this technique is reliable and can be used to build the robust chronology of Paleolithic sites. The upper age limit of luminescence dating is determined by the luminescence properties of dated samples and environmental dose rates. At some sites, reliable luminescence ages up to 1 Ma have been obtained. The upper dating limit of 500 ka is feasible for sediment samples from the majority of Paleolithic sites, and this age range covers the entire period of modern humans. It should be noted that the luminescence properties of sediment samples vary widely from location to location, from sample to sample, and even from grain to grain. The most important of these properties include the stability of luminescence signals and the shape of the dose-response (growth) curve, which are demonstrated by the lifetime of luminescence signals and characteristic dose (D0). The difference in luminescence properties between samples or grains results in different upper dating limits for different samples and even different grains. For the same sample, the upper luminescence age limit of quartz is generally lower than that of potassium feldspar. For the same mineral, different luminescence signals and procedures used to determine equivalent doses may result in different upper limits. Therefore, the upper age limit of luminescence dating is a relatively complicated issue, which depends on the sample’s location, luminescence behaviors, environmental dose rate, and analytical methods.

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    Research progress on the relationship between Paleolithic hominid activities and environmental changes in the Nihewan Basin
    ZHANG Zhen, WANG Ying, LI Yuecong
    Acta Anthropologica Sinica    2024, 43 (01): 184-198.   DOI: 10.16359/j.1000-3193/AAS.2024.0004
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    The Nihewan Basin in northern China has the largest number, densest distribution and most complete chronological sequence of Paleolithic hominid remains, and as such is an ideal region for the research on Paleolithic hominins and environment. Based on published data of 65 Paleolithic sites (groups) in the Yangyuan and Yuxian basins of the Nihewan, this paper discusses the relationship between Paleolithic hominid activities and environmental changes during Pleistocene. The results are as follows. 1. Sites of early Pleistocene mainly appeared 1.8 to 1.0 Ma BP, and were distributed in the northern margin area of the Cenjiawan platform. In the Middle Pleistocene (i.e., after 0.78 Ma BP), with reduction of the paleolake, the range of hominid sites expanded significantly from the Early Pleistocen. These sites were distributed not only in the southern margin of the Cenjiawan platform and the Yuxian basin, but also in the other margins of the ancient lake, such as the central and western parts of the Yangyuan basin. In the Late Pleistocene (i.e., after 0.126 Ma BP), the range of hominid sites further expanded, but with the gradual disappearance of the Nihewan paleolake and the formation of the Sanggan and Huliu rivers, the distribution pattern of sites changed to concentrate on the river terraces reflecting a dependence on water sources. 2. More than 80% of Early-Middle Pleistocene hominid sites correspond to the low Earth Orbit Eccentricity, and more than 70% sites correspond to the Marine Isotope Stage (MIS) interglacial stage, which showed that the climate was relatively warm and with small fluctuations; suitable climate conditions for hominins. 3. During periods of hominin occupation, plant types are mostly steppe dominated by Artemisia and Chenopodiaceae, or forest-steppe dominated by Pinus, mixed with some broad-leaf tree species such as Betula, Ulmus and Quercus. The overall biodiversity was high, which provided not only rich food sources but also relatively wide spaces for hominin occupation. 4. In the Late Pleistocene, advances in stone technology and the use of fire, humans began to appear in later cold glacial periods.

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    Relationship between the human activity and environment changes during the Neolithic and Bronze Age in different precipitation areas of Northwestern China
    LU Yongxiu, DONG Guanghui
    Acta Anthropologica Sinica    2022, 41 (04): 749-763.   DOI: 10.16359/j.1000-3193/AAS.2022.0026
    Abstract346)   HTML130)    PDF(pc) (5999KB)(346)       Save

    The relationship between humans and the environment during the prehistoric period has been receiving increased attention by multiple disciplinarians, including but not limited to anthropologists, archaeologists, and geographers. Northwestern China, the core location of the prehistoric trans-continental exchange, is characterized by complex and diverse topographical features, and rich archaeological remains from the Neolithic period to the Bronze age. However, the prehistoric relationship between humans and the environment in northwestern China with different precipitation remains unknown. Here we based on a review and comprehensive analysis of the multidisciplinary data, such as radiocarbon dates, archaeobotanical and zooarchaeological data, carbon isotopic data of human bone, the spatiotemporal changes of human activities and subsistence strategy during the Neolithic and Bronze periods in northwestern China were reported. And combined with high-resolution paleoclimate records, the trajectory of human-environment interaction, as well as the possible influencing factors were discussed. The final dataset used for analysis included 1440 (349 sites) published radiocarbon dates, 432542 (208 sites) identified crop remains data, 97256 (49 sites) identified animal remains data, and 862 (46 sites) measured carbon isotopic data from human bone were analyzed, respectively. Our results indicate that during the 10000-6000 BP humans in northwestern China mainly lived in the areas that had more than 400 mm of precipitation. As the millet agriculture was still in the early stage of development, the intensity of human activities was relatively low during this time, therefore, the relationship between climate and human activity is not decipherable. During the 6000-4000 BP, intensification of millet agriculture promoted westward dispersal of human activities, which were still mainly distributed in the area with precipitation more than 400 mm, but the human activities leading to migration into areas with precipitation less than 200 mm during the final phase of this period. The intensity of human settlement was declined with the influence of the cold-dry climate events, and the natural vegetation/land were degraded by human agricultural activities in this period. By 4000-2200 BP, the diversification of subsistence strategy was enhanced by the utilization of diverse crops and livestock, especially wheat, barley, and herbivorous livestock that were introduced into northwestern China through prehistoric trans-Eurasia exchange. Meanwhile, the ability of humans to adapt and impact the local environment in different precipitation areas was significantly increased in this period, especially the ability of human to adapt the dry climate in the area with precipitation less than 200 mm. This study will allow us to gain a comprehensive understanding of the processes and driving factors of human-environment interaction in northwestern China during the Neolithic and Bronze periods.

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    The stone artifacts discovered in the Paleolithic survey in the Chaohu Lake Region, Anhui Province in 2019
    ZHAN Shijia, DONG Zhe, YI Shuangwen, ZHANG Hongyan, LI Hao, PEI Shuwen
    Acta Anthropologica Sinica    2022, 41 (05): 927-935.   DOI: 10.16359/j.1000-3193/AAS.2021.0066
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    This report presents the preliminary results of a Paleolithic survey in the Chaohu Lake Region (CLR), Anhui Province. The investigation was conducted by Institute of Archaeology and Cultural Relics of Anhui Province in 2019, and a total of sixteen new paleolithic localities and one animal fossil locality were discovered. A former Paleolithic site-complex, named Wangchenggang, discovered in 1980’s was also reexamined. Nine hundred and thirty-nine stone artifacts and four pieces of broken animal fossils were found during the investigation. Quartzite dominates the raw materials of stone artifacts and most of them are made on cobbles. Technologically, the stone artifacts can be classified into flaked pieces, detached pieces, retouched pieces and bipolar technique products. The exploitation of free-hand core is high and the ratio of cortex is low. Most of flakes belong to type V and II, with some utilized materials coexistent. There are also some large flakes (L>10 cm) in the assemblage. According to the characteristics of stone artifacts, early human detached large flakes from the large cores and further used them as blanks to manufacture heavy-duty tools. On the basis of Zhangjiawan OSL dating results, The age of these paleolithic localities in the CLR were no later than 125 kaBP. The new discoveries bear great significance for studying early human dispersals, technological diversity and the possibility of Acheulean technology large flake in the lower reaches of the Yangtze River.

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