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    Review of the domestic and international progress in paleodemography
    HOU Kan
    Acta Anthropologica Sinica    2026, 45 (01): 1-17.   DOI: 10.16359/j.1000-3193/AAS.2026.0002
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    Paleodemography is the scientific analysis of past population dynamics, utilizing archaeological human skeletal remains for reconstruction. This review traces the methodological evolution of these techniques on a global scale, with a particular emphasis on China, highlighting significant paradigm shifts in addressing two fundamental challenges: age estimation bias and the representativeness of skeletal samples.

    Paleodemography first emerged in the 1930s, when early studies were largely confined to rudimentary statistical descriptions and comparative analyses of population sex and age structures. In the 1960s, the introduction of the life table method marked a turning point, eventually establishing it as the predominant analytical approach. However, in 1982, the methodological foundations of the field were profoundly challenged by a seminal critique that exposed systematic errors in adult age estimation. Critically, the critique revealed the “age mimicry” effect, whereby estimated age distributions unintentionally replicate those of reference samples. This revelation triggered four decades of innovation: Bayesian statistics became instrumental in refining age estimation methods. These efforts culminated in the 1999 Rostock Manifesto, which advocated for probabilistic methods. Transition Analysis (TA) emerged as a pivotal technique, leveraging the progression of skeletal traits to effectively mitigate bias. Concurrently, a fundamental shift occurred in the field of demographic modeling, transitioning from the life table method to parametric hazard models. Additionally, proxy indicators (e.g., D5-14/D20+, D0-14/D ratios) were developed to indirectly estimate fertility and growth rates when direct evidence was unavailable.

    In China, paleodemographic research began in the 1980s, focusing on analyses of Neolithic cemeteries’ sex ratios and age structures. Early interpretations often attributed observed imbalances to sociocultural factors, such as reproductive risks and gender differences in labor intensity. During the 1990s and 2000s, research expanded to include regional syntheses, exploring the correlations between demographic patterns and social complexity, agricultural intensification, and environmental stress. Life table analysis gained prominence during this period, particularly for estimating life expectancy. Since 2010, methodological sophistication has accelerated: model life tables have been adjusted to correct for infant underrepresentation; Bayesian-inspired age estimation and transition analysis have been experimentally applied; and fertility proxies have been employed to test hypotheses about agricultural transitions. Increasingly, studies have adopted integrated approaches, combining demographic data with paleopathology and settlement patterns to investigate health disparities, conflict, and population dynamics.

    Recent advancements in methods and technologies have further refined age estimation techniques. including Transition Analysis software (TA2, TA3) for Bayesian-based adult aging, reducing mimicry bias and enhancing accuracy. Complementing these developments, improvements in demographic modeling have seen parametric hazard models (e.g., Gompertz-Makeham, Siler) replace traditional life tables for mortality analysis, while fertility proxies were used to estimate population growth. Semi-parametric and non-parametric models have also been applied in paleodemography.

    This review also examines four pivotal theoretical issues. First, the application of the uniformitarian hypothesis to paleodemography raises questions about its validity, particularly in light of the osteological paradox— the observation that skeletal samples may not accurately reflect living populations due to factors such as selective mortality and heterogeneity in physical health. Second, the conceptual misalignment between death assemblages and living populations poses a significant challenge. Third, the finding that mean age-at-death primarily reflects fertility levels rather than mortality has reshaped interpretations. Finally, the Neolithic Demographic Transition theory, an archaeological framework derived from paleodemographic research, explains how agricultural practices drove demographic changes, such as increased fertility.

    The future of paleodemography in China holds substantial promise. To fully realize this potential, it is essential to further integrate interdisciplinary research, including aDNA and isotope studies, into migration research. Leveraging China’s extensive archaeological record will enable rigorous evaluations of global theories, such as the Osteological Paradox and the Neolithic Demographic Transition. Crucially, future research would actively develop indigenous theoretical frameworks rooted in China’s unique archaeological and historical contexts, thereby advancing the discipline’s localized development. Sustained interdisciplinary collaboration remains vital for methodological innovation and robust demographic reconstruction.

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    Morphological variations of circum-nasal region of the Pleistocene human skulls in China
    LIU Wu, HE Jianing, WU Xiujie
    Acta Anthropologica Sinica    2026, 45 (01): 18-33.   DOI: 10.16359/j.1000-3193/AAS.2025.0001
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    When studying the Homo erectus fossils from Zhoukoudian in the 1940s, Weidenreich noticed that the lower border of the nasal aperture of Zhoukoudian hominins exhibited patterns different from those of modern populations from Europe, Australia, and Melanesia. In the 1960s, when studying the crania of Upper Cave, Wu Xinzhi proposed that the Late Pleistocene humans in China had wide nasal apertures. Even so, so far, no study of the circum-nasal region morphology of Chinese hominins has been conducted, and the morphological patterns and variabilities of the circum-nasal region in Chinese hominins remain unclear.

    In this study, the morphological features in the circum-nasal region of 22 Chinese hominin fossils were described and compared. Our study indicates that the circum-nasal region morphology of Pleistocene humans in China exhibited marked evolutionary changes. Homo erectus, Middle Pleistocene humans, and Late Pleistocene early modern humans showed different patterns. In addition, there were intragroup variations among Chinese hominins from different chronological periods.

    The nasal aperture of H. erectus exhibited some common morphological patterns: 1) a sharp lateral margin; 2) a sharp lower margin that formed a clear border dividing the naso-alveolar clivus and the nasal cavity; 3) the absence of a subnasal fossa, resulting in a flat upper portion of the naso-alveolar clivus; 4) a weak or absent anterior nasal spine.

    The nasal apertures of late Middle Pleistocene hominins showed some specific patterns: 1) the nasal aperture was wide and low, with the horizontal size larger than the vertical size; 2) a sharp lateral margin; 3) a sharp lower margin forming a clear border; 4) all the specimens had a subnasal fossa that, together with the lower margin, divided the naso-alveolar clivus and the nasal cavity; 5) the anterior nasal spines were either weak or moderately developed; 6) the subnasal fossae showed different morphological patterns.

    The nasal apertures of Late Pleistocene hominins also showed some common patterns: 1) the height of the nasal aperture increased; 2) the lower margin in most specimens was open, with a flat transition between the naso-alveolar clivus and the nasal cavity; 3) nearly all the specimens had a subnasal fossa, with the exception of Yahuaidong; 4) the anterior nasal spines were pronouncedly developed in most specimens; 5) the relative size of the nasal apertures seemed to be irregular; 6) the lower margins in some specimens (UC 101 and Maludong) exhibited a morphological pattern resembling that of late Middle Pleistocene hominins and different from those of other specimens from this time period.

    Except for these characteristics of the nasal aperture mentioned above, compared with Holocene populations, the nasal apertures of Pleistocene hominins were lower. Both H. erectus and late Middle Pleistocene hominins had clear lower borders of the nasal aperture. The lower borders of the nasal aperture in most Late Pleistocene hominins were open, with a flat transition between the naso-alveolar clivus and the nasal cavity. The subnasal fossa seemed to appear from the late Middle Pleistocene. The anterior nasal spine also seemed to appear in the late Middle Pleistocene and became more pronounced gradually. Starting from the Late Pleistocene, the development of the anterior nasal spine showed variabilities, with the northern specimen of Upper Cave having a pronounced anterior nasal spine, and the southern specimens of Liujiang and Longlin showing weak anterior nasal spines.

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    Simulation experiment on the flaking of boat-shaped core from the Erdaoliang site in the Nihewan Basin
    TONG Guang, LI Feng, GAO Xing
    Acta Anthropologica Sinica    2026, 45 (01): 46-58.   DOI: 10.16359/j.1000-3193/AAS.2025.0017
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    Although the boat-shaped core is regarded as a distinct lithic technology, it has been categorized within microblade technology. Arguments regarding its morphological characteristics, preparation methods, and classification are prevalent in scientific literature. Similar to other microblade technologies, research on boat-shaped cores has primarily concentrated on the preparation of their cores, which has been extensively explored by researchers. However, there has been relatively little investigation into its percussion technique. The percussion technique plays a crucial connecting role in microblade technology, restricting the structure of fine stone nuclei and influencing the morphology of fine stone blades. Moreover, the study of percussion technology can aid in the identification of microblade technology.

    The aim of this study is to determine the percussion technique for the boat-shaped core by using archaeological materials from the Erdaoliang site in the Nihewan Basin, North China. To identify the striking technique of the boat-shaped cores, a research paradigm was developed that integrated stone-knapping experiments with quantitative analysis. A sample of bladelets was obtained using various percussion techniques, such as pressure, direct percussion with a hard hammer, direct percussion with a soft hammer, and others. These experimental products were then compared with archaeological materials using quantitative methods. Traditional linear data analysis, which involved parameters like thickness and width, along with geometric morphometric and correspondence analysis, was employed to assess the similarity between the experimental samples and the bladelets from the Erdaoliang site. Bladelet length was not used in linear data analysis because it is easily affected by factors other than the percussion technique. Ellipse Fourier analysis was utilized to analyze the platform and outline (ventral side down) of the bladelets. The analysis shows that the archaeological materials from the Erdaoliang site are similar in width, thickness, etc. to the products of pressure and direct percussion with a soft hammer. However, their exterior angles are closer to those of direct percussion with a soft hammer and smaller than those of pressure products. The Ellipse Fourier analysis yielded consistent results. The correspondence analysis also indicates that the products of soft-hammer flaking are more similar to the Erdaoliang bladelets.

    Based on the quantitative study, the bladelets from the Erdaoliang site were most likely produced using the soft-hammer technique, which differs from microblade technology in that it involves pressure flaking. Therefore, boat-shaped cores should be considered within the context of bladelet technology rather than microblade technology. This finding contributes to a better understanding of the diversity of microblade and bladelet technologies in the Upper Paleolithic of Northeast Asia, as well as the diffusion patterns and environmental adaptations of different late Upper Paleolithic technologies.

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    Origin of the ash-pit burial people at the Duzhong site in Mianchi, Henan
    ZHOU Ligang, WU Zhijiang, SUN Lei, DU Yue, HAN Weiwei, WU Xiaotong
    Acta Anthropologica Sinica    2026, 45 (01): 59-73.   DOI: 10.16359/j.1000-3193/AAS.2025.0012
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    This study explores the provenance and social affiliations of individuals from the ash-pit burials in the late Yangshao period through multi-isotopic analysis. Systematic isotopic measurements (carbon, nitrogen, strontium, oxygen) were carried out on the skeletal remains of 15 individuals from four burial pits at the Duzhong site in Mianchi County, Henan Province. The stable carbon and nitrogen isotope values of 15 bone samples and 10 dental samples(δ13C=-8.4‰±2.7‰, δ15N=9.0‰±1.0‰; n=25) reveal a predominantly millet-based diet, which is consistent with that of the contemporaneous Central Plains populations. Notably, a comparative analysis of intra-individual bone and dental isotope values shows significant dietary shifts from childhood to adulthood, potentially reflecting changes in lifestyle or living environment. The similarity of strontium and oxygen isotope values of bone samples (87Sr/86Sr=0.71210±0.00004, δ18O=-7.8‰±0.5‰; n=9) indicates that all the individuals spent their last few years at the same site. However, the significant variation in tooth values shows that most male individuals did not grow up locally and had spent their youth in different areas. They might have migrated to the current site from the plains in the east or some areas close to the sea, which is consistent with the direction of cultural factor origins reflected in cranial morphology and tooth-extraction customs. Individuals buried in the same pit include both locals and non-locals. Some non-locals in the same pit share similar dietary patterns and migration paths, indicating a close relationship among them and suggesting that they might belong to a certain form of social-organization unit. The traumatic injuries observed on the skulls of certain individuals suggest that these migration events may have involved elements of violence. In addition, the high frequency of human migration observed among the individuals from the late Yangshao ash-pit burials differentiates this mortuary practice from conventional rectangular-pit interments. Male individuals were more likely to be involved in migration events compared to females, which might be related to the marital customs. These findings provide important clues for further research on the nature of late Yangshao period ash-pit burials and cultural exchanges between the Central Plains and the eastern areas. Moreover, this study also demonstrates the value of multiple-isotopic analysis methods in prehistoric archaeological research.

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    The 2023 excavation report on the Yuanmou hominin site, Yunnan Province
    RUAN Qijun, LI Tianguang, CHE Decai, HE Jinmei, SUN Boyang, SHI Qinqin, HOU Sukuan, ZHANG Shuangquan, WANG Guofu, LI Jun, YONG Chun, ZHANG Fei, SHI Junwen, ZHANG Wenjing, JIA Zhenxiu, LI Hao
    Acta Anthropologica Sinica    2025, 44 (06): 939-951.   DOI: 10.16359/j.1000-3193/AAS.2025.0094
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    The Yuanmou hominin site is located at the Jinshajiang River valley, southeastern of the Yuanmou Basin, and is a key and important paleoanthropological site in China. From July 2023 to January 2024, Yunnan Provincial Institute of Cultural Relics and Archaeology conducted a joint excavation at Guojiabaoliangzi that is located at the southeastern part of the site. In total, an area of 200 m2 was excavated, including four sub-excavation areas in varied elevations. The depth of excavated stratigraphy ranges from 5 to 13 m, with a total depth of 29 m. Twenty-three fossil layers were identified, by a depth of 15.2 m. Through the systematic excavation, 12727 pieces of large mammal fossils and 112 pieces of coprolites were unearthed from the four excavation areas. There are 1070 large mammal fossils can be assigned to specific types, including four orders, 13 families, 18 genus and 19 speices, whereas all others are fragmented bones. Preliminary zooarchaeological analysis identified a few number of bone fragments that probably related to the intentional activity of hominins. The 2023 excavation provides important materials for further understanding of the stratigraphy and paleoenvironmental context of the site.

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    Evolution of Cenozoic geomorphology in the Yuanmou hominin site area
    ZHANG Weilin, YAN Maodu, ZAN Jinbo, MIAO Yunfa, SONG Xiangsuo, ZHANG Tao, XU Zunbo, Cairangdaoji , RUAN Qijun, LI Hao
    Acta Anthropologica Sinica    2025, 44 (06): 952-966.   DOI: 10.16359/j.1000-3193/AAS.2025.0098
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    The study on the formation and evolution of geomorphology and the surface erosion of paleo-drainage of the Yuanmou paleolithic site and its surrounding region can well reveal the coupling relationship between tectonic uplift, climate, ecological environment and ancient human activities on the southeastern margin of the Tibetan Plateau. The geomorphologic formation and evolution and the surface erosion of its internal paleo-drainage around the Yuanmou paleolithic site, have profoundly influenced by the multiple tectonic uplifts and paleo-drainage reorganization on the southeastern Tibetan Plateau (SETP) since the Eocene. The ancient bedrock of the paleo-planation surface and the Cenozoic strata above the river terraces have formed a surface weathering crust under long-term physical and chemical processes, becoming an important ecological barrier for the distinctive regional ecological environment, Agricultural and livestock production, and ancient human activities. Based on magnetostratigraphic chronology, tectonic events, and lithofacies changes, our study systematically elucidated the development, formation, and breakup processes of the geomorphology from the paleo-planation surface, the paleo-drainage and the river terraces. The research results indicate that the Yuanmou paleolithic site and its surrounding region have undergone significant tectonic events and paleo-drainage reorganization events in different periods since the Cenozoic, such as during the late Oligocene to early Miocene, early Late-Miocene, early Pliocene, late Early-Pleistocene, middle Pleistocene, late Pleistocene and Holocene, and ultimately formed to its present configuration. In addition, the formation process of the Yuanmou Paleolithic Site is highly related to the formation of the third paleo-planation surface and the development of river terraces, reflecting the close association between ancient human activities and tectonic movements, paleo-drainage changes, and their controlled geomorphic evolution patterns. This work would provide significant geological evidence for exploring the impact mechanisms of geomorphic processes and ecological environment changes on the survival activities of Yuanmou Man and other ancient humans, and also offer essential proof for future archaeological work on ancient humans and Paleolithic artifacts in the Yuanmou Paleolithic Site and its surrounding region.

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    Discovery and advances in the study of Middle Paleolithic Quina technology in Southwest China
    XIAO Peiyuan, RUAN Qijun, LI Hao
    Acta Anthropologica Sinica    2025, 44 (06): 1009-1018.   DOI: 10.16359/j.1000-3193/AAS.2025.0096
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    The Middle Paleolithic or Middle Stone Age, dating approximately between 300,000 and 40,000 years ago, represents a critical phase in human evolution, characterized by significant advancements in technology, adaptive behaviors, and complex interactions among different hominin groups, including Homo erectus, Neanderthals, Denisovans, and early modern humans. During this period, lithic technology underwent substantial diversification and refinement, reflecting key cognitive and behavioral developments. Among these innovations, the emergence and widespread adoption of Levallois technology—also known as prepared core technology—stands out as a representative feature of Middle Paleolithic technological innovation.

    Despite the global significance of these developments, the present and nature of Middle Paleolithic technologies in East Asia—particularly in China—have long been debated. A dominant perspective has maintained that lithic technologies in China lacked the innovative characteristics observed in other regions before the Upper/Late Paleolithic. However, this view has been increasingly challenged by recent archaeological discoveries, which have identified diagnostic Middle Paleolithic elements—such as Levallois and discoid core reduction strategies—at several sites spanning diverse geographical regions of China. These findings suggest that technological innovations were not absent in East Asia but may have followed distinct regional trajectories.

    This study provides a comprehensive global review of Quina technology, focusing on its core diagnostic features: 1) plan-secant volumetric organization for blank production, 2) scalariform stepped retouch (i.e. Quina retouch) on thick, asymmetric and lateral flakes, and 3) complex ramification of the Quina chaîne opératoire. The Quina Mousterian is one of the major technological variants of the European Middle Paleolithic, often interpreted as a Neanderthal adaptation to cold climates, marked by high degrees of tool curation and repeated maintenance during seasonal subsistence.

    By synthesizing archaeological reports and incorporating new evidence from northwestern Yunnan, this research demonstrates the presence of a well-defined Quina techno-complex in southwestern China. This discovery significantly expands the known geographical distribution of Quina technology beyond its traditional association with Europe.

    The identification of Quina techno-complex underscores the diversity and complexity of Middle Paleolithic traditions in China, offering important insights into cultural transmission, regional adaptation, and potential interactions among hominin populations across East and West. Future research should prioritize targeted excavations and interdisciplinary studies at Quina-related sites in northwestern Yunnan. Such investigations will be crucial for establishing a more precise spatial-temporal framework for Quina technology in East Asia and, for exploring the behavioral and taxonomic identity of the hominins who produced it.

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    A preliminary exploration of the phenomenon of miniaturization of stone artifacts during the late Paleolithic period in South China
    LI Sanling, LIU Yalin, ZHAO Wenjie, CHEN Qingyi, LI Hao
    Acta Anthropologica Sinica    2025, 44 (06): 1034-1046.   DOI: 10.16359/j.1000-3193/AAS.2025.0095
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    Recent discoveries of Upper Paleolithic sites across southern China featuring miniaturized lithic assemblages have led to a growing recognition that this trend may represent a significant technological innovation with important evolutionary implications. However, scholarly discussion on the subject remains limited, and consensus has yet to emerge regarding its occurrence time and specific technological characteristics. To address these gaps, this study begins by clarifying the conceptual distinctions between “miniaturized lithic” in southern China and “small stone tool” in the northern region, next systematically reviews key sites in southern China that exhibit lithic miniaturization, and finally focuses on the timing of its appearance, technological features, and adaptive strategies.

    Findings indicate that lithic miniaturizatiwon first emerged around 40,000 years before present during late Marine Isotope Stage (MIS) 3, observed in cave sites throughout Lingnan and Southwest China, such as Yahuai Cave, Fengyan Cave, and Zhaoguodong Cave. By approximately 30,000 years before present, amid the climatic transition from MIS 3 to MIS 2, the technological phenomenon had become widespread around Poyang Lake, with key sites including Shanghu Site and Xianrendong-Diaotonghuan Cave.

    Technologically, these miniaturized lithic assemblages found across southern China exhibit far more commonalities than regional variations, maintaining a remarkable evolutionary continuity over tens of millennia. Key features of the miniaturized lithic assemblages include a pronounced preference for siliceous raw materials such as chert and quartz, the systematic production of miniaturized size of stone artifacts, the widespread adoption of bipolar flaking techniques, and the occasional presence of backed tools. These shared technological traits, though seemingly ordinary, display notable parallels with lithic technologies found in broader geographic regions, such as Southeast Asia and South Asia. This, on the one hand, indicates that the lithic miniaturization in southern China might be an integral part of the global process of lithic miniaturization in the late Pleistocene period. On the other hand, it also underscores the need for a wider comparative framework in future research to better understand technological connections and potential population interactions across these regions.

    The extensive occurrence of miniaturized lithic assemblages and the associated minialithic technocomplex during Upper Paleolithic in southern China reflects a survival strategy adopted by the population to cope with the high mobility of hunting activities. Essentially, it is the product of multi-dimensional technological integration, reflecting the comprehensive assessment by hunting group of variables such as the texture of raw materials, the efficiency of tool production and use, and the maintenance costs.

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    The hominin fossils from Hualongdong and their significance on human evolution
    LIU Wu, WU Xiujie
    Acta Anthropologica Sinica    2025, 44 (05): 727-741.   DOI: 10.16359/j.1000-3193/AAS.2025.0065
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    Starting in 2014, ten years field work of excavations and deposit cleaning at the Hualongdong site, Dongzhi County, Anhui Province have resulted in more than fifty pieces of hominin fossils (including one well preserved skull), and stone tools and other evidence of hominin activities. Through fauna composition analysis and isotope dating, the hominin fossils were dated to about 300 ka. With these findings, the Hualongdong has been ranked as the most abundant hominin fossils and stone tool sites of Middle Pleistocene with Zhoukoudian. For the past ten years, a series of research with hominin fossils of cranium, facial bones, mandible, limb bones and teeth from Hualongdong have been conducted. Some new discoveries and understandings have been achieved from these studies. Our studies indicate the morphological traits of cranium, facial bones, mandible, limb bones and teeth from Hualongdong exhibit mosaics with combinations of East Asian Middle Pleistocene Homo erectus, Late Pleistocene hominin and modern human patterns. The cranium of Hualongdong has a suit of archaic features resembling those of East Asian Homo erectus, including low cranial vault, frontal keel, pronounced supraorbital torus, low position of maximum cranial breadth, slopping nasal floor and relatively small cranial capacity. Moreover, the cranium, facial bones, mandible and teeth show some derived features linking with Later Pleistocene hominins and modern humans. The modern human features in the Hualongdong hominin fossils include thin cranial wall, flat and gracile face, nearly vertical mandible symphysis, occurrence of initial mandibular trigon, and small and simple morphology teeth.

    The hominin fossils discovered from the Hualongdong site were regarded as the one population living in the same time from 270~330 ka. During the studies of the hominin fossils, we noticed some variabilities in the expressions of some morphological features. The lower second molar and the frontal bone discovered in 2006 exhibit a suit of feature patterns that are usually found in East Asian Homo erectus. The frontal bone shows a robust temporal line and thick cranial wall. Besides, the frontal bone has a metopic suture and enlarged frontal sinus. The occlusal surface of the molar has cusp 5, cusp 6 and cusp 7 plus complicated occlusal morphological pattern. Crown dimensions are within variations of Homo erectus and much larger than those of early modern human, contemporary human and European Middle Pleistocene humans. With these feature patterns, we proposed they may represent Homo erectus living during the Middle Pleistocene. In addition, the three pieces of Hualongdong femurs exhibit mosaic patterns with resemblance to Middle Pleistocene archaic hominins and Late Pleistocene early modern humans respectively, including lacking a pilaster, subtrochanteric pieces similar to Middle Pleistocene, and a prominent gluteal buttress and a small third trochanter resembling to many Upper Paleolithic hominins.

    These morphological patterns suggest that the 300 ka Hualongdong hominin fossils already exhibit the evolutionary trend towards the modern humans, and the Hualongdong hominins are the earliest Middle Pleistocene hominins in East Asia with most modern human features. The discoveries and related studies of Hualongdong hominin fossils provide new evidence for the hominin evolutionary diversities of East Asian late Middle Pleistocene.

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    Sedimentary feature and chronology of Hualongdong site in Dongzhi, Anhui Province
    CAI Yanjun, PEI Shuwen, JIN Zetian
    Acta Anthropologica Sinica    2025, 44 (05): 742-753.   DOI: 10.16359/j.1000-3193/AAS.2025.0075
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    Resolving sedimentary processes and constraining the ages of the Hualongdong site in Dongzhi County, Anhui Province, are crucial for researching ancient human evolution, as well as its living environment and adaptive survival behaviors. This paper comprehensively analyzes the geological, geomorphological, and sedimentary characteristics of the deposits at the Hualongdong site and its surroundings. In addition, we also examine the 230Th-234U-238U dating results of the speleothem debris and animal fossils collected during the excavation. It is confirmed that the deposits at the Hualongdong site formed from a mixture of cave deposits and surrounding rock fragments during the collapse of an ancient karst cave. The transition from the ancient karst cave to the accumulation at the Hualongdong site occurred in three main stages: the cave formation and development period, a relatively stable deposition period, and a rapid collapse and accumulation period. The collapse of the ancient karst cave and the formation of mixed deposits at the site occurred later than approximately 216 thousand years before present (ka BP), and ancient cave deposits containing fossils are the main components of the mixed accumulation at the site. Along with the dating results attained previously, the 230Th-234U-238U dating results of the recently discovered flowstone within the deposits indicate that the cave underwent at least two accumulation periods during its stable sedimentation phase, with early deposition occurring prior to 600 ka BP and later deposition spanning from around 331 to 275 ka BP. The mixing of deposition across at least two depositing episodes adds complexity to the chronological study of the site. By integrating the 230Th-234U-238U dating results of all available speleothem, fossil teeth and bones, this study speculates that the burial age of the most complete human skull fossil discovered at the Hualongdong site can be bracketed between 275 and 331 ka BP, placing it in the late Middle Pleistocene. We suggested that Uranium-series dating of representative fossil specimens can offer vital insights for the chronological study of the site and is strongly recommended for understanding the evolution of the fauna and ancient humans at this site.

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    Craniofacial reconstruction and morphological characteristics of Hualongdong No.6 hominid skull
    JIN Zetian, WU Xiujie, DENG Guodong, LIU Wu
    Acta Anthropologica Sinica    2025, 44 (05): 754-764.   DOI: 10.16359/j.1000-3193/AAS.2025.0063
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    The Hualongdong (HLD) site is situated in Wangcun Village, Yaodu Town, Dongzhi County, Anhui Province, China, on the southern slope of Meiyuan Hill. The site is characterized by a collapsed cave comprising carbonate-cemented cavern breccia, unconsolidated clay and gravel. It was discovered in late 1988. Following several excavation campaigns between 2006 and 2024, approximately 20 human individuals, more than 400 artificial stone tools, numerous bone fragments with signs of manual cutting and chopping, and over 80 species of animal fossils have been uncovered. These findings date back to between 331,000 and 275,000 years ago.

    In this paper, we carried out facial restoration on the HLD No.6 skull fossil unearthed at this site. The HLD 6 hominid skull was found in 2015. When unearthed, the skull was broken into 20 fragments of different sizes, among which 7 were wrapped in a large cementing material, and the other 13 dispersed around the large cementing material. According to the bone thickness, bone sutures, cross-sections, the middle cerebral artery and the occlusal state of the teeth, a three-dimensional model of the HLD skull was 3D virtual restored. After reconstruction, it preserves almost entire face, most of the mandibular and a largely cranium.

    To show the pre-life appearance of HLD hominid, according to the relationship between facial bones and soft tissues, a manual method was adopted to reconstruct the outer surface of the skull with muscle, skin, and facial features using plasticized materials (silly putty and plaster) on the 3D virtual reconstruction of the 3D printed skull model. After craniofacial reconstruction, the HLD hominid showed more modern human features with a flat glabella, a backward forehead, a flat face, and the appearance of a chin, however, it still retained some archaic features such as a developed brow ridge, a low cranial height. The HLD human fossils exhibit a mix of physical characteristics transitional between Homo erectus and modern humans. The cranium displays more primitive traits, the facial structure resembles that of modern humans, and the mandible shows early signs of modern human chin. Compared with the "pre-Homo sapiens" Jebel Irhoud found in Morocco, Africa, dated to the same age, the two show similar transitional physical features from archaic to Homo sapiens. The HLD hominin fossils provide crucial evidence of the diversity of late Middle Pleistocene human evolution in East Asia, indicating that modern forms related to Homo sapiens emerged in this region around 300,000 years ago.

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    Lithic assemblage and adaptive behaviors of hominins at Hualongdong site
    PEI Shuwen, DONG Zhe, GENG Shuaijie, YE Zhi, MA Dongdong, ZHANG Yameng, JIN Zetian
    Acta Anthropologica Sinica    2025, 44 (05): 765-778.   DOI: 10.16359/j.1000-3193/AAS.2025.0070
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    The Hualongdong (HLD) site (latitude 30°06′34.1′′N, longitude 116°56′54.2′′E, 40 m above sea level) is located in Dongzhi County, Anhui Province, China. It was initially discovered in 1988, the excavations at the site in 2006, and from 2014 to 2024 resulted in the discovery of more than 20 individual human fossils, an abundance of lithic artifacts and mammalian fauna. The original cave deposits was about 20 m higher above its current location. Synsedimentary dismantlement, downward slippage, and bedrock weathering are indicated by the brecciated arrangement of the limestone rock blocks, cemented angular, subangular clasts and archaeological remains within the excavation area. Uranium-Thorium dating of speleothems and animal teeth from the brecciated deposits indicated that early human occupied the site most probably took place in the late Middle Pleistocene, ca. 300 ka (270~330 ka). This paper presents the lithic technology and the adapted behaviors adopted by humans at the site.

    The Hualongdong lithic assemblage consists of 322 artifacts which can be divided into Detatched pieces [flakes (N=79; 24.6%), debitage shatters (N=96; 29.8%), bipolar elements (N=45; 14.0%)], Flaked pieces [cores (N=65, 20.2%), core fragments (N=4; 0.3%), bipolar cores (N=2; 0.6%), retouched pieces (N=22; 6.8%)] and Pounded pieces (8 hammerstones and 1 anvil). Lithic raw material includes quartz/quartzite and lava show fluvial cortex and suggests sourcing from streams, while chert nodules and some quartz rock block derive from the outcrop of chert and quartz -bearing bed in bands within siliceous carbonate-clastic strata formation in the surrounding landscape. Quartz is the predominant (87.9%) rock type. Technologically, cores, debitage shatter, and bipolar elements from HLD indicate that freehand percussion was the major knapping technique, while the use of hammer-and-anvil technique is the complementary technique to knap cobble and low-quality quartz. HLD reduction sequences are relatively short, non-organized and without core preparation, resulting in a low degree of standardization in flake morphologies and dimensions. Albeit scarce, retouched pieces are present in HLD lithic assemblage, with an average proportion of 6.8%. Retouch is normally on flakes or flake fragments even cobbles. Scraper dominants the tool type, followed by chopper, denticulate, notch and point. Retouch is casual in HLD assemblages, with no imposition of standardized shapes on blanks. The HLD lithic assemblage can be assigned to Oldowan-like or Mode 1 technology in east Asia as characterized by a simple technological design, low degree of standardization, expedient flaking, and a few non-standardized retouched flakes.

    All in all, the HLD core and flake technology includes bipolar flaking of low-quality quartz rock block and cobbles, and freehand flaking of chert, lava and quartz block fragments, which demonstrate knappers intentionally selected good-quality raw materials to manufacture small flakes and use them for some function. Most chert and relatively good quality of quartz flakes show use wear, probably associated with carcass processing given the presence of cutmarks on some bones. Furthermore, it can be inferred that the general feature of HLD toolkits were expediently made for the function of getting food from animal resources and the knapping strategy was adapted to the local resources in the HLD archaeological landscape.

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    New mammalian fossils from the Hualongdong site in Dongzhi County, Anhui
    TONG Haowen, JIANGZUO Qigao, LI Qiang, CHANG Meijing, LIU Boxuan, JIN Zetian
    Acta Anthropologica Sinica    2025, 44 (05): 779-798.   DOI: 10.16359/j.1000-3193/AAS.2025.0066
    Abstract1330)   HTML43)    PDF(pc) (7993KB)(198)       Save

    The Hualongdong site (Hualongdong Loc.1) in Dongzhi County, Anhui Province is the most important fossil site of mid-Pleistocene Homo found in China in recent years. The Hualongdong site was discovered in 1988 and has undergone 9 formal excavations in 2006, 2014~2016, 2017~2019 and 2023 respectively. The mammalian fossils unearthed during the periods 2014~2016 have been preliminarily reported; Since 2017 onward, a large number of mammal fossils have been discovered, and more species have been added to the fauna list: Rhinopithecus sp., Canis sp., Ailuropoda wulingshanensis, Panthera pardus, Neofelis nebulosa, Prionailurus kurteni, Prionodon hualongensis, Paguma larvata, Urva urva, Crocuta ultima, Equus sp., Stephanorhinus sp., Rusa unicorlor, Hydropotes sp. and Capricornis sp. At present, there are as many as 93 species, including undetermined species of mammals have been recognized from the Hualongdong site. More and more complete fossil specimens have been added to the previously reported genera and species, such as the Ursus thibetanus, Ailuropoda baconi, Panthera tigris, Sus lydekkeri, Cervus grayi, and Bos (Bibos) sp., among which Sus lydekkeri and Bos (Bibos) sp. have the largest body sizes for their kinds ever known. The fossils of brown bear (Ursus arctos), horse (Equus sp.), Lydekker's pig (Sus lydekkeri) and giant deer (Sinomegaceros sp.) from Hualongdong represent the southernmost occurrence of their kinds in eastern China, and they are more frequently recovered in the northern faunas. The age of the fauna of the Hualongdong site is complicated by the discovery of the fossil of Ailuropoda wulingshanensis, because this species was only found in the late Early Pleistocene sites, which is obviously inconsistent with the formation time (ca. 300 ka) of the Hualongdong site as currently dated. The explanation for this phenomenon is most likely due to the collapse and re-accumulation of the original cave deposits, resulting in a mixture of old and new strata. The dominant species of the Hualongdong fauna are gaurs and diverse cervids, which are very similar to those of the Bailongdong fauna in Hubei Province. The Hualongdong fauna is different from that of the nearby Hexian Man Site in the lackness of gaurs in the latter. In general, the dominant species of the Hualongdong fauna is comparable to the Ailuropoda-Stegodon fauna of Middle Pleistocene in southern China, but with a few invaders from the North, which suggests a relatively cold substage at which the Hualongdong Man once experienced. The Hualongdong fauna is different from the Late Pleistocene fauna of southern China, the latter is usually dominated by the Sus scrofa-cervids assemblage.

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