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    15 December 2025, Volume 44 Issue 06
    Yuanmou Hominin Site
    Review and prospect of the discovery and research on the Yuanmou hominin site
    RUAN Qijun, WANG Youping
    2025, 44(06):  927-938.  doi:10.16359/j.1000-3193/AAS.2025.0092
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    Since the discovery of Yuanmou hominin site, several research teams have conducted comprehensive studies on the site, focusing on human fossils, cultural remains, stratigraphy and chronology, fauna, and paleoenvironment, yielding significant research outcomes. However, due to limitations in research materials, studies on human fossils and cultural remains require further refinement, while long-standing discrepancies persist regarding the site’s stratigraphy, chronology, and paleoenvironment. This paper reviews the history of the discovery and research of the Yuanmou hominin site, summarizes and reflects on the key issues and debates in existing studies, and proposes future directions for systematic research. In future, we suggest that the most fundamental and critical tasks include conducting scientific and meticulous archaeological excavations to identify the site’s precise cultural layers, clarify stratigraphic relationships, and discover additional hominin and cultural remains. Moreover, it is imperative to uphold and strengthen interdisciplinary collaboration, integrating methodologies and techniques from archaeology, paleoanthropology, geology, paleontology, geomorphology, chronology, taphonomy, paleoenvironmental studies, zooarchaeology, archaeobotany, and molecular biology. Such a multi-proxy approach will be indispensable not only for the Yuanmou hominin site but also for the study of other paleoanthropological sites in China.

    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
    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.

    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
    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.

    Ecologic and zoogeographic significances of large mammal assemblage from the Yuanmou hominin site
    SUN Boyang, SHI Qinqin, HOU Sukuan, LI Yu, MENG Yue, GUAN Jianyu, WEI Jinkai, RUAN Qijun
    2025, 44(06):  967-977.  doi:10.16359/j.1000-3193/AAS.2025.0101
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    Homo erectus yuanmouensis is renowned as the earliest hominin discovered in China and has attracted global scholarly interest regarding its physical evolution and cultural aspects. Since its initial discovery, multiple excavations have been carried out by institutions such as the Institute of Vertebrate Paleontology and Paleoanthropology of the Chinese Academy of Sciences and the Beijing Museum of Natural History. These efforts have yielded a rich diversity of vertebrate fossils at the Yuanmou Hominin site. The most recent excavation began in July 2023, led by the Yunnan Provincial Institute of Cultural Relics and Archaeology. Across all excavation seasons, the fossil mammalian assemblage identified so far comprises 4 orders, 13 families, 26 genera, and 30 species. Among these, Homotherium crenatidens, Megaviverra pleistocaenica, Ailuropoda melanoleuca, and Tapirus sp. represent the first recorded occurrences at the Yuanmou Hominin site. Notably, the latter two are typical taxa of the Ailuropoda-Stegodon fauna found in southern China. This study has analyzed the genus-level resemblance between the Yuanmou hominin site fauna and other early Pleistocene faunas from different locations and ages in China, aiming to discuss the zoogeographic pattern of Early Pleistocene large mammalian faunas in China. The results indicate that the Yuanmou hominin site fauna, being a mammalian fauna in the early stage of the Early Pleistocene in southern China, shows a higher degree of resemblance with faunas from southern China in general, compared to those from northern China, and a higher degree of resemblance with faunas in the early stage of the Early Pleistocene, compared to those in the late stage of the Early Pleistocene. This suggests that geographic location is a significant factor influencing the dispersal and exchange of large mammals, and that the composition of mammalian fauna would shift due to environmental events in critical periods. In the analysis of all the localities in this study, Tuozidong fauna in southern China had less similarity with Yuanmou hominin site fauna, in contrast, Gongwangling fauna in northern China had more similarity with Yuanmou hominin site fauna, which indicating that due to their special environments, exchange and co-residence of mammals from southern and northern China had occurred in these two localities. Based on the comparison of all the localities in this study, it is found that there was a higher proportion of shrubby grassland in the area around the Yuanmou hominin site, making the habitat of the fauna more open than those in other localities, which has led to the minor difference between the Yuanmou hominin site fauna and the typical mammalian faunas from Oriental realm in the Early Pleistocene.

    A preliminary report on the survey of Laoyatang Paleolithic site-complex in the Yuanmou Basin, Yunnan Province
    RUAN Qijun, ZHANG Shuai, LI Xiang, LIU Jianhui, GUO Xiangqi, LI Jun, CHE Decai, LI Junyi, ZHENG Xiaoyong, YONG Chun, WANG Zhenzhen, JIA Zhenxiu, LI Hao
    2025, 44(06):  978-988.  doi:10.16359/j.1000-3193/AAS.2025.0090
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    During 2022~2023, the joint archaeological team of the Yuanmou hominin site conducted a systematic investigation in the Laoyatang region of the Yuanmou Basin. In total, eight Paleolithic sites with clear strategraphy have been found, along with 391 stone artifacts. Together, we name them as the Laoyatang Paleolithic site-complex. According to the depostional relationship among different sites, we can divide all stone artifacts into three phases. The first phase contains only two pieces, and thus the technological feature is not clear. The age of the first phase likely falls in the Middle Pleistocene or earlier. The second phase contains 133 stone artifacts and has been dated to ca. 74 ka-72 ka based on OSL dating, while the third phase contains 74 stone artifacts and was dated to ca. 56 ka-33 ka by OSL method. In addition, 182 stone artifacts have been collected from both surface and disturbed deposits. Lithic technologies in the second and third phases are close to each other and show expedient core-flake tools industry in general. On one hand, the finding of the Laoyatang Paleolithic site-complex provides valuable materials for reconstructing the evolutionary sequence of humans and Paleolithic culture following the Yuanmou hominind, and on the other hand, it provides important materials for deepening our understanding of human evolutionary history in Southwest China during the Late Pleistocene.

    Paleolithic Archaeology of South China
    A comparison study of three-dimensional geometry of handaxes from the Baise Basin and the Danjiangkou Reservoir Region
    LEI Lei, YE Xin, Li Dawei, XIE Guangmao, LI Chaorong, LI Hao
    2025, 44(06):  989-997.  doi:10.16359/j.1000-3193/AAS.2025.0048
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    The Baise Basin and the Danjiangkou Reservoir Region (DRR) in South China stand as important areas where handaxe artifacts are concentrated, serving as invaluable resources for understanding the complex details of Acheulean technology in East Asia. These regions have witnessed the discovery of numerous handaxes, which have the potential to contribute to our understanding of the technological and cultural developments in this region. However, previous studies mainly focused on the morphological features of handaxes from particular areas. While such studies have provided valuable insights into the morphological and regional characteristics of these artifacts. Notably, a notable divergence in technological complexity and morphological characteristics across different regions.The absence of cross-regional comparison has limited our understanding of the variations and similarities of handaxes’ morphology across disparate areas. In order to compensate for this shortcoming of prior investigations, this study employs a systematic research methodology. Firstly, a three-dimensional (3D) scanning was applied to collected models of handaxes from both the Baise Basin and the DRR. Subsequently, the AGMT-3D software was utilized to analyze the 3D geometric morphology of these handaxes. Through the generation of heat maps, this software enables an intuitive visualization of the variation extent and characteristics. Heat maps provide a straightforward way to identify areas of high and low variation, allowing researchers to quickly grasp the overall morphological trends. Besides this, a series of advanced statistical methods were employed. Principal Component Analysis (PCA), correlation analysis of principal component scores and the Wilcoxon rank-sum test was applied to reveal the morphological differences among handaxes between the two regions. The results of this study reveal several significant findings. It was found that the morphological variation of handaxes in the Baise Basin is notably higher than that in the DRR, indicating a greater diversity in the shape of handaxes produced in the Baise Basin. Moreover, significant morphological difference exist between the handaxes from the two regions. Specifically, the handaxes in the Baise Basin exhibit lower elongation, thinning index, and tip contraction compared to those in the DRR. Such differences in morphological characteristics may suggest that the handaxes from these two regions might have fulfilled different function, been crafted from different types of raw materials with distinct properties, or been influenced by different cultural traditions and chronological factors. In conclusion, this research offers key evidence for a more profound understanding of the morphological feature of Chinese handaxes and the diversity and variability within Acheulean in East Asian.

    Acheulean large tools discovered in Anhui
    DONG Zhe, ZHAN Shijia
    2025, 44(06):  998-1008.  doi:10.16359/j.1000-3193/AAS.2025.0097
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    Large cutting tools (LCTs) are the most typical tools assemblages of Acheulean Industry. The toolkits include handaxes, picks, cleavers and knives etc. Besides of tools mentioned above, the Acheulean large tools assemblage also includes massive scrapers and massive denticulates, which comprise a small numer of tool types based on large flakes other than LCTs. Although quantities of Acheulean large tools were discovered in Dingcun site, Luonan Basin, Danjiangkou Reservoir Region, Baise (Bose) Basin and Piluo site etc. recently, there were still rarely reports mentioned about them in the lower reach of the Yangtze River. Some scholars believed that a Pebble Tool Industry, Oldowan technology, Core and Flake techno-complex dominated the lithic technology dating from Early to Late Pleistocene in this area. Actually, the Institute of Archaeology and Cultural Relics, Anhui Province had discovered numerous Acheulean large tools in the open-air sites which located at the Shuiyangjiang River Basin, Chaohu Lake Region, Wanjiang River Basin and Xin’anjiang River Basin since the 1980’s, with unifacial handaxes, picks, massive scrapers and massive denticulates were the most common tool types during Middle Pleistocene. River cobbles, natural split cobbles and chunks were the most common tools blanks, with unifacial dominated tools shaping directions. Bifacial handaxes, cleavers and knives made on large flakes, which detached from large cores through cobble opening or sliced-slab methods, also existed in the Chaohu Lake Region from Middle to Late Pleistocene. In this paper, we will discuss much more details about 246 Acheulean large tools found in Anhui, especially on the chronology, raw material, type, blank, refinement index and shaping strategy. The combined characters of Acheulean large tools discovered in Anhui showed high variation compared with those found in other areas. The research bears great significance for studying the appearance, diffusion and variation of Acheulean technology in the lower reach of the Yangtze River and even China.

    Discovery and research progress of Quina technology in the middle Paleolithic period in Southwest China
    XIAO Peiyuan, RUAN Qijun, LI Hao
    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 review of Quina technology from a global perspective, focusing on its diagnostic features: 1) the plan-secant volumetric organization for blank production, 2) scalariform stepped retouch (i.e. Quina retouch) on thick, asymmetric and lateral flakes, and 3) the 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 activities.

    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.

    Core reduction strategies and retouch technologies at Guanyindong site, Guizhou Province
    HU Yue
    2025, 44(06):  1019-1033.  doi:10.16359/j.1000-3193/AAS.2025.0091
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    The lithic technology of the Middle Paleolithic in East Asia has traditionally been regarded as primarily characterized by simple choppers and core-flake industries, with limited evidence of complexity and innovations. Recent archaeological discoveries and research findings have increasingly challenged this perspective. Based on the latest research progress on the Guanyindong cave site, this paper systematically reviews and summarizes the key characteristics of its lithic industry. The study reveals that between 180000 and 80000 years ago, hominins at Guanyindong employed diverse flaking strategies and demonstrated proficient tool retouch techniques.

    Flakes are mostly knapped by unifacial detachments. Other core reduction systems include Levallois concept, discoidal production, volumetric exploitation, and core-on-flakes, etc. The Levallois assemblage comprises 11 cores, 30 flakes, and 4 retouched flakes. Both preferential and recurrent knapping approaches were employed in the production of oriented flakes. The primary method used to maintain the convexity of the upper surface is centripetal, supplemented by bidirectional, unidirectional, and convergent configurations. Coefficients of variation calculated for Levallois flakes and other flakes indicates that Levallois flakes exhibit a higher degree of uniformity. Core-on-flakes are commonly found at the Guanyindong site. The reduction strategy is predominantly similar to unifacial detachments, although truncated-faceted pieces and the Kombewa method are also present. A total of 10 discoidal cores were identified, which can be classified into bifacial and unifacial types based on the number of exploited surfaces. At Guanyindong, most of these cores were unifacially detached. Volumetric exploitation cores appear in small quantities (n=12) as well. This reduction strategy focuses on the narrow frontal face of the core, resulting in elongated products. Retouched pieces constitute a significant portion of the assemblage (n=999, 45%), primarily made on flakes. The tool types are diverse, including scrapers, denticulates, borers, and notches. Most tools display two or more retouched edges with steep edge angles, indicating a high frequency of recycling or resharpening. A dual pattern of curation is evident, consisting of both simple and elaborate forms. The elaborated tools include elongated-pointed pieces, tanged points, end-scrapers with parallel removals, standardized denticulates and borers. Additionally, 70 specimens exhibit Quina retouch. These Quina retouches may result from either intentional modification or repeated resharpening during the tool’s use-life. A potential Quina exploitation system may be discernible across multiple aspects, although further investigation is required for confirmation.

    These technological features demonstrate a level of complexity comparable to Middle Paleolithic /Middle Stone Age sites in Western Eurasia and Africa, providing crucial evidence for reassessing the position of East Asian Middle Paleolithic industries within the global framework of lithic technological systems.

    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
    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.

    Exploitation and utilization of chert raw materials from the Tiaotougang Paleolithic site in the Daoshui River Basin, Hunan Province
    LI Yiyuan
    2025, 44(06):  1047-1059.  doi:10.16359/j.1000-3193/AAS.2025.0093
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    The prominent utilization of chert raw material constitutes a defining characteristic of Early-to-Middle Late Pleistocene Paleolithic sites in the Daoshui River Basin, Hunan Province, Central South China. At the Tiaotougang site, for example, chert predominates, comprising 69.96% of the assemblage, followed by quartz sandstone (21.83%) and quartzite (7.92%). These chert materials exhibit diverse coloration, predominantly brown, yellow, and cyan, with secondary occurrences of white and red varieties. Quantitative quality assessment based on grain fineness, internal fissure density, and surface luster characteristics revealed three distinct grades of the chert in this site: good (grade 1, 9.54%), medium (grade 2, 47.28%), and poor (grade 3, 43.18%).

    As all raw materials at Tiaotougang originated as river cobbles, this study prioritized gravel source tracing to investigate chert provenance. Comprehensive lithological surveys of bedrock, modern river gravels, and ancient fluvial gravels near the site indicate that the upper Daoshui River Basin contains relatively abundant and accessible chert resources. However, available chert consists predominantly comprises grade 2 and grade 3 cobbles, indicating medium-to-poor quality. Notably, while chert constitutes only 20%-30% of gravels in local riverbeds comparing with other lithologies, it dominates the assemblage of the Tiaotougang site. This significant discrepancy demonstrates that the site’s ancient inhabitants exhibited marked selectivity and organizational sophistication in exploiting chert resources, reflecting their sophisticated understanding of its superior flaking properties. Furthermore, lithic analysis reveals that medium-to-large tools were manufactured primarily from quartz sandstone and quartzite, whereas small tools were predominantly produced using chert. This pattern indicates hominins’ comprehensive understanding of the lithology-specific characteristics of different cobble types. Based on the spatial distribution of surveyed chert sources, we infer that most chert materials were procured locally from river gravels within a 1-2 km radius of the site. Critically, however, a small quantity of the highest-quality chert appears to have been intentionally procured from ancient terrace gravel deposits located approximately 10 km from the site.

    Preliminary knapping experiments confirm that high-quality chert resources within the Daoshui Basin present no impediment to implementing sophisticated core preparation technologies, including Levallois reduction strategies and bladelet production techniques. The application of complex flaking methods in this region faced no raw material constraints and the persistent dominance of simplistic core-and-flake reduction sequences throughout the southern Chinese Paleolithic record cannot be attributed to limitations in raw material quality or availability. Consequently, this study provides new regional evidence challenging the long-standing paradigm that attributes the gradual trajectory of Chinese Paleolithic cultural evolution to deficiencies in high-quality lithic resources.

    Steep-edged flaking technology of stone tools and adaptation and diffusion of populations in South China during the Middle to Late Pleistocene
    DENG Wanwen, LIU Suoqiang
    2025, 44(06):  1060-1071.  doi:10.16359/j.1000-3193/AAS.2025.0089
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    In recent years, new archaeological discoveries in Southwest China have gradually revealed the adaptability of ancient humans to diverse environments and their cultural complexity during the Middle and Late Pleistocene in East Asia. In particular, the newly discovered Quina-type lithic artefacts in northwestern Yunnan Province have provided new evidence for understanding the cultural connotations of the Middle Palaeolithic in East Asia. Among them, the technological features of Quina-type scrapers with unidirectional multi-tiered retouch are particularly striking. On the other hand, it is noteworthy that some cobble tools bearing characteristics of the Hoabinhian technocomplex previously reported in southwestern Yunnan, as well as those steep-edged cobble tools found in the Lingnan region (i.e., south to the Five-Ranges) and Mainland Southeast Asia, also exhibited multi-tiered stepped flake scars on a nearly vertical flaking surface. Despite their very different morphologies and their production concepts, the two types of products share a technological strategy of unidirectional multi-tiered retouch on the margin(s) of a blank, resulting in steep-edged lithic artefacts. Therefore, this article aims to review the archaeological finds of steep-edged lithic artefacts from Southwest China and the Lingnan region, and try to explore the development of both types of steep-edged lithic artefacts in this vast area, the adaptation of ancient hominins to diverse environments, and possible cultural diffusion among them.

    This article focuses on two types of steep-edged lithic artefacts. The first type is on thick flake blanks. Taking the ventral surface of a thick flake as a striking platform, after continuous unidirectional flaking on the margin(s), multi-tiered retouch would normally be seen on the dorsal surface with edge angle(s) gradually increasing. Those flake scars usually end in the shape of a step or a hinge, wherein earlier flake scars tend to be large and wide while later ones tend to be small and short. Recently in western and eastern Yunnan Province, there found some Quina-like scrapers and semilunar-shaped stone tools respectively, bearing features of multi-tiered retouch scars and nearly steep edge angles. They are representatives for the first type of steep-edged lithic artefacts. Such type of scrapers is currently only found in Southwest China. For example, the Longtan open-air site and Tianhuadong cave site in Heqing, northwestern Yunnan, around 60-50 ka BP, are thought to have yielded lithic artefacts of the Quina system, wherein scrapers clearly show the technological features of unidirectional multi-tiered retouch. The Dahe cave site in Fuyuan, eastern Yunnan, around 50~30 ka BP, also found multi-tiered stepped flake scars on dorsal surface of thick flake blanks.

    The second type is on shaping cobbles. Taking a relatively flat surface of a cobble as a striking platform, after continuous unidirectional flaking on one side or around the periphery of a cobble, multi-tiered retouch would also be seen on a vertical flaking surface with nearly steep edge angle(s). Similarly, those flake scars end in the shape of a step. The end choppers and side choppers found in the limestone cave sites in the Lingnan region from the 1950s to 1960s are representatives for the second type of steep-edged lithic artefacts. Such type of steep-edged cobble tools is widely distributed in a vast area covering Southwest China, the Lingnan region, as well as Mainland Southeast Asia.

    In fact, some researchers used to collect chopping tools with steep edge angles from river terraces in the western Hunan mountainous areas, wherein deposits are presumed to be around the late Middle Pleistocene-early Late Pleistocene. In the western part of the Yunnan-Guizhou Plateau, some core-axes were found in the Xiaodong rockshelter site in Cangyuan, exhibiting quite steep edge angles after shaping around the entire margin of a cobble, claimed to be as early as 43.5 cal ka BP. Thereafter steep-edged cobble tools became quite popular in Southwest China until Terminal Pleistocene, such as the Laohudong (Tiger Cave) site in Baoshan and the Maomaodong (Kitty Cave) site in Xingyi, Guizhou. While in the Lingnan region and Mainland Southeast Asia, steep-edged cobble tools seemed to occur during the MIS 2, such as the Qingtang and Niulandong cave sites in Yingde, Guangdong Province; Bailiandong and Fengyan cave sites in Liuzhou, Guangxi; the Dieu rockshelter site in northern Vietnam, and even reaching far east to the Taiwan Island. Till the Early Holocene, they were more widely distributed, involving the Hainan Island and western Thailand. It could be assumed that steep-edged cobble tools were widely distributed from southern China to Mainland Southeast Asia during the late Late Pleistocene, and that the preference for multi-tiered retouch on shaping cobbles may have gradually spread from north to south, and eastwards to the Taiwan Island.

    The two types of steep-edged lithic artefacts differ greatly in both production concept and morphology, but the late Late Pleistocene lithic industries in the Southwest China-Lingnan region seem to share a technological preference for invasive multi-tiered retouch on lithic blanks. So far, it is difficult to associate all those lithic industries with certain populations, despite fossil and genetic evidence suggesting that a variety of population groups should have inhabited in this vast area during the late Middle Pleistocene-Late Pleistocene. This vast area covers a wide range of topographic and climatic environment, and the interrelationships with lithic industries or population groups remain to be explored.

    It has been suggested that the European Quina system was a technological strategy developed by Neanderthals in response to specific environmental circumstances or economic needs. If the variability of Quina lithic industries in the Europe-Near East region is a manifestation of the adaptability of Neanderthals in responding flexibly to their surrounding environment, then the existence of regional variations in similar technological lithic assemblages is equally understandable in China. Prehistoric archaeologists have also pointed out that modern humans in different regions have creatively exploited diverse resources in their regions as their cognitive abilities improved and they adapted to new environments, thus demonstrating their unique behaviours and cultural modernity to varying degrees.

    Regardless of complex relationships among ancient hominin populations, the late Late Pleistocene lithic industries from Southwest China to the Lingnan region produced different types but relatively standardised forms of stone tools based on different kinds of raw materials, resources, and tasks. Such technological practices reflect a high level of creativity in the adaptation of ancient humans to different environments and their subsistence strategies during the Middle-Late Pleistocene in southern China. The technological preference for multi-tiered retouch on different types of blanks may be related to the adaptation of Middle-Late Pleistocene hominins to different environments and the exploitation strategy of diversified resources in southern China.

    Starch granules in dental residues of ancient humans from the Maludong and Tangzigou sites, Yunnan
    DU Ruiyan, JI Xueping, ZHOU Zhenyu, GUAN Ying, ZHANG Maolin, ZHOU Xiaoyan, XING Song
    2025, 44(06):  1072-1082.  doi:10.16359/j.1000-3193/AAS.2025.0099
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    This study extracted and analysis of micro-residues preserved on ancient human teeth excavated from two terminal Paleolithic sites, Maludong and Tangzigou, in Yunnan Province. Through comparative analysis of starch granule types within the residues, this research investigates plant resource utilization strategies adopted by ancient populations in Southwest China during the late Pleistocene-Holocene transition. Dental surfaces yielded five morphologically distinct starch granule categories: A) Disc-shaped; B) Spheroidal; C) Elliptical or rounded triangular; D) Polyhedral and irregular; E) damaged forms. These starch types correspond to botanical sources including Poaceae seeds, subterranean storage organs, and acorns from the Quercus of Fagaceae.

    Category A (2 granules): Granule diameters range from 12.33-23.57 μm. The planar structure exhibits disc-shaped or elliptical morphology. Under polarized light, extinction crosses appear vertical or X-shaped, with broad and indistinct extinction areas and faint lamellae. These characteristics suggest a likely origin from Poaceae seeds.

    Category B (2 granules): Granule diameters range from 11.34-11.55 μm. Spherical in shape with slightly eccentric and open hila. Polarized microscopy reveals X-shaped extinction crosses and absent lamellae. These granules are tentatively attributed to Amorphophallus species.

    Category C (2 granules): Granule diameters range from 12.4-12.91 μm. Morphologies include smooth elliptical (Fig: 2d) and rounded triangular (Fig: 2e) forms with eccentric hila. Brightfield microscopy highlights distinct hila and faint lamellae, while polarized light shows broad vertical and narrow curved extinction crosses. These are likely derived from Quercus species.

    Category D (4 granules): Granule diameters range from 11.95-24.5 μm. Polyhedral and irregular shapes with slightly eccentric hila, fissures, and uneven surfaces. Polarized microscopy displays X-shaped and narrow curved extinction crosses. These are provisionally classified as originating from root/tuber plants or Fagaceae plants.

    Category E (3 granules): Damaged and unidentifiable due to structural degradation.

    Analytical results indicate three identifiable starch types in Maludong specimens: Poaceae-type (likely wild cereals), Quercus-type (acorns), and Amorphophallus-type (konjac tubers). Notably, gelatinized starch aggregates observed on the surface of specimen MLDG1902 (deciduous first molar) from Maludong suggest plant-based dietary practices involving food processing techniques such as cooking or roasting. In contrast, Tangzigou samples yielded Quercus-type starch alongside unclassified root/tuber varieties. These findings indicate prolonged reliance on subterranean plant resources and Fagaceae nuts. Integrating regional Holocene climate data, this dietary pattern may correlate with the high biomass production of nut-bearing trees (e.g.,Quercus) and geophytes under warm, humid conditions characteristic of evergreen broad-leaved forests. Such environments provided a sustainable resource base for human exploitation. The persistent utilization of acorns and underground storage organs reflects adaptive strategies to ecological constraints, balancing caloric returns with seasonal availability.

    Future research should systematically expand sampling to include ancient human dental remains from other terminal Paleolithic sites in Yunnan, such as the Yiliang Zhangkou Cave site, Fuyuan Dahe site, Chenggong Longtanshan site, and Jinghong Naminnan Cave site—locations with both regional representativeness and chronological continuity. This approach aims to trace the evolution of plant resource utilization by prehistoric humans during critical periods of environmental change, explore how dietary adaptations responded to ecological shifts, and provide key evidence for understanding human adaptive strategies in Southwest China’s mountainous regions since the late Pleistocene.

    A preliminary report of the 2021-2022 paleolithic archaeological survey in Duilong River valley, Lhasa, Xizang
    JIA Zhenxiu, TINLEY Tsring, LI Hao, TONG Yan, SHARGAN Wangdue, CHEN Fahu
    2025, 44(06):  1083-1093.  doi:10.16359/j.1000-3193/AAS.2025.0019
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    From 2021 to 2022, a joint archaeological survey was carried out in the Duilong River valley, Lhasa, Xizang, with the support of the Second Tibetan Plateau Scientific Expedition and Research Program. This collaborative effort involved researchers from the Institute of Tibetan Plateau Research, Chinese Academy of Sciences, and the Institute for Conservation and Research of Tibetan Cultural Relics. The main objective was to investigate prehistoric human activities in this high-altitude region, especially to identify Paleolithic sites buried in primary strata.

    The survey area, located in the hinterland of the Tibetan Plateau at an average altitude of about 4,000 m, includes the Duilong River valley and its tributary systems. These river valleys have well-developed fluvial terraces, which not only serve as the location for modern villages but also as favorable areas for prehistoric human habitation. A total of 13 Paleolithic localities were discovered, consisting of 3 sites with primary buried deposits (Shanggagang, Qiusangsi, and Jiawu) and 10 surface lithic scatters. The elevation of these sites ranges from 3837 m to 4182 m, reflecting the adaptability of early humans to extremely high-altitude environments.

    A systematic analysis of 79 stone artifacts shows a consistent technological pattern dominated by core-flake assemblages. The lithic industry lacks advanced products such as handaxes, blades, or microblades. In terms of the number of stone artifacts and well-preserved buried strata, Shanggagang and Qiusangsi sites are the two most important sites identified in this survey.

    For the 54 stone artifacts discovered at the Shanggagang site, the raw materials were mainly igneous rocks (64.8%), followed by chert (16.7%) and quartz (11.1%), sourced locally from river gravels. Among the 7 cores, the classification includes discoid cores (n=4), polyhedral cores (n=2), and a bipolar core (n=1). The 27 flakes include 15 Type VI, 7 Type V, 3 Type III, 1 Type II, and 1 bipolar flake. The tool assemblage (n=12) is mainly composed of scrapers (n=11), with only 1 pointed tool identified. The number of stone artifacts discovered at the Qiusangsi site is relatively small, but all 5 stone artifacts were found in the primary strata. The raw materials of the 5 artifacts are all igneous rocks, and the knapping method used is the percussion method. The only core found is a polyhedral core. Among the two whole flakes, one is a Type V flake and the other is a Type VI flake. Unfortunately, no tools were discovered. Due to the limited number of stone artifacts found in this investigation, it is difficult to conduct comprehensive and in-depth research and analysis on the technological attributes and cultural connotations of the site.

    Optically stimulated luminescence (OSL) dating of cultural layers at Shanggagang and Qiusangsi provided preliminary age estimates, indicating human occupation no later than 100 kaBP. However, signal saturation prevented precise chronological resolution.

    The discovery of buried sites in the Duilong River valley significantly expands the geographical and temporal scope of known Paleolithic activity on the Tibetan Plateau. This survey confirms that humans inhabited the hinterland of the Tibetan Plateau at least by the Middle Paleolithic.

    Future work should focus on formal excavations, refined chronometric methods, and comparative studies with adjacent regions to reveal the dynamics of early human colonization and adaptation on the Tibetan Plateau. This survey lays a crucial foundation for understanding the adaptability and creativity of Pleistocene hominins in the challenging environments of the Tibetan Plateau.

    Progress and reflections on paleolithic archaeology in Sichuan
    ZHENG Zhexuan, TAN Peiyang
    2025, 44(06):  1094-1105.  doi:10.16359/j.1000-3193/AAS.2025.0110
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    Sichuan Province is located in the hinterland of southwestern China, spanning the eastern part of the Tibetan Plateau and the Sichuan Basin. Its unique geographical location and stepped geomorphology have led to a rich ecological diversity, making it a key area for early human migration and cultural exchange. Although the Paleolithic archaeology in this region started early, with important Paleolithic remains such as the “Ziyang Man” and the “Fulin Culture” being discovered shortly after the founding of the People’s Republic of China, limited research led to many gaps in temporal and spatial framework and a vague understanding of regional Paleolithic culture.

    Since 2019, the Paleolithic archaeological work in Sichuan has gradually achieved a series of breakthroughs. A large number of Paleolithic sites have been discovered on the western Sichuan Plateau and in the Sichuan Basin. These sites feature pebble tools, typical handaxes, Middle and Upper Paleolithic cultural elements, late period remains, and microblades from the Paleolithic-Neolithic transition. These discoveries reflect the complexity and diversity of the Paleolithic culture in Sichuan in terms of time, space, and technology. Important sites such as Piluo site in Daocheng and Mengxihe site in Ziyang have been excavated, yielding lithic artifacts that include various technological traditions and rich evidence for behavioral modernity. Piluo site revealed a continuous sequence of three lithic technology. Its typical handaxes reshaped the understanding of the Acheulean in East Asia, indicating complex interactions between East and West Eurasia and the ability of archaic populations to adapt to high-altitude extreme environments. Mengxihe site discovered abundant organic remains,such as wooden and bone artifacts, which were rare worldwide. It also displayed an early case of broad-spectrum use of plant and animal resources and engraving behaviors, providing key evidence for the study of human behavioral complexity in the early to mid-Late Pleistocene in East Asia. Sites in Fujiang River Basin revealed the uniqueness of the regional “large flake industry”, while the Mengxihe site group showed the miniaturization of flake tools during the early Late Pleistocene

    Abundant materials from these sites documented the technological change of lithic assemblages in southwestern China, providing significant evidence for major scientific questions such as the evolution of the pebble tool traditions, East Asian handaxes and the “Movius Line”, behavioral complexity and the emergence of modern human in East Asia, etc. This paper reanalyzes the previous and recent archaeological records in Sichuan and reconstruct the developmental trajectory of regional Paleolithic cultures, and further discusses its implication in above-mentioned questions. The research reveals clear spatiotemporal diversity and technological sequences—from early simple core-flake techniques, through Acheulean assemblages, to late-stage miniaturization of tools and emerging behavioral complexity—across the highlands of western Sichuan, the basin, and adjacent transitional zones. These advances not only fill gaps in regional cultural development but also provide crucial evidence for understanding migration interactions, technological transmission, and adaptive strategies among ancient populations in northern and southern China, as well as between Eastern and Western Eurasia.

    2022 excavation report of the Jiuligang Paleolithic site in Dangyang, Hubei
    XIANG Qifang, ZHONG Qian, LI Hang, SHEN Yanru, WANG Mingqiang, LI Mingyang
    2025, 44(06):  1106-1119.  doi:10.16359/j.1000-3193/AAS.2025.0008
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    The Jiuligang site is an open-air Paleolithic site located in the 4th Group of Jinggang Village, Miaoqian Town, Dangyang City, Hubei Province. Standing at an altitude of approximately 73 meters, it lies in the transition zone from the mountainous region of western Hubei to the western edge of the alluvial - lacustrine plain formed by the Yangtze River and the Han River. The site was discovered during the construction of the Zaodang Highway in 1996 and was systematically excavated over an area of 500 square meters in 2022. A total of 443 lithic artifacts were unearthed from the Xiashu Loess stratum, which dates back approximately 323000 - 85000 years ago.

    The inhabitants of the Jiuligang site mainly preferred quartz sandstone, quartzite, sandstone, siliceous rocks, and a small amount of chert, vein quartz, etc., as the raw materials for producing lithic artifacts. The large - sized rounded cobbles, probably manuports transported into the site, and the cortex remaining on different - type artifacts indicate that the raw materials were likely collected from the nearby river beaches at that time.

    The lithic assemblage consists of hammers, cores, flakes, tools, chunks, cobbles, and a small amount of debris. Using flakes mainly as the blanks, the retouched stone tools are mainly composed of small - and medium - sized flake tools such as scrapers, as well as a few notches, denticulates, points, and spur - like tools. They are typically characterized by heavy - duty tools like choppers, picks, and knives. In addition, 31 flakes might have been used directly, as small and irregular scars are distributed along their edges.

    Both the main flaking technique and the retouching method are direct percussion with a hard hammer, while bipolar knapping is also observed in a small number of flakes and cores. The tools are mostly retouched unidirectionally, while bifacial processing occasionally occurs in choppers and scrapers.

    In general, the Jiuligang stone artifacts show a typical industry, predominantly distinguished by small - and medium - sized flake tools such as scrapers and supplemented by heavy - duty choppers, picks, knives, etc. Considering the optical stimulated luminescence dating age of 323,000 years ago, the flake tools of the Jiuligang site probably indicate an early stage of the miniaturization of stone artifacts in southern China. Moreover, the appearance of picks, knives, and cores for oriented continuous cyclic flaking of long flakes implies that another cultural factor emerged in the Yangtze River reaches since the mid - to - late Pleistocene.

    With clear stratigraphy and rich cultural connotations, the excavation of the Jiuligang site provides important information for understanding the Paleolithic culture and constructing the cultural sequence in southern China from the mid - late Middle Pleistocene to the early Late Pleistocene.

    A preliminary report of the excavation of Shangbaitang site in Anji County, Zhejiang Province
    LIU Yalin, WEI Tianxu, SHI Xiao, WANG Chunxue, SUN Xuefeng, QIU Hongliang
    2025, 44(06):  1120-1130.  doi:10.16359/j.1000-3193/AAS.2025.0088
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    The Shangbaitang site is located in Anji County, Huzhou City, Zhejiang Province. The site is buried in red clay deposits within the Xitiaoxi River basin. In 2022, the Zhejiang Provincial Institute of Cultural Relics and Archaeology and the Anji County Museum carried out excavations at the Shangbaitang site, covering an area of 1100 m2. Stone artifacts were unearthed in layer 3 and layer 4. Layer 3 is a homogeneous red soil layer, and stone products were mainly unearthed in this layer. Layer 4 is a reticulated red soil layer, and just unearthed a small amount of stone artifacts. According to the dating results, the age of layer 3 is 35~88 ka before present, and the age of layer 4 is more than 100 ka before present. A total of 889 stone artifacts were founded at this site, including 817 from Layer 3 and 47 from Layer 4, along with 25 collected from ground survey. The artifacts include stone cores, flakes, tools, broken blocks and fragments. Preliminary analysis indicates that the raw materials were mainly local gravels, primarily quartz sandstone and a high proportion of siliceous cobbles. Stone cores were percussed through freehand hammering without a prepared process, but the presence of discoidal and prismatic cores suggests some degree of organization in the reduction sequence, reflecting a progressive aspect of core-flake industry. Flakes were predominantly small. There is a low proportion of tools. Scraper was the dominant tool type, along with a small number of choppers, spheriods, and hammers. Tool blanks were mostly flakes with limited retouching, and finely retouched tools were almost absent. Additionally, 18 refitted groups of artifacts were identified, indicating minimal post-depositional disturbance. The early and middle Late Pleistocene was a crucial phase in human evolutionary history. During this period, the majority of sites in northern South China transformed into a lithic industry dominated by flake tools, but the cultural landscape of the lower Yangtze River region during this period remains unclear. Shangbaitang is a rare site that has undergone scientific excavation and dating, and has yielded a large number of stone artifacts. Compared to the Middle Pleistocene, the raw materials, sizes, and types of stone artifacts at this site have undergone significant changes. The proportion of small and medium-sized flake tools is significantly higher than that of large pebble tools, making it a typical representative site of the miniaturization and flaking of the pebble industry. In conclusion, the chronological data and lithic assemblages from the Shangbaitang site provide crucial materials for understanding the emergence and development of small flake tool industries in southern China.