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    Eco-functional divergence of Crocuta and Pachycrocuta: a Huainan specimen reappraisal
    LIU Jin-Yi, Zhijie Jack TSENG, JIN Chang-Zhu, ZHENG Long-Ting, SUN Cheng-Kai, TONG Hao-Wen
    Vertebrata Palasiatica    2025, 63 (4): 277-322.   DOI: 10.19615/j.cnki.2096-9899.250912
    Abstract (3072)   HTML (41)    PDF(pc) (4061KB)(2013)       Save

    Crocuta and Pachycrocuta are widely regarded as the most prevalent and emblematic hyenas across Eurasia during Quaternary. They are easily distinguished by their distinctive carnassial teeth. However, the disparities in non-carnassial elements are less pronounced and have received minimal attention in previous studies. This has resulted in erroneous identifications when dealing with fragmented specimens, particularly in cases where carnassial teeth are poorly preserved or absent. Such misidentifications have the potential to give rise to erroneous inferences regarding the paleozoogeography and biochronology of the animals in question. The bone-cracking hyena specimens from Huainan, Anhui (Tseng et al., 2008) are re-examined and re-evaluated here through a series of morphological comparisons and data analyses (univariate, bivariate, and multivariate analyses etc.). The results provide unequivocal confirmation that the specimens from Xiliexi are not spotted hyenas, but belong to Pachycrocuta perrieri instead. Conversely, the specimen from Dadingshan is the only genuine representative of the spotted hyena, which is supposed to be a possible earliest fossil record for Crocuta ultima thus far in China. Furthermore, the disparities in dentognathic morphology between Crocuta and Pachycrocuta are systematically summarized and analyzed, with an explanation of their eco-functional significance. The present study hypothesizes that Pachycrocuta retains a certain degree of active predatory capability, attributable to the robustness of the canine and the symphysis of the jaw, among other factors. This finding indicates that Pachycrocuta exhibits a form of flexible foraging behavior, combining opportunistic scavenging and active hunting in a manner analogous to Crocuta. Finally, the dynamic evolutionary history of hyenas in East China since Pleistocene has also been broadly reconstructed.

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    First discovery of the spiral-horned antelope Antilospira (Bovidae, Artiodactyla) from the Linxia Basin, Gansu, China
    XU Xing-Dong, SHI Qin-Qin
    Vertebrata Palasiatica    2026, 64 (1): 47-58.   DOI: 10.19615/j.cnki.2096-9899.251030
    Abstract (2041)   HTML (15)    PDF(pc) (1372KB)(749)       Save

    Antilospira is a small to medium-sized antelope with heteronymously spiraled horn cores. It was widely distributed in northern China from the Late Pliocene to the Early Pleistocene. It is a typical fossil bovid with important implications for biostratigraphy and antilopin evolution in China. Antilospira robusta is a species with highly fragmentary materials and has previously only been briefly discussed. Here we report on a new frontal with horn cores from the Early Pleistocene Wucheng Loess in Nalesi Township, Dongxiang Autonomous County, Linxia Basin, Gansu Province. This new material features heteronymously spiraled horn cores, deep longitudinal grooves, a sharp anterior carena on the horn core, and a large body size, which are characteristics similar to those of A. robusta. However, the horn base of the new material is more compressed than all the previously discovered spiral-horned antelopes, so we attributed it to Antilospira cf. A. robusta. This is the first time Antilospira has been found in northwestern China, and this discovery provides more morphological data for the classification of this group. CT scans of the horn core reveal the well-remodeled horn core trabeculae in Antilospira, which is different from what is observed in Spirocerus. The frontal sinuses are moderately developed in the Linxia specimen, extending backwards to the orbit but not to the horn base. The virtual reconstruction of the endocranial cast indicated that Antilospira has bending and narrow frontal lobes, wide temporal lobes, and relatively complex sulci on the cerebral hemisphere, which differ from extant Antilopini bovids in China.

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    Career of Chang Meemann and her contributions to vertebrate paleontology
    ZHU Min, ZHU You-An
    Vertebrata Palasiatica    2026, 64 (2): 125-136.  
    Abstract (824)   HTML (32)    PDF(pc) (2094KB)(727)       Save

    Over more than six decades of dedicated research, Chang Meemann’s career has spanned a critical era marked by a paradigm shift in vertebrate evolution studies. Beginning in the 1950s, inspired by the pioneering ichthyologists of the older generation, including Wu Xianwen, O. P. Obrucheva, and E. Stensiö, she conducted systematic investigations of fish fossils preserved in Paleozoic, Mesozoic, and Cenozoic strata across China. Her work yielded landmark achievements across multiple research domains: the evolution of early vertebrates, the phylogeny of sarcopterygians (lobe-finned fishes), the biostratigraphy and faunal evolution of Mesozoic-Cenozoic fishes, and the Cenozoic paleoecology of the Qinghai-Tibet Plateau as inferred from fish evolutionary patterns. A strong advocate for integrating new technologies and methodologies into fossil vertebrate research, Chang Meemann founded the “Chinese School” of early vertebrate studies, which has since gained international recognition. Her meticulous anatomical analyses of a series of Early Devonian lobe-finned fishes reshaped the classical understanding of tetrapod origins. She played a pivotal role in introducing cladistics, a then-controversial new paradigm in systematic biology, into China. Serving two terms as the director of the Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, she led the institute’s internationalization during China’s Era of Reform and Opening-up. Under her leadership, a new generation of scientists was guided into the study of some of the world’s most significant fossil biotas, such as the Jehol Biota. Through her lifelong dedication, Chang Meemann elevated China’s fossil vertebrate research to a world-leading level.

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    Two anurognathid pterosaur specimens from the Yanliao Biota and a new interpretation of anurognathid skulls
    TONG Shi-Da, JIANG Shun-Xing, CHENG Xin, WANG Xiao-Lin
    Vertebrata Palasiatica    2026, 64 (2): 191-220.   DOI: 10.19615/j.cnki.2096-9899.260411
    Abstract (1828)   HTML (23)    PDF(pc) (17478KB)(703)       Save

    Anurognathids are a clade of small, early-diverging non-pterodactyloid pterosaurs distributed across Eurasia from the Middle Jurassic to the Early Cretaceous. Their defining characteristic is a short and broad skull, a morphology distinct from all other pterosaur clades. Due to limited preservation, the cranial anatomy of this group has long been difficult to understand in detail. In this study, we provide a detailed description of two anurognathid specimens from the Tiaojishan Formation of the Yanliao Biota. The relatively well-preserved skull of one specimen was reconstructed through computed tomographic scanning. This reveals a unique skull element, possibly functionally analogous to the supraorbital bone of varanid lizards. The CT reconstruction offers new insights into the anurognathid skull. Based on these findings, we revised the skulls of previously described taxa, ultimately integrating them into a new reconstruction for this clade. We present a detailed comparative analysis and discussion of the postcranial osteology within Anurognathidae.

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    The discovery of a large ceratodontiform lungfish from the Middle Triassic (Anisian) of Shanxi, China
    SHI Jian-Ru, KANG Zhi-Shuai, DONG Li-Yang, JIA Gao-Wen, WANG Jin, JIA Lei, XU Guang-Hui
    Vertebrata Palasiatica    2026, 64 (2): 183-190.   DOI: 10.19615/j.cnki.2096-9899.251111
    Abstract (1764)   HTML (29)    PDF(pc) (3300KB)(597)       Save

    Ceratodontiformes is the only extant order of Dipnoi (lungfishes). Fossil remains of this group are rare in Triassic deposits in China. Here, we report the recent discovery of a large ceratodontiform lungfish from the Anisian (Middle Triassic) Sinokannemeyeria Fauna in the Taigu District of Jinzhong City, Shanxi Province, China. The specimen was preserved in the argillaceous siltstones from the Third (uppermost) Member of the Ermaying Formation, including remains of 20 caudal vertebrae and associated elements (‘supraneurals’, interhaemals and dorsal and ventral radials) as well as a series of dorsal fin rays. The discovery documents the oldest articulated ceratodontiform in East Asia, predating the previously known articulated ceratodontiform from the Early Jurassic Yuzhou Biota by at least 43 Ma. With an estimated length of ~162 cm, it represents the largest articulated ceratodontiform known so far in the Triassic. The new finding adds to our knowledge regarding body size, morphological diversity, and the paleogeographic distribution of early ceratodontiforms.

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    A new fossil of Galliformes with close relationship to extant turkey and grouse from Linxia Basin
    YU Ting-Yu, LI Zhi-Heng
    Vertebrata Palasiatica    2026, 64 (3): 238-253.   DOI: 10.19615/j.cnki.2096-9899.250731
    Abstract (1760)   HTML (14)    PDF(pc) (8228KB)(568)       Save

    The Linxia Basin, located in Northwest China at the edge of the Tibetan Plateau, preserves a rich fossil record of mammals and birds. Here, we report an exquisitely preserved skeleton representing a new species of small-bodied phasianid from the Linxia Basin, dated to approximately the latest Miocene to Early Pliocene. Gracilisgallus linxia represents the first discovery in China of a taxon closely related to extant grouse and turkey. The new species exhibits a small body size and slender limb bones. Phylogenetic analysis supports its close relationship with extant grouse (Tetraoninae) and turkey (Meleagridinae). The scapula, carpometacarpus, femur, and tarsometatarsus of Gracilisgallus linxia share morphological similarities with its extant relatives, but diagnostic features—such as relatively long spurs on the tarsometatarsus—support its classification as a distinct genus and species, separate from both turkey and grouse. This fossil provides a Late Miocene to Early Pliocene calibration point for the divergence of the turkey—grouse lineages and reveals complex patterns in their radiation across North America and eastern Asia.

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    Osteohistology on Liaoceratops yanzigouensis (Dinosauria: Neoceratopsia) from the Early Cretaceous Jehol Biota
    GUO Te, HE Yi-Ming, ZHAO Qi
    Vertebrata Palasiatica    2026, 64 (3): 221-237.   DOI: 10.19615/j.cnki.2096-9899.250708
    Abstract (1808)   HTML (21)    PDF(pc) (30340KB)(514)       Save

    Ceratopsia is among the most extensively studied groups of dinosaurs. However, research on ceratopsian osteohistology remains extremely limited, leaving significant gaps in our understanding of their growth rates, growth patterns, and life histories. This study presents a detailed histological analysis of the fibulae and ribs from two Liaoceratops yanzigouensis specimens (IVPP V18616 and V17910). V18616 was identified as a juvenile, estimated to be less than one year old, while V17910 was classified as a subadult, at least three years of age. The results indicate that Liaoceratops experienced rapid growth during its juvenile stage, with fibrolamellar bone dominating the cortical bone. By the subadult stage, the growth rate had gradually slowed. This study also highlights the importance of standardized sampling protocols, as evidenced by the rib sections. The feasibility of conducting comparative studies is constrained by the non-standardized sampling locations. The presence of LAGs (Lines of Arrested Growth) in V17910 suggests that Liaoceratops had a cyclical, interrupted growth pattern. In contrast to the continuous growth seen in chasmosaurinae, early-diverging neoceratopsians may have predominantly experienced cyclic growth interruptions.

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    Depositional history, contact relationships, and characterization of Upper Miocene Baogeda Ula Formation in central Nei Mongol with a description of fossil skunks
    WANG Xiao-Ming, SUN Lu, LI Lu, LI Qiang, QIU Zhu-Ding, Zhijie Jack TSENG
    Vertebrata Palasiatica    2026, 64 (1): 100-124.   DOI: 10.19615/j.cnki.2096-9899.251029
    Abstract (1720)   HTML (15)    PDF(pc) (6705KB)(462)       Save

    In addition to its well-known fossils, the Upper Miocene Baogeda Ula Formation is coupled with multiple basaltic lava flows, creating an ideal setting for studying its depositional history, geochronology, and associated vertebrate fossils. This paper, in honor of Prof. Qiu Zhanxiang for his widely admired emphasis on the geological contexts of vertebrate fossils, attempts to synthesize known contact relationships, existing K-Ar dates, and capping basalt elevations to reframe our concept of the lithostratigraphy, magnetostratigraphy, and lateral distribution of the Baogeda Ula Formation. Within this new framework, the Baogeda Ula Formation is defined by unconformable contact with the underlying Tunggur Formation at the lower boundary and a capping basalt at the upper boundary. In many sections, two or three layers of basalts are interbedded within sedimentary strata, with the capping basalts typically belonging to the top two basalts. The newly defined Baogeda Ula Formation includes a lower member as exemplified by Halajin Hushu section and Ulan Hushuyin Nur section, and an upper member at Baogeda Ula section. This expanded concept of the Baogeda Ula Formation includes two major faunas, i.e., the Bahean Halajin Hushu Fauna and Baodean Baogeda Ula Fauna, both falling within the Upper Miocene. We also describe rare fossil skunks (Promephitis) found in recent years that support the age assessments presented herein.

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    Cricetids (Rodentia, Mammalia) from the Late Miocene Yihachi locality of Gansu, China
    QIU Zhu-Ding, Lawrence J. FLYNN, WANG Ban-Yue, LI Lu
    Vertebrata Palasiatica    2026, 64 (1): 1-25.   DOI: 10.19615/j.cnki.2096-9899.251117
    Abstract (1990)   HTML (25)    PDF(pc) (2568KB)(435)       Save

    Our purpose in this paper is to describe the hamster-like rodents (Cricetidae) from a Late Miocene age site in Linxia Basin, Gansu Province, and discuss their significance for the changing ecology of central Asia. The micromammal site known as Yihachi was introduced previously (Qiu et al., 2023; Qiu and Li, 2023), when its squirrels were discussed in some detail. We take this opportunity to describe the more abundant cricetids. There are four genera, common Nannocricetus and Sinocricetus plus the less abundant living Mesocricetus. A few specimens represent the high-crowned and lophodont Rhinocerodon. The cricetids and other faunal elements indicate an early Late Miocene age, and the pattern of occurrence of the hamster species is consistent with a picture of a changing paleoenvironment due to increasing effects of the East Asia monsoon system. After the disappearance of older and archaic genera, Yihachi represents growing endemism in the Late Miocene of northern China due to increasing seasonal rain and the declining average temperature.

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    Asioaspis, a new genus of Polybranchiaspiformes (Galeaspida, stem-gnathostomes) from the Lower Devonian of Yunnan, China
    ZHANG Rui-Rui, ZHANG Ning, LI Qiang, ZHU Min, GAI Zhi-Kun
    Vertebrata Palasiatica    2026, 64 (2): 137-150.   DOI: 10.19615/j.cnki.2096-9899.260113
    Abstract (1840)   HTML (32)    PDF(pc) (17167KB)(427)       Save

    A new genus and species, Asioaspis brachyotus gen. et sp. nov. of Polybranchiaspiformes, is described from the Lower Devonian Lochkovian Xishancun Formation near Miandian Reservoir, Qujing City, Yunnan Province, China. The new genus is characterized by an elongated ovoid headshield with serrated lateral margins, a small subcircular median dorsal opening, short and laterally projecting cornual processes, an exceptionally broad ventral rim, 12 pairs of branchial fossae, and coarse granular tubercles (~3/mm²). It displays a mosaic of characters of the most primitive polybranchiaspiform (Platylomaspis), derived Polybranchiaspiformes, and even the basal members of the galeaspid family Dayongaspidae. Phylogenetic analysis resolves A. brachyotus as an intermediate taxon between the most primitive Gumuaspidae and other derived Polybranchiaspiformes. Although A. brachyotus also shares the broad ham-brim-like ventral rim with the Gumuaspidae, its other characters are more like other derived Polybranchiaspiformes. In particular, its median dorsal opening and paired orbital openings are not highly close-set on the top of the headshield as in the Gumuaspidae, but rather significantly separated from each other and close to the margin of the ventral rim as in the Pentathyraspidae, Duyunolepididae, and Polybranchiaspidae. These proportions indicate that it was unlikely to have lived a semi-infaunal lifestyle and are more consistent with the epibenthic habit typical of most galeaspids, representing an evolutionary transition from the semi-infaunal benthic to epibenthic lifestyle within Polybranchiaspiformes.

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    New oospecies of Parafaveoloolithus from the Lower Cretaceous of Xiuning, Anhui Province
    MAO Lei, WANG Qiang, HUANG Jian-Dong, ZHU Xu-Feng, CHEN Yan-Bin, WANG Xiao-Lin
    Vertebrata Palasiatica    2026, 64 (3): 294-300.   DOI: 10.19615/j.cnki.2096-9899.250930
    Abstract (1463)   HTML (2)    PDF(pc) (12266KB)(425)       Save

    Here we describe an incomplete dinosaur egg nest composed of 12 subspherical dinosaur eggs from Xiuning, southern Anhui Province, China. The eggshell measures about 1 mm in average thickness and is generally comprised of only one layer, although 2-3 layers of eggshell unit can be seen in some places of the eggshell radial section. The pore canals appear honeycomb-like in tangential section, and are characterized by a density of 12 per mm2 in the middle part of eggshell, and diameters between 0.14 and 0.34 mm. Based on these characteristics, we erect Parafaveoloolithus wannanensis oosp. nov. to accommodate the eggs from Xiuning, which clearly belong to Parafaveoloolithus but differ from all previously known oospecies within the Faveoloolithidae. This occurrence of the new oospecies P. wannanensis increases the diversity of dinosaur egg types in southern Anhui Province, extends the previously known distribution of Parafaveoloolithus, and provides more paleontology evidence to help comparison of the Cretaceous strata of southern Anhui Province.

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    A new cranium of Metacervocerus longdanensis (Cervidae, Mammalia) and the genus Metacervocerus in China
    WANG Shi-Qi, MA Jiao, FU Jiao, BAI Wei-Peng
    Vertebrata Palasiatica    2026, 64 (1): 59-73.   DOI: 10.19615/j.cnki.2096-9899.251118
    Abstract (1702)   HTML (6)    PDF(pc) (2486KB)(408)       Save

    This study documents a skull of the large cervid Nipponicervus longdanensis from the Early Pleistocene (~2.6-2.1 Ma) of Longdan, Gansu, China. Morphological comparisons indicate that N. longdanensis exhibits the type of “adaptive” distal fork (anterior tine smaller and oriented along the beam) that differs from the type species Nipponicervus praenipponicus, while it is aligned with Metacervocerus Dietrich, 1938, necessitating reclassification as Metacervocerus longdanensis. The cranium exhibits posteriorly inclined pedicles demonstrating phylogenetic affinity with M. elegans (Nihewan Basin) and M. rhenanus (Europe), while derived features including a shortened neurocranium, rostrally tapered basioccipital, and duplicated P4 protocone distinguish it as an advanced lineage within the genus. Character assessments reveal that Metacervocerus is potentially paraphyletic because Metacervocerus? shansius and Metacervocerus? punjabiensis retain plesiomorphic conditions (elongated braincase, simple P4 morphology), while they exhibit pronouncedly erected pedicles and lyrated antler beams, suggesting a divergent lineage from Metacervocerus longdanensis. Previously published isotopic data (δ13C = −10.9‰ ± 0.9‰, δ18O = −7.5‰ ± 0.9‰, n = 4) indicate a semi-open habitat and a browsing-to-mixed feeding ecology of M. longdanensis. This revision resolves persistent taxonomic uncertainties in Eurasian Cervinae while elucidating East Asia’s biogeographic significance in driving cervid morphological radiation during the Plio-Pleistocene transition.

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    New material of Eospalax simplicidens (Spalacidae, Rodentia) from Jianyucha, Zichang, northern Shaanxi
    CHANG Mei-Jing, SHI Qin-Qin, NI Xi-Jun, LI Qiang
    Vertebrata Palasiatica    2026, 64 (1): 26-46.   DOI: 10.19615/j.cnki.2096-9899.251201
    Abstract (2053)   HTML (13)    PDF(pc) (2565KB)(369)       Save

    Eospalax, one of the only two extant genera within the Myospalacinae, has a high species richness. Each species is distinguished by unique cranial and dental morphologies, as well as variations in temporal and spatial distribution. Consequently, Eospalax serves as a reliable indicator for the biochronologic and paleoenvironmental studies of the Quaternary of East Asia. A recent discovery of a complete fossil skull in a conglomerate deposit, a part of the Lower Pleistocene Sanmen Formation, near Jianyucha Town, Zichang County, northern Shaanxi Province, has been subjected to a detailed analysis. The specimens were identified as Eospalax simplicidens, an extinct species of Eospalax, based on dental morphology. The recent discovery of E. simplicidens in Jianyucha offers significant insights into the species’ cranial morphology and contributes to a more comprehensive understanding of its geographical distribution. The distinctive feature of the posterodorsal location of the external acoustic meatus indicates either a plesiomorphy or an evolutionary convergence among E. simplicidens, African root rats (Tachyoryctes), and bamboo rats (Rhizomyini). A skull (IVPP V5398.1) and four upper jaws (V5398.2) from Gongwangling in Lantian, Shaanxi, previously identified as Myospalax fontanieri, is transferred to the species E. lingtaiensis. A skull (IVPP RV35055) from Jingou, Xin’an, Henan, previously identified as E. simplicidens, is transferred to the species E. youngianus. In this study, body mass estimates are made for extinct Eospalax. Both E. lingtaiensis and E. simplicidens are small-sized zokors, with an estimated body mass of less than or approximately 300 g, respectively.

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    Preliminary exterior skull osteology of Prionodon pardicolor
    WANG Yi-Duo, PAN Yue, ZHANG Ying-Qi
    Vertebrata Palasiatica    2026, 64 (1): 74-99.   DOI: 10.19615/j.cnki.2096-9899.251027
    Abstract (1772)   HTML (15)    PDF(pc) (2008KB)(354)       Save

    Linsangs (Prionodon Horsfield, 1822) are small, arboreal feliform carnivorans that live in the tropical and subtropical forests of Southeast Asia and southern China. Several lines of morphological evidence from the soft tissues, dentition, and basicranium support their placement in either Prionodontinae or Viverrinae of Viverridae. However, molecular evidence has not only excluded the linsangs from Viverridae but also established that they constitute a monogeneric family Prionodontidae sister to Felidae. For that reason, the examination of the skull osteology of linsangs and related taxa is necessary to better understand how morphological and molecular data - particularly morphology - have contributed to the reconstruction of the Feliformia phylogeny. During the summer field season in July of 2020, we stumbled across the carcass of a spotted linsang (P. pardicolor) in a karst cave on the outskirts of Chongzuo City. To contribute to the knowledge about the morphology of this enigmatic feliform carnivoran, we present a preliminary description of the exterior skull osteology of P. pardicolor. The craniodental morphology provides strong evidence for a closer phylogenetic relationship between P. pardicolor and Viverrinae. However, since both morphological and molecular approaches have inherent limitations, caution is urged when inferring feliform phylogeny based on either discipline alone.

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    Stepwise formation of autostyly in lungfishes revealed by comparative analysis of palatoquadrate
    QIAO Tuo, LIU Cheng-Xi, CUI Xin-Dong, ZHU Min
    Vertebrata Palasiatica    2026, 64 (2): 167-182.   DOI: 10.19615/j.cnki.2096-9899.260408
    Abstract (1103)   HTML (14)    PDF(pc) (6460KB)(263)       Save

    Autostyly, defined by fusion of the palatoquadrate to the neurocranium and loss of the hyomandibula as a suspensory element, is a hallmark of lungfish cranial organization among sarcopterygians, yet its evolutionary origin remains incompletely understood. This study elucidates this transition through a detailed comparative analysis of the palatoquadrate and its articulations in three sequentially diverging stem dipnoans: Youngolepis, Diabolepis, and the earliest eudipnoan Paleolophus. Youngolepis exhibits a reoriented palatoquadrate, indicating functional reorganization of jaw mechanics prior to autostyly. In Diabolepis, reduction of the pars autopalatina and retention of a primitive suborbital articulation suggest further modification of jaw suspension. Paleolophus documents the earliest unambiguous autostyly, with direct palatoquadrate-neurocranial integration preceding complete fusion with the lateral commissure, along with an enlarged adductor fossa. Comparison with Middle and Late Devonian lungfishes indicates that full autostyly was achieved only after the development of a robust, integrated otic process. These results demonstrate that lungfish autostyly evolved stepwise, driven by increasing biomechanical demands associated with durophagous feeding.

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    Early Pleistocene mammals from Yeka locality in Shangri-La, northwestern Yunnan
    ZHANG Li-Min, CHANG Mei-Jing, LU Dan, GONG Hao, QIN Chao, GAO Feng, PAN Gao-Yuan, LI Gang, DENG Tao, SHI Jing-Song, NI Xi-Jun, LI Qiang
    Vertebrata Palasiatica    2026, 64 (3): 254-293.   DOI: 10.19615/j.cnki.2096-9899.260210
    Abstract (1078)   HTML (10)    PDF(pc) (5853KB)(243)       Save

    The Early Pleistocene Yeka Fauna was first identified during the Hengduan Mountains Scientific Expedition in the 1980s. New mammal fossil remains were collected during the execution of the Second Tibetan Plateau Scientific Expedition and Research Project (STEP) in 2020 and 2024. The most recent findings have been identified as 5 orders, 12 families, 15 genera, and 15 species. The updated Shangri-La fossil mammal combination (Yeka and Zhongdian faunas) has been compared to several Early Pleistocene faunas in China. It has been found to be most closely correlated to the Yuanmou Man Fauna. The faunal composition of the Shangri-La fossil mammal combination is distinguished by the co-occurrence of boreal and austral elements, a pattern that is analogous to the modern biogeography observed in the Hengduan Mountains. Faunal analysis suggests that during the Early Pleistocene, the Shangri-La region was characterized by a moderate-elevation forest intermingled with open grassland.

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    Early Devonian fish material from Posongchong Formation of Guangnan, Yunnan, China
    XIAN Zu-Min, MO Xiong, GUAN Qi, ZHAO Ying-Tian, XUE Qin-Yuan, LI Qiang, LIU Jun-Ping, ZHU Min
    Vertebrata Palasiatica    2026, 64 (2): 151-166.   DOI: 10.19615/j.cnki.2096-9899.260206
    Abstract (1410)   HTML (25)    PDF(pc) (16006KB)(211)       Save

    New findings of early vertebrates, including placoderms, sarcopterygians, and the galeaspids Sanqiaspis rostrata, Macrothyraspis longicornis, Gantarostraspis gengi, Wenshanaspis sp., are described from Posongchong Formation (Pragian, Lower Devonian) in Zhujie, Guangnan County, Wenshan Prefecture, Yunnan, China. The new specimen of Macrothyraspis longicornis exhibits the ventral side of its headshield, revealing a large branchial chamber encompassed by a very narrow ventral rim. The material of Yunnanolepidoidei and Petalichthyida represents the first fossil record of placoderms from Wenshan Prefecture, southwestern Yunnan. These new findings enrich the fish diversity of the Pragian Xujiachong Vertebrate Assemblage and provide additional paleoichthyological data for the biostratigraphic correlation between Posongchong Formation and its coeval strata in southwestern China and northern Vietnam.

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    New tridactyl theropod tracks from the Cretaceous Chaochuan Formation, Dongyang, Zhejiang, southeastern China
    ZHENG Wen-Jie, TSUKIJI Yuta, JIN Xing-Sheng, FU Yan-Fang
    Vertebrata Palasiatica    DOI: 10.19615/j.cnki.2096-9899.260828
    Accepted: 28 August 2026