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    20 January 2026, Volume 64 Issue 1
    Cricetids (Rodentia, Mammalia) from the Late Miocene Yihachi locality of Gansu, China
    QIU Zhu-Ding, Lawrence J. FLYNN, WANG Ban-Yue, LI Lu
    2026, 64(1):  1-25.  DOI: 10.19615/j.cnki.2096-9899.251117
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    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.

    New material of Eospalax simplicidens (Spalacidae, Rodentia) from Jianyucha, Zichang, northern Shaanxi
    CHANG Mei-Jing, SHI Qin-Qin, NI Xi-Jun, LI Qiang
    2026, 64(1):  26-46.  DOI: 10.19615/j.cnki.2096-9899.251201
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    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.

    First discovery of the spiral-horned antelope Antilospira (Bovidae, Artiodactyla) from the Linxia Basin, Gansu, China
    XU Xing-Dong, SHI Qin-Qin
    2026, 64(1):  47-58.  DOI: 10.19615/j.cnki.2096-9899.251030
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    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.

    A new cranium of Metacervocerus longdanensis (Cervidae, Mammalia) and the genus Metacervocerus in China
    WANG Shi-Qi, MA Jiao, FU Jiao, BAI Wei-Peng
    2026, 64(1):  59-73.  DOI: 10.19615/j.cnki.2096-9899.251118
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    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.

    Preliminary exterior skull osteology of Prionodon pardicolor
    WANG Yi-Duo, PAN Yue, ZHANG Ying-Qi
    2026, 64(1):  74-99.  DOI: 10.19615/j.cnki.2096-9899.251027
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    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.

    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
    2026, 64(1):  100-124.  DOI: 10.19615/j.cnki.2096-9899.251029
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    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.