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    20 April 2026, Volume 64 Issue 2
    Career of Chang Meemann and her contributions to vertebrate paleontology
    ZHU Min, ZHU You-An
    2026, 64(2):  125-136. 
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    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.

    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
    2026, 64(2):  137-150.  DOI: 10.19615/j.cnki.2096-9899.260113
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    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.

    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
    2026, 64(2):  151-166.  DOI: 10.19615/j.cnki.2096-9899.260206
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    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.

    Stepwise formation of autostyly in lungfishes revealed by comparative analysis of palatoquadrate
    QIAO Tuo, LIU Cheng-Xi, CUI Xin-Dong, ZHU Min
    2026, 64(2):  167-182.  DOI: 10.19615/j.cnki.2096-9899.260408
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    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.

    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
    2026, 64(2):  183-190.  DOI: 10.19615/j.cnki.2096-9899.251111
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    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.

    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
    2026, 64(2):  191-220.  DOI: 10.19615/j.cnki.2096-9899.260411
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    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.