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    15 March 2007, Volume 45 Issue 1
    FIRST DISCOVERY OF HUANANASPIDAE FROM THE XISHANCUN FORMATION (LOCHKOVIAN, DEVONIAN) OF YUNNAN, CHINA
    GAI Zhi-Kun, ZHU Min
    2007, 45(1):  1-12. 
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    A new genus of the family Huananaspidae(Galeaspida), Stephaspis is described in this paper. Fossil materials were recovered from the Xishancun Formation(early Lochkovian, Devo-nian) of Qujing, Yunnan Province, China. The new genus is not only the first discovery of the Huananaspidae in the Xishancun Formation but also represents the earliest occurrence of the Huananaspidae in the Devonian to date.
    CHONDRICHTHYAN MICROREMAINS UNDER PERMIAN-TRIASSIC BOUNDARY BOTH IN ZHEJIANG AND JIANGXI PROVINCES, CHINA — FIFTH REPORT ON THE FISH SEQUENCE STUDY NEAR THE PERMIAN-TRIASSIC BOUNDARY IN SOUTH CHINA
    WANG Nian-Zhong, ZHU Xiang-Shui, JIN Fan, WANG Wei
    2007, 45(1):  13-36. 
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    The Permian-Triassic boundary strata are stable throughout the whole Yangtze Platform, es-pecially, the GSSP of Permian-Triassic boundary defined at the Meishan section D, Changxing County of Zhejiang Province, China. But none of fish microfossils in the Permian-Triassic boundary beds in South China were formally described before. This is the first report on fish microfossils in the GSSP of P/T boundary in the world. The chondrichthyan microfossils dealt with in this paper were collected from the Permian-Triassic boundary beds in Meishan section of Changxing County, Zhejiang Province, Dongling section of Xiushui County and Tieshikou section of Xinfeng County, Jiangxi Province, South China. The chondrichthyan remains include Elasmobranchii order and family incertae sedis: Meishanselache liui gen. et sp. nov., Chang-xingselache wangi gen, et sp. nov., Ctenacanthidae gen. et sp. indet.; Hybodontoidea: Hybo-dontoid scale type-1, Hybodontidae gen. et sp. indet.; Acrodontidae: Sinacrodus donglingensis gen. et sp. nov.; Polyacrodontidae: Lissodus xiushuiensis sp. nov., Polyacrodus jiangxiensis sp.nov.; and Neoselachian tooth type-1, Neoselachian scale type-1. The material described herein is housed in the Institute of Vertebrate Paleontology and Paleoanthropology(IVPP), Chinese Academy of Sciences.
    A JUVENILE TANYSTROPHEUS SP. (PROTOROSAURIA, TANYSTROPHEIDAE) FROM THE MIDDLE TRIASSIC OF GUIZHOU, CHINA
    LI Chun
    2007, 45(1):  37-42. 
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    An incomplete skeleton(IVPP V 14472) of protorosaur, in which only the last five neck vertebrae, the trunk and the forelimbs are preserved(Fig.1), is identified as a juvenile Tanystropheussp. based on the unique structure of the cervical vertebrae: neural arch poorly developed; centrum obviously elongate, ratio of the length to height large (from 4.43 to 8.98, similar to Tanystropheus but distinctly larger than Dinocephalosaurus orientalis (Table 1,2). The total number of cervical vertebrae is assumed as 12, as in Tanystropheus); double-headed cervical rib extremely long and slender, extending backwards across 2~3 cervical vertebrae. Most elements of the shoulder girdle overlap each other. Both of the scapula and coracoid are plate shaped, and there are a lot of tiny humps on the surface of the scapula. The distal end of the interclavicle somewhat triangle in shape; fourcarpals ossified (only 3 preserved in the left forelimb); digital formula of the forelimb is2-3-4-4-3(Fig 1). The distal end of the rib expanded. The shape of the ilium and the ischium is the same as that of Tanystropheus longobardicus. Some slight difference between V 14472 and T. longobardicus was probably due to development stages. For example, the longest cervical vertebra of V14472 is the 10h one, while in T. longobardicus, the 9h is the longest one. Along the neck and in the abdomen part of the specimen, there are some tiny bones that look like the digested draft.A few of them could be recognized as the tooth or vertebral centrum of the fish. In contrast to the terrestrial and insectivore at juvenile stages, as suggested by Wild (1973),V 14472 should be seen as a marine predator based on the number and the structure of the carpus. Derived sauropterygian and marine protorosaur developed the extremely long neck by different ways. With very short centrum and cervical rib, some plesiosaurs had 60~70 verte-brae. In Tanystropheus and Dinocephalosaurus, both the individual centrum and the cervical rib are greatly elongate, while the number of neck vertebrae only moderately increased (12 for Tanystropheus and 25 for Dinocephalosaurus). As bounded by 2~3 cervical ribs in each side, the intervertebral joint must be fixed and the whole neck must be stiffened. Marine reptiles with such an unskillful long neck, not only the protorosaur but also some archosaurian(Li et al.,2006), would have adopted the"suction"way to catch the prey(Li et al.,2004). The new material(V 14472) was found from the Middle Triassic(Falang Formation, Ladinian) of Chajiang, Guizhou Province, southwestern China. This is the first record of Tanystropheus outside Europe and Middle East(Rieppel,2001), confirming a close relationship between eastern and western Tethyan fauna province during the middle Triassic. The affinity between the two regions is also represented by some other marine reptile groups, including Lariosaurus(Rieppel et al.,2003), Nothosaurus(Li and Rieppel,2004), askeptosaurid(Liu and Rieppel,2005) and cyamodontoid placodont(Li,2000; Li and Rieppel,2002).
    LATE EOCENE LAGOMORPHS FROM NEI MONGOL, CHINA
    WANG Ban-Yue
    2007, 45(1):  43-58. 
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    During 1980~90's, some fossil lagomorphs were collected from Late Eocene of Erenhot, Urtyn Obo(=Erden Obo) and Haosiburdu Basin, Nei Mongol, by the teams of IVPP using screen washing technique. They are first discovered in these localities. The new discovery not only expanded the distribution of the lagomorphs in Asia, added new material of the lagomorphs and augmented the content of the faunas at the localities, but also played an important role in determining the ages of the fossiliferous beds in these localities. The undescribed specimen collected from Jhamo Obo by the Third Asiatic Expedition is also described here.
    COMPARISON OF EUROPEAN AND CHINESE LATE MIOCENE SUOIDEA: IMPLICATIONS FOR BIOSTRATIGAPHY AND PALAEOECOLOGY
    LIU Jian-Hui, Martin PICKFORD
    2007, 45(1):  59-73. 
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    Global physical events during the Late Miocene affected not only the European and Chinese Suoidea but also the environment. In the early Vallesian(MN9) the suoid assemblages indicate that both areas were influenced by previous immigration from the Indian Subcontinent, whereas in the late Vallesian(MN10) and early Turolian(MN11) they evolved independently in each area. In thelate Turolian(MN12, MN13) European and southern Chinese suid lineages appeared for the first time in northerm China. It seems that the Indian Subcontinent biome was isolated from that of Europe and China during the early Late Miocene or even earlier. The Late Miocene environment in southernChina ranged from humid, warm and closed to relatively arid, cold and open.A comparable pattern isseen in Europe during this period. In contrast, the environment changed from open, cold and arid to close, warm and humid in northern China. During the same time suids spread gradually from southern China northwards and Europe eastwards to northern China. The European environment was slightly colder and more open than the Chinese one.
    LUNANOSOREX(INSECTIVORA, MAMMALIA)FROM THE PLIOCENE OF NORTH CHINA
    JIN Chang- Zhu, SUN Cheng- Kai, ZHANG Y ing- Qi
    2007, 45(1):  74-88. 
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    Lunanosorex is one of in portant insectivoe m m bers of Neogene m icrm ammal fauna in North China Itw as established by Jin and Kawamua in 1996 based on only one m andible fim he Late P liocene fissure deposit in Q ipanshan Hill Yinan County Shandong Povince Thereaf ter itwas reported in Bilke and Gao tege NeiM ongol(Q iu and Storch 2000 Lietal 2003).In 2004 more Lunanosorex specim ensw ere excava ted by a team of the ⅣPP frm Queshan County, Henan Prov ince On the basis of the evolutionay. stage of micm amm als the, fossil bearing deposits of the Queshan County is possibly the La te P liocene in age W ith a detaied sudy of he aforem en tioned specim ens he evision of the genus and species and the relationship among sme of the large sized shews ane discussed in the present paper
    Fossils of Palaeoloxodon naumani from Jixian, Tianjin, China
    ZHENG Min
    2007, 45(1):  89-92. 
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    Fossils of Palaeoloxodon naumani, mainly of molars or incisors, were discovered sporadically in Jixian, Tianjin previously. In September 2005, a broken skull, a complete mandible and two limb bones of Palaeoloxodon naumani (Tianjin Natural History Museum specimen no. TNP04133, TNP04112) were found near Xiaochenzhuang, Jixian. The discovery of the complete mandible fossil with m3 is of some value to stratigraphy and paleontology.