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    15 September 2013, Volume 51 Issue 3
    The systematic position of the enigmatic theropod dinosaur Yixianosaurus longimanus
    XU Xing, Corwin SULLIVAN, WANG Shuo
    2013, 51(3):  169-183. 
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    Yixianosaurus longimanus is a small theropod from the Lower Cretaceous of western Liaoning Province, China. It was originally suggested to be a derived maniraptoran, but this interpretation was challenged by a recent study that proposed instead that Y. longimanus was a basal maniraptoran. Given that the systematic position of this taxon will affect our understanding of such broad issues as the evolution of the theropod forelimb and plumage, it is important to carefully evaluate both systematic hypotheses and determine which is better supported. Here we review all available morphological features in Y. longimanus that appear informative with regard to its systematic position. We demonstrate that this small theropod is a basal paravian and most likely a basal deinonychosaurian, a result that conforms to the original interpretation of this specimen. The hypothesis that Y. longimanus is a basal paravian is consistent with the probable presence of pennaceous feathers in this taxon, and avoids implying a complicated evolutionary history for the maniraptoran forelimb.
    Earliest records of theropod and mammal-like tetrapod footprints in the Upper Triassic of Sichuan Basin,China
    XING Li-Da, Hendrik KLEIN, Martin G. LOCKLEY, CHEN Wei, YEYong, Masaki MATSUKAWA, ZHANG Jian-Ping
    2013, 51(3):  184-198. 
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    Eubrontes- and Grallator-sized theropod footprints are known from two localities in the Upper Triassic Xujiahe Formation of the Sichuan Basin, southwest China. The larger footprints include a partial trackway with two successive pes imprints that were named asPengxianpus cifengensis. Compared with robust Eubrontes, they have slender digits, less well-defined pad impressions and display a wider digit divarication similar to the theropod ichnotaxon Kayentapus from the Late Triassic-Early Jurassic. Presently, a synonymy of the latter cannot be proved conclusively and the ichnotaxon is retained here.For both footprints, some small areas preserve skin texture with polygonal scales, the clearest preservation is in a small area on the metatarsal-phalangeal pad IV of the second imprint. The smaller theropod footprints are also part of an incomplete trackway. They show a wide digit divarication similar to Kayentapus and Pengxianpusbut they are here tentatively referred to theropod footprints indet. A peculiarity on the surface with Pengxianpus is the presence of small pes or manus imprints that can be assigned to mammal-like tetrapods somewhat similar to those known from Triassic-Jurassic strata of North America and southern Africa. This is the first report of mammal-like footprints in the Triassic of southeastern Asia.
    New specimens of pareiasaurs from the Upper Permian Sunjiagou Formation of Liulin, Shanxi and their implications for the taxonomy of Chinese pareiasaurs
    LI Xing-Wen, LIU Jun
    2013, 51(3):  199-204. 
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     New pareiasaur specimens from the Sunjiagou Formation of Xuecun, Liulin, Shanxi, China are described. These new specimens comprise two marginal teeth from the upper jaw (IVPP V 18613) and an incomplete left dentary with teeth (IVPP V 18614). They provide novel anatomical information and allow the direct comparison of Sanchuansaurus pygmaeuswith Huanghesaurus liulinensis. The two taxa cannot be differentiated by the known features, and both taxa are declared junior synonyms of Shansisaurus xuecunensis.
    The taxonomic status of “Macrotherium cf. M.brevirostris” from the Middle Miocene of Jiulongkou,Cixian County, Hebei Province
    CHEN Shao-Kun, LIU Yan
    2013, 51(3):  205-210. 
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    Materials of chalicothere from Jiulongkou, Cixian County, Hebei Province were identified as Macrotherium cf. M. brevirostris by Hu (1959) and Macrotherium sp. by Chen and Wu (1976). However, Macrotherium was Nomen nudum and erected as Chalicotherium by Anquetin et al. (2007). Recent phylogenetic analysis (Chen et al., 2012) and new discoveries from Tunggur (Liu and Zhang, 2012) showed that the Cixian materials were markedly distinct from Chalicotherium brevirostris. Further observation and comparison suggest that the Cixian materials should represent a new species.
    Myospalacines (Cricetidae, Rodentia) from the Miocene-Pliocene red clay section near DongwanVillage, Qin’an, Gansu, China and the classification of Myospalacinae
    LIU Li-Ping, ZHENG Shao-Hua, CUI Ning, WANG Li-Hua
    2013, 51(3):  211-241. 
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    A new classification scheme of the Myospalacinae on the generic level is proposed mainly based on the interparietal existed or absent, the occiput flat, convex or concave, and the molar rooted or rootless. The classification keys of the Myospalacinae: I. Interparietal existed; occciput convex; molars rooted···················Tribe Prosiphneini Leroy, 1940 Ia..Interparietal is quadrilateral and locates posterior to the lambdoid crest. On m1, the bra2 is opposite to the lra3, and parameters a, b, c, d and e are 0.0-0.5, 0.0-1.8, 0.3-1.6, 0.0-1.4 and 0.0-1.0 respectively········································Genus Prosiphneus Teilhard de Chardin, 1926 Ib..Interparietal is fusiform and locates between two wings of the lambdoid crest. On m1, the bra2 is opposite to the lra3, and parameters a, b, c, d and e are 0.0-0.3, 0.5-3.2, 0.7-3.3, 1.3-5.5 and 0.0-4.5 respectively······················································Genus Pliosiphneus Zheng, 1994 Ic..Interparietal is semicircle-shaped and locates anterior to the lambdoid crest. On m1, the bra2 located posterior to the lra3, and parameters a, b, c, d and e are 0.0-0.5, 1.8-4.0, 1.4-3.2, 1.6- 5.2 and 0.7-4.9 respectively····················································· Genus Chardina Zheng, 1994 II. Interparietal disappeared; occiput convex, flat or concave; molars rooted or rootless ················································································Tribe Myospalacini Miller & Gidley, 1918 II-I..Upper occiput locates posterior to the lambdoid crest, molars rootless, anterior enamel absent on m1 and the lra3 very shallow (convex occiput) II-Ia..Lingual reentrant (salient) angles on upper and buccal reentrant (salient) angles on lower molars are strong. The lra4 absent on m1······························ Genus Eospalax Allen, 1938 II-Ib..Lingual reentrant (salient) angles on upper and buccal reentrant (salient) angles on lowermolars are weak. The lra4 exists on m1 ·······················Genus Allosiphneus Kretzoi, 1961 II-II. Upper occiput locates anterior to the lambdoid crest (concave occiput) II-IIa..Molars rooted. The bra 2 on m1 locates posterior to the lra3 and parameters a, b, c, d, and e are 0.4-7.2, >1.8-8.0, 2.1-7.5, 1.7-7.9 and 1.1-8.0 respectively ··················································································Genus Mesosiphneus Kretzoi, 1961 II-IIb..Molars rootless. The anterior enamel band on m1 exists and the bra2 is opposite or posterior to the lra3 ············································· Genus Yangia (=Youngia) Zheng, 1997 II-III. Upper occiput locates at the same position with lambdoid crest (flat occiput) II-IIIa..Molars rooted. The lra 3 on m1 is shallower than the bra2 and parameters a, b, c, d, and e are 0.3->3.6, >3.7->6.8, >4.2->7.7, >3.3->8.2 and >3.9->7.6 respectively ····················································································· Genus Episiphneus Kretzoi, 1961 II-IIIb..Molars rootless. The lingual reentrant angles on m1 is very shallow and an anterior enamel exists······························································Genus Myospalax Laxmann, 1769 Myospalacines (including 10 species) from the Upper Miocene-Lower Pliocene red clay section (consisting of 12 layers) near the Dongwan Village consistute approximately one fourth of the known mammal forms listed by Liu et al. in 2011. Because Myospalacines occurred in a single section with precise stratigraphic or chronological data (~7.2-3.5 Ma), they are extremely significant to understand the phylogeny and evolutionary history of the subfamily in this period.
    A review of methods in carbon and oxygen isotopic analyses of tooth enamel from small fossil mammals
    BAI Bin, WANG Xu
    2013, 51(3):  242-251. 
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     Measurements of carbon and oxygen isotopes in mammalian tooth enamel have been widely used for the paleoenvironmental and paleoclimatic reconstructions. However, previous studies mainly focused on relatively large mammals owing to sample size and technique constraints. As the result of recent developments in laser and ion microprobe techniques, stable isotopic analyses can be also applied to small mammal teeth (e.g. rodents and lagomorphs). Based on the previous reports, three techniques with high accuracy and precision but requiring much smaller quantity of samples are reviewed and compared in the present paper. These techniques include: 1) laser ablation Gas Chromatography/Isotope Ratio Mass Spectrometry (GC/IRMS); 2) Direct Laser Fluorination (DLF); 3) Sensitive High Resolution Ion MicroProbe (SHRIMP II). Compared with large fossil mammals, small ones are characterized by much higher abundance, more rapid evolution and more restricted habitats. Thus, small fossil mammals can be widely used for long-term local paleoenvironment and paleoclimate studies with high-resolution in the Cenozoic Era.