Issue 2,1964 Table of Contents

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  • 1  LATE JURASSIC—EARLY CRETACEOUS BELEMNITES FROM SOUTHERN TIBET,CHINA
    YANG TSUN-YI WU SHUN-BAO
    1964(2):200-216. DOI: 10.19800/j.cnki.aps.1964.02.002
    [Abstract](24) [HTML](0) [PDF 2.60 M](421)
    Abstract:
    The belemnites described here were collected by two field parties visiting southernTibet respectively in 1960 and 1961 from(1)the Lungma—Kapula area,east of Ziang-zhi and(2)Dingje and Dingri,all of which are situated southwest of Lhasa.Theyconsist of two genera and twelve species with six new species and they may be differen-tiated into two assemblages:the first assemblage of upper Oxfordian—lower Tithonianage with Belemnopsis gerardi(Oppel)as its leading species and the second of early Cre-taceous age with Hibolites subfusiformis(Raspail)as its chief element.The geologic sections which bear the belemnites are given as follows(in descendingorder)
    2  MIDDLE AND UPPER CARBONIFEROUS FUSULINIDS FROM JIANGYOU DISTRICT,NORTHWESTERN SZECHUAN
    CHANG LIN-HSIN
    1964(2):228-235. DOI: 10.19800/j.cnki.aps.1964.02.004
    [Abstract](20) [HTML](0) [PDF 1.11 M](363)
    Abstract:
    The fusulinids studied here were collected in 1961 by Mr.C.G.Shi and the writerfrom the Middle and Upper Carboniferous rocks exposed near Majiaoba,a town ofJiangyou district,Northwestern Szechuan.The Middle and Upper Carboniferous depositsin this region are composed almost of limestones with a total thickness about 122 meters.
    3  YUSHANOGRAPTUS,A NEW GRAPTOLITE GENUS FROM THE NINGKUO SHALE(LOWER ORDOVICIAN)OF YUSHAN,NORTHEASTERN JIANGXI(KIANGSI)
    X.CHEN X.R.SUN N.R.HAN
    1964(2):239-240. DOI: 10.19800/j.cnki.aps.1964.02.006
    [Abstract](19) [HTML](0) [PDF 149.83 K](238)
    Abstract:
    The new genus Yushanograptus described in the present paper is a monotypic genuswith Yushanograptus separatus gen.et sp.nov.as the genotype which is represented by5 specimens securd by one of the writers(Han)in the summer of 1961 from the NingkuoShale at the locality near Lijiapeng of the Yushan district,northeastern Jiangxi(Kiangsi)Province(Field No.F61001).The marked features of the new genus are the two long and slender primary stipesand the Goniograptid type in branching.The young forms of this new graptolite bear astriking resemblance to the slender Didymograpti,such as Didymograptus gracilis T?rn-quist,D.cognatus Harris et Thomas etc.The same is the case in Zygograptus,particul-arly in Zygograptus irregularis Harris et Thomas.In the mode of branching of the
    4  OSTRACODS FROM GANSEN DISTRICT,CHAIDAM BASIN
    HUANG BAO-REN
    1964(2):256-270. DOI: 10.19800/j.cnki.aps.1964.02.008
    [Abstract](17) [HTML](0) [PDF 3.78 M](460)
    Abstract:
    The Ostracods studied in this paper were collected by the members of a geologicalparty in 1955 from the yellowish silt-clay in Gansen district,Chaidam Basin.Accord-ing to the collecter’s opinion,the geological age of the fossil bearing bed is Pliocene toQuaternary.The Ostracods are found in association with a charophyta,Chara gansenensis Wang(S.Wang,1961),gastropods and some indeterminable fragments of plant and fish bone.The species of Ostracoda described and illustrated in this paper are as follows:Ilyo-cypris gibba(Ramdohr),Eucypris inflata(Sars),Prionocypris gansenensis Huang(sp.nov.),Cypricercus brevis Huang(sp.nov.),Cypridopsis reticulata Huang(sp.nov.),Cyc-locypris serena(Koch),Candona neglecta Sars,C.houae Huang(sp.nov.),Limnocythere dubiosa Daday,L.sancti-patricii Brady et Robertson,L.binoda Huang(sp.nov.)and Cyprideis littoralis(Brady).From the geological distribution of this Ostracod assemblage,the fossil bearing bedmay be of Pleistocene in age.
    5  НЕКОТОРЫЕ МАТЕРИАЛЫ ПО ОСТРАКОДАМ ИЗ ΓУАНЪЮАНСКОЙ СЕРИИ В ПРОВИНЦИИ СЫЧУАНИ
    Хэ Цзюнь-дэ
    1964(2):276-279. DOI: 10.19800/j.cnki.aps.1964.02.010
    [Abstract](30) [HTML](0) [PDF 802.24 K](429)
    Abstract:
    1961:Darwinula aff.contracta Mandelstam D.cf.impudica Sharapova D.sarytirmenensis Sharapova D.guangyuanensis sp.nov.Metacypris sp.
    6  STROMATOPOROIDS FROM THE EARLY CARBONIFEROUS OF KWANGSI AND KUEICHOW
    DONG DE-YUAN
    1964(2):292-311. DOI: 10.19800/j.cnki.aps.1964.02.012
    [Abstract](51) [HTML](0) [PDF 5.80 M](405)
    Abstract:
    The specimens dealt with here were furnished by Prof.K.C.Yang and Miss W.S.Wu in 1961 to the writer for study.They were collected from the lower part of theShizixu formation of Luocheng and Huanjiang districts,Kwangsi province and from thelower part of the Kolaoho formation of Dushan and Duyun districts,southern Kuei-chow province.All the stromatoporoids obtained from Kwangsi are associated with coral:Cystophrentis sp.;and those from Kueichow are associated with brachiopods:Schucher-tella sp.,Athyris sp.,Camarotoechia sp.,a little bit below the horizon of Cystophrentis.
    7  NOTES ON SOME MARINE EARLY TRIASSIC LAMELLIBRANCHIATA FROM EAST TSINLING,SOUTHERN SHANXI(SHENSI)
    L.LIU
    1964(2):321-325. DOI: 10.19800/j.cnki.aps.1964.02.014
    [Abstract](68) [HTML](0) [PDF 634.72 K](407)
    Abstract:
    Some fossils,mainly lamellibranchs,were recently discovered by a field party of theGeological Bureau of Shanxi Province at some 20 km SSE from Zhenan(Chenan)city ineastern Tsinling.The fossil locality is within the type area of the“Chenan series”(Chaoand Huang,1931)and near to the southern border of the Tsinling Axis.The collectionwas made in a series of grey-black calcareous and slaty shales,the lower part of the“Jin-jiling Qun”.After a careful study on these life-remains,Mr.C.C.Chen and the writerhave arrived at the same conclusion that these fossils are undoubtly of marine earlyTriassic.The fauna consists of the following forms:Claraia hunanica(Hsü)Cl.zhenanica Chen et Liu(sp.nov.)Cl.cf.wangi(Patte)Cl.ex gr.stachei(Bittner)Cl.sp.ind.Spirorbis?sp.cf.S.valvata(Goldfuss)Cephalopoda gen.et sp.ind.Brachiopods genera ind.
    8  SOME LOWER CARBONIFEROUS STRAIGHT NAUTILOIDS FROM HUNAN AND KANSU
    LAI CHAI-GEEN
    1964(2):334-339. DOI: 10.19800/j.cnki.aps.1964.02.016
    [Abstract](161) [HTML](0) [PDF 922.04 K](681)
    Abstract:
    The straight nautiloids are not abundant in the Lower Carboniferous strata of China.The works of studing and collecting have been greatly neglected.Recently,a few speci-mens were collected by Messrs.H.Liu and Y.T.Lin.Among them Mr.Liu describedtwo species from Hunan.In this paper the following species(comprising a full re-description of Liu’s species)are described:Rayonnoceras hunanense(Liu)Rayonnoceras sp.Dolorthoceras guijangense Lai(sp.nov.)Euloxoceras orientale Lai(sp.nov.)Michelinoceras sp.
    9  NEW FINDS OF MARIOPTERIS-REMAINS FROM CHINA
    LEE HSING-HSüEH
    1964(2):344-351. DOI: 10.19800/j.cnki.aps.1964.02.018
    [Abstract](43) [HTML](0) [PDF 1.90 M](431)
    Abstract:
    Mariopteris is one of the most important Carboniferous pteridosperms in the Eura-merican floras.It is represented by more than fifty species,most of which occur ratherwidely and abundantly in the Westphalian,and not uncommon in the Upper Namuriandeposits.A thorough study of the family Mariopterides including the form genera Mariopteris,Tetratmema,Dicksonites,Pseudomariopteris and many species attributed tothem commonly found in the Carboniferous of North France has been made by P.Danzé-Corsin in 1953.The genus has hitherto not definitely been known in Eastern Asia;only a few frag-mentary specimens have been described by Kawasaki(1931—34,p.157,pl.28,fig.53)as?Mariopteris sp.from the Jido Series of Korea,by Sze(1934,p.604,pl.5,fig.8)as Mariopteris?sp.from the Hsuanmachuang Series of Tachingshan,Inner Mongolia and by Stockmans and Mathieu(1939,p.8,pl.8,fig.3)as Mariopteris?hallei from the Chaoko-chuang Series of Kaiping Basin.
    10  НЕСКОЛЬКО НОВЫХ ИСКОПАЕМЫХ ДРЕВНЕЙШИХ ВОДОРОСЛЕЙ ИЗ ДОКЕМБРИЙСКИХ ОТЛОЖЕНИЙ КИТАЯ И ИХ СТРАТИΓРАФИЧЕСКОЕ ЗНАЧЕНИЕ
    Цао Жуй-цзн
    1964(2):360-366. DOI: 10.19800/j.cnki.aps.1964.02.020
    [Abstract](46) [HTML](0) [PDF 1.67 M](381)
    Abstract:
    1960—19618 6 52 7

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