Issue 2,1954 Table of Contents

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1 UPPER CAMBRIAN TRILOBITES FROM SANTU,SOUTHEASTERN KUEICHOU

LU YEN-HAO

1954(2):136-152. DOI: 10.19800/j.cnki.aps.1954.02.001 CSTR:

[Abstract](11) [HTML](0) [PDF 2.72 M](377)

Abstract:
The Upper Cambrian fossils were not known in South and SouthwesternChina before 1938,though a thick limestone series ranging from not less than100m to over one thousand meters known as the Ichang Limestone of the Gorgedistrict of the Yangtze and the Loushankwan Limestone of North Kueichou hasbeen partially referred by various authors to represent some part of the Upper

2 THE EARLY MIDDLE DEVONIAN BRYOZOANS FROM WUTSUN SHALE,KWANGSI.

K.C.YANG

1954(2):217-225. DOI: 10.19800/j.cnki.aps.1954.02.008 CSTR:

[Abstract](12) [HTML](0) [PDF 552.92 K](394)

Abstract:
INTRODUCTIONThe material dealt with in this paper came from the upper part of the Wu-tsun shale near Liuchingyu.The village is located on the right bank of Yukiang,about 12 km.to the north of Yungchun city.The Wutsun shale consists mainlyof shales and sandstones with a bed of argillaceous limestone in the upper partvarying from a few to 15 meters thick.The bryozoans occur in the uppermostpart of the formation,where the rock contains high iron contents.They are

3 SOME LOWER PERMIAN OSTRACODS FROM WESTERN HUPEH

Y.T.HOU

1954(2):246-264. DOI: 10.19800/j.cnki.aps.1954.02.010 CSTR:

[Abstract](18) [HTML](0) [PDF 1.08 M](417)

Abstract:
IntroductionThe material described in the present paper was collected from the LowerPermian Chihsia limestone by Messrs.K.C.Yang and A.T.Mu in 1951 dur-ing their excursion in Western Hupeh.The Chihsia limestone is underlain by theMaan Coal series containing Lepidodendron ituense and is succeeded by the Mao-kou limestone bearing Verbeekina verbeeki.The most characteristic fossils collect-ed from the Chihsia limestone are:Hayasakaia elegantula Yabe et Hayasaka,Fistulipora chinensis Yoh,Stylidophyllum of intermidicum Huang,Polythecalisof.yangtzeensis Huang,Corwenia of.chihsiaensis Yoh.The Ostracods came

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