Issue 1,1958 Table of Contents

1 ДВΥСТВОРЧАТЫЕ ΜОЛЛЮСНИ-МРΑССИЕЛЛЫ В УГЛЕНОСНЫХ ОТЛОЖЕНИЯХ КУЗБΑССΑOT]]OH^EH HFIX H Y35ACCA

Л.А.Рагозин

1958(1):15-34. DOI: 10.19800/j.cnki.aps.1958.01.002 CSTR:

[Abstract](18) [HTML](0) [PDF 1.26 M](451)

Abstract:

2 SOME UPPER CARBONIFEROUS FUSULINIDS FROM THE VICINITY OF BEIYIN OBO,INNER MONGOLIA

J.C.SHENG

1958(1):44-50. DOI: 10.19800/j.cnki.aps.1958.01.004 CSTR:

[Abstract](15) [HTML](0) [PDF 439.50 K](489)

Abstract:
The fusulinids dealt with in this paper were collected in 1955 by Mr.L.S.Wong of a field party sent by the Ministry of Geology in the vicinity of BeiyinObo,Inner Mongolia(formerly province Suiyuan).The fusulinid-bearing bedof this area was named by Mr.Wong the Lalaotu limestone.No data of stra-tigraphical sequence of this region are readily available.Since no informationof the fusulines in this region has been hitherto known,the present discoveryaffords therefore some interest.

3 SOME PLEISTOCENE MAMMALIAN FOSSILS FROM CHIENPING AND KONGPING,LIAONING

HSIEH HSIANG-HSU

1958(1):54-58. DOI: 10.19800/j.cnki.aps.1958.01.006 CSTR:

[Abstract](17) [HTML](0) [PDF 301.77 K](333)

Abstract:
The few mammalian fossils from the Upper Pleistocene deposite of Chien-ping and Kongping of Liaoning province,briefly described in this paper weresent to the Institute of Vertebrate Palaeontology for study in early 1957 throughthe courtesy of the Provincial Cultural Bureau of Liaoning.Although no dataregarding the exact localities and stratigraphical occurrences of these fossilsare available and the specimens are for the most part very fragmentary,it ispalaeontologically quite interesting because there are remains of Pleistocenemammals in the collection which either are of very rare occurrence(such asSpirocerus and Ovis ammon)or so far has never been recorded from the Ple-

4 SOME SILURIAN CORALS FROM THE VICINITY OF BEIYIN OBO,INNER MONGOLIA

WU WANG-SHIH

1958(1):66-70. DOI: 10.19800/j.cnki.aps.1958.01.008 CSTR:

[Abstract](17) [HTML](0) [PDF 330.47 K](327)

Abstract:
The material dealt with in this paper was collected in 1955 by Mr.L.H.Wong and others of 241.Party of the Geological Bureau of North China,Ministry of Geology,at a locality about 20 km north-east of Beiyin Obo,InnerMongolia.According to the collectors’field observation,all the corals occur ina limestone imbedded in a red sandstone series,striking east to west and dip-ping to north.The thickness of the red sandstone series is unknown,it is over-lain by the Upper Carboniferous Triticites bed.The coral-horizon is estimatedat about 2,500 meters below the Triticites bed.No detailed stratigraphical dataare available.The corals described here comprise the following species

5 STRATIGRAPHY,PALAEONTOLOGY AND PALAEOGEOGRAPHY OF THE AMMONITE FAUNA OF THE CLYMENEENKALK FROM GREAT KHINGAN WITH SPECIAL REFERENCE TO THE POST DEVONIAN BREAK(HIATUS)OF SOUTH CHINA

A.C.CHANG

1958(1):83-89. DOI: 10.19800/j.cnki.aps.1958.01.010 CSTR:

[Abstract](29) [HTML](0) [PDF 450.12 K](519)

Abstract:
Ⅰ.INTRODUCTION The Devonian has been known in China since 1920 through the workof Grabau and C.C.Tien(on brachipods),Y.C.Sun and K.K.Chao(onammonites),Y.C.Sun,Y.S.Chi,C.C.Yu and H.C.Wang(on corals),butthe Upper Devonian stratigraphy of China remains obscure.Grabau first pointed out the fact that the Clymenia fauna originated inthe Boreal Sea and widely distributed in Northern Europe such as SouthernEngland,Western France,Poland,and also the Pyrence,and the Alps.Thiscan be clearly indicated by the fact that the Clymenia fauna is well developed inthe rocks of the Ural geosyncline,and Southern Russia appears to be the onlypossible line of their connection.Thus,the Boreal sea was connected withboth the Caledonian and Uralian Geosynclinès,which laid along the periphery

6 LUDLOVIAN GRAPTOLITE FAUNAS OF THE YANGTZE GORGES DISTRICT AND THEIR STRATIGRAPHICAL SIGNIFICANCE

Y.C.HONG

1958(1):108-116. DOI: 10.19800/j.cnki.aps.1958.01.012 CSTR:

[Abstract](25) [HTML](0) [PDF 519.38 K](502)

Abstract:
Ⅰ.INTRODUCTION The Silurian stratigraphy of the Yangtze Gorges district has been reportedby various authors since this century.Early in 1924 J.S.Lee and Y.T.Chao subdivided the Silurian of Sintandistrict into two parts—the lower Lungma shale and the upper Sintan forma-tion,thus laying down the fundation of the silurian stratigraphy of China.Inthe following year C.Y.Hsieh and Y.T.Chao went to Lojoping area of I-Chang district and again subdivided the Silurian of that area into three sub-

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