Issue 3,1964 Table of Contents

1 SOME SPECIES OF TETRAGRAPTUS FROM THE NINGKUO SHALE(LOWER ORDOVICIAN)OF ZHEJIANG(CHEKIANG)

M.Y.GEH

1964(3):391-410. DOI: 10.19800/j.cnki.aps.1964.03.002 CSTR:

[Abstract](15) [HTML](0) [PDF 685.09 K](321)

Abstract:
The present paper describes the following 19 species and varieties of Tetragraptusfrom the Ningkuo Shale of Zhejiang,among them 8 are new to science.1.Tetragraptus quadribrachiatus(Hall)

2 BRACHIOPOD FAUNA OF THE NANPANJIANG LIMESTONE OF EASTERN YUNNAN AND ITS GEOLOGICAL AGE

HOU HUNG-FEI , XIAN SI-YUAN

1964(3):419-421. DOI: 10.19800/j.cnki.aps.1964.03.004 CSTR:

[Abstract](9) [HTML](0) [PDF 185.93 K](203)

Abstract:
The Nanpanjiang Limestone of eastern Yunnan has long been known as one of theimportant Devonian beds in South China.It was first proposed by Prof.Y.C.Sun in1943,and tentatively included in the upper member of the Miaokaoshan formation ofEarly Devonian age with Gypidula pseudogleata Hall as a leading fossil.Since thenmost geologists and palaeontologists have followed Sun’s assignment,while few othershave held it to be Early Middle Devonian.At the type locality near Poshi districtalong the Nanpanjiang Valley the Nanpanjiang Limestone is composed of yellowish-greyor dark grey limestone with an approximate thickness of 40—70 meters,and is overlainby the Bothriolepis-bearing beds of Lunghuashan formation.

3 UPPER TRIASSIC AND MIDDLE JURASSIC OSTRACODS FROM THE ORDOS BASIN

ZHONG XIAO-CHUN

1964(3):448-474. DOI: 10.19800/j.cnki.aps.1964.03.006 CSTR:

[Abstract](18) [HTML](0) [PDF 929.32 K](379)

Abstract:
The material described in this paper was collected from the Upper Triassic andMiddle Jurassic formations of Tungchuan,Liulingchuan,Yenhe-Xixingzihe and Dalihe inthe Ordos Basin of Shensi Province by the members of the Geological Expedition of theInstitute of Geology of Lanchow,Academia Sinica,in April,1961.A considerable number of ostracods have been discovered nearly from all formationsin many parts of China,yet the Triassic ostracods are comparatively rare.As far asthe writer is aware,only a few species have been known from the Lower Triassic of

4 ON THE DISCOVERY OF EIFELIAN FAUNA FROM WESTERN TSINLING

JIAN WAN-CHOU , KUO YONG-LING

1964(3):480-481. DOI: 10.19800/j.cnki.aps.1964.03.008 CSTR:

[Abstract](14) [HTML](0) [PDF 141.59 K](238)

Abstract:
In soumeastern Kansu,there is a vast area of metamorphosed sedimentary rockscomposed of quartzites,crystallized limestones and slates with some intercalations ofhematites exposed in the valley of Lengputze to the north of Wen Xian,and in the valleyof Sunchiayuan to the west of Kang Xian.In 1944,Yeh and Kwan named the abovementioned strata at Lengputze Lupanchiao Quartzite and referred it to Lower Carbo-niferous.Lately(1959),by the discovery of Tabulata(Favosites sp.),C.H.Huang re-garded it as the upper part of the so-called Pikou Group of Lower Palaeozoic in age.While carrying on a field exploration in 1960,one of the writers,Kuo,collected a fewfossils from the same section and the corresponding strata in Kang Xian.They arelisted helow

5 A PRELIMINARY REPORT ON SPORAE DISPERSAE FROM THE LOWER SHIHHOTZE SERIES OF HOKÜ DISTRICT,NW SHANSI

OUYANG SHU

1964(3):512-519. DOI: 10.19800/j.cnki.aps.1964.03.010 CSTR:

[Abstract](7) [HTML](0) [PDF 447.62 K](421)

Abstract:
The literatures on the Permian Sporae dispersae are rather meagre and scattered ascompared with those on the Carboniferous.The correlation of sediments of long geo-graphical distance in this period is thus nearly impossible at this moment.As far as isknown to the present writer,the contributors to the Permian microflora are Dalhunty(1945,49),Balme(1952,1955,1956),Imgrund(1952,1960),Klause(1953),Potonie& Klause(1954),Leschik(1956);Luber(1938),Kara-Murza(1952),Samoilovich(1953),Zoricbeva & Sedova(1954),Andreeva(1956),Zauer(1960),Medvedeva(1960)andothers.

Issue 3,1964 Table of Contents

Current Issue

Volume

Issue

Most Read

Most Cited

Most Downloaded

WeChat

Mobile website