1964年第3期文章目次

葛梅钰

1964(3):367-391. DOI: 10.19800/j.cnki.aps.1964.03.001 CSTR:

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摘要:
浙江的四笔石,过去报导的不多,仅有孝丰、富阳、江山等地的下列少数几种:Tetragraptus pendens Elles (盛莘夫,1950—51)Tetragraptus bigsbyi(Hall) (高平,1936;盛莘夫,1950—51;穆恩之,1959)Tetragraptus bigsbyi var.latus Hsü(穆恩之,1959)Tetragraptus sp. (穆恩之,1959)1961年,笔者在整理浙江奥陶纪笔石标本过程中,发现四笔石的种类相当繁多,经鉴定共有19种及变种。其中有8个新种。这些笔石名称如下

2 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:

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摘要:
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)

3 滇东南盘江灰岩的腕足类动物羣及其时代

侯鸿飞，鲜思远

1964(3):411-418. DOI: 10.19800/j.cnki.aps.1964.03.003 CSTR:

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摘要:
滇东地区泥盆系出露良好、发育完善,为我国泥盆系研究最早和比较深入的地区之一。1945年,孙云铸教授进行了系统的地层总结;对其中所含的生物羣如:腕足类、珊瑚、植物、鱼类、藻类,也都进行过程度不等的描述,为深入研究滇东地区泥盆纪地层打下了基础。解放以来,野外地质人员对该区泥盆系又进行了详细研究,测制了大量剖面,采集了丰富化石。随着研究程度的深入,出现了更多的问题:诸如海相下泥盆统的存在;婆兮组的时代及其分布;泥盆系的上界问题等。在下、中泥盆统的争论问题中,最突出的是南盘

4 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:

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摘要:
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.

5 鄂尔多斯盆地上三迭统及中侏罗统的介形类化石

钟小春

1964(3):426-447. DOI: 10.19800/j.cnki.aps.1964.03.005 CSTR:

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摘要:
本文研究的材料是中国科学院兰州地质研究所鄂尔多斯地质大队的地层分队于1961年4月采集的。这些化石标本采自铜川、柳林川、延河—西杏子河以及大理河等地区,其中一部分采自上三迭统延长羣,另一部分采自侏罗系。在延长羣共采得4属23种及一些无法鉴定的碎片,其中有1个新属、15个新种和7个未定名的种。在侏罗系共采得2属6种,其中有4个新种。侏罗纪介形类近年在我国许多地区的陆相地层中,已有不少的发现,但三迭纪的介形类还很稀罕,据笔者所知,迄今仅新疆克拉玛依地区下三迭统曾有过一

6 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:

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摘要:
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

7 秦岭西段的爱菲尔期生物羣

翦万筹，郭勇岭

1964(3):475-479. DOI: 10.19800/j.cnki.aps.1964.03.007 CSTR:

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摘要:
甘肃中南部文县临江以北,冷堡子至沙湾间,沿公路两旁分布有一套不整合复于早古生代碧口羣之上的轻变质沉积岩系。叶连俊、关士聪(1944)曾称为鲁班桥石英岩,并划入下石炭统,其剖面摘录如下:上复岩系——略阳灰岩

8 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:

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摘要:
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

9 山西河曲下石盒子组孢子花粉的初步研究

欧阳舒

1964(3):486-511. DOI: 10.19800/j.cnki.aps.1964.03.009 CSTR:

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摘要:
全世界二迭纪(尤其是早二迭世)的孢粉研究基础要比石炭纪薄弱得多,以致国际间的地层目前还难以借化石孢粉组合进行对比。在我国,则无论是石炭纪或是二迭纪,基础都是十分薄弱的。地质部有关单位自1954—1962年间曾在徐仁先生指导下对我国某些石炭、二迭纪煤田作了不少工作,但正式著作尚待发表。有关华北已发表的论著,小孢子方面,就我们所知,仅有德国人伊木格隆(Imgrund,1960)一篇“开平盆地的分散孢子组合”。他在这篇文章中共描述孢粉33属68种,包括4

10 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:

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摘要:
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.

11 修理化石的新技术

王德孚

1964(3):536-536. DOI: 10.19800/j.cnki.aps.1964.03.011 CSTR:

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摘要:
最近利查德·霸德(Richard Boyt)在杂志上介绍(1962,Earth Science,Vol.15,No.5.pp.217—220)在美国艾奥华州博物馆的工厂里,增添了一种新的、又有价值的研究设备。这种设备利用喷砂原理,修理出非常精致的化石标本。利用这个新装置(指喷砂器,一种用压缩空气高速喷出的砂流清理铸件的机器)进行修理化石,既不生热,亦不振动,并能很好地定向来磨损需要修去的附着物。工具本身并不接触标本,只是从它的碳化钨喷管,喷出一种仅次于

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