收稿日期: 1995-03-20
修回日期: 1995-05-16
网络出版日期: 1996-02-01
基金资助
中科院南京地质古生物研究所开放研究实验室资助项目。
THE DISTRIBUTION OF PRECAMBRIAN TRACE FOSSILS OF CHINA AND THEIR PALAEONTOLOGICAL AND STRATIGRAPHICAL SIGNWICANCE
Received date: 1995-03-20
Revised date: 1995-05-16
Online published: 1996-02-01
齐永安,吴贤涛 . 中国前寒武纪痕迹化石的分布及其古生物学、地层学意义[J]. 地球科学进展, 1996 , 11(1) : 45 -49 . DOI: 10.11867/j.issn.1001-8166.1996.01.0045
Trace fossils are abundant in Precambrian strata of China.Some found before the glacial age of Precambrian are distributed mainly in Changcheng System and Qingbaikou System of North China.The old geological age of these trace fossils shows that some metazoans might live in the old sea of North China before 1400~1700Ma.Their discovery is of great significance for further understanding of the origin and early evolution of metazoan.The trace fossils found after the glacial age of Precambrian are widely distributed in Late Sinian of Southwestern China.They may furnish important evidences for division and correlation of Sinian and the boundary of Sinian-Cambrian.
Key words: China; Stratigraphical distribution; Precambrian; Trace fossils.
[1]袁鄂荣.怀来县长城系团山子组内发现潜穴.地球科学,1993,18(5):597 - 601.
[2]华洪等.中元古代长城纪遗迹化石在宁夏贺兰山的发现.西北大学学报,1993,23(5):459 - 462.
[3]李文厚.陕西洛南长城系一种可能的场形动物的发现.西北大学学报,1987, 17(3):64-67.
[4]胡建民等.豫西长城系遗迹化石及其惫义.地质论评,1991,37(5), 437-444.
[5]杨式溥等.北京昌平青白口群长龙山组遗迹化石.北京大学专刊,庆祝乐森寻教授教学科研60周年、北京:科学出版社,1986.
[6]段吉业等.辽南晚前寒武纪后生动物群的特征及时代范围.长春地质学院学报,1980, (2), 20-28.
[7]吴贤涛等.新获展旦纪痕迹化石Planolites, Chondrites的发现及其意义.地质科学,1987, (3) : 239- 245.
[8]殷继成等.淇东展旦系一寒武系界线层遗迹化石新发现及对比意义.地质学报,1993,67(2):146 - 157.
[9]林世敏等.陕南展旦系上统高家山组发现的后生动物、遗迹化石和宏观藻类化石.陕西地质,1986,4(1):9-17.
[10]邢裕盛等.长江三峡地区生物地层学:(1)展旦纪分册(遗迹化石部分).北京:地质出版社,1985,21-30.
[11]杨式溥等.宁夏贺兰山展且纪正目观组遗迹化石.地球科学,1985 ,10, 9-17.
[12]杨瞿和.川滇地区展旦纪后生动物、宏观藻类及遗迹化石新知.西南地质科技情报,1987,(3-4),9-12.
[13]Simpson G G. Editorial essay. Precambrian Research, 1978, (7):101-103.
[14]Towe K M. Oxygen-collagen priority and the early Metazoan fossil record. Natl Acad Sci Proc, 1970, (65):781-788.
[15] Kauffman E G and Steidtmann J R. Are these the oldest metazoan trace fossils? J Palaeontol, 1981,55(5) :923-947.
[16] Crimes T P. The period of early evolutionary failure and the down of evolutionary success: The record of biotic changes across the Precambrian-Cambrian Boundary. In:S K Donovan(ed.).The Palaeobiology of Trace Fossils. Engiand,1994:105-133.
[17] 宋天锐等.最古老的后生动物痕迹化石?—对北京十三使前寒武系常州沟组充填管状构造的探讨.沉积学报,1985,3(2):85-94.
[18]陈孟获等.先伊迪卡拉期的淮南生物群.地质科学,1986,(3),221 - 231.
[19] Seiiacher A. Der beginn des Kambrium ale biologische Wende. Neues Jahrbuch fur Geologie and Palaeontologie, Abhandlungen, 1956,103:155-l80.
[20] Alpert S P. Trace fossils and the basal Cambrian boundary. In, Crimes T P and Harper J C (eds.).Trace fossils 2. Gaol Jour Spec lssu,1977,(9):1-8.
/
〈 |
|
〉 |