地球科学进展 ›› 1993, Vol. 8 ›› Issue (2): 9 -13. doi: 10.11867/j.issn.1001-8166.1993.02.0009

学科发展与研究 上一篇    下一篇

我国早期生命进化研究的进展和展望
陈孟莪   
  1. 中国科学院地质研究所 北京
  • 收稿日期:1992-04-10 修回日期:1992-10-26 出版日期:1993-03-01

PROGRESS AND PROSPECT IN THE STUDIES ON EARLY EVOLUTION OF LIFE IN CHINA

Chen Meng'e   

  1. Institute of Geology; Academia Sinica; Beijing 100029
  • Received:1992-04-10 Revised:1992-10-26 Online:1993-03-01 Published:1993-03-01

概述了中国在晚前寒武纪——寒武纪生物化石群研究多方面(尤其是大化石)的主要成就。其中,近年发现的震旦纪陡山沱期化石生物(包括庙河生物群和蓝田植物群),对植物界的进化说来是个重要阶段;早寒武世澄江生物群(包括软躯体生物和软部保存的带骨骼生物)早于国外著名的布吉斯页岩生物群,逼近了带骨骼动物最初的爆发式辐射期。这些珍稀化石的研究将促进对早期生物进化历程的重新认识。这个研究领域有无可限量的前景。

The many achievements in the study on. the fossils (in especial megafossils) of late Precambrian - Cambrian in China are outlined. Among them, the organic fossils (including Miaohe Biota and Lan-tian Flora) in the Doushantuo stage of Upper Sinian discovered in recent years demonstrated an important stage for the early diversification of the plant kingdom; the early Cambrian Chengjiang Biota (bearing the soft-bodied fossils and skeletal fossils but with well-preserved soft-parts) is earlier than the famous Burgess shale fauna and very close to the first `explosion',radiation of the metazoam with hard part(so-called small shelly fossils).The sturdies on such exceptional and valuable fossil communities will lead to reconsidering the evolutionary processes of early life. The prospectsin this field are then brilliant.

[1]中国地质科学院天津地质矿产研究所主编.中国震旦亚界.天津科学技术出版社,1980, 407
[2]毕治国,王贤方,朱鸿,王自强,丁放.皖南震旦系.地层古生物论文集,1987, (19): 27- 60
[3]朱为庆.陈孟莪.峡东区上震旦统宏体化石藻类的发现.植物学报,1984,26(5):558-560
[4]邢裕盛,段承华,梁玉左,曹仁关等.中国晚前寒武纪古生物.地质出版社.1985,241
[5]杜汝霖,田立富.燕山地区青白口纪宏观藻类.河北科学技术出版社,1986,114
[6]张文堂,侯先光. Naraoia在亚洲大陆的发现.古生物学报,1985. 24 (6): 591-595
[7]张录易.陕西宁强晚震旦世晚期高家山生物群的发现与初步研究.中国地质科学院西安地质矿产研究所所刊.1986,(13):67-88
[8]张昀.前寒武纪生命演化与化石记录.北京大学出版社.1989,221
[9]陈均远,侯先光,路洁之.早寒武世带网状鳞片的蠕形海生动物.古生物学报,1989,28(1):1-16
[10]陈孟莪.辽南晚前寒武纪地层中的宏体化石之地层意义的探讨.地质科学,1991,(2):120-128
[11]陈孟莪.中国晚前寒武纪的宏体化石概观.地质科学,1989,(3):244-255
[12]陈孟莪,萧宗正.峡东区上震旦统发现宏体化石.地质科学,1991(4):317-324
[13]陈孟莪,郑文武.先伊迪卡拉期的淮南生物群.地质科学,1986, (3):221-230
[14]洪作民,杨雅君,黄镇福.辽东半岛南部先寒武纪宏体生物序列.辽宁地质,1991.(3):21-23
[15]钱逸.中国小壳化石研究现状与展望.微体古生物学报,1992,9(3):327-329
[16] S M Awramik,Mec Menamin D S,  Yin Chongyu, Zhao Ziqiang,  Ding Qixiu & Zhang Shusen.  Prokaryotic and Eukarytic Microfossils from a Proterozoic/phanerozoic Transition in China. Nature,  1985,(334):655-658
[17]Chen Junyuan & Erdtman B D.Lower Cambrian Fossil Lagerstatte from Chengjiang, Yunnan,China:insights for Reconstructing early Metazoan lift. In The Early Evolution of Metazoa and the significande of problematic Taxa (eds. by A M Simonetta and S Conway Morris).1991,57-76
[18]Conway Morris, S Mattes, B M & Chen Menge.The Early Skeletal organism Cloudina: new occurences from oman and possibly China. Amer. J. Sci. 1990,  (290)A, 245-260
[19]M F Glaessner.The Dawn of Animal Life. Cambridge University Press,1984,244p

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