[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.
|