全球早、中寒武世藻类生物地理分区初探

doi:10.7605/gdlxb.2002.02.002

Abstract
Figure/Table
References()
Related Citation (15)
Read Tracking
Download Tracking

Download: PDF (0 KB) HTML (1 KB)
Export: BibTeX | EndNote (RIS) Supporting Info

Abstract

Abundant and well-preserved Cambrian macroalgal fossils occured in the Chengjiang Biota, Kaili Biota, Burgess Shale Biota and Siberian flora. Based on the patterns of geographic distributions of Precambrian macroalgae, and the similarities to both algae and metazoan fossils in the Kaili Biota and the Burgess Shale, the factors controlling the biogeographic provincialization of the interval of Precambrian—Middle Cambrian are discussed. Comparing algae and metazoan of the Kaili biota with those of the Burgess Shale and the Siberian flora, we discover that the regions of the same palaeolatitude present the similar bio-assemblage, while the regions of distinct different palaeolatitude present obviously different bio-assemblage. Because evolutional level of metazoan is low in the Precambrian—Middle Cambrian and biotic diversifying energy is low, the main factor controlling the provincialization of Precambrian—Middle Cambrian biogeography is palaeolatitude. Schopf's model of biogeographic region is not suitable for metazoan on the basis of the patterns of geographic distribution of metazoan in the Precambrian—Cambrian. A new model for dividing the Precambrian—Middle Cambrian biogeographic regions is established in this paper. The model could explain the similarities among the composition of the Chengjiang Biota, the Kaili Biota and the Burgess Shale Biota.

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors

Published: 01 April 2002

About author: Yang Ruidong, born in 1963, graduated from the Department of Earth Sciences, Nanjing University and obtained Ph.D. degree in 1999. Now he is a post-Ph.D. of Institute of Geochemistry, Chinese Academy of Sciences and a professor at Guizhou University of Technology, and is engaged in sedimentology, palaeontology and stratigraphy.

Cite this article:

. PRIMARY STUDY ON GLOBAL DISTRIBUTION OF ALGAE BIOGEOGRAPHIC BIOTA IN EARLY AND MIDDLE CAMBRIAN[J]. JOURNAL OF PALAEOGEOGRAPHY, 2002, 4(2): 12-18.

. PRIMARY STUDY ON GLOBAL DISTRIBUTION OF ALGAE BIOGEOGRAPHIC BIOTA IN EARLY AND MIDDLE CAMBRIAN[J]. JOPC, 2002, 4(2): 12-18.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2002.02.002 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2002/V4/I2/12

[1] 陈均远, 周桂琴, 朱茂炎．澄江动物群．台湾：国立自然博物馆, 1996. l—150
[2] 侯先光, Bergstrom J, 王海峰, 等. 澄江动物群—5.3亿年前的海洋动物. 昆明: 云南科技出版社, 1999. 1—170
[3] Conway Morris S, Robison R A. More soft-bodied animals and algae from Middle Cambrian of Utah and British Columbia. University of Kansas Paleontological Contributions, 1988, 122:1—48
[4] Conway Morris S. The crucible of creation – the Burgess Shale and rise of animals. Oxford: Oxford University Press, 1998. 1—210
[5] 赵元龙, 袁金良, 黄友庄, 等. 贵州台江中寒武世凯里动物群. 古生物学报, 1994, 33(3):263—271
[6] 赵元龙, 袁金良, 朱茂炎, 杨瑞东. 贵州中寒武世早期凯里生物群研究新进展. 古生物学报, 1999, 38(增刊), l—14
[7] Schopf J M. The role of biogeographic provinces in regulating marine faunal diversity through geologic time, In: Gray J. and Boucot A J., eds. Historical biogeography, plate tectonics, and the changing environment. Corvallis :Oregon State University Press, 1976. 449—457
[8] Walcott C D. Cambrian geology and paleontology IV, No.5--Middle Cambrian algal. Smith. Miscel. Collec., 1919, 67(5): 217—260
[9] Johnson J H. A review of the Cambrian algae. Colorado School of Mines, 1966, 61(1): 1—162
[10] Conway Morris S, Whittington H B. Fossils of the Burgess shale: a national Park, British Columbia. Geol. Sur. Canada Miscel. Report, 1985, 43:1—31
[11] Briggs D E G, Erwin D H, Collier F J. The fossils of Burgess Shale. Washington: Smithsonian Institution Press, 1994. 1—238
[12] Korde S C. Cambrian algae. Moskow, 1973, 1—173 (Press in Russian)
[13] 杨瑞东, 赵元龙, 郭庆军, 施贵军. 贵州早、中寒武世凯里组中带状宏观藻类. 地质论评, 1999, 45(3): 282—290
[14] 杨瑞东, 赵元龙. 贵州早、中寒武世凯里组中具节珊瑚藻类的发现及其意义. 科学通报, 1999, 11:1202—1206
[15] Yang Ruidong, Zhao Yuanlong. Discovery of Corallina fossil from the Middle Cambrian of Taijiang County, Guizhou Province, China. Chinese Science Bulletin, 2000,45(6): 544—547
[16] 杨瑞东, 毛家仁, 赵元龙, 等. 贵州中寒武世凯里组中分枝状宏观藻类化石. 地质学报, 2001, 75(4): 433—340
[17] Yang Ruidong, Mao Jiaren, Zhao Yuanlong. New macroalgal fossils from Middle Cambrian Kaili biota in Guizhou Province, China. Acta Botanica Sinica, 200l, 43(7):742—749
[18] 吴跃东. 皖南东至地区寒武系层序地层. 古地理学报, 2001, 3(3): 55—62
[19] Steiner M, Fatka O. Lower Cambrian tubular micro-to macrofossils from the Paseky Shale of the Barrandian area (Czech Republic). Palaont. Z., 1996,70(3):275-299
[20] Conway Morris S, Peel J S, Higgins A K, et al. A Burgess Shale-like fauna from the Lower Cambrian of north Greenland. Nature, 1987, 326: 181-183
[21] 福迪. B著. 藻类学. 罗迪安译. 上海: 上海科学技术出版社, 1980, 1—449
[22] 李伟新, 朱仲嘉, 刘凤贤. 海藻学概论. 上海: 上海科学技术出版社, 1982, 1—240
[23] Brasier M D. Background to the Cambrian explosion. J. Geo. Soc. London, l992,149: 585—587
[24] Mckerrow W S, Scotese C G, Brasier M D. Early Cambrian continental reconstructions. J. Geo. Soc. London, 1992, 149: 599—606
[25] Sundberg F A, Mccollum L B. Oryctocephalids (Corynexochida: trilobita) of the Lower-Middle Cambrian boundary interval from Valifornia and Nevada. J. Palaeontology, 1997, 71(6): 1065—1090
[26] 石光荣. 一个定量估计地质时期海洋生物地理分区性的模式. 地质学报, 1996, 70(4): 351—359
[27] Conway Morris S. Burgess Shale faunas and the Cambrian explosion. Science, 1989, 246: 339—246
[28] 蒋志文.初期生物的带壳演化及晚前寒武纪的终止. 前寒武纪地质, 1986, 3:515—522
[29] Dodd J R and Stanton R J. 古生态学概念与应用. 徐珊红, 钱文龙, 王雪, 等译. 南京: 南京大学出版社, 1989, 1—345
[30] 盖保民. 地球演化, 第3册. 北京: 中国科学技术出版社, 1996, 692—705
[31] 康育义. 生命起源与进化. 南京: 南京大学出版社, 1997, 1—180