华南陡山沱期晚期宏体生物生态系统的出现及其意义<sup>*</sup>

doi:10.7605/gdlxb.2009.06.004

Abstract
Figure/Table
References()
Related Citation (13)
Read Tracking
Download Tracking

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

Abstract The evolution of ecosystem is a major force on the origin and evolution of life. In the early evolution of life， the process of ecosystematic evolution was from the Mat-dominated Ecosystem， through the Plankton-eukaryotic Ecosystem and Marcoalgal Ecosystem， to the Macro-organismal Ecosystem， then to a relatively mature ecosystem in the Cambrian. The evolution of the early ecosystem mainly exhibited the developments:(1)what the habitats expanded from the surface layer of deposits to the water column and then to the inner of deposits in habitat;(2)what the relation of different species was from passive accepters to active competitors in life demands for environment factors;(3)what the energy transformation changed from the extra-intussuscepting or extra-assimilating to the endo-assimilating after extra-feeding;(4)the ecological pyramid changed complication and multilevel; and(5)what the organisms gradually enhanced the ability improving environment. In the macro-organismal ecosystem which emerged in the Late Doushantuoian of the Ediacaran in South China， organisms drastically enhanced the competition and reform for environment factors demanded by them， and began to actualize the energy transformation in the inner body of organism. The multilevel and complication of the ecological pyramid show that the macro-organismal ecosystem in the Late Doushantuoian is a key transition in the evolutional speed of life and a prelude of the Cambrian explosion.

	Service

	E-mail this article
	Add to my bookshelf
	Add to citation manager
	E-mail Alert
	RSS
	Articles by authors
	Wang Yue
	Zhao Mingsheng
	Yang Yanfei
	Wang Xunlian

Key words： ecosystem energy transformation environmental factor biotic competition Doushantuoian South China

Received: 14 May 2009 Published: 01 December 2009

ZTFLH:

Q913.84

About author: Wang Yue， born in 1964， was graduated from the Geology Department of Wuhan Geological College in 1984. Now he is a professor at School of Resources and Environments of Guizhou University， and is engaged in palaeontology and stratigraphy. E-mail: gzyuewang@126.com.

Cite this article:

Wang Yue,Zhao Mingsheng,Yang Yanfei et al. Emergence of marco-organismal ecosystem of the Late Doushantuoian in South China and its significance[J]. JOURNAL OF PALAEOGEOGRAPHY, 2009, 11(6): 641-651.

Wang Yue,Zhao Mingsheng,Yang Yanfei et al. Emergence of marco-organismal ecosystem of the Late Doushantuoian in South China and its significance[J]. JOPC, 2009, 11(6): 641-651.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2009.06.004 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2009/V11/I6/641

陈长胜. 2003. 海洋生态系统动力学与模型［M］. 北京：高等教育出版社，1-287.
陈孟莪. 1989. 中国晚前寒武纪的宏体化石概观［J］. 地质科学，(3): 244-255.
陈孟莪，萧宗正，袁训来. 1994a. 晚震旦世的特种生物群落——庙河生物群新知［J］. 古生物学报， 33(4):391-403.
陈孟莪，鲁刚毅，萧宗正. 1994b. 皖南上震旦统蓝田组的宏体藻类化石——蓝田植物群的初步研究［J］. 中国科学院地质研究所集刊，(7): 252-267.
陈孟莪，陈其英，萧宗正. 2000. 试论宏体植物的早期演化［J］. 地质科学， 35(1):1-15.
丁莲芳，李勇，胡夏嵩，等. 1996. 震旦纪庙河生物群［M］. 北京: 地质出版社， 1-221.
杜汝霖. 1982. 冀西北青白口系Chuaria等化石的发现及其意义［J］. 地质论评， 28(1):1-7.
杜汝霖，田立富，李汉棒. 1986. 蓟县长城系高于庄组宏观生物化石的发现［J］. 地质学报，(2): 115-120.
郭庆军，杨卫东，刘丛强，等. 2003.贵州瓮安生物群和磷矿形成的沉积地球化学研究［J］. 矿物岩石地球化学通报，22(3):202-208.
胡健民，孟庆任，李文厚. 1991.1400Ma前的后生动物实体化石？［J］. 西安地质学报学报， 13(2):1-6.
蒋志文. 2002. 澄江动物群群落及生态分析［M］. 见: 陈良忠，等.云南东部早寒武世澄江动物群.云南昆明: 云南科技出版社， 47-87.
梅冥相，孟庆芬，刘智荣. 2007. 微生物形成的原生沉积构造研究进展综述［J］. 古地理学报， 9(4):353-367.
彭永波，王丹，袁训来. 2009. 长城系串岭沟组球形疑源类的超微结构［J］. 微体古生物学报， 24(2):194-204.
唐烽，高林志. 1999. 北京及邻区青白口纪化石生物相研究［J］. 地质论评， 45(1):50-58.
唐烽，尹崇玉，高林志. 1997. 安徽休宁陡山沱期后生植物化石的新认识［J］. 地质学报， 71(4):289-296.
王约，王训练. 2006. 黔东北新元古代陡山沱期宏体藻类的固着器特征及其沉积环境意义［J］. 微体古生物学报， 23(2):154-164.
王约，王训练. 2007. 贵州中寒武世凯里生物群的生活环境及古生态系统［J］. 古地理学报， 9(4):407-418.
王约，何明华，喻美艺，等. 2005.黔东北震旦纪陡山沱晚期庙河型生物群的生态特征及埋藏环境初探［J］. 古地理学报， 7(3):327-335.
王约，王训练，黄禹铭. 2007a. 黔东北伊迪卡拉纪陡山沱组的宏体藻类［J］. 地球科学——中国地质大学学报， 32(6):828-844.
王约，王训练，黄舜铭. 2007b. 华南伊迪卡拉系陡山沱组Protoconites的分类位置与生态初探［J］. 地球科学——中国地质大学学报， 32(增): 41-50.
吴凯，马东升，潘家永，等. 2006.贵州瓮安磷矿陡山沱组地层元素地球化学特征［J］. 华东理工学院学报，29(2):108-114.
阎玉忠. 1995. 中国蓟县团山子组（17亿年）宏体藻类的发现和初步研究［J］. 微体古生物学报， 12(2):107-126.
阎玉忠，刘志礼.1993. 论长城系微化石群的真核生物意义［J］. 微体古生物学报， 10(2):167-180.
阎玉忠，刘志礼.1997. 中国蓟县长城系团山子宏观藻群［J］. 古生物学报， 36(1):18-41.
杨式溥. 1993. 古生态学——原理与方法［M］. 北京: 地质出版社， 1-228.
袁训来，肖书海，尹磊明，等. 2002. 陡山沱期生物群—早期动物辐射前夕的生命［M］.安徽合肥：中国科学技术大学出版社，26-133.
张鹏远. 1979. 蓟县蓟县系雾迷山组多核体绿藻化石［J］. 地质学报，(2): 87-90.
张同钢，储雪蕾，张启锐，等. 2003. 陡山沱期古海水的硫和碳同位素变化［J］. 科学通报， 48(8):850-855.
朱士兴，孙淑芳，黄学光，等. 1999. 燕山常州沟组（约1800Ma）碳质压型化石及其多细胞组织的发现［J］. 科学通报， 44(14):1552-1557.
朱为庆，陈孟莪. 1984. 峡东区上震旦统宏体藻类化石的发现［J］. 植物学报， 26(5):558-560.
Awramik S M. 1971. Precambrian columnar stromatolite diversity: Reflection of metazoan appearance［J］. Science， 174: 825-827.
Awramik S M， Schopf J W， Walter M R. 1983. Filamentous fossil bacteria from the Archean of Western Australia［J］. Precambrian Research， 20: 357-374.
Bottjer D J， Clapham M E. 2006. Evolutionary paleoecology of Ediacaran benthic marine animals. In: Xiao S，Kaufman A J(eds). Neoproterozoic Geobiology and Paleobiology［M］. Dordrecht：Springer，91-114.
Bouougri E， Porada H. 2002. Mat-related sedimentary structures in Neoproterozoic peritidal passive margin deposits of the West African Craton(Anti-Atlas， Morocco)［J］. Sedimentary Geology， 153: 85-106.
Droser M L， Gehling J G， Jensen S R. 2006. Assemblage palaeoecology of the Ediacaran biota: The unabridged edition？［J］. Palaeogeography， Palaeoclimatology， Palaeoecology，232: 131-147.
Fedonkin M A. 1985. Precambrian metazoans: The problem of preservation， systematics and evlution［J］. Philosophical Transactions of the Royal Society of London，Series B， 311: 27-45.
Fedonkin M A. 1990. Systematic description of Vendian Metazoa. In: Sokolov B S， Ivanovskij A B(eds).The Vendian System: Palaeontology， v.1［M］. Berlin：Springer-Verlag，71-120.
Glaessner M F. 1984. The Dawn of Animal Life， A Biohistorical Study［M］. Cambridge：Cambridge University Press，1-236.
Grey K， Williams I R. 1990. Problematic bedding-plane markings from the Middle Proterozoic Manganese Subgroup， Bangemall Basin， Western Australia［J］. Precambrian Research， 46: 307-327.
Hofmann H J. 1985. The mid-Proterozoic Little Dal macrobiota， Mackenzie Mountains， north-west Canada［J］. Palaeontology， 28: 331-354.
Kasting J F， Siefert J L. 2002. Life and the evolution of earths atmosphere［J］. Science， 296: 1066-1068.
Knoll A H. 1992. The early evolution of eukaryotes: A geological perspective［J］. Science， 256: 622-627.
Knoll A H， Javaux E J， Hewitt D， et al. 2006. Eukarvotic organisms in Proterozoic ocean［J］. Philosophical Transactions of the Royal Society Biological Sciences， 361: 1023-1038.
Li C， Chen J， Hua T. 1998. Precambrian sponges with cellular structures［J］. Science， 279: 879-882.
Ling Hongfei， Jiang Shaoyong， Feng Hongzhen， et al. 2004. Oxygen isotope geochemistry of phoshorite and dolomite and palaeo-ocean temperature estimation: A case study from the Neoproterozoic Doushantuo Formation， Guizhou Province， South China［J］. Progress in Natural Science， 14(1):77-84.
McCall G J H. 2006. The Vendian(Ediacaran)in the geological record: Enigmas in geologys prelude to the Cambrian explosion［J］. Earth-Science Reviews， 77: 1-229.
Noffke N， Gerdes G， Klenke T. 2003. Benthic cyanobacteria and their influence on the sedimentary dynamics of peritidal system(siliclastic， evaporitic salty， and evaporitic carbontic)［J］. Earth-Science Reviews， 62: 163-176.
Olcott A， Corsetti F A， Awramik S M. 2002. A new look at stromatolite form diversity［J］. GSA Abstracts with Programs， 34: 271.
Pflüger F. 1999. Matground structures and redox facies［J］. Palaios， 14: 25-39.
Runnegar B. 1982. Oxyen requirements， a biology and phylogenetic significance of the late Precambrian worm Dickinsonia and the evolution of the burrowing habit［J］. Alcheringa， 6: 223-239.
Runnnegar B. 1992. Evolution of the earliest animals. In: Schopf J W(ed.). Major Events in the History of Life［M］. Boston: Jones and Bartlett， 65-93.
Schopf J W， Packer B. 1987. Early Archean(3.3-billion-3.5-billion-year-old)microfossils from the Warrawoona Group， Australia［J］. Science， 237: 70-73.
Schopf J W. 1992. The oldest fossils and what they mean［M］. In: Schopf J W(ed).Major Events in the History of Life. Boston:Jones and Bartlett， 29-63.
Seilacher A. 1989. Vendozoa: Organismic construction in the Proterozoic biosphere［J］. Lethaia， 22: 229-239.
Seilacher A. 1999. Biomat-related lifestyles in the Precambrian［J］. Palaios， 14: 86-93.
Seilacher A， Pflüger F. 1994. From biomats to benthic agriculture: A biohistoric revolution［M］. In: Krumbein W E， et al.(eds). Biostablization of Sediments: Bibliotheks und Informations system der Carl von Ossietzky. Univeersitat oldenburg， 97-105.
Seilacher A， Bose P K， Pflüger F. 1998. Animals more than 1 billion years ago: Trace fossil evidence from India［J］. Science， 282: 80-83.
Shi Xiaoying， Zhang Chuanheng， Jiang Ganqing， et al. 2008. Microbial mats in the Mesoproterozoic carbonaes of the North China Platform and their potential for hydrocarbon generation［J］. Journal of China University of Geosciences， 19(5):549-566.
Steiner，M.1994. Die neoproterozoishen Megaalgen SudChinas［J］. Berliner Geowissrnschaftliche Abhandlungen， 15(E): 1-146.
Stiling P D. 1996. Ecology: Theories and Applications［M］. New Jersey: Prentice Hall， Upper Saddle River， 1-441.
Summons R E， Powell T G， Boreham C J. 1988. Petroleum geology and geochemistry of the middle Proterozoic McArthur Basin， Northern Australia， Ⅲ Composition of extractable hydrocarbons［J］. Geochimica et Cosmochimica Acta， 52: 1747-1763.
Tang Feng， Yin Chongyu， Bengtson S， et al. 2008. Octoradiate spiral organisms in the Ediacaran of South China［J］. Acta Geologica Sinica， 82(1):27-34.
Walter C D， Du R， Horodyski R J. 1990. Coiled carbonaceous megafossils from the middle Proterozoic of Jixian(Tianjin)and Montana［J］. American Journal of Science， 290-A: 133-148.
Walter M R， Oehler J H， Oehler D Z. 1976. Megascopic algae 1300 million years old from the Belt Supergroup， Montana: A reinterpretation of Walcotts Helminthoidichnites［J］. Journal of Paleontology， 50(5):872-881.
Wang Yue， Wang Xunlia. 2008. Annelid from the Neoproterozoic Doushantuo Formation in Northeast Guizhou， China［J］. Acta Geologica Sinica，82(2):257-265.
Wang Yue， Wang Xunlia， Huang Yiming. 2008. Megascopic Symmetrical Metazoans from the Ediacaran Doushantuo Formation in the Northeastern Guizhou， South China［J］. Journal of China University of Geosciences， 19(3)：200-206.
Wray G， Levinton J S， Shapiro L H. 1996. Molecular evidence of deep Precambrian divergences among the metazoan phyla［J］. Science， 274: 568-573.
Xiao S， Dong L. 2006. On the morphological and ecological history of Proterozoic macroalgae［M］. In: Xiao S，Kaufman A J(eds). Neoproterozoic Geobiology and Paleobiology. Dordrecht： Springer，57-90.
Xiao S， Zhang Y， Knoll A H. 1998. Three-dimensional preservation of algae and animal embryos in a Neoproterozoic phosphorite［J］. Nature， 391: 553-558.
Xiao S， Yuan X， Steiner M，et al. 2002. Macroscopic carbonaceous compressions in a terminal Proterozoic shale: A systematic reassessment of the Miaohe biota， South China［J］. Journal of Paleontology， 76: 347-376.
Yin Leiming， Zhu Maoyan， Knoll A H， et al. 2007. Doushantuo embryos preserved inside diapause egg cysts［J］. Nature， 446: 611-663.
Zhu Maoyan， Gehling J G， Xiao Shuhai， et al. 2008. Eight-armed Ediacaran fossil preserved in contrasting taphonomic windows from China and Australia［J］. Geology， 36(11):867-870.
Zhu S， Chen H. 1995. Megascopic multicellular organisms from the 1700-million-old Tuanshanzi Formation in the Jixian area， North China［J］. Science， 270: 620-622.