论生态地层学理论模式

doi:10.11867/j.issn.1001-8166.1994.03.0071

地球科学进展 ›› 1994, Vol. 9 ›› Issue (3): 71 -75. doi: 10.11867/j.issn.1001-8166.1994.03.0071

论生态地层学理论模式

肖传桃,姜衍文,李维峰

江汉石油学院地质系湖北荆州 434102

收稿日期:1994-01-26 出版日期:1994-05-01
通讯作者: 肖传桃

ON THE THEORETICAL ECOSTRATIGRAPHIC MODEL

Xiao Chuantao,Jiang Yanwen,Li Weifeng

Geological Departmen, Jianghan College of petroleum,Jingzhou,Hubei 434102

Received:1994-01-26 Online:1994-05-01 Published:1994-05-01

下载PDF ( 597 )

关键词: 生态地层学, 生态相, 生态地层模式

The term ecostratigraphic facies(abbreviated as EF) is presented for the first time in this paper, which is defined as the association of fossils(including trace fossils) community and sedimentary features in a given paleo-environment. According to the association type of fossils and sedimentary features, eight types of ecostratigraphic facieses have been proposed,i.e. supratidal type(EF1). Intertidal(foreshore) type (EF2), subtidal (shoreface) type(EF3), upper shelf type(EF4), middle shelf type(EF5), low shelf type(EF6), bathyal type (EF7) and abyssal type (EF8). On the basis of the association law of ecostratigraphic facies in both space and time, lateral ecostratigraphic model including ecostratigraphic facies tract(EFT), ecostratigraphic facies region (EFR) and ecostratigraphic facies system (EFS) as well as vertical ecostratigraphic model containing ecostratigraphic facies zone (EFZ). Ecostratigraphic facies formation (EFF) and ecostratigraphic facies group (EFG) are described.

Key words: Ecostratigraphic facies, Ecostratigraphic facies type, Vertical ecostratigraphic model, Lateral ecostratigraphic model.

[1] Waterhouse J B.The significance of ecostratigraphy and need for biostratigraphic hierarchy in stratigraphic nomenclature. Lethaia, 1976.9:317-325.
[2] Kauffman E G.Basic concepts of community palaeoecology. Geol Soc Amer Abst,1974,6:815-816.
[3] Boucot A J. Evolution and extinction rate controls. Elsevier Ameterdam, Oxford,NewYork,1975.427.
[4] Boucot A J.Principles of benthic marine paleoecology. Academic Press, New York,1981,463.
[5] Boucot A J. Ecostratigraphic framework for the lower Devonian of the North American Appohimchi, subprovince. Geol Palaeont Abs, 1982,163(1):81-121.
[6] Boucot A J.Does evolution take place in an ecological vacum II?Jour Palaeont,1983,57(1):1-30.
[7] 陈源仁.生态地层学原理.地质出版社,1992.141-143.
[8] 肖传桃.生态地层学及其研究进展.地球科学进展,1991,6(1):40-48.
[9] 肖传桃,殷鸿福.若尔盖红星地区早中三叠世群落研究及地质意义.江汉石油学院学报,1990,12(2);10-15.
[10] 肖传桃.古群落演化的耗散结构模式.地球科学,1991,16(6):621-625.
[11] 肖传桃,李维峰等.中扬子地区下奥陶统分乡组生物礁古生态特征.江汉石油学院学报,1993,15(1):8-13.
[12] 肖传桃,姜衍文等.中扬子地区早奥陶世早中期Batostoma属的发现及其地质功能和生态学研究.科学通报,1993,38(14):1314-1316.
[13] 肖传桃,朱忠德.湖南石门杨家坪早寒武世三叶虫动物群.石油与天然气地质,1993,14(4).
[14] 肖传桃,朱忠德,刘秉理.生态地层单位及其在生物礁研究中的应用.石油勘探与开发,1994,21(2).
[15] 肖传桃,姜衍文,朱忠德.江汉盆地早寒武世生态地层及生物古地理特征.地质论评,1994(待刊).
[16] 肖传桃,李维峰.中扬子地区二叠纪生态地层学及古地理特征.石油学报,1995(待刊).
[17] 肖传桃,李维峰,郭成贤.江汉盆地早三叠世生态地层学及古地理特征.石油与天然气地质,1994(待刊).
[18] 王珍如,杨湘宁等译.海洋生态学导论.地质出版社,1990.
[19] 同济大学海洋地质系.海洋地质学.地质出版社,1982.
[20] 同济大学海洋地质系.古海洋学概论.同济大学出版社,1989.
[21] 王琦,朱而勤.海洋沉积学.科学出版社,1989.
[22] 殷鸿福,谢树成.四川松潘东北寨金矿预富集过程中的菌藻成矿作用.地球科学,1992,17(3):241-249.

[1]	金玉玕，李淳. 综合地层学的发展趋势[J]. 地球科学进展, 1991, 6(6): 6-12.
[2]	肖传桃. 生态地层学及其研究进展[J]. 地球科学进展, 1991, 6(1): 40-48.

阅读次数

全文

摘要