Advanced Search

YANG Rui-dong, ZHAO Yuan-long, MAO Jia-ren, NIE Ai-guo, CHEN Xiao-yuan. Paleoecology of the Kaili Biota from Middle Cambrian in Taijiang County, Guizhou Province, China[J]. Acta Sedimentologica Sinica, 2002, 20(1): 129-135.
Citation: YANG Rui-dong, ZHAO Yuan-long, MAO Jia-ren, NIE Ai-guo, CHEN Xiao-yuan. Paleoecology of the Kaili Biota from Middle Cambrian in Taijiang County, Guizhou Province, China[J]. Acta Sedimentologica Sinica, 2002, 20(1): 129-135.

Paleoecology of the Kaili Biota from Middle Cambrian in Taijiang County, Guizhou Province, China

  • Received Date: 2000-09-14
  • The Kaili Biota is the third most diverse Burgess Shale-type biota after the Burgess Shale and Chengjiang biota. In the paper, on the basis of the study on the burial characteristics of fossils, the ecological be-havior of animal and algae, and the analysis of depositional characteristics and the geochemical parameter, we consider that most animals and algae in the Kaili Biota lived at the shallow water, and these organisms are carried into continental shelf by tempesite or turbidity flow and is buried in contnental shelf. At the same time, the burying mechanism of the Kaili biota is put forward in this paper. On the basis of the analyses of sedimentary sequences and taphonomic sequences of fossil in Kaili Fm. bearing-Kaili Biota, and combining research of geochemistry and paleo-ecology and taphonology, the Kaili Biota is considered that most organisms are characterized by ecological behavior of shallow water, these animals and algae living in shallow water were destroyed by event of tempesite or turbidity flow, and carried into deeper shelf, and buried at shelf. Some researches suggested that the Kaili Biota live at 150~200 meters water in depth; they reached this conclusion from lithology and lithofacies, and trace fossil assemblage in Kaili Formation. We disagree with above-mentioned view about the Kaili Biota lived below 150~200 meter deep, but agree that the Kaili Biota uas buried at shelf below 150~200 meter water in depth. Therefore, we consider that most animals and algae in the Kaili biota lived at shallow water, and they were carried into shelf by tempesite or turbidity flow and were buried in shelf. The conclusion is suggested by the following sedimentary characteristics and fossil assemblage in Kaili Fm. 1, A lot of algal fossils (about 20 genus), containing red algae, blue algae, and brown algae, occur in the Kaili Biota. According to ecological distribution of modern algae, so high diverse algae only live at shallow sea (less than 90 meter in depth). 2, Until now, the Kaili Biota contains more than 100 genus animal fossils, so high diverse animals only live at shallow sea (less than 90 meter in depth). 3, Most fossils were persevered at D layer of tempesite or turbidity sequence, this is the fossil buried sequence C, but shelf shale (analogous to E layer of tempesite or turbidite sequence) only contains few fossils. On the basis of fossil distribution in the tempesite or turbidity sequence, we believe that most organisms were carried into shelf from shallow water region by tempesite or turbidity flow.
  • [1] 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[J].古生物学报,1999,38(增刊):1~14
    [2] 浦心纯,周浩达,王熙林等.中国南方寒武纪岩相古地理与成矿作用[M].北京:地质出版社,1993.40~100
    [3] 桑惕,王立亭.贵州岩相古地理图集[M].贵阳:贵州科技出版社,1992.1~77
    [4] 杨式溥.贵州台江早、中寒武世凯里组的遗迹化石[J].古生物学报,1994,33(3):350~358
    [5] 张正华,沈建伟,赵元龙等.贵州台江中寒武世凯里动物群保存环境初探[J].古生物学报,1996,35(5):607~622
    [6] 朱立军,赵元龙.贵州台江中、下寒武统界线剖面微量元素地球化学特征[J].古生物学报,1996,35(5):623~630
    [7] 杨瑞东,赵元龙.贵州早,中寒武世凯里组中带状宏观藻类[J].地质论评,1999a,45(3):282~290
    [8] 杨瑞东,赵元龙.我国早期后生生物群的埋藏学、沉积古地理探讨[J].沉积学报,1999b,17(1):161~165
    [9] 杨瑞东,毛家仁,赵元龙等.贵州台江早-中寒武世凯里组中分枝状宏观藻类化石[J].地质学报,2001,(1):(印刷中)
    [10] 杨瑞东,赵元龙.贵州台江凯里生物群中化石埋藏序列分析[J].古生物学报,1999c,38(增刊):95~101
    [11] 朱茂炎,Erdtmann B D,赵元龙.贵州中寒武世凯里化石库的埋藏学和生态学初步研究[J].古生物学报,1999,38(增刊):28~57
    [12] 李凡,徐善民,姜秀珩等.南黄海海水中悬浮体跃层及底部浑水层[J].海洋科学,1991,(5):42~45
    [13] 黄友庄,王化羽,赵元龙.贵州台江早、中寒武世凯里组的腕足动物[J].古生物学报,33(3):335~344
    [14] 杨瑞东.黔中、黔南三叠纪古生态、古群落研究[J].岩相古地理,1996,16(6):42~47
    [15] Crimes T P,Legg I,Marcos A.Late Precambrian-Lower Cambrian trace fossils from Spain[J].Trace fossils,1977,2:91~38
    [16] 福迪 B著,罗迪安译.藻类学[M].上海:上海科学技术出版社,1980.1~449
    [17] Yang Ruidong,Zhao Yuanlong.Discovery of Bryophyte fossil from the Middle Cambrian of Taijiang country,Guizhou province,China[J].Chinese Science Bulletin,2000,45(6):544~547
    [18] 尹磊明,杨瑞东.贵州台江中寒武世凯里组疑源类[J].古生物学报,1999,38(增刊):66~78
    [19] 尹磊明.吉林浑江、湖北宜昌早奥陶世疑源类[M].北京:地质出版社,1995.1~92
    [20] 尼贝肯 J W著,林光恒,李和平译.海洋生物学-生态学探讨[M].北京:海洋出版社,1991.1~311
    [21] 刘岫峰.沉积岩实验室研究方法[M].北京:地质出版社,1991.206~22
    [22] 吴明清,欧阳自远.铈异常- 一个寻迹古海洋氧化还原条件变化的化学示踪剂[J].科学通报,1992,37(3):242~244
  • 加载中
通讯作者: 陈斌, bchen63@163.com
  • 1. 

    沈阳化工大学材料科学与工程学院 沈阳 110142

  1. 本站搜索
  2. 百度学术搜索
  3. 万方数据库搜索
  4. CNKI搜索

Article Metrics

Article views(649) PDF downloads(548) Cited by()

Proportional views
Related
Publishing history
  • Received:  2000-09-14

Paleoecology of the Kaili Biota from Middle Cambrian in Taijiang County, Guizhou Province, China

Abstract: The Kaili Biota is the third most diverse Burgess Shale-type biota after the Burgess Shale and Chengjiang biota. In the paper, on the basis of the study on the burial characteristics of fossils, the ecological be-havior of animal and algae, and the analysis of depositional characteristics and the geochemical parameter, we consider that most animals and algae in the Kaili Biota lived at the shallow water, and these organisms are carried into continental shelf by tempesite or turbidity flow and is buried in contnental shelf. At the same time, the burying mechanism of the Kaili biota is put forward in this paper. On the basis of the analyses of sedimentary sequences and taphonomic sequences of fossil in Kaili Fm. bearing-Kaili Biota, and combining research of geochemistry and paleo-ecology and taphonology, the Kaili Biota is considered that most organisms are characterized by ecological behavior of shallow water, these animals and algae living in shallow water were destroyed by event of tempesite or turbidity flow, and carried into deeper shelf, and buried at shelf. Some researches suggested that the Kaili Biota live at 150~200 meters water in depth; they reached this conclusion from lithology and lithofacies, and trace fossil assemblage in Kaili Formation. We disagree with above-mentioned view about the Kaili Biota lived below 150~200 meter deep, but agree that the Kaili Biota uas buried at shelf below 150~200 meter water in depth. Therefore, we consider that most animals and algae in the Kaili biota lived at shallow water, and they were carried into shelf by tempesite or turbidity flow and were buried in shelf. The conclusion is suggested by the following sedimentary characteristics and fossil assemblage in Kaili Fm. 1, A lot of algal fossils (about 20 genus), containing red algae, blue algae, and brown algae, occur in the Kaili Biota. According to ecological distribution of modern algae, so high diverse algae only live at shallow sea (less than 90 meter in depth). 2, Until now, the Kaili Biota contains more than 100 genus animal fossils, so high diverse animals only live at shallow sea (less than 90 meter in depth). 3, Most fossils were persevered at D layer of tempesite or turbidity sequence, this is the fossil buried sequence C, but shelf shale (analogous to E layer of tempesite or turbidite sequence) only contains few fossils. On the basis of fossil distribution in the tempesite or turbidity sequence, we believe that most organisms were carried into shelf from shallow water region by tempesite or turbidity flow.

YANG Rui-dong, ZHAO Yuan-long, MAO Jia-ren, NIE Ai-guo, CHEN Xiao-yuan. Paleoecology of the Kaili Biota from Middle Cambrian in Taijiang County, Guizhou Province, China[J]. Acta Sedimentologica Sinica, 2002, 20(1): 129-135.
Citation: YANG Rui-dong, ZHAO Yuan-long, MAO Jia-ren, NIE Ai-guo, CHEN Xiao-yuan. Paleoecology of the Kaili Biota from Middle Cambrian in Taijiang County, Guizhou Province, China[J]. Acta Sedimentologica Sinica, 2002, 20(1): 129-135.
Reference (22)

Catalog

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return