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柴达木盆地西部第三系碳酸盐岩层的古生物特征

Paleontologic characteristics of the Tertiary carbonate beds in the west of Chaidamu Basin

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【作者】 柳祖汉杨孟达钟建华郭月清温志峰

【Author】 LIU Zu-han~(1), YANG Meng-da~(1), ZHONG Jian-hua~(2),GUO Yue-qing~(2), Wen Zhi-feng~(2)(1.Hunan University of Science and Technology,Xiangtan 411201,China;2.China Petroleum University,dongying 257061,China)

【机构】 湖南科技大学地质研究所中国石油大学资源系中国石油大学资源系 湖南湘潭411201湖南湘潭411201山东东营257061山东东营257061

【摘要】 柴达木盆地西部第三系的碳酸盐岩层中发现有藻类、介形虫、有孔虫、腹足类、多毛类等化石.除藻类外各种生物的数量都比较少.生物具有个体小,壳体构造简单,多样性低等特点.所有生物都属于广盐性生物.根据该区古生物特征分析和与其它地区的对比,认为当时该区生物生长于内陆半咸化湖至咸化湖环境,而不是海相或海陆过渡相环境.参11.

【Abstract】 The fossils of algae,ostracoda,foraminifera,gastropod and polychaeta were found in the Tertiary carbonate beds in the west of Chaidamu Basin.The quantity of various kinds of fossils was few,except the algae.The organisms were characterized by small size,simple structures of shells and low diversity.All kinds of organisms belonged to euryhaline organisms.It indicated that these organisms were developed in the environments of brackish lakes or salt water lakes and were not developed in the environments of marine facies or the transitional facies between the marine and land,according to the analysis of the paleontological characteristics in this area and the comparison with the paleocoenosis developed in other areas.11refs.

  • 【文献出处】 湖南科技大学学报(自然科学版) , 编辑部邮箱 ,2005年02期
  • 【分类号】Q911
  • 【被引频次】9
  • 【下载频次】237
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