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东海表层沉积中有孔虫、介形虫组合分布的初步研究

A Preliminary Study of Foramiriferal and Ostracod Assemblages’ Distribution in Bottom Sediments of the East China Sea

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【作者】 汪品先闵秋宝卞云华章纪军

【Author】 Wang Pin Xian, Min Qiu Bao, Bian Yun Hua, Zhang Ji Jun

【机构】 同济大学同济大学海洋局二所

【摘要】 东海沉积中有孔虫、介形虫定量研究的结果表明:河口、陆架内部、中部、外部、陆坡与海槽,分別具有不同的有孔虫、介形虫组合,它们受水深,水温与盐度等因素控制。

【Abstract】 Foraminifera and ostracods were identified from more then 400 bottom samples taken from the East China Sea. As shown by the results of the qualitative and quantitative micropaleontological analyses, the basic factor controlling the distribution of the foraminiferal and ostracod assemblages is water depth and offshore distance, although water temperature, currents and salinity have strong influence on their distribution. These general distribution patterns have been complicated by occurences of Late Pleistocene relict fauna. Six benthic foraminiferal assemblages, each representative of increasing water depth and salinity, were recognized from estuaries to Ryukyu trench: 1. Ammonia convexidorsa-Epistominella naraensis assemblage-estuaries: 2. Ammonia beccarii var.-Elphidium advenum assemblage-water depth<55m.; 3. Bolivina cochei-Ammonia compressiuscula assemblage-50-100m.; 4. Textularia pseudocarinata-Cibicides margaritifera assemblage-100-150m.; 5. Cassidulima spp. assemblage-150-700m.; 6. Lagena spp. assemblage-700-2000m.; Accordingly, G ostracod assemblages may be distinguished as follows: 1. Albileberis sinensis assemblage-estuaries; 2. Leguminocytkereis hodgii assemblage;-<50m.; 3. Munseyella-Cytheropteron assemblage-50100m.; 4. Bairdia-Cytherelloidea assemblage-100-150m.; 5. Krithe producta assemblage-150-2000m.. There are two groups of planktonic foraminiferal species occuring in the East China Sea bottom sediments: eurythermal species such as Globigerina bulloides, Globigerina iuiniueloba and G. pumilio, and warm water species such as Orbulina universa, Globoroialia menardii. The warm water planktonic foraminifera are absent in region with water depth less than 50m., but are partly present in 50-100m. depth region and abundant beyond the 100m. isobath, thus indicating the infuence of the Kuroshio warm water current. The test size of planktonic foraminifera, the ratio of planktonic specimens to total foraminiferal mumber, as well as the ratio of ostracod to foraminiferal number increase generally with distances from coastline to trench.

  • 【文献出处】 同济大学学报 ,Journal of Tongji University , 编辑部邮箱 ,1979年02期
  • 【被引频次】21
  • 【下载频次】368
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