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胶州湾表层沉积颗石藻Gephyrocapsa oceanica的分布模式及其与环境的关系
引用本文:钟石兰,汪亚平,等.胶州湾表层沉积颗石藻Gephyrocapsa oceanica的分布模式及其与环境的关系[J].古生物学报,2001,40(4):505-513.
作者姓名:钟石兰  汪亚平
作者单位:1. 中国科学院南京地质古生物研究所,
2. 中国科学院海洋研究所,
基金项目:中国科学院南京地质古生物研究所现代古生物学与地层学开放研究实验室(No.953102)、国家自然科学基金杰出青年基金(No.49725612)资助课题
摘    要:对胶州湾和邻近海域表层沉积中颗石藻Gephyrocapsa oceanica的分布进行初步研究,并提出胶州湾内这个种的分布模式,研究结果表明,该种在胶州湾和邻近海域表层沉积颗石藻组合占绝对优势,几个从属种类Braarodosphaera bigelowill,Syracosphaera histrica,S.lamina和Acantholithus sp.等,在一些样品中稀少,在胶州湾,依据Gephyrocapsa oceanica丰度的变化,自岸向海可以划分三个分布带:向岸常见带,浅水丰富带和深水富集带,这一分布模式与海湾水下地貌有密切的关系,在湾外的近岸海域,该种的分布呈现出与湾内相似的特征。

关 键 词:颗石藻  分布模式  沉积动力学  胶州湾  海湾  水下地貌
修稿时间:2001年1月8日

DISTRIBUTION PATTERNS OF NANNOFOSSIL GEPHYROCAPSA OCEANICA IN SURFICIAL SEDIMENTS OF JIAOZHOU BAY, SOUTHERN SHANDONG PENINSULA,CHINA
ZHONG Shi Lan ,WANG Ya Ping ,GAO Shu ,CAO Qi Yuan and ZHU You Hua Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing Institute of Oceanology,Chinese Academy o.DISTRIBUTION PATTERNS OF NANNOFOSSIL GEPHYROCAPSA OCEANICA IN SURFICIAL SEDIMENTS OF JIAOZHOU BAY, SOUTHERN SHANDONG PENINSULA,CHINA[J].Acta Palaeontologica Sinica,2001,40(4):505-513.
Authors:ZHONG Shi Lan  WANG Ya Ping  GAO Shu  CAO Qi Yuan and ZHU You Hua Nanjing Institute of Geology and Palaeontology  Chinese Academy of Sciences  Nanjing Institute of Oceanology  Chinese Academy o
Institution:ZHONG Shi Lan 1),WANG Ya Ping 2),GAO Shu 2),CAO Qi Yuan 2) and ZHU You Hua 1) 1) Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing 210008 2) Institute of Oceanology,Chinese Academy o
Abstract:Surficial sediment samples were collected from the Jiaozhou Bay and adjoining seawaters to study the spatial distribution patterns of calcareous nannofossils within the embayment. The result shows that Gephyrocapsa oceanica monopolized the nannofossil assemblage, whilst some subordinate taxa Braarudosphaera bigelowii, Syracosphaera histrica, S. lamina and Acantholithus sp. etc. scarcely occur in some samples. Three zones for the distribution of Gephyrocapsa oceanica are recognized, according to variations in its abundance value: They are the onshore common zone, shallow water rich zone and deep water accumulation zone, from the coastline to deep waters. Geomorphologically, these zones successively correspond to silty clay tidal flat, sub tidal erosional channels and submarine erosional highlands. The same nannofossil assemblage with an analogous distribution pattern is also observed on the adjacent continental shelf. It is well known that Emiliania huxleyi is one of the most common species in the ocean and Florisphaera profunda is a marker of deep water environments. However, these two species were not found in the study area, which may be explained by ecological controls related to water fertility and quality, and to water depth.
Keywords:Calcareous nannofossil  Distribution pattern  Sediment dynamics  Jiaozhou Bay
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