王飞飞, 赵全民, 丁旋, 刘健. 渤海东北海域有孔虫埋葬群特点与沉积环境的关系[J]. 海洋地质与第四纪地质, 2009, 29(2): 9-14. DOI: 10.3724/SP.J.1140.2009.02009
引用本文: 王飞飞, 赵全民, 丁旋, 刘健. 渤海东北海域有孔虫埋葬群特点与沉积环境的关系[J]. 海洋地质与第四纪地质, 2009, 29(2): 9-14. DOI: 10.3724/SP.J.1140.2009.02009
WANG Feifei, ZHAO Quanmin, DING Xuan, LIU Jian. CHARACTERISTICS OF THE FORAMINIFERAL TAPHOCOENOSE IN THE NORTHEAST BOHAI AND RELATIONSHIP TO THE SEDIMENTARY ENVIRONMENT[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 9-14. DOI: 10.3724/SP.J.1140.2009.02009
Citation: WANG Feifei, ZHAO Quanmin, DING Xuan, LIU Jian. CHARACTERISTICS OF THE FORAMINIFERAL TAPHOCOENOSE IN THE NORTHEAST BOHAI AND RELATIONSHIP TO THE SEDIMENTARY ENVIRONMENT[J]. Marine Geology & Quaternary Geology, 2009, 29(2): 9-14. DOI: 10.3724/SP.J.1140.2009.02009

渤海东北海域有孔虫埋葬群特点与沉积环境的关系

CHARACTERISTICS OF THE FORAMINIFERAL TAPHOCOENOSE IN THE NORTHEAST BOHAI AND RELATIONSHIP TO THE SEDIMENTARY ENVIRONMENT

  • 摘要: 对渤海东北海域211个表层样品中有孔虫的定量和定性分析,共得底栖有孔虫48属109种,浮游有孔虫匮乏。对底栖有孔虫中58个种运用Q型因子分析,经方差最大化旋转,获得3个主因子的方差累计贡献为98.62%。组合Ⅰ为毕克卷转虫变种-冷水面颊虫,代表低温低盐沿岸流分布的滨岸环境;组合Ⅱ为异常诺宁虫-伊格尔虫未定种,代表黏土粉砂沉积物分布的近岸浅海;组合Ⅲ为压扁卷转虫-覆盖面颊虫,代表30 m水深线以外的较深水环境。研究区有孔虫埋葬群分布主要受冬季低温低盐沿岸流、沉积物分布、潮流、沉积速率及CaCO3含量等因素的控制。

     

    Abstract: Based on the quantitative and qualitative analysis of 211 surface sediment samples in the northeast Bohai, 109 benthic foraminifera species which belong to 48 genera were recognized. Very few planktonic foraminifera were found in this studied area. Q-mode factor analysis was made for the 58 benthic foraminifera species, and 3 varimax factors with a cumulative contribution of 98.62% have been revealed as follows:AssemblageⅠ(Ammonia beccrii vars.-Buccella frigida), which represents a littoral environment with low-temperature and low-salinity alongshore currents; AssemblageⅡ(Nonion anomalinoidea-Eggerella sp.), which represents a nearshore shallow-sea environment with distributions of fine sand and clay; Assemblage Ⅲ (Ammonia compressiuscula-Buccella tunicate), which indicates shallow-sea environment of more than 30 m water depth. The distribution of foraminiferal taphocoenose in the study area is mainly controlled by such factors as alongshore currents typical of low temperature and low salinity in winter season, sediment types, tidal currents, sedimentation rates, and CaCO3 contents.

     

/

返回文章
返回