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渤海湾西北岸滨海湖埋藏牡蛎礁硅藻及其记录的古环境

方晶 胡克 范昌福 商志文 杨永强 齐乌云 王福 裴艳东 王宏

海洋地质与第四纪地质2012,Vol.32Issue(5):81-88,8.
海洋地质与第四纪地质2012,Vol.32Issue(5):81-88,8.DOI:10.3724/SP.J.1140.2012.05081

渤海湾西北岸滨海湖埋藏牡蛎礁硅藻及其记录的古环境

DIATOM RECORDS OF THE BINHU BURIED OYSTER REEF,IN BINHAIHU,NORTHWEST BOHAI BAY AND PALEO-ENVIRONMENTAL IMPLICATIONS

方晶 1胡克 2范昌福 3商志文 4杨永强 2齐乌云 3王福 5裴艳东 2王宏2

作者信息

  • 1. 天津师范大学城市与环境科学学院,天津300378
  • 2. 中国地质调查局天津地质调查中心,天津300170
  • 3. 中国地质大学(北京)海洋学院,北京100083
  • 4. 中国地质科学研究院矿产资源研究所,北京100037
  • 5. 中国社会科学院考古研究所古科技中心,北京100710
  • 折叠

摘要

Abstract

The muddy sediments filling into the oyster shells in Binhaihu oyster reef of the northwest Bohai Bay were collected for diatom analysis. Auliscus caelatus , an indicator of intertidal zone environment, is as high as 19%—42% in the reef that suggested that the Binhaihu oyster reef was formed in an intertidal environment. Based on the diatoms and 14C dating, three zones were subdivided from the bottom to the top. The Zone I, formed during the period of 2 445~2 327 cal. aBP, was deposited in an open lagoon-intertidal environment with strong river influence. The marine influence decreased as the influence of intertidal zone increased upwards. In the Zone II, which was formed around 2 327cal. aBP, marine species Thalassionema nitzschioides increased while oceanic species Coscinodiscus spp. And Actinocyclus spp. Decreased, showing a closed inner lagoon-intertidal environment, and the salinity of lagoon was increased due to the decrease in river input. The Zone III, formed 2 327~2 287 cal. aBP, was resulted of the change from a closed lagoon to an open lagoon-intertidal environment.

关键词

埋藏牡蛎礁/硅藻分析/潟湖/潮间带/渤海湾

Key words

buried oyster reef/diatom analysis/lagoon/ intertidal zone/Bohai Bay

分类

海洋科学

引用本文复制引用

方晶,胡克,范昌福,商志文,杨永强,齐乌云,王福,裴艳东,王宏..渤海湾西北岸滨海湖埋藏牡蛎礁硅藻及其记录的古环境[J].海洋地质与第四纪地质,2012,32(5):81-88,8.

基金项目

国家自然科学基金项目(40872106) (40872106)

地质调查项目(1212010911069,1212011120089) (1212010911069,1212011120089)

海洋地质与第四纪地质

OA北大核心CSCDCSTPCD

0256-1492

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