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珠江三角洲晚第四纪环境演变的微体生物记录

董艺辛 刘春莲 阴家润 杨小强 Franz T.F(U)RSICH 高芳蕾

古脊椎动物学报2007,Vol.45Issue(2):161-172,12.
古脊椎动物学报2007,Vol.45Issue(2):161-172,12.

珠江三角洲晚第四纪环境演变的微体生物记录

LATE QUATERNARY MICROFAUNAS AND PALEOENVIRONMENTAL CHANGES RECORDED IN CORE SEDIMENTS OF THE PEARL RIVER DELTA, SOUTH CHINA

董艺辛 1刘春莲 1阴家润 2杨小强 1Franz T.F(U)RSICH 3高芳蕾1

作者信息

  • 1. 中山大学地球科学系,广州,510275
  • 2. 中国地质大学地质系,北京,100083
  • 3. 德国维尔兹堡大学古生物研究所,维尔兹堡,97070
  • 折叠

摘要

Abstract

Late Quaternary core sediments from the middle area of the Pearl River Delta can be lithologically divided into six units. Unit 1,2, and 5 contain foraminifers and ostracods in different abundances. Faunal analysis suggests that they were deposited in brackish to marine environments. Unit 3 does not contain any fossils except plant debris, indicating a fluvial plain environment. Unit 4, characterized by a layer of mottled clay that is widely distributed in the Pearl River Delta area, is completely barren of fossils, representing an interval of continental weathering. Unit 6 bears only non-marine ostracods and was deposited on a fluvial plain. Combining foraminiferal and ostracod data with geochemical and susceptibility records allows to establish the following environmental stages in this area; A. Delta front stage (25 100~24 000 aB. P. ) ; B. Estuary stage (24 000~22 400 aB. P. ) ; C. Fluvial plain stage (22 400~21 700 aB. P. ) ; D. Continental weathering stage (21 700 ~ 3 700 aB. P. ) ; E. Tidal flat stage ( 3 700~2 600 aB. P. ) , and F. Upper fluvial plain stage (since 2 600 aB. P. ). In the Late Quaternary sedimentary succession two transgression-regression cycles can be recognized in the study area, corresponding to stages A to D and E to F, respectively. The palaeoenvironmental changes are believed to have been controlled by fluctuations of sea level.

关键词

珠江三角洲/晚第四纪/有孔虫/介形类/环境演化

Key words

Pearl River Delta/Late Quaternary/foraminifers/ostracods/environmental change

分类

天文与地球科学

引用本文复制引用

董艺辛,刘春莲,阴家润,杨小强,Franz T.F(U)RSICH,高芳蕾..珠江三角洲晚第四纪环境演变的微体生物记录[J].古脊椎动物学报,2007,45(2):161-172,12.

基金项目

国家自然科学基金重点项目(编号:40331007)和面上项目(编号:40272011)、广东省自然科基金项目(编号:04009757)资助.This research was funded by the Natural Science Foundation of China ( Grant No. 40331007 and 40272011 ) and the Natural Science Foundation of Guangdong Province ( Grant No. 04009757 ) , respectively. (编号:40331007)

古脊椎动物学报

OA北大核心CSCDCSTPCD

1000-3118

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