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厦门湾-九龙江口地区MIS 4以来孢粉组合特征及古气候意义

瓦西拉里 王建华 郑艳伟 骆美美 陈慧娴 黄康有 曹玲珑

中山大学学报(自然科学版)Issue(6):53-62,10.
中山大学学报(自然科学版)Issue(6):53-62,10.

厦门湾-九龙江口地区MIS 4以来孢粉组合特征及古气候意义

Pollen Characteristics and their Paleoclimatic Significance since MIS 4 in Xiamen Bay and Jiulong River Estuary

瓦西拉里 1王建华 1郑艳伟 2骆美美 1陈慧娴 1黄康有 1曹玲珑1

作者信息

  • 1. 中山大学地球科学与地质工程学院∥广东省地质过程与矿产资源探查重点实验室,广东 广州510275
  • 2. 广州地理研究所,广东 广州510070
  • 折叠

摘要

Abstract

According to pollen assemblage analysis of 3 boreholes in Xiamen Bay-Jiulong River Estuary region,combined with the results of sedimentary facies and dating analysis,this paper explore the paleo-climatic and paleoenvironmental evolution in this area since Late Pleistocene.Pollen analysis show that:since the early stage of MIS4,the main paleoclimatic evolution of the region includes the fluctuations and changes such as:slightly dry-cold in Late Pleistocene,dry-warm then wet-warm in early Mid Holocene (8~5.5 cal.ka BP),wet-warm then slightly moderate-dry climate in late Mid Holocene (5.5 ~2.5 cal.ka BP)and wet-warm in Late Holocene (since 2.5 cal.ka BP).Global scale substantial cooling e-vent in Late Pleistocene impacts clearly in this area.Characteristic of the climate change in Holocene is that the temperature and humidity varies fluctualy between some ranges.The human activity infects clear-ly the vegetation form since Late Holocene.

关键词

孢粉/古气候/第四纪/厦门湾/九龙江口

Key words

pollen/paleoclimate/Quaternary/Xiamen Bay/Jiulong River Estuary

分类

地质学

引用本文复制引用

瓦西拉里,王建华,郑艳伟,骆美美,陈慧娴,黄康有,曹玲珑..厦门湾-九龙江口地区MIS 4以来孢粉组合特征及古气候意义[J].中山大学学报(自然科学版),2014,(6):53-62,10.

基金项目

国家自然科学基金资助项目(41276079);中国地质调查局“厦门湾地质环境调查”资助项目 ()

中山大学学报(自然科学版)

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