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成都平原4 000aBP以来的孢粉记录与环境变化
引用本文:罗丽萍,朱利东,向芳,杨文光,阚瑷珂,罗虹,张擎,朱章义.成都平原4 000aBP以来的孢粉记录与环境变化[J].古生物学报,2008,47(2).
作者姓名:罗丽萍  朱利东  向芳  杨文光  阚瑷珂  罗虹  张擎  朱章义
作者单位:1. 中国地质科学院矿产综合利用研究所,成都,610041
2. 成都理工大学沉积地质研究院,成都,610059
3. 同济大学海洋地质国家重点实验室,上海,200092
4. 成都理工大学信息工程学院,成都,610059
5. 成都市文物考占研究所,成都,610072
基金项目:国家科技攻关计划,国家重点实验室基金
摘    要:成都平原晚全新世以来沉积的泥质层发现丰富的孢粉。根据孢粉成分组合特征和生态类型可划分出5个孢粉组合带,结合剖面上6个14^C测年数据,提出在过去的4000a研究区植被类型及气候环境经历了5个阶段的变化:3800-3600aBP为亚热带常绿阔叶林,气候暖偏湿;3600-3400aBP为含常绿树种的落叶阔叶林,气候温暖湿润;3400-2600aBP为草/湿地,气温下降,环境更潮湿;2600-900aBP为落叶阔叶林,温度又开始逐渐回升,气候温和偏湿;900-300aBP再次变为草/湿地,偏干冷的气候环境。

关 键 词:孢粉组合  气候变化  晚全新世  成都平原

SPORE-POLLEN ASSEMBLAGE AND ENVIRONMENTAL CHANGES OF THE CHENGDU PLAIN DURING THE LATE HOLOCENE
LUO Li-ping,ZHU Li-dong,XIANG Fang,YANG Wen-guang,KAN Ai-ke,LUO Hong,ZHANG Qin,ZHU Zhang-yi.SPORE-POLLEN ASSEMBLAGE AND ENVIRONMENTAL CHANGES OF THE CHENGDU PLAIN DURING THE LATE HOLOCENE[J].Acta Palaeontologica Sinica,2008,47(2).
Authors:LUO Li-ping  ZHU Li-dong  XIANG Fang  YANG Wen-guang  KAN Ai-ke  LUO Hong  ZHANG Qin  ZHU Zhang-yi
Abstract:On the Chengdu Plain,a four-meter thick sedimentary succession has accumulated during the past 4 000a of Holocene.In this study,82 samples were collected at 5cm intervals.Based on the characteristics of spore-pollen and 6 datasets from 14 C analysis,the vegetation-climatic changes on the Chengdu Plain during the last 4 000a are discussed.Five phases of paleovegetation successions and climatic fluctuations are revealed for the past 4 000 years,and five climate periods can be recognized and correlated regionally and globally.The results of this study suggest that the climate on Chengdu Plain has been affected by global climate to a certain degree.
Keywords:Spore-pollen assemblages  climatic changes  late Holocene  Chengdu Plain
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