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应用生态学报 ›› 2004, Vol. ›› Issue (4): 575-578.

• 研究论文 • 上一篇    下一篇

吉林省莫莫格泡1500年来的孢粉组合与古环境

介冬梅1,2, 王升忠1, 郭继勋1, 吕金福1, 李津1   

  1. 1. 东北师范大学城市与环境学院地理系, 国家草地工程实验室, 长春 130024;
    2. 吉林大学地球科学学院, 长春 130061
  • 收稿日期:2003-07-16 修回日期:2003-11-05
  • 通讯作者: 介冬梅,女,1969年生,博士后,副教授,主要从事第四纪环境学和古生态学研究,已发表论文20余篇.Tel:0431-5683097;E-mail:Jiedongmei@nenu.edu.cn
  • 基金资助:
    国家自然科学基金资助项目(49671077,40201052)

Pollen combination and paleo-environment of Momoge Lake since 1500 years before

JIE Dongmei1,2, WANG Shengzhong1, GUO Jixun1, LÜ Jinfu1, LI Jin 1   

  1. 1. Geography Department Institute of Grassland Engineering, Northeast Normal University, Changchun 130024, China;
    2. School of Earth Science, Jilin University, Changchun 130061, China
  • Received:2003-07-16 Revised:2003-11-05

摘要: 通过对莫莫格泡人工剖面14个样品的孢粉分析笔者划分了3个孢粉带:孢粉贫乏带、蒿-藜麻黄孢粉带和蒿-藜孢粉丰富带,根据孢粉组合,14C测年和沉积相的综合分析认为莫莫格泡是1500aB.P.由古河道洼地为砂丘所堵塞形成的,它经历了河湖转换期、湖泊发育早期和湖泊稳定期,其周围植被由菊科蒿-藜草甸草原逐渐过渡为蒿藜为主的疏林草甸草原和草甸草原,古气候由冷干、温凉偏干向温凉转化,近50年来有暖干化趋势.

关键词: 莫莫格泡, 古植物群落, 孢粉记录, 古环境演变

Abstract: Based on the pollen combination, 14C dating,and depositional facies analysis of Momoge profile in Zhenlai County,Jilin Province,three pollen belts were divided.The results showed that Momoge Lake was formed by blocked paleo-river course depression 1500 years ago,which included three development stages,i.e.,the period when river converted into lake,the early period of lake development,and the steady period.Its corresponding plant types were Artemisia-Chenopodium grassland,Artemisia-Chenopodium grassland accompanied by Betula,and meadow grassland,and its paleo-climate was dry-cold,warm-dry,and then cool-wet,and there was a warm-dry tendency in recent fifty years.

Key words: Momoge Lake, Paleo-plant community, Pollen record, Paleo-environment evolution

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