吉林大学学报(地球科学版) ›› 2020, Vol. 50 ›› Issue (1): 170-184.doi: 10.13278/j.cnki.jjuese.20180337

• 地质与资源 • 上一篇    

植硅体记录的敦化北部山地近2 ka泥炭沼泽演化气候背景

杜玉1,2,3, 张新荣1,2,3, 平帅飞1,2,3, 焦洁钰1,2,3, 马春梅4   

  1. 1. 吉林大学地球科学学院, 长春 130061;
    2. 吉林大学东北亚生物演化与环境教育部重点实验室, 长春 130026;
    3. 吉林省油页岩与共生能源矿产重点实验室, 长春 130061;
    4. 南京大学地理与海洋科学学院, 南京 210023
  • 收稿日期:2018-12-20 发布日期:2020-02-11
  • 通讯作者: 张新荣(1975-),女,副教授,博士,主要从事沉积学与第四纪地质学研究,E-mail:zhangxr@jlu.edu.cn E-mail:zhangxr@jlu.edu.cn
  • 作者简介:杜玉(1994-),女,硕士研究生,主要从事沉积学与第四纪地质学研究,E-mail:m15546115261@163.com
  • 基金资助:
    国家自然科学基金项目（41371202）

Climate Background of Peat Swamp Evolution Recorded by Phytolith over Past 2 ka in Northern Mountainous Area in Dunhua

Du Yu1,2,3, Zhang Xinrong1,2,3, Ping Shuaifei1,2,3, Jiao Jieyu1,2,3, Ma Chunmei4   

  1. 1. College of Earth Science, Jilin University, Changchun 130061, China;
    2. Key-Laboratory for Evolution of Past Life and Environment in Northeast Asia, Ministry of Education, Changchun 130026, China;
    3. Key Laboratory of Oil Shale and Coexistent Enerny Minerals of Jilin Province, Changchun 130061, China;
    4. School of Geography and Ocean Science, Nanjing University, Nanjing 210023, China
  • Received:2018-12-20 Published:2020-02-11
  • Supported by:
    Supported by National Natural Science Foundation of China (41371202)

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摘要： 对敦化北部山地205 cm深泥炭剖面中的植硅体进行提取、鉴定和分析，结合AMS14C测年，重建研究区近2 ka的古气候环境过程，探讨其变化规律及影响因素。植硅体组合、有序聚类和植硅体指数变化趋势显示，研究区泥炭沼泽经历了4个显著阶段：即45-680 A.D.暖湿阶段；680-1340 A.D.温暖偏干阶段；1340-1870 A.D.由干转湿的寒冷阶段；1870-2017 A.D.转暖、干湿波动阶段。其中，680-1225 A.D.对应中世纪暖期（MWP），1340-1870 A.D.对应小冰期（LIA）。在此气候变化背景下，泥炭沼泽发展经历了由缓慢逐渐加快的过程。对比太阳辐射和太阳活动的变化、石笋δ18O序列、重建的东北地区古温度以及Niño3.4重建曲线，泥炭剖面的植硅体分析显示MWP和LIA期间的古气候过程受到太阳活动、太阳辐射、季风环流和ENSO（El Niño-Southern Oscillation）的控制。

关键词: 植硅体, 泥炭演化, 气候变迁, 区域差异, 敦化山地

Abstract: Based on the AMS14C dating and the phytoliths extracted from the 205 cm peat profile in the northern part of Dunhua, the paleoclimate environmental progresses of the study area near 2 ka were reconstructed,and the changing rules and influencing factors were discussed. The phytolith assemblages, ordered cluster analysis, and phytolith indexes showed that the peat swamp in the studied profile had experienced four significant stages:45-680 A. D. warm and wet stage; 680-1340 A. D. warm and dry stage; 1340-1870 A. D. cold and dry to wet stage; 1870-2017 A. D. warm, dry, and wet fluctuation stage. The paleoclimate condition in 680-1225 A. D. was similar to that in the Medieval Warm Period (MWP), and the condition in 1340-1870 A. D. was similar to that in the Little Ice Age (LIA). In such a climate context, the peat swamp developed a slow to gradually accelerated period. Compared with solar irradiation, stalagmite δ18O sequence,Niño3.4, and the paleotemperature reconstruction in Northeast China, the phytolith analysis in the studied peat profile indicated that the paleoclimate process during MWP and LIA was controlled by solar activity, solar irradiation, monsoon circulation, and ENSO (El Niño-Southern Oscillation).

Key words: phytolith, peat swamp evolution, climate changes, regional differences, moutainous area in Dunhua

中图分类号: 

  • P532
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