Journal of Jilin University(Earth Science Edition) ›› 2020, Vol. 50 ›› Issue (1): 170-184.doi: 10.13278/j.cnki.jjuese.20180337

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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)

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

CLC Number: 

  • P532
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