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

doi:10.13278/j.cnki.jjuese.20180337

Abstract

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

Du Yu, Zhang Xinrong, Ping Shuaifei, Jiao Jieyu, Ma Chunmei. Climate Background of Peat Swamp Evolution Recorded by Phytolith over Past 2 ka in Northern Mountainous Area in Dunhua[J].Journal of Jilin University(Earth Science Edition), 2020, 50(1): 170-184.

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

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