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- W2380218319 abstract "Peatland of Yangmu in Mishan region is located at45°34′N,132°2 3′E. 5 spore pollen zones are divided throngh the spore pollen analysis. The change process of paleovegetation and paleoclimate was obtained. Warm- inclined broad- leaved forest predom inated in the environment of warm climate with a little dry climate before34 0 0 a B.P..Deciduous broad- leaved and conferous mixed forestpredominated,in which Pinus, Picea and Abies were main speries,together with wet meadow in the environiment of the cool and wet climate during34 0 0～ 1940 a B.P..Deciduous broad- leaved and coniferous mixed forestpredominated in the environmentof dry and warm clim ate from1940 to10 90 a B.P..Broad- leaved forest was predominant,and the climate was the warm and wetfrom 10 90～ 5 45 a B.P..Bog m eadow predominated when the climate changed to cool and dry from5 45 a B.P.. The compostion of the upper part of the143～ 12 5 cm peat profile presented the cold period in the early of Christian era through the mutual identification between the records of historical material such as spore pollen,magnetization rate,organic matter,and archaeology study.The composition of the parts of12 5～ 85 cm and85～ 38cm presented the warm climate in Nan Bei Dynasty and Sui- Tang Dynasty.Since34 0 0 a B.P.for the reason of frequent human activites in Mishan region,the amunt of cultural relics in Sui- Tang Dynasty increased,which represented thatancient man took much more woods from the forest,while it was in an environment of warm climate." @default.
- W2380218319 created "2016-06-24" @default.
- W2380218319 creator A5091551174 @default.
- W2380218319 date "2000-01-01" @default.
- W2380218319 modified "2023-09-25" @default.
- W2380218319 title "Peat record of climate change sincce 3000 years in Yangmu,Mishan region" @default.
- W2380218319 hasPublicationYear "2000" @default.
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