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Pollen assemblage and palaeo-vegetation of Late Holocene fen in Dunhua of Jilin Province

ZHAO Hongyan1,2;ZHOU Daowei1   

  1. 1Key Laboratory for Ecological Restoration & Ecosystem Management of Jilin Province,Northeast Normal University,Changchun 130024,China;2State Environment Protection Key Laboratory of Wetland Ecology & Vegetation Restoration,Northeast Normal University,Changchun 130024,China

  • Received:2005-03-21 Revised:2003-09-02 Online:2006-02-18 Published:2006-02-18

Abstract: Based on the study of pollen,stratum and 14C dating of Daqiao fen in Dunhua of Jilin Province,four pollen zones were distinguished, i.e.,Pinus-Picea-Abies assemblage (2 195±70~2 045±70 B.P.),Carex-Pinus-Betula-Corylus-Juglans assemblage (2 045±70~1 745±70 B.P.),Pinus-Corylus-Carpinus-Carex-Ranunculus assemblage (1 745±70~705±70 B.P.),and Pinus-Picea-Abies-Betula-Carex assemblage (705±70~1 950 AD).The vegetation changed from coniferous forest (similar to the vegetation currently found over 1 100 m a.s.l.in this area),through conifer-broad-leaved mixed forest (similar to the vegetation currently found between 400~600 m a.s.l.) and conifer-broad-leaved mixed forest (similar to the vegetation currently found between 600~800 m a.s.l.),to conifer-broad-leaved mixed forest (similar to the vegetation currently found between 800~ 1 100 m a.s.l.).Accordingly,Daqiao fen underwent the periods of gestation,fast development,expansion,and dieing out.

Key words: Phosphorus efficiency, Plant, High phosphorus use efficiency, Genotypes, Mechanism