Palynological Evidence on Climate Changes in the East China Sea During Mid and Late Holocene-中国期刊网

摘要 ThepollenanalysisofDGKS9617coreintheEastChinaSea(coveringaboutthelast6800years)showsfiveobviouspollenassemblagesandsevensub-assemblages.Combinedwiththesedimentandtheresultofdiatomanalysis,theclimatechangesarereconstructedduringtheMiddleandLateHolocene.Correspondingtothepollenassemblages,theclimateshiftsjustasfollows:AssemblageⅠ-WarmandDryStage,AssemblageⅡ-CoolandHumidStage,AssemblageⅢ-HotandDryStage(themeanannualtemperatureis2～3℃higherthanthattoday),AssemblageⅣ-CoolandHumidStage,AssemblageⅤ-WannandDryStage.Thethirdstageisdividedintothreesubstagesi.e.aslightcolderanddryone,aslightwannerandhumidoneandaslightwarmeranddryone.Duringthefifthstage,theclimatebecomessimilartothattodaywiththreewarmsubstagesandtwocoolsubstages.

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Palynological Evidence on Climate Changes in the East China Sea During Mid and Late Holocene

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Palynological Evidence on Climate Changes in the East China Sea During Mid and Late Holocene

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