地理科学 ›› 1994, Vol. 14 ›› Issue (2): 186-192,200.doi: 10.13249/j.cnki.sgs.1994.02.186

• 研究报道 • 上一篇    下一篇

长白山岳烨林带泥炭沼泽孢粉分析及其意义

许清海1, 王子惠1, 徐全洪1, 夏玉梅2   

  1. 1. 河北省科学院地理研究所 石家庄050011;
    2. 中国科学院长春地理研究所 长春130021
  • 收稿日期:1993-09-01 出版日期:1994-03-20 发布日期:1994-03-20
  • 基金资助:
    国家自然科学基金资助课题.

POLLEN ANALYSIS OF PEAT MARSH IN BIRCH FOREST,THE CHANGBAI MOUNTAINS AND THE SIGNIFICANCE

Xu Qinghai1, Wang Zihui1, Xu Quanhong1, Xia Yumei2   

  1. 1. The Institute of Geography, Hebei Academy of Sciences, Shijiazhuang, 050011;
    2. Changchun Institute of Geography, Academia Sinica, Changchun, 130021
  • Received:1993-09-01 Online:1994-03-20 Published:1994-03-20

摘要: 长白山岳桦林带赤池泥炭沼泽堆积开始于3400aBP.前后,其周围植被有过针叶林和岳桦林的交替过程.长白山地区于3400a B.P.前气温已开始下降;3400~2200a B.P.为相对温暖时期;2200a B.P.之后气温下降加快;1800a B P.以后气温冷暖交替变化.

Abstract: Pollen analysis and 14C dating of Chichi peat marsh in Betula ermanii forest, the Changbai Mountains show that the peat deposit of the marsh probably accumulated after 3400aB. P. There might be vegetation succesion between dark coniferous forest and Betula ermanii forest there since then. The palaeoclimate estimated from major factor anal-ysis of pollen data reveals that the climate had begun to descent before 3400aB. P. It was a relative warm period between 3400-2200aB. P. Then the climate declined rapidly and reached the lowest level in 1800aB. P. Later,it changed alternatively in warm and cool. The comparatively warm periods were respectively 1200,800 and 200aB. P.,and relative cool periods 1000 and 400aB. P.