THE CLIMAX OF LANGYA MOUNTAIN AND THE ZONAL VEGETATION OF JIANGHUAI AREA

Expand
  • Department of Environmental Science, East China Normal University, Shanghai 200062

Received date: 1993-03-01

  Online published: 1994-05-20

Abstract

The forest of Langya Mountain has been well protected. Qu Zhongxiang studied it in 1953,and we investigated the forest in 1992.Comparing Qu’s data with that of ours, we consider that the forest of Langya Mountain will develop into Pteroceltis-Zelkova-Platycarya-Acer-Paliurus Forest.This paper indicates the zonal vegetation of the area between the Changjiang and the Huaihe in Jiangsu and Anhui Province should be deciduous broad-leaf forest and "the area"should belong to the warm temperate deciduous broad-leaf forest region.

Cite this article

Yan Chuanhai . THE CLIMAX OF LANGYA MOUNTAIN AND THE ZONAL VEGETATION OF JIANGHUAI AREA[J]. SCIENTIA GEOGRAPHICA SINICA, 1994 , 14(3) : 233 -239 . DOI: 10.13249/j.cnki.sgs.1994.03.233

References

[1] 曲仲湘,文振旺.邢娜山林木现况的分析.植物学报,1953.2(3):349~370.
[2] 曲仲湘,文振旺,朱克贵.南京灵各寺森林现况的分析.植物学报,1952,1(1),18~49.
[3] 熊文愈,韩福庆,姚琢.南京灵各寺森林的变化分析.南京林产工业学院学报,1983(2):1~23.
[4] 中国植被编委会.中国植被.北京:科学出版社,1980. 838~847.
[5] 刘防助,黄致远.江苏地带性植被的基本特点与分布规律.植物生态学与地植物学丛刊,1982,6(3):236~246.
[6] 韩也良.安徽省境内亚热带常绿阔叶林带的北界问题(摘要).植物生态学与地植物学丛刊,1981.5(1):54~57.
[7] 竺可桢.中国近五千年来气候变迁的初步研究.考古学报,1972(1):168~188.
[8] 龚高法,张王远,张瑾瑢.历史时期我国气候带的变迁及生物分布界线的推移.历史地理.第五期,1988. 1~10.
[9] 张王远,龚高法.十六世纪以来中国气候变化的若干特征.地理学报,1979,34(3):238~247.
[10] 龚高法,张王远,张瑾瑢.十八世纪我国长江下游等地区的气候.地理研究,1983,2(2):20~33.
[11] 竺可祯.中国的亚热带.科学通报,1958(17):524~528.
[12] 侯学煜.试论历次中国植被分区方案中所存在的争论性问题.植物生态学与地植物学丛刊,1963,1(1-2): 1~23.
[13] 周光裕.试论“北亚热带常绿落叶阔叶林带”的归属间题.山东大学学报(自然科学版).1980(1):108~119.
[14] 中国自然地理编委会.中国自然地理.气候.北京:科学出版社,1980. 151~158.
Outlines

/