J4 ›› 2003, Vol. 5 ›› Issue (2): 217-223. doi: 10.7605/gdlxb.2003.02.009

• 第四纪古地理学及沉积学 • 上一篇    下一篇

云南西部羊邑和龙陵地区晚上新世植被和古气候

徐景先    王宇飞   杜乃秋   

  1. 1中国科学院植物研究所 北京 100093
    2中国科学院地球环境研究所黄土与第四纪地质国家重点实验室 陕西西安 710075
  • 出版日期:2003-04-01 发布日期:2003-04-01
  • 作者简介:Xu Jingxian, born in 1974, graduated from Institute of Botany, Chinese Academy of Sciences and obtained Ph.D. degree in 2002. Now he is engaged in palynology and palaeoecology at the Institute of Earth Environment, Chinese Academy of Sciences as a post-doctor.

Late Pliocene vegetation and palaeo climate of Yangyi and Longling of western Yunnan Province

Xu Jingxian  Wang Yufei   Du Naiqiu   

  1. 1Institute of Botany, Chinese Academy of Sciences, Xiangshan, Beijing 100093
    2State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi’an 710075, Shanxi
  • Online:2003-04-01 Published:2003-04-01
  • About author:徐景先,男,1974年出生,2002年毕业于中国科学院植物研究所,获得博士学位。现为中国科学院地球环境研究所博士后,从事孢粉学和古生态学研究。

摘要:

云南西部羊邑和龙陵地区晚上新世孢粉组合均以被子植物占优势,蕨类和裸子植物次之,藻类类群少。龙陵孢粉组合比羊邑孢粉组合含有更丰富的亚热带被子植物成分;裸子植物类群相对较少;蕨类类群较多,但孢子含量低。与研究地区现生植被对比研究的结果显示羊邑孢粉组合的大部分类群来自常绿针阔叶混交林,现在分布于羊邑地区海拔2800—3100m的地带,其余部分来自海拔3200m以上的云冷杉林;而龙陵孢粉组合的大部分类群来自山地湿润常绿阔叶林,分布于今日龙陵地区海拔1600—2500m的地带,其余部分来自海拔2300—2900m的常绿针阔叶混交林。这些云南西部晚上新世植被反映了湿润的亚热带山地立体气候。

Abstract:

 Late Pliocene palynofloras of both Yangyi and Longling are dominated by angiosperms, along with a moderate number of ferns and gymnosperms, and a few algae. Compared with Yangyi playnoflora, Longling palynoflora contains more abundant subtropical elements of angiosperms, more ferns and less gymnosperms. Based on comparison with the vertical zones of modern vegetations, most elements of Longling palynoflora derived from the montane humid evergreen broad-leaved forest at elevation of 1600—2500m, with less contributions of the evergreen coniferous and broad-leaved mixed forest from 2300 to 2900m, whereas most of Yangyi palynoflora derived from the evergreen coniferous and broad-leaved mixed forest at elevation of 2800—3100m, with less contributions of evergreen coniferous forest above 3200m. Both Late Pliocene vegetations reflect a mountain subtropical climate with humidity.