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晚更新世晚期以来昆仑山垭口区的植被与环境
张宁佳1; 许清海1; 李文漪2; 王子惠1; 崔之久3; 阳小兰1
1996
Source Publication微体古生物学报
ISSN1000-0674
Volume013Issue:004Pages:387
Abstract昆仑山垭口区小南川剖面和雪水河热水剖面的孢粉分析揭示了该区44000aB.P.以来的植被演替和气候变化。40000aB.P.前,推测昆仑山垭口区为典型的灌木荒漠植被,气候极端干燥。40000-30000aB.P.,气候稍有好转。30000-24000aB.P.为草原荒漠,降水增加。24000-18000aB.P.为末次冰期极盛期,气候干冷。18000-13000aB.P.气候凉偏干。13000-8
Language英语
Document Type期刊论文
Identifierhttp://ir.igsnrr.ac.cn/handle/311030/128640
Collection中国科学院地理科学与资源研究所
Affiliation1.河北省地理科学研究所
2.中国科学院地理科学与资源研究所
3.北京大学
Recommended Citation
GB/T 7714
张宁佳,许清海,李文漪,等. 晚更新世晚期以来昆仑山垭口区的植被与环境[J]. 微体古生物学报,1996,013(004):387.
APA 张宁佳,许清海,李文漪,王子惠,崔之久,&阳小兰.(1996).晚更新世晚期以来昆仑山垭口区的植被与环境.微体古生物学报,013(004),387.
MLA 张宁佳,et al."晚更新世晚期以来昆仑山垭口区的植被与环境".微体古生物学报 013.004(1996):387.
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