中山大学生物系
纸质出版:1995
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[1]潘晓玲,张宏达.柴达木盆地植物区系分析及其形成的探讨[J].新疆大学学报(自然科学版),1995(01).
潘晓玲, 张宏达. 柴达木盆地植物区系分析及其形成的探讨[J]. Journal of Xinjiang University (Natural Science Edition in Chinese and English), 1995, (1).
柴达木盆地植物区系以古地中海成分占主要地位.本区系中的中亚成分同样是古地中海区系的一部分.其中的温带成分是由华夏植物区系发展起来的.并与安加拉区系有联系.区系中的喜马拉雅成分是当地起源的.它们是本区系中的年青成员.无疑是华夏区系的后裔.而一定数量的特有成分则表明了区系的特殊性.柴达本盆地的植物区系虽然经历了干旱到湿润、湿润到干旱的反复交替.但有充足的抱粉资料证明:现代的柴达木盆地干旱植物区系在第三纪时就已形成.且一直处于干旱、寒冷的气候控制之下.
The element of Tethys is very important in the flora of Tsaidam Basin. Since the regression of Tethys and the rising of elevation
the Climate of environment had become dry and cold
it has formed in this locality. identically
the element of Central Asia is a part of Tethys flora too. The element of temperate in this flora was formed by Cathayslan flora
and connected with Angola flora. The element of Himalaya was formed in this locality
It is the J bungest nelnber in this flora
indubltatlvely. it is the descendants of cathaysian flora. The being of the element of Endemic to China special properties of this flora.Although the flora in Tsaidam Basin
had undergone from aridity to moisture and from moisture to aridity
exchanging repeatedly
there are many evidences of pollen
which fully prove: the xerophytic flora from modern Tsaidarn Basin had formed in Quaternary
and was controled straight by the dry and cold climate.
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