摘要
Ecological investigation has been done in some saline lakes in the Vestfold Hills (60°38’S, 78°06’ E), East Antarctica. The results show that changes of natural environment and physicalchemical factors, as well as the structure of biotic species and succession do occur in some lakes, due to seasonal and local climate changes and geographic variances in regions. These should be strong ecological proofs to explain that the processes of globle climate change and ice sheet retreating, and isostatic uplift raising, could be continueing in present time, and should be significant to the study on Antarctic and global changes.
Ecological investigation has been done in some saline lakes in the Vestfold Hills (60°38'S, 78°06' E), East Antarctica. The results show that changes of natural environment and physicalchemical factors, as well as the structure of biotic species and succession do occur in some lakes, due to seasonal and local climate changes and geographic variances in regions. These should be strong ecological proofs to explain that the processes of globle climate change and ice sheet retreating, and isostatic uplift raising, could be continueing in present time, and should be significant to the study on Antarctic and global changes.
出处
《冰川冻土》
CSCD
北大核心
1998年第4期451-457,共7页
Journal of Glaciology and Geocryology
