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- W2364931243 abstract "In order to probe into the vegetation succession and environmental transition of Milin region during the Late Pleistocene,a measured section nearby the Milin airport,Southern of Tibetan Plateau,was carried out.The sediment of Milin section represents a set of lake sedimentary facies in the late stage of Late Pleistocene.The age of the sediment is between 40-12 kaBP by the test of 14C.According to the pollen analysis from bottom to up,this section is divided into four sporo-pollen assemblage belts and the corresponding four vegetation succession stages of development.(1) the first stage(corresponding with sporo-pollen assemblage belt I;36-28 kaBP): the forest meadow vegetation type;(2) the second stage(corresponding with sporo-pollen assemblage belt Ⅱ;28-23 kaBP): the alpine grassland vegetation type;(3) the third stage(corresponding with sporo-pollen assemblage belt Ⅲ;23-18 kaBP): the Artemisia grassland vegetation type;(4) the fourth stage(corresponding with sporo-pollen assemblage belt Ⅳ;16-13 kaBP): the desert grassland vegetation type.Based on these analysis,it indicats that from 40 KaBp to Holocene the climate of the southern Tibetan Plateau is in general cold and drought with small fluctuations,and it has good coherence with global glacial stage and interglacial stage." @default.
- W2364931243 created "2016-06-24" @default.
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- W2364931243 date "2013-01-01" @default.
- W2364931243 modified "2023-09-25" @default.
- W2364931243 title "Vegetation Succession and Environmental Transition During Late Pleistocene in Milin Area,Tibetan Plateau" @default.
- W2364931243 hasPublicationYear "2013" @default.
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