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- W2369710902 abstract "One continuous glacio-lacustrine sedimentary deposits, Laotanfang located on the southern side of Hulifang peak of Xiaojiang river, Yunan province were studied here in. Using grain size, environmental magnetic susceptibility and pollen analysis, together with the 14C dating methods, the climatic environmental change since the Holocene epoch was discussed. The results reflected that the climate fluctuated in different stages during the Holocene, that is, the climate was cool and wet during 8.4～7.7ka with average grain size of 5.46φ and low frequency magnetic susceptibility(Xlf)1.62～3.88μm3kg-1; Cold and wet during 7.7～6.5ka with average grain size of 5.95φand Xlf of 1.44～2.28μm3kg-1; Cold and dry during 6.5～4.7ka with average grain size of 5.83φand Xlf of 1.53～3.65μm3kg-1; Cool and wet during 4.7～2.1 ka with average grain size of 5.91φand Xlf of 2.0～5.2μm3kg-1; Warmer and wet since the 2.1 ka with average grain size of 5.63φand Xlf of 5.63φ; Results reflect that the study area was influenced by both the southwest and southeast monsoons of different stages during Holocene." @default.
- W2369710902 created "2016-06-24" @default.
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- W2369710902 date "2008-01-01" @default.
- W2369710902 modified "2023-09-28" @default.
- W2369710902 title "CLIMATIC ENVIRONMENTAL CHANGE DURING HOLOCENE IN GONGWANGSHAN, NORTHEAST OF YUNNAN PROVINCE" @default.
- W2369710902 hasPublicationYear "2008" @default.
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