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KMID : 0368419820250010037
Journal of Plant Biology
1982 Volume.25 No. 1 p.37 ~ p.53
Late-Quaternary Vegetation in the Lake of Korea
Chang Cheong-Hee

Kim Choon-Min
Abstract
Pollen analysis from lake districts, Youngnangho, Wolhamji and Bangeojin, revealed vegetational patterns in Korea. The pollen stratigraphy was divided into five zones, zone L, ¥°, ¥±, ¥²a and ¥²b for the past 15,000 years. During zone L (earlier than 10, 500 yr BP), late-glacial period, Youngnangho was vegetated with a coniferous forest dominated by spruce, larch, haploxylon pine and fir with considerable amount of herbs. Zone ¥°(10,5000¡­7,500 yr BP) was predominantly herbaceous vegetarion with significant amount of oak and diploxylon pine. It suggests that the overall environment became milder and drier than late-glacial period. Zone ¥± (7,500¡­4,000 yr BP), hypsithermal period, showed significant warming condition, indicated by high pollen concentrations of oak, diploxylon pine and hornbeam, and by more diverse flora of deciduous broad-leaved trees than before. Herbs were not an improtant part of vegetaion. Zone ¥²a(4,000¡­1,500 yr BP) had pine and oak as main elements. Birch increased slightly while hornbeam decreased in this time. It indicates cooling condition. Zone ¥²b (1,5000-present) which can be called pine period showed obvious human interference. Following forest clearance, agriculture was intensified. The beginning of logging and agriculture was discernible by a sudden decline of arboreal species and by considerable amount of rice, buckwheat, sorrel and plantain. Numerous charcoal fragments were observed in zone ¥° and zone ¥²b.
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