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http://dx.doi.org/10.5141/JEFB.2005.28.1.037

Vegetation History since the Mid-Lateglacial from Yeongsan River Basin, Southwestern Korea  

Choi, Kee-Ryong (Dept. of Biological Sciences, University of Ulsan)
Kim, Ki-Heon (Dept. of Biological Sciences, University of Ulsan)
Kim, Jong-Won (Dept. of Biology, Keimyung University)
Kim, Jong-Chan (Dept. of Physics, Seoul National University)
Lee, Gi-Kil (Dept. of History, Chosun University)
Yang, Dong-Yoon (Dept. of Biological Sciences, University of Ulsan)
Nahm, Wook-Hyun (Korea Institute of Geoscience and Mineral Resources)
Publication Information
The Korean Journal of Ecology / v.28, no.1, 2005 , pp. 37-43 More about this Journal
Abstract
This study presents the Mid-Lateglacial vegetation history of southwestern Korea. From the result of AMS dating and pollen analysis, four local pollen assemblage zones(BS) were recognized. The four local pollen assemblage zones are BS 1. 12,222cal BC$\sim$9,160cal BC: cool-temperate northern/altimontane mixed coniferous & deciduous broad-leaved forest, BS 2. 9,160cal BC$\sim$ 4,210cal BC: cool-temperate central/montane deciduous broad-leaved forest, BS 3. 4,210cal BC$\sim$125cal BC: cool-Temperate southern/submontane mixed coniferous & deciduous broad-leaved forest. BS 4. BC125cal ${\sim}$present: warm-temperate/cool-temperate southern/submontane coniferous forest. Pine forest expanded since 4,210cal BC and full-scale rice cultivation might started since 2,120cal BC. A radical expansion of Pinus densiflora forest after postglacial stage might be caused by human impacts including full-scale agriculture.
Keywords
Lateglacial; Pollen analysis; Postglacial; Rice cultivation; Vegetation history;
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