충남 아산 곡교천 유역의 제4기 후기 화분분석 -최종빙기 최성기∼만빙기 식생 및 기후환경에 주목하여- = The Late Quaternary Pollen Analysis of Gokgyo River Basin in Asan-City, Korea -Focused on Vegetation and Climate Environment between the Last Glacial Maximum and the Late Glacial-

다국어 초록 (Multilingual Abstract)

The pollen analysis was performed targeting the valley plain alluvium of Jangjae-ri, Asan area in order to clarify the climate and vegetation environment of the Last glacial maximum and the Late glacial in terms of Gokgyo River Watershed In Asan-City, Korea. The sample collection point gets included in the current deciduous broadleaf forest zone (south cool temperate zone). The results are as follows. ① The vegetation environment of about 19,300-14,100yrB.P. at the investigation area is mainly classified into YJ-I period and YJ-Ⅱ period while YJ-Ia period is classified once again into YJ-Ia period and YJ-Ib period. YJ-Ia period (19,300-17,500yrB.P.) is correlated with the Last Glacial Maximum while the vegetation at the time has relatively a little wide distribution area of grassland compared to the forest and the forest vegetation of this time period is the mixed conifer and deciduous broad-leaved forest. YJ-Ib period (15,400-14,750yrB.P.) is correlated with the Late glacial (or the Last Glacial Maximum) and the distribution area of grassland became wider compared to the forest. While the forest vegetation of this time period is the mixed conifer and deciduous broad-leaved forest, a difference exists in terms of the dominant tree species. YJ-Ⅱperiod (about 14,650-14,100yrB.P.) is correlated with the Last glacial while the distribution area of grassland became even wider than the forest compared to the YJ-Ib in case of the vegetation at the time and the forest vegetation of this time period is the coniferous forest. ② Both YJ-I period and YJ-Ⅱ period were relatively cold and dry compared the End of Late Glacial (about 12,000-10,000yrB.P.)∼Early Holocene (10,000-8,500yrB.P.), Also, YJ-Ⅱ period was relatively colder than the YJ-I period and the YJ-Ib period was relatively more humid than the YJ-Ia period.