| Project/Area Number |
08041033
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| Research Category |
Grant-in-Aid for international Scientific Research
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| Allocation Type | Single-year Grants |
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| Section | Field Research |
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| Research Field |
考古学(含先史学)
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| Research Institution | NATIONAL MUSEUM OF JAPANESE HISTORY |
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Principal Investigator |
TSUJI Sei-ichiro NATIONAL MUSEUM OF JAPANESE HISTORY,HISTORY DEPARTMENT,ASS.PROF., 歴史研究部, 助教授 (20137186)
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| Co-Investigator(Kenkyū-buntansha) |
NISHIMOTO Toyohiro NATIONAL MUSEUM OF JAPANESE HISTORY,ARCHAEOLOGY DEPARTMENT,ASS.PROF., 歴史研究部, 助教授 (70145580)
NOSHIRO Shuichi THE MINISTRY OF AGRICULTURE,FORESTRY & FISHERIES,FORESTRY & FOREST PRODUCT RESEA, 森林総合研究所, 主任研究官
MINAKI Mutsuhiko UNIVERSITY OF MARKETING & DISTRIBUTION SCIENCE,PROF., 商学部, 教授 (80209824)
SUZUKI Mitsuo TOHOKU UNIVERSITY,FACULTY OF SCIENCE,PROF., 大学院・理学研究科, 教授 (80111483)
MAEDA Ushio TSUKUBA UNIVERSITY,INSTITUTE OF HISTORY & ANTHROPOLOGY,ASS.PROF., 歴史・人類学系, 助教授 (40015897)
VASILEVSKI A ユジノ=サハリンスク教育大学, 助教授
GOLUBEV Vale ユジノ=サハリンスク教育大学, 教授
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| Project Period (FY) |
1996 – 1997
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| Project Status |
Completed (Fiscal Year 1997)
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| Budget Amount *help |
¥4,900,000 (Direct Cost: ¥4,900,000)
Fiscal Year 1997: ¥2,500,000 (Direct Cost: ¥2,500,000)
Fiscal Year 1996: ¥2,400,000 (Direct Cost: ¥2,400,000)
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| Keywords | VEGETATION HISTORY / BURIED FOREST / FOREST PEAT / LAST GLACIAL AGE / PALEOVEGETATION / DENDROCHRONOLOGY |
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| Research Abstract |
The relationship between human and nature in the coastal regions since the Jomon Transgression in the southern Skhalin was studied based on the geological, chronological, geomorphological, and archaeological investigations. We showed that the peopling of Epi-Jomon, Okhotsk.Satsumon, Ainu continuously occurred along inland lake-side or river-side on the lake or river terrace after the formation of sand dune. Stratigarphy and chronology of the Kurosuna and charcoal sediments intercalated the dune sand showed occasional forest fire during the time of formation of sand dune in prehistory.
We found the continuous peat deposit around the last 12,000 years in the south coast of the Bawai Lake along the Aniwa Bay in southern Sakhalin. The high precision carbon datings and paleobotanical analyzes showed the drastic vegetational change from a glacial environment to the coniferous forest around 12,000 yr BP,an increasing of prentiful tree and herbaceous species around 10,000 yr BP.a climatic deterioration or drastic climatic changes around 5,000 and 2,000 yr BP.
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