Project/Area Number |
20340138
|
Research Category |
Grant-in-Aid for Scientific Research (B)
|
Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Geology
|
Research Institution | Shimane University |
Principal Investigator |
SETO Koji Shimane University, 汽水域研究センター, 准教授 (60252897)
|
Co-Investigator(Kenkyū-buntansha) |
SATO Takaharu 広島大学, 総合科学研究科, 准教授 (90196246)
TANAKA Satoshi 京都教育大学, 教育学部, 准教授 (00252536)
NOMURA Ritsuo 島根大学, 教育学部, 教授 (30144687)
IRIZUKI Toshiaki 島根大学, 総合理工学部, 准教授 (60262937)
YAMAGUCHI Keiko 島根大学, 生物資源科学部, 准教授 (80322220)
SAMPEI Yoshikazu 島根大学, 総合理工学部, 准教授 (00226086)
|
Project Period (FY) |
2008 – 2010
|
Project Status |
Completed (Fiscal Year 2010)
|
Budget Amount *help |
¥18,460,000 (Direct Cost: ¥14,200,000、Indirect Cost: ¥4,260,000)
Fiscal Year 2010: ¥4,550,000 (Direct Cost: ¥3,500,000、Indirect Cost: ¥1,050,000)
Fiscal Year 2009: ¥5,330,000 (Direct Cost: ¥4,100,000、Indirect Cost: ¥1,230,000)
Fiscal Year 2008: ¥8,580,000 (Direct Cost: ¥6,600,000、Indirect Cost: ¥1,980,000)
|
Keywords | 第四紀学 / 海跡湖 / 汎世界的な環境変動 / 人為的環境変化 / 古環境変化 / 中海 / 能取湖 / 藻琴湖 / 濤沸湖 / 中海本庄水域 / 浜名湖 |
Research Abstract |
Antarctic region shows dry climate during the little ice age. After that, climate changed to relative wet condition in this area. In the coastal area of the Sea of Okhotsk in the east part of Hokkaido located to for subarctic zone, distinguished paleoenvironmental changes are not observed except for anthropogenic environment change. The closure or reduction of lake mouth is observed in Lake Tofutsu. This is suggest the slightly fall of sea level. In the coastal area of the Japan Sea located to for temperate zone, the flood sediments are observed around the end of little ice age (AD1600-1800). After that, anthropogenic environment changes are distinguished in this area.
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