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28,055,000 Yen
The Holocene coastal sediments of the Nokke-zaki and Saroma lake in Hokkaido facing the sea of Okhotsk are characterized by somewhat warmer conditions(2℃ to 3℃) and a higher sea level(possibly up to 5m) which may represent useful analogues for future changes in the present interglacial epoch. Resultant changes in the coastal geomorphology and ecosystem offers an appropriate scenario for the next century in the coastal region of the northwestern Pacific.
Holocene, Sea level changes, Saroma lake, Nokke-zaki cape, PAGES