南太平洋, 東ポリネシアの完新世海面変化―温暖化に伴う海岸環境変化の自然史的背景―
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概要
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Holocene sea-level changes have been mainly discussed in the light of two points of view: whether eustatic highstand of sea level existed or not, and whether eustatic sea level has fluctuated or not. While extensive regional differences of sea-level heights, which have ever been elucidated, can be geophisically interpreted, various factors are responsible for local sea level heights. Hydro-isostasy, volcanic loading, tectonic movements and sea-temperature change etc. are considered to be responsible for the Holocene highstands and sea-level fall, which have been extensively recognized in the southern Cook islands. Studies on Holocene sea-level change provide fundamental data to discuss sea-level rise associated with global warming and its influence on coastal environments and people.
- 2007-03-15
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