摘要
Ouvéa Island in New Caledonia emerges as a new sea level standard. It has excellent morphological records of former sea level positions at interglacial high-stands as well as records of Holocene changes in sea level from a maximum at about +1.5 m via a significant +70 cm level of sub-recent, probably 17<sup><span style="font-family:Verdana;">th</span></sup><span style="font-family:Verdana;"> century, age to a stable to falling sea level in present time.</span>
Ouvéa Island in New Caledonia emerges as a new sea level standard. It has excellent morphological records of former sea level positions at interglacial high-stands as well as records of Holocene changes in sea level from a maximum at about +1.5 m via a significant +70 cm level of sub-recent, probably 17<sup><span style="font-family:Verdana;">th</span></sup><span style="font-family:Verdana;"> century, age to a stable to falling sea level in present time.</span>
作者
Nils-Axel Mörner
Nils-Axel Mörner(Paleogeophysics & Geodynamics, Stockholm, Sweden)
