@article{oai:nipr.repo.nii.ac.jp:00003032,
 author = {Zwartz, Daniel Peter and Miura, Hideki and Takada, Masashi and Moriwaki, Kiichi},
 journal = {Polar geoscience},
 month = {Oct},
 note = {P(論文), At sites where glacio-isostatic rebound has occurred, the record of sea-level change can be used to infer the former ice thickness and its melting history At Mt Riiser-Larsen, former sea-levels higher than present are indicated by the presence of raised beach deposits and ancient sediments deposited in brackish water Sediment cores from three ice-marginal lakes contained only fresh-water sediment, and a basal radiocarbon age shows that there has been no marine incursion in the last ～10000 years, limiting sea-level during that time to lower than 18 4m above present A well-defined marine limit is present 15 m a s 1, which will be dated using radiocarbon ages on stranded seals and abandoned penguin rookeries We anticipate an age of ～6 ka, because of the interaction between eustatic and isostatic components of sea-level change},
 pages = {249--259},
 title = {Holocene lake sediments and sea-level change at Mt. Riiser-Larsen},
 volume = {11},
 year = {1998}
}