@article {583,
	title = {Holocene relative sea-level history of the Southern Victoria Land Coast, Antarctica},
	journal = {Global and Planetary Change},
	volume = {42},
	year = {2004},
	note = {845idTimes Cited:40Cited References Count:25},
	month = {Jul},
	pages = {241-263},
	abstract = {More than 130 radiocarbon dates of penguin remains and guano, sealskin, shells, and seaweed from raised beach ridges afford relative sea-level information for southern Victoria Land. A new relative sea-level curve suggests that the final unloading of grounded ice from the coast took place about 6600 C-14 years BP, in keeping with previous estimates of the timing of deglaciation. Since this time, the coast has experienced 32 m of relative sea-level fall at rates ranging from 2 to 15 mm/year, consistent with glacioisostatic rebound. (C) 2004 Elsevier B.V. All rights reserved.},
	issn = {0921-8181},
	doi = {10.1016/j.gloplacha.2003.09.004},
	author = {Hall, B. L. and Baroni, C. and Denton, G. H.}
}
