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Sea level and global ice volumes from the Last Glacial Maximum to the Holocene

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dc.contributor.authorRouby, Helene
dc.contributor.authorPurcell, Anthony
dc.contributor.authorSun, Yiying
dc.contributor.authorSambridge, Malcolm
dc.contributor.authorLambeck, Kurt
dc.date.accessioned2015-12-13T22:33:01Z
dc.date.issued2014
dc.date.updated2015-12-11T09:13:23Z
dc.description.abstractThe major cause of sea-level change during ice ages is the exchange of water between ice and ocean and the planet's dynamic response to the changing surface load. Inversion of ∼1,000 observations for the past 35,000 y from localities far from former ice
dc.identifier.issn0027-8424
dc.identifier.urihttp://hdl.handle.net/1885/75836
dc.publisherNational Academy of Sciences (USA)
dc.rightsAuthor/s retain copyrighten_AU
dc.sourcePNAS - Proceedings of the National Academy of Sciences of the United States of America
dc.titleSea level and global ice volumes from the Last Glacial Maximum to the Holocene
dc.typeJournal article
dcterms.accessRightsOpen Accessen_AU
local.bibliographicCitation.issue43
local.bibliographicCitation.lastpage15303
local.bibliographicCitation.startpage15296
local.contributor.affiliationLambeck, Kurt, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationRouby, Helene, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationPurcell, Anthony, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationSun, Yiying, University of Hong Kong
local.contributor.affiliationSambridge, Malcolm, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidLambeck, Kurt, u7701269
local.contributor.authoruidRouby, Helene, u5064769
local.contributor.authoruidPurcell, Anthony, u8903837
local.contributor.authoruidSambridge, Malcolm, u8414462
local.description.notesImported from ARIES
local.identifier.absfor040407 - Seismology and Seismic Exploration
local.identifier.absseo970104 - Expanding Knowledge in the Earth Sciences
local.identifier.ariespublicationU3488905xPUB4816
local.identifier.citationvolume111
local.identifier.doi10.1073/pnas.1411762111
local.identifier.scopusID2-s2.0-84908275503
local.identifier.thomsonID000343729500027
local.type.statusPublished Version

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