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Continental ice in Greenland during the Eocene and Oligocene

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dc.contributor.authorEldrett, James S.
dc.contributor.authorHarding , Ian C
dc.contributor.authorWilson, P.A.
dc.contributor.authorButler, Emily
dc.contributor.authorRoberts, Andrew
dc.date.accessioned2015-12-07T22:23:45Z
dc.date.issued2007
dc.date.updated2015-12-07T09:22:34Z
dc.description.abstractThe Eocene and Oligocene epochs (∼55 to 23 million years ago) comprise a critical phase in Earth history. An array of geological records supported by climate modelling indicates a profound shift in global climate during this interval, from a state that
dc.identifier.issn0028-0836
dc.identifier.urihttp://hdl.handle.net/1885/20856
dc.publisherMacmillan Publishers Ltd
dc.sourceNature
dc.subjectKeywords: carbon dioxide; depositional environment; depositional sequence; Eocene; glaciation; ice cap; ice rafting; ice-rafted debris; Oligocene; paleoenvironment; sea ice; stratigraphy; article; atmosphere; concentration (parameters); Eocene; geology; glacier; gl
dc.titleContinental ice in Greenland during the Eocene and Oligocene
dc.typeJournal article
local.bibliographicCitation.startpage4
local.contributor.affiliationEldrett, James S., University of Southampton
local.contributor.affiliationHarding , Ian C, University of Southampton
local.contributor.affiliationWilson, P.A., Southampton University
local.contributor.affiliationButler, Emily, University of Southampton
local.contributor.affiliationRoberts, Andrew, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidRoberts, Andrew, u4817957
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040406 - Magnetism and Palaeomagnetism
local.identifier.ariespublicationu4539375xPUB14
local.identifier.citationvolume05591
local.identifier.doi10.1038/nature05591
local.identifier.scopusID2-s2.0-33947174307
local.type.statusPublished Version

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