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50 Myr recovery from the largest negative δ 13 C excursion in the Ediacaran ocean

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dc.contributor.authorLe Guerroue, Erwan
dc.contributor.authorAllen, Philip A
dc.contributor.authorCozzi, Andrea
dc.contributor.authorEtienne, James L
dc.contributor.authorFanning, Christopher
dc.date.accessioned2015-12-07T22:39:24Z
dc.date.issued2006
dc.date.updated2015-12-07T10:48:44Z
dc.description.abstractSedimentary rocks deposited during the Ediacaran period (∼630542 Ma) contain carbonates whose carbon isotopic ratios show a marked negative excursion consisting of a precipitous drop from +5‰ to - 12‰, followed by a sub-linear recovery to positive �
dc.identifier.issn0954-4879
dc.identifier.urihttp://hdl.handle.net/1885/23847
dc.publisherBlackwell Publishing Ltd
dc.sourceTerra Nova
dc.subjectKeywords: carbon isotope; Ediacaran; sedimentary rock
dc.title50 Myr recovery from the largest negative δ 13 C excursion in the Ediacaran ocean
dc.typeJournal article
local.bibliographicCitation.lastpage153
local.bibliographicCitation.startpage147
local.contributor.affiliationLe Guerroue, Erwan, Swiss Federal Institute of Technology (ETH)
local.contributor.affiliationAllen, Philip A, Swiss Federal Institute of Technology (ETH)
local.contributor.affiliationCozzi, Andrea, Swiss Federal Institute of Technology (ETH)
local.contributor.affiliationEtienne, James L, Swiss Federal Institute of Technology (ETH)
local.contributor.affiliationFanning, Christopher, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidFanning, Christopher, u4029993
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.identifier.absfor040203 - Isotope Geochemistry
local.identifier.absfor040311 - Stratigraphy (incl. Biostratigraphy and Sequence Stratigraphy)
local.identifier.ariespublicationu4027924xPUB29
local.identifier.citationvolume18
local.identifier.doi10.1111/j.1365-3121.2006.00674.x
local.identifier.scopusID2-s2.0-33645089913
local.type.statusPublished Version

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