Did global tectonics drive early biosphere evolution? Carbon isotope record from 2.6 to 1.9 Ga carbonates of Western Australian basins.

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dc.contributor.authorLindsay, John
dc.contributor.authorBrasier, Martin
dc.date.accessioned2015-12-10T23:16:07Z
dc.date.issued2002
dc.date.updated2015-12-10T09:50:08Z
dc.description.abstractThe δ13Ccarb record of well preserved carbonates in outcrop and core is here examined from the 2.6 to 1.9 Ga old basins of Western Australia. These data, which are constrained by a well defined stratigraphic and tectonic framework, and by U-Pb zircon age
dc.identifier.issn0301-9268
dc.identifier.urihttp://hdl.handle.net/1885/64925
dc.publisherElsevier
dc.sourcePrecambrian Research
dc.subjectKeywords: carbon; carbonic acid derivative; gallium; lead; oxygen; uranium; zirconium; biosphere; carbon isotope; carbonate; early Earth; paleoatmosphere; Precambrian; tectonic evolution; archaean; article; asthenospheric upwelling; atmosphere; Australia; biosphere Archean; Biosphere; Carbon isotopes; Hamersley basin; Palaeoproterozoic; Pilbara
dc.titleDid global tectonics drive early biosphere evolution? Carbon isotope record from 2.6 to 1.9 Ga carbonates of Western Australian basins.
dc.typeJournal article
local.bibliographicCitation.lastpage34
local.bibliographicCitation.startpage1
local.contributor.affiliationLindsay, John, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationBrasier, Martin, Oxford University
local.contributor.authoremailrepository.admin@anu.edu.au
local.contributor.authoruidLindsay, John, u1500166
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040313 - Tectonics
local.identifier.ariespublicationMigratedxPub1022
local.identifier.citationvolume114
local.identifier.doi10.1016/S0301-9268(01)00219-4
local.identifier.scopusID2-s2.0-0036472951
local.identifier.uidSubmittedByMigrated
local.type.statusPublished Version

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