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dc.contributor.authorZalasiewicz, Jan
dc.contributor.authorWaters, C.N.
dc.contributor.authorWilliams, M.
dc.contributor.authorBarnosky, A.D.
dc.contributor.authorCearreta, A.
dc.contributor.authorCrutzen, P.
dc.contributor.authorEllis, E.
dc.contributor.authorEllis, M.A.
dc.contributor.authorFairchild, Ian J.
dc.contributor.authorGrinevald, J.
dc.contributor.authorHaff, P.K.
dc.contributor.authorHajdas, I.
dc.contributor.authorLeinfelder, R.
dc.contributor.authorMcNeill, J.
dc.contributor.authorOdada, E.O.
dc.contributor.authorPoirier, C.
dc.contributor.authorRichter, D.
dc.contributor.authorSteffen, W.
dc.contributor.authorSummerhayes, C
dc.contributor.authorSyvitski, J. P. M
dc.contributor.authorVidas, Davor
dc.contributor.authorWagreich, M.
dc.contributor.authorWing, S.L.
dc.contributor.authorWolfe, A.P.
dc.contributor.authorZhisheng, A.
dc.contributor.authorOreskes, N.
dc.date.accessioned2018-02-20T10:17:29Z
dc.date.available2018-02-20T10:17:29Z
dc.date.created2015-09-28T14:16:51Z
dc.date.issued2015
dc.identifier.citationQuaternary International. 2015, 383 196-203.
dc.identifier.issn1040-6182
dc.identifier.urihttp://hdl.handle.net/11250/2485908
dc.language.isoeng
dc.titleWhen did the Anthropocene begin? A mid-twentieth century boundary level is stratigraphically optimal
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersion
dc.source.pagenumber196-203
dc.source.volume383
dc.source.journalQuaternary International
dc.identifier.doi10.1016/j.quaint.2014.11.045
dc.identifier.cristin1276104
dc.relation.projectNorges forskningsråd: 209819
cristin.unitcode7430,0,0,0
cristin.unitnameFridtjof Nansens institutt
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode1


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