IDENTIFICATION OF PRIMARY CE-ANOMALY SIGNATURES IN FOSSIL BIOGENIC APATITE: IMPLICATION FOR THE CAMBRIAN OCEANIC ANOXIA AND PHOSPHOGENESIS

dc.contributor.authorMorad S.
dc.contributor.authorFelitsyn S.
dc.date.accessioned2021-02-22T07:40:52Z
dc.date.available2021-02-22T07:40:52Z
dc.date.issued2001
dc.description.abstractBased on REE analyses of 105 world-wide distributed Cambrian fossil apatite samples and eight late Neoproterozoic phosphate concretions, a close relationship is established between the concentrations of MREE and Ce anomalies. Shale La/SmN ratios of 0.35 is suggested as a critical value for the discrimination of the natural Ce anomaly acquired during pre-burial/early diagenesis by biogenic apatite from an artificial Ce anomaly induced due to the calculation. Ce anomalies in apatites with flat REE distribution and La/SmN ratio >0.35 may be used as indicative of oceanic anoxia.
dc.identifierhttps://elibrary.ru/item.asp?id=13377081
dc.identifier.citationSedimentary Geology, 2001, 143, 3-4, 259-264
dc.identifier.issn0037-0738
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/25345
dc.subjectCambrian
dc.subjectCe-anomaly
dc.subjectoceanic anoxia
dc.subject.agePaleozoic::Cambrianen
dc.titleIDENTIFICATION OF PRIMARY CE-ANOMALY SIGNATURES IN FOSSIL BIOGENIC APATITE: IMPLICATION FOR THE CAMBRIAN OCEANIC ANOXIA AND PHOSPHOGENESIS
dc.typeСтатья

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