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Žigaitė, Živilė, Fadel, Alexandre, Pérez-Huerta, Alberto, Jeffries, Teresa, Goujet, Daniel, Ahlberg, Per Erik (2016) Paleoenvironments revealed by rare-earth element systematics in vertebrate bioapatite from the Lower Devonian of Svalbard. Canadian Journal of Earth Sciences, 53 (8) 788-794 doi:10.1139/cjes-2015-0206

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Reference TypeJournal (article/letter/editorial)
TitlePaleoenvironments revealed by rare-earth element systematics in vertebrate bioapatite from the Lower Devonian of Svalbard
JournalCanadian Journal of Earth Sciences
AuthorsŽigaitė, ŽivilėAuthor
Fadel, AlexandreAuthor
Pérez-Huerta, AlbertoAuthor
Jeffries, TeresaAuthor
Goujet, DanielAuthor
Ahlberg, Per ErikAuthor
Year2016 (August)Volume53
Issue8
PublisherCanadian Science Publishing
DOIdoi:10.1139/cjes-2015-0206Search in ResearchGate
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Mindat Ref. ID485280Long-form Identifiermindat:1:5:485280:7
GUID0
Full ReferenceŽigaitė, Živilė, Fadel, Alexandre, Pérez-Huerta, Alberto, Jeffries, Teresa, Goujet, Daniel, Ahlberg, Per Erik (2016) Paleoenvironments revealed by rare-earth element systematics in vertebrate bioapatite from the Lower Devonian of Svalbard. Canadian Journal of Earth Sciences, 53 (8) 788-794 doi:10.1139/cjes-2015-0206
Plain TextŽigaitė, Živilė, Fadel, Alexandre, Pérez-Huerta, Alberto, Jeffries, Teresa, Goujet, Daniel, Ahlberg, Per Erik (2016) Paleoenvironments revealed by rare-earth element systematics in vertebrate bioapatite from the Lower Devonian of Svalbard. Canadian Journal of Earth Sciences, 53 (8) 788-794 doi:10.1139/cjes-2015-0206
In(2016, August) Canadian Journal of Earth Sciences Vol. 53 (8) Canadian Science Publishing
Abstract/Notes In situ rare-earth element (REE) compositions have been measured in early vertebrate microremains from the Lower Devonian basin of Andrée Land (Svalbard), with the aim of obtaining information about their early depositional environment and potential reworking. Vertebrate microremains with different histology were used for the analyses, sourced from two different localities of marginal marine to freshwater sediments from geographically distant parts of the Grey Hœk Formation (Skamdalen and Tavlefjellet members). We selected thelodont and undescribed ?chondrichthyan scales, which allowed us to define potential taxonomic, histological, and taphonomic variables of the REE uptake. Results showed REE concentrations to be relatively uniform within the scales of each taxon, but apparent discrepancies were visible between the studied localities and separate taxa. The compilation of REE abundance patterns as well as REE ratios have revealed that thelodont and ?chondrichthyan originating from the same locality must have had different burial and early diagenetic histories. The shapes of the REE profiles, together with the presence and absence of the Eu and Ce anomalies, equally suggested different depositional and diagenetic environments for these two sympatric taxa resulting from either stratigraphical or long-distance reworking. The REE concentrations appear to have visible differences between separate dental tissues, particularly between enameloid and dentine of thelodonts, emphasizing the importance of in situ measurements in microfossil biomineral geochemistry.


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