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DC poleHodnotaJazyk
dc.contributor.authorKraft, Petr
dc.contributor.authorMergl, Michal
dc.date.accessioned2022-10-31T11:00:14Z-
dc.date.available2022-10-31T11:00:14Z-
dc.date.issued2022
dc.identifier.citationKRAFT, P. MERGL, M. Struggle for phosphorus and the Devonian overturn. Trends in Ecology and Evolution, 2022, roč. 37, č. 8, s. 645-654. ISSN: 0169-5347cs
dc.identifier.issn0169-5347
dc.identifier.uri2-s2.0-85129803143
dc.identifier.urihttp://hdl.handle.net/11025/49814
dc.format10 s.cs
dc.format.mimetypeapplication/pdf
dc.language.isoenen
dc.publisherElsevieren
dc.relation.ispartofseriesTrends in Ecology and Evolutionen
dc.rights© Elsevieren
dc.titleStruggle for phosphorus and the Devonian overturnen
dc.typečlánekcs
dc.typearticleen
dc.rights.accessopenAccessen
dc.type.versionpublishedVersionen
dc.description.abstract-translatedOrganisms with external phosphatic shells diversified and became abundant at the beginning of the Early Paleozoic but gradually declined and were rare by its end. The decreasing availability of phosphorus in oceans is thought to be responsible for this evolutionary trend. Responses of organisms to changes in the phosphorus cycle can be traced to the late Neoproterozoic, and likely had a significant role in the Cambrian explosion, the Great Ordovician Biodiversification Event (GOBE), and the Devonian nekton revolution. Effective use of phosphorus by vertebrates during the Devonian nekton revolution caused the phosphorus pool to shift from benthic external shells to the skeletons of pelagic vertebrates, and moved the marine faunas toward the dominance patterns and ecological structure of the Modern Evolutionary Fauna.en
dc.subject.translatedDevonianen
dc.subject.translatedGOBEen
dc.subject.translatedphosphateen
dc.subject.translatedphosphorus cycleen
dc.subject.translatedshellsen
dc.identifier.doi10.1016/j.tree.2022.03.009
dc.type.statusPeer-revieweden
dc.identifier.document-number847218700006
dc.identifier.obd43936189
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