Search results for " conodonts"

showing 3 items of 3 documents

Exploring the major depletions of conodont diversity during the Triassic

2014

International audience; In this paper, we show that the Triassic fossil record reflects just two great depletions of conodont diversity before the Rhaetian, which occurred in the Smithian (Olenekian, Early Triassic) and in the Julian (Carnian, Late Triassic). By exploring this context, our results highlighted that they respond to different origination?extinction dynamics. Thus, while the Smithian diversity depletion can be interpreted as a consequence of elevated extinction, the Julian diversity depletion was triggered by fluctuations in origination regime. This evidence suggests that, despite the role of extinction on diversity losses, conodonts suffered crucial changes on the origination …

Diversity changeEarly TriassicContext (language use)Diversity depletion[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomyPaleontology[SDV.EE.ECO]Life Sciences [q-bio]/Ecology environment/EcosystemsProportional extinctionOrigination regimeBackground extinction rateTriassic conodontsExtinctionFossil RecordbiologyEcologysocial sciences[SDV.BV.BOT]Life Sciences [q-bio]/Vegetal Biology/Botanicsbiology.organism_classificationhumanities[SDE.BE]Environmental Sciences/Biodiversity and EcologyGeneral Agricultural and Biological SciencesConodonthuman activitiesOriginationGeologyDiversity (business)Historical Biology
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Conodonts versus Triassic Climatic and Eustatic Changes

2015

Kılıç, Ali Murat (Balikesir Author)

Extinction eventExtinctionproteromorphosis.PermianSiberian TrapsProgenesisTriassic ConodontsEarth and Planetary Sciences(all)General MedicineProteromorphosisSingle massShort lifePaleontologyPeriod (geology)PhylogenyGeologyRetrogradationProcedia Earth and Planetary Science
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New biostratigraphic data from the Ladinian pelagic limestones of Pizzo di Sant’Otiero - Madonie Mountains, Sicily

2014

New biostratigraphic data, based on conodont investigations, were collected from the Ladinian limestones recently described at Sant’Otiero, a locality near the Village of Petralia Sottana in the Madonie Mountains (Central-Northern Sicily). At this locality a new calcareous succession lying at the base of a major tectonic unit of the Maghrebian chain is described. This succession consists of a lower massive part formed by a carbonate megabreccia, the elements of which are shallow water extraclasts with dasycladalean algae (Diplopora annulatissima Pia), benthic foraminifers, “Tubiphytes” and problematic organisms commonly described from Anisian carbonate platforms. Upward a well-bedded succes…

Triassic Ladinian conodontsstratigraphy deep-water limestones SicilySettore GEO/02 - Geologia Stratigrafica E SedimentologicaStratigraphydeep-water limestonesConodontsTriassic; Ladinian; Conodonts; Stratigraphy; deep-water limestones; SicilySettore GEO/01 - Paleontologia E PaleoecologiaTriassicLadinianSicily
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