Search results for "NCT"

showing 10 items of 16712 documents

Revision of the genus Anasibirites Mojsisovics (Ammonoidea): An iconic and cosmopolitan taxon of the late Smithian (Early Triassic) extinction

2016

34 pages; International audience; The family Prionitidae Hyatt represents a major component of ammonoid faunas during the Smithian (Early Triassic), and the genus Anasibirites Mojsisovics is the most emblematic taxon of this family. Its stratigraphical range is restricted to the beginning of the late Smithian (Wasatchites distractus Zone). The genus is also characterized by an unusual cosmopolitan distribution, thus contrasting with most earlier Smithian ammonoid distributions that were typically restricted by latitude. Because the late Smithian witnessed an extinction of the nekton (e.g. ammonoids, conodonts) whose amplitude is equal to or larger than that of the end-Permian crisis, the nu…

010506 paleontologyFaunaAnasibiritesEarly Triassic10125 Paleontological Institute and Museum010502 geochemistry & geophysics[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomy01 natural sciencesTimorPaleontology0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyTaxonomybiologyPaleontologySpecies diversityAmmonoideabiology.organism_classification1911 Paleontology[SDV.BA.ZI]Life Sciences [q-bio]/Animal biology/Invertebrate ZoologyTaxon560 Fossils & prehistoric lifeintraspecific variationAnasibiritesCosmopolitan distributionTaxonomy (biology)late Smithian extinction[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology
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Translating taxonomy into the evolution of conodont feeding ecology

2016

Conodont research has long been divided between utilitarian applications to solve geological problems versus analysis of their palaeobiology. However recent advances in conodont functional analysis allow these independent stands of research to be unified, decoding the functional implications of their morphological variation. We demonstrate this using synchrotron tomography and Finite Element Analysis, informed by occlusal and microwear analyses, to analyze functionally the classic evolutionary sequence of the genus Polygnathus. Our study shows that the evolution of the platform in Polygnathus occurred to accommodate and dissipate the stress accumulation derived from the tooth-like function …

010506 paleontologyFunctional ecologySynchrotron tomographybiologyPaleobiologyGeology010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesPaleontologyPhylogeneticsTaxonomy (biology)ConodontCladeFeeding ecology0105 earth and related environmental sciences
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Évolution rétrograde de Neospathodus au cours de la crise Permo - Triasique

2016

The Permian - Triassic evolution of platform conodonts (Gondolellidae) consists mainly in developing the carina and the platform. During the sublethal environmental stress conditions subsequent to the Permian - Triassic extinction, the Wuchiapingian - Griesbachian Clarkina lineage is replaced by the primitive looking platform-lacking Dienerian - Aegean Neospathodus kummeli - Kashmirella timorensis lineage. Moreover, above Jinogondolella denticulata, end of the Capitanian Jinogondolella lineage, “Neospathodus” arcucristatus, an atavistic blade-like homeomorph that lacks a platform, underlies Protoclarkina crofti, of the base of the anagenetic Clarkina lineage. These primitive-looking forms a…

010506 paleontologyLineage (genetic)ExtinctionPermianbiologyEvolutionTriasConodontsPaleontologyÉvolutionProteromorphosis010502 geochemistry & geophysicsbiology.organism_classificationTriassic01 natural sciencesEnvironmental stressPaleontologyPhylogenèseTriasAtavismPeriod (geology)ConodontesProtéromorphosePhylogeny0105 earth and related environmental sciencesRevue de Micropaléontologie
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Erratum to “Palaeoecological context for the extinction of the Neanderthals: A small mammal study of Stratigraphic Unit V of the El Salt site, Alcoi,…

2021

El Salt is an important reference site for understanding the extinction of Neanderthal populations in the eastern Iberian Peninsula during MIS 3. In this paper, we describe the small mammal assemblage from Stratigraphic Unit V, the youngest unit with evidence of human presence, based on nearly 1300 specimens. A total of seven rodents (Microtus arvalis, Microtus duodecimcostatus, Microtus cabrerae, Sciurus vulgaris, Arvicola sapidus, Eliomys quercinus and Apodemus sylvaticus), three insectivores (Talpa occidentalis, Crocidura sp., Sorex sp.) and one lagomorph (Oryctolagus cf. cuniculus) were identified. Palaeocological analyses point to drier conditions in this part of the stratigraphic sequ…

010506 paleontologyNeanderthalZoologySorex010502 geochemistry & geophysicsOceanography01 natural sciencesMicrotus cabrerae//purl.org/becyt/ford/1 [https]//purl.org/becyt/ford/1.5 [https]El SaltCrocidurabiology.animalSmall mammalsEliomysMicrotusEcology Evolution Behavior and SystematicsNeanderthals0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyMicrotus duodecimcostatusPaleontologyExtinctionbiology.organism_classificationPleistocenePalaeoclimatologyArvicolaGeologyIberian PeninsulaPalaeogeography, Palaeoclimatology, Palaeoecology
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Unravelling extrinsic and intrinsic factors of the early Palaeozoic diversification of blastozoan echinoderms

2010

19 pages; International audience; The Subphylum Blastozoa represents more than one third of the early Palaeozoic echinoderm fauna. A comprehensive database including all records of blastozoans was built to provide quantitative analyses of palaeogeography and diversity patterns and processes, for the 10 classes currently included in this subphylum during the early Palaeozoic. The global pattern of taxonomic diversity shows two peaks during the Cambrian Series 3 and the Late Ordovician intervals. In Cambrian times, the high taxonomic diversity seems to be related with a high turnover rate and a high endemicity of blastozoan genera, whereas in Ordovician times, the rise in diversity is associa…

010506 paleontologyPaleozoicEvolutionBlastozoaEvolutionary fauna010502 geochemistry & geophysicsOceanography01 natural sciencesBlastozoaPaleontologyEcology Evolution Behavior and Systematics[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesEarth-Surface ProcessesExtinction eventDiversitybiologyCambrian Series 3EcologyEarly PalaeozoicPaleontology15. Life on landbiology.organism_classification13. Climate actionOrdovicianSiliciclastic[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyPalaeogeographyOriginationGeologyEchinodermataPalaeogeography, Palaeoclimatology, Palaeoecology
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COMMENT TO LEHRMANN ET AL. NEW SECTIONS AND OBSERVATIONS FROM THE NANPANJIANG BASIN, SOUTH CHINA

2016

In the study of Earth-surface environmental processes during the events associated with the Permian–Triassic boundary, a key issue is the nature of the latest Permian pre-extinction surface in shallow marine limestones in numerous sites, principally within the Tethyan realm. Sediments below this surface pre-date the extinction event, so that the limestones comprising these latest Permian facies contain diverse fossil remains of organisms that lived just before the extinction. At all reported sites, this surface is disconformably overlain by post-extinction sediments, which contain microbialites in many places, particularly in Tethys. The nature of the youngest pre-extinction surface remains…

010506 paleontologyPermianOutcropStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesPaleontology14. Life underwaterGeopetal sediemntComputingMilieux_MISCELLANEOUSEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesExtinction eventExtinctionPendent CementsMicrobialitePaleontologyOcean acidification13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesSubaerial[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyErosional historyPALAIOS
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Ammonite paleobiogeography during the Pliensbachian-Toarcian crisis (Early Jurassic) reflecting paleoclimate, eustasy, and extinctions.

2011

14 pages; International audience; The Pliensbachian-Toarcian crisis (Early Jurassic) is one of the major Mesozoic paleoecological disturbances when ca. 20% of marine and continental families went extinct. Contemporaneously, profound paleobiogeographical changes occurred in most oceanic domains including a disruption of ammonite provincialism during the Early Toarcian. Here, we quantitatively reappraise the structure and evolution of paleobiogeographical patterns displayed by ammonite faunas before, during, and after the biological crisis, over a time-interval including 13 biochronozones. The high-resolution study presented here involves the use of hierarchical Cluster Analyses, non-metric M…

010506 paleontologyRange (biology)Biome010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontologyPaleoclimatologypaleoclimateprovincialism14. Life underwaterMesozoic0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyExtinction eventAmmoniteGlobal and Planetary ChangeExtinctionammonitesEarly Jurassicpaleobiogeography15. Life on landlanguage.human_languageArctic13. Climate actionlanguagemass extinction[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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The end-Triassic mass extinction: A new correlation between extinction events and δ13C fluctuations from a Triassic-Jurassic peritidal succession in …

2018

Abstract A new δ13Ccarb curve was obtained from an expanded peritidal succession in western Sicily and was used to investigate the relationships between isotopic signatures and biological events on carbonate platforms across the Triassic-Jurassic boundary (TJB). The resulting curve shows two main negative carbon isotopic excursions (CIEs) that fit well with the “Initial” and “Main” CIEs that are recognized worldwide and linked to the End-Triassic Extinction (ETE). In the studied section, the first negative CIE marks the disappearance of the large megalodontids, which were replaced by small and thin-shelled specimens, while the “Main” CIE corresponds to the last occurrence (LO) of the megalo…

010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaCarbonate platformStratigraphyAcidification; Carbon isotopes; Mass extinction; Sicily; Triassic-Jurassic boundary; Western Tethys; Geology; Stratigraphy010502 geochemistry & geophysics01 natural sciencesMass extinctionCarbon cycleAcidificationPaleontologychemistry.chemical_compoundSicily0105 earth and related environmental sciencesExtinction eventExtinctionCarbon isotopesGeologyTriassic-Jurassic boundarychemistryBenthic zoneIsotopes of carbonTriassic-Jurassic boundary Mass extinction Carbon isotopes Acidification Western Tethys SicilyCarbonateGeologyMarine transgressionWestern Tethys
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Conodonts from Late Devonian island arc settings (Baruunhuurai Terrane, western Mongolia)

2020

Abstract Upper Devonian marine deposits of the Baruunhuurai Terrane in western Mongolia represent island arc settings, which yielded a diverse conodont assemblage of 30 taxa, including species of Ancyrognathus (as well as one new species), Icriodus, Mehlina, Polygnathus and Palmatolepis. Biodiversity analysis of Ancyrognathus, Pelekysgnathus, Mehlina and Icriodus shows that the Mongolian conodont assemblage consists of two endemic and few cosmopolitan taxa. Representatives of the otherwise globally distributed genus Pelekysgnathus are absent. An important factor influencing the regional distribution of conodont taxa seems to be the siliciclastic-dominated sedimentation of the Baruunhuurai T…

010506 paleontologybiologyBiodiversityPaleontology010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesDevonianPaleontologyGenusAssemblage (archaeology)Island arcLate Devonian extinctionConodontEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTerranePalaeogeography, Palaeoclimatology, Palaeoecology
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Soil physicochemical and microbial drivers of temperature sensitivity of soil organic matter decomposition under boreal forests

2020

Abstract Soil organic matter (SOM) in boreal forests is an important carbon sink. The aim of this study was to assess and to detect factors controlling the temperature sensitivity of SOM decomposition. Soils were collected from Scots pine, Norway spruce, silver birch, and mixed forests (O horizon) in northern Finland, and their basal respiration rates at five different temperatures (from 4 to 28 °C) were measured. The Q10 values, showing the respiration rate changes with a 10 °C increase, were calculated using a Gaussian function and were based on temperature-dependent changes. Several soil physicochemical parameters were measured, and the functional diversity of the soil microbial communit…

0106 biological sciences$Q_{10}$ metabolic coefficientQ10Soil ScienceSoil scienceglobal warmingcomplex mixtures010603 evolutionary biology01 natural sciences$CO_{2}$ evolutionbiologySoil organic matterTaigaScots pineCarbon sink$MicroResp^{TM}$04 agricultural and veterinary sciencesbiology.organism_classificationEnvironmental chemistrySoil watermicrobial functional diversity040103 agronomy & agriculture0401 agriculture forestry and fisheriesEnvironmental scienceSoil horizonMicroResp™Q10 metabolic coefficientRespiration rateCO2 evolutionPedosphere
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