Search results for "RP"

showing 10 items of 25034 documents

Les Ammonoïdes (Mollusca, Cephalopoda) : avancées et contributions récentes à la paléobiologie évolutive.

2009

12 pages; Les ammonoïdes qui perdurent 335 Ma constituent un modèle de choix dans l'analyse du fait évolutif. Cet article de synthèse se propose d'aborder (1) : leur place phylogénétique au sein des céphalopodes et le choix d'un modèle actuel de référence ; (2) : la construction d'espaces phénotypiques qui offrent un angle d'étude pertinent de l'évolution biologique ; (3) : les concordances et discordances entre reconstruction phylogénétique et registre fossile et (4) : les reconquêtes postcrises, modèles d'étude de l'évolution à grande échelle. Il ressort que les ammonoïdes peuvent servir d'appui à de nombreuses thématiques paléontologiques (dynamique de la biodiversité, analyse phylogénét…

010506 paleontologyPhylogénieCrise et radiationÉvolutionBiostratigraphy010502 geochemistry & geophysics01 natural sciencesTetrabranchiataAmmonoïdeAllométrieMesozoicRegistre fossile0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyFossil Recordbiology[SDV.BID.EVO]Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]General EngineeringAmmonoideabiology.organism_classificationGeography[ SDV.BID.EVO ] Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]Crise et radiation.Espace morphologique[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyHumanities
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Amphibians and reptiles as palaeonvironmental proxies during the Late Pleistocene (MIS3): The case of Stratigraphic Unit V of El Salt, Alcoi, Spain

2021

The locality of El Salt (Alcoi, Spain) is a key site for understanding the extirpation of Neanderthals in the eastern part of Iberia. In this paper, we analyse an assemblage of amphibians and reptiles from Stratigraphic Unit V (45.2 ± 3.4 ka to 44.7 ± 3.4 ka), which corresponds to one of the last regional records of Neanderthals, to improve knowledge of the palaeoecology and palaeoclimate of this event. The assemblage comprises three anurans (Pelodytes sp., Alytes obstetricans, and Epidalea calamita), two lizards (Lacertidae indet. and Chalcides bedriagai), and five snakes (Colubridae indet., Coronella sp., Coronella sp./Zamenis sp., Natrix maura, and Vipera latastei). Palaeoclimatic recons…

010506 paleontologyPleistocene[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory010502 geochemistry & geophysicsOceanography01 natural sciences//purl.org/becyt/ford/1 [https]HWMLATE PLEISTOCENE//purl.org/becyt/ford/1.5 [https]PALAEOCLIMATEZamenisLacertidaeCoronellaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyChalcides bedriagaiEcologyEpidalea calamitaIBERIAN PENINSULAPaleontology15. Life on landHERPETOFAUNAbiology.organism_classificationAridificationMERPaleoecologyGeology
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Using growth and geochemical composition of Clathromorphum compactum to track multiscale North Atlantic hydro-climate variability

2020

International audience; Records of ocean/atmosphere dynamics over the past centuries are essential to understand processes driving climate variability. This is particularly true for the Northwest Atlantic which is a key region with an essential role in global climate regulation. Over the past two decades, coralline red algae have been increasingly used as environmental and climatic archives for the marine realm and hold the potential to extend long-term instrumental measurements. Here, we investigate the possibility to extract climate and environmental information from annual growth patterns and geochemical composition of the coralline red algae, Clathromorphum compactum, from Saint-Pierre …

010506 paleontologyPopulationClimate change010502 geochemistry & geophysicsOceanography01 natural sciencesCoralline algaeAtmosphereSclerochronologyEnvironmental reconstructionSclerochronologyClathromorphum compactumClimate change14. Life underwatereducationArctica islandicaEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processeseducation.field_of_studygeographygeography.geographical_feature_categorybiologyACLEnvironmental proxyPaleontologyCoralline algaebiology.organism_classification13. Climate actionArchipelagoPhysical geography[SDE.BE]Environmental Sciences/Biodiversity and EcologyGeology
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The metamorphic rocks of the Nunatak Viedma in the Southern Patagonian Andes: Provenance sources and implications for the early Mesozoic Patagonia-An…

2019

The Nunatak Viedma within the Southern Patagonian Icefield has been considered as a volcanic center based on its geomorphologic features, despite the fact that field explorations by Eric Shipton determined its metamorphic nature 70 years ago. We carried out fieldwork to characterize this isolated outcrop and performed the first U-Pb dating in detrital zircons from the basement rocks located inside the Southern Patagonian Icefield. We recognized very-low grade metamorphic rocks, corresponding principally to metapelites and metapsammites, and scarce metabasites. Detrital zircons in three metapsammitic samples (composite group of 240 grains) yielded prominent age population peaks at ∼1090, ∼96…

010506 paleontologyProvenanceNunatakVery-low grade metamorphic rocksOutcropMetamorphic rockPopulationDetrital zircons agesDETRITAL ZIRCONS AGES[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysics01 natural sciencesSouthwestern GondwanaCiencias de la Tierra y relacionadas con el Medio Ambiente//purl.org/becyt/ford/1 [https]Southern Patagonian Andes//purl.org/becyt/ford/1.5 [https]PaleontologyAntarctic PeninsulaCarboniferousGeologíaVERY-LOW GRADE METAMORPHIC ROCKSeducationCiencias Exactas y NaturalesSOUTHWESTERN GONDWANA0105 earth and related environmental sciencesEarth-Surface Processesgeographyeducation.field_of_studygeography.geographical_feature_categoryVolcanic arcGeologySOUTHERN PATAGONIAN ANDESGondwanaANTARCTIC PENINSULANUNATAK VIEDMANunatak ViedmaCIENCIAS NATURALES Y EXACTASGeology
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An aeolian or a glaciolacustrine record? A case study from Mieļupīte, Middle Gauja Lowland, northeast Latvia

2017

Abstract In the Middle Gauja Lowland, northeast Latvia, dunes are distributed over a vast glaciolacustrine plain that formed during the retreat of the Fennoscandian ice sheet. Such a direct contact between aeolian and glaciolacustrine sediments can be used to infer depositional settings and decipher to what extent these sediments bear an aeolian component. Our proxies, although preliminary, reveal a limited range of variation in grain-size parameters, a significant presence of quartz grains with silica precipitation and matt-surface grains of various rounding degrees and massive structure combined with horizontal lamination. These are indicative of periglacial-aeolian depositional condition…

010506 paleontologyQE1-996.5Optically stimulated luminescenceEarth sciencequartz grainsGeologyBaltic states010502 geochemistry & geophysicsbaltic states01 natural sciencesduneice-dammed lakelinkuva ice-marginal zoneGeneral Earth and Planetary SciencesAeolian processesLinkuva ice-marginal zoneoptically stimulated luminescenceGeomorphologyGeology0105 earth and related environmental sciencesGeologos
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Quaternary marine and continental unconformity-bounded stratigraphic units of the NW Sicily coastal belt

2017

In the coastal sector of NW Sicily, the regional correlation of relevant unconformities recognised within the Quaternary sedimentary successions allowed the mapping of seven unconformity-bounded stratigraphic units (UBSUs). The regional unconformities are marine or subaerial erosional surfaces, as well as non-depositional surfaces, locally marked by paleosoils. The erosional surfaces were produced from marine abrasion, surface water overland/concentrated flow, river erosion, karst solution, mass movement, or wind erosion. The main lithofacies of the Quaternary UBSUs consist of: (a) marine and coastal bioclastic calcarenites, (b) aeolian sandstones, (c) river deposits, (d) colluvial deposits…

010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaNW Sicilyquaternary continental and marine depositsGeography Planning and DevelopmentGeochemistryquaternary continental and marine deposit010502 geochemistry & geophysics01 natural sciencesUnconformitylcsh:G3180-9980Earth and Planetary Sciences (miscellaneous)tectonicsclimateGeomorphologyUnconformity-bounded stratigraphic unit0105 earth and related environmental sciencesColluviumlcsh:Mapsgeographygeography.geographical_feature_categoryUnconformity-bounded stratigraphic unitsKarsttectonicsea-level changeTectonicsSubaerialErosionSedimentary rocksea-level changesQuaternaryGeologyUnconformity-bounded stratigraphic units; quaternary continental and marine deposits; tectonics; sea-level changes; climate; NW SicilyJournal of Maps
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The space-time relationship of taxonomic diversity and morphological disparity in the Middle Jurassic ammonite radiation.

2007

14 pages; International audience; The Middle Jurassic ammonite radiation (from the late Aalenian to the end of the mid-Bathonian) is traced using combined analyses of morphological disparity and taxonomic diversity. The global signals of disparity and diversity are compared. These signals are then broken down by paleogeographical provinces to detect any heterogeneity in the radiation. An examination of the global signals reveals three biodiversity crises (discordances between signals) where morphological disparity grows while taxonomic diversity declines. The subdivision of the signals indicates the radiation was heterogeneous between provinces: the global signal is an aggregate of signals …

010506 paleontologyTaxonomic diversitymedia_common.quotation_subjectBiodiversity[SDV.BID]Life Sciences [q-bio]/BiodiversityJurassic010502 geochemistry & geophysicsOceanography01 natural sciencesPaleontologyAmmonitesPalaeogeographyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesSubdivisionmedia_common[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyAmmonite[ SDV.BID ] Life Sciences [q-bio]/Biodiversitybusiness.industrySpace timePaleontologylanguage.human_languagePaleogeographylanguagebusiness[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyDiversity (politics)Morphological disparity
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Radial Symmetry, the Anterior/Posterior Axis, and Echinoderm Hox Genes

2008

20 pages; International audience; The strangeness of echinoderm pentaradiality results from superposition of radial symmetry onto ancestral deuterostome bilaterality. The Extraxial- Axial Theory shows that echinoderms also have an anterior/posterior (A/P) axis developed independently and ontogenetically before radiality. The A/P axis is first established via coelomic stacking in the extraxial region, with ensuing development of the pentamerous hydrocoel in the axial region. This is strongly correlated with a variety of gene expression patterns. The echinoid Hox cluster is disordered into two different sets of genes. During embryogenesis, members of the posterior class demonstrate temporal, …

010506 paleontology[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomyphylogeny01 natural sciencesHomology (biology)03 medical and health sciencesmorphologyextraxial-axial theoryHox geneEcology Evolution Behavior and Systematics030304 developmental biology0105 earth and related environmental sciences0303 health sciencesDeuterostomeEcologybiology[SDV.BID.EVO]Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]Symmetry in biologyevo-devoAnterior Posterior AxishomologyAnatomybiology.organism_classification[ SDV.BID.EVO ] Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]EchinodermEvolutionary developmental biologySymmetry (geometry)[ SDV.BID.SPT ] Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomyAnnual Review of Ecology, Evolution, and Systematics
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Les Gregoryceras (Ammonitina) de l'Oxfordien moyen terminal et supérieur téthysien : révision systématique, biostratigraphie et évolution.

2009

43 pages; Les Gregoryceras Spath, 1924 (Ammonitina, Peltoceratina) de la fin de l'Oxfordien moyen (sous-zone à Rotoides) et de la base de l'Oxfordien supérieur (zone à Bifurcatus) sont révisés. Les coupes ayant fourni la plupart des spécimens de ce travail (Espagne et Maghreb) sont décrites et datées sur la base de comparaisons fauniques entre les domaines téthysien et subtéthysien. Le meilleur outil pour ces corrélations est la présence du genre Gregoryceras. La succession des espèces de Gregoryceras est identique pour les deux domaines suscités, ce qui permet de compléter l'échelle biostratigraphique proposée antérieurement et parallèle à la zonation standard. Les espèces reconnues et red…

010506 paleontologybiologyAmmonitinaPaleontologyÉvolutionEcological succession[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesSpecies successionPaleontologyGeographyCorrélations biostratigraphiquesSpace and Planetary ScienceGregoryceras (Ammonitina)Taxinomie[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyDimorphismeOxfordien[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciences
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Carbonate slope re‐sedimentation in a tectonically‐active setting (Western Sicily Cretaceous Escarpment, Italy)

2020

Tectonic processes are widely considered as a mechanism causing carbonate platform margin instabilities leading to the emplacement of mass transport deposits and calciturbidites. However, only few examples establishing a clear link between tectonics and re-sedimentation processes are known from the lit- erature. The two-dimensional and three-dimensional wire-cut walls of hun- dreds of quarries extracting ornamental limestones (for example, Perlato di Sicilia) from the Western Sicily Cretaceous Escarpment in Italy expose a series of mass transport deposits. The depositional architecture, spatial facies distri- bution and sedimentary features of these deposits were studied in detail. Thin sec…

010506 paleontologygeographyPillow lavageography.geographical_feature_categoryCarbonate platformStratigraphyGeochemistryGeologyEscarpment010502 geochemistry & geophysics01 natural sciencesCretaceousSedimentary depositional environmentTectonicsFaciesGeneral Earth and Planetary SciencesSedimentary rockGeologyCarbonate slope Cretaceous mass transport deposits re-deposited facies tectonics0105 earth and related environmental sciencesGeneral Environmental ScienceSedimentology
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