Search results for " Systematics"

showing 10 items of 6576 documents

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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Continental late Pliocene paleoclimatic history recorded in the Bresse Basin (France)

1992

International audience; We present results to show that the Beaune P & C borehole, cored in the Bresse Basin (France), records late Pliocene climatic variations. Pollen analysis allows precise correlations with northern and southern European stratigraphies. Using Kukla et al.'s (1981) climate index, we show that cold climate phases occur during the Brunssumian, at around 3.2, 3.6 and 5.2 Myr B.P., respectively, in agreement with Atlantic core results. The onset of a general cooling trend is felt early in the Reuverian, at about 3 Myr B.P. which corresponds to the end of a warm event characterized by high percentages of oak. This is followed by minor climatic pulses of increasing magnitude s…

010506 paleontology[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistory[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryBoreholePaleontologyMagnitude (mathematics)myrStructural basin010502 geochemistry & geophysicsOceanographymedicine.disease_causeNeogene01 natural sciences[SHS]Humanities and Social SciencesPaleontology13. Climate actionPollenPaleoclimatologymedicine[SHS] Humanities and Social SciencesQuaternaryEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface Processes
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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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NICHE PARTITIONING OF THE EUROPEAN CARNIVOROUS MAMMALS DURING THE PALEOGENE

2018

We here describe the first partial cranium of Hyaenodon leptorhynchus, the type species of the taxonomically diverse and widely distributed hypercarnivorous genus Hyaenodon (Hyaenodonta). The cranium is from the Seon Saint-Andre deposits (Marseille, France; Chattian, MP26). It is preserved in a dense red marl matrix that obscures key morphological features. CT-scans were used to reconstruct the specimen. The morphology of the cranium reinforces the homogeneity previously observed in Hyaenodon despite its specific diversity. The fossil represents a juvenile: it preserves its deciduous canines and the P3 is almost fully erupted. This pattern of delayed canine eruption is a trait shared among …

010506 paleontologybiologyFaunaNiche differentiationPaleontologyZoology010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesCursorialType speciesBody planGenusHyaenodonPaleogeneEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesPALAIOS
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<p><strong><em>Chilocoris</em> <em>serratus</em> n. sp., the first burrower bug species (Hemiptera: Heteroptera: …

2016

The first burrower bug species recorded in Guinea-Bissau, Chilocoris serratus n. sp., is described and compared with morphologically related species. Additionally, an annotated checklist of Afrotropical species of the genus Chilocoris is provided.

010506 paleontologybiologyHeteroptera010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesHemipteraChecklistGuinea bissauBotanyAnimal Science and ZoologyTaxonomy (biology)CydnidaeEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesZootaxa
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Tree-ring δ2H values from lignin methoxyl groups indicate sensitivity to European-scale temperature changes

2020

Abstract Stable hydrogen isotope ratios of lignin methoxyl groups (δ2HLM) of wood have been shown to reflect climate-sensitive δ2H values of precipitation (δ2Hprecip). However, a detailed calibration study between high-resolution δ2HLM and δ2Hprecip data has not been performed yet. Here, we present annually resolved δ2HLM values from nine tree-ring series (derived from four Fagus sylvatica L. trees) collected near a station of the Global Isotope Network of Isotopes in Precipitation (GNIP) and the meteorological observatory at Hohenpeisenberg (Germany; ~48°N, 11°E). The nine δ2HLM tree-ring series show highly significant inter-series correlations (Rbar = 0.52) over the common period of overl…

010506 paleontologybiologyIsotopePaleontologyScale (descriptive set theory)010502 geochemistry & geophysicsOceanographybiology.organism_classificationAtmospheric sciences01 natural scienceschemistry.chemical_compoundchemistryFagus sylvaticaMeteorological observatoryDendrochronologyLigninPrecipitationEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesChronologyPalaeogeography, Palaeoclimatology, Palaeoecology
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First Perigondwanan record of actinolepids (Vertebrata: Placodermi: Arthrodira) from the Lochkovian (Early Devonian) of Spain and its palaeobiogeogra…

2011

Different palaeogeographic models have been proposed for the position of Laurussia ( including Baltica) and Gondwana-derived microcontinents ( including Ibero-Armorica) during Ordovician to Late Carboniferous times. Principal differences concern the presence and duration of a large ocean, the Rheic Ocean, acting as a faunal barrier between these areas. The timing of the collision of Laurussia with Gondwana and/or Gondwana-derived terranes continues to be debated. Here we present new faunal data revealing close biogeographical relations between Ibero-Armorica ("Perigondwanan" or Gondwanan derivate terranes) and Podolia (SE margin of Baltica, in Laurussia). The placoderm assemblage found in t…

010506 paleontologybiologyPaleontology15. Life on land010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesDevonianPaleontologyGondwanaCarboniferousPlacodermiOrdovicianBaltica14. Life underwaterArthrodiraEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesTerranePalaeogeography, Palaeoclimatology, Palaeoecology
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Emsian (Lower Devonian) conodonts from the Daliantang Formation at Daliantang, southeastern Yunnan, China

2021

Abstract The lower/upper Emsian boundary witnessed prominent diversification of biostratigraphically important genera Polygnathus Hinde, Caudicriodus Bultynck, and Latericriodus Muller. In contrast, conodonts previously reported around this boundary from the South China Block were characterized by relatively low species or subspecies diversity, and only a few widely distributed and extensively studied zone-defining taxa were recorded. In this paper, conodonts from the Daliantang Formation at the Daliantang section (Guangnan, southeastern Yunnan), one of the representative sections of the transitional facies between the benthic Xiangzhou facies and the pelagic Nandan facies, are investigated…

010506 paleontologybiologyStratigraphyFaunaPaleontologyPelagic zoneSubspecies010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesDevonianPaleontologyTaxonBenthic zoneFaciesConodontEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesPalaeoworld
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Givetian (Middle Devonian) historical bio- and chronostratigraphical subdivision based on conodonts

2017

The conodont record supports the intended threefold subdivision of the Givetian as envisaged by the International Subcommision on Devonian Stratigraphy into Lower, Middle and Upper Givetian substages. The lower boundary of the Lower Givetian Stage coincides with the lower boundary of the Givetian and it is recognized with the entry of Polygnathus hemiansatus. The lower boundary of the Middle Givetian is identified with the entry of either P. varcus or P. rhenanus. The base of the Upper Givetian is defined with the entry of Schmidtognathus hermanni. The historical review shows the conceptual evolution from a stage with just one and a half zones to one with ten zones that are the basis for th…

010506 paleontologybiologybusiness.industryPaleontologybiology.organism_classification01 natural sciencesDevonianPaleontologyStratigraphyStage (stratigraphy)Facies010503 geologybusinessConodontEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesSubdivisionLethaia
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Calcareous nannofossil response to Late Cretaceous climate change in the eastern Tethys (Zagros Basin, Iran)

2020

Abstract Coniacian to Maastrichtian changes in calcareous nannofossil assemblages have been investigated in the eastern Tethyan Shahneshin section (central Zagros Basin, Iran). The nannofossil assemblages are mainly composed of Watznaueria spp. (avg. 54%), Retecapsa spp (avg. 7.9%), Cribrosphaerella ehrenbergii (avg. 7.7%) and Micula spp. (avg. 5.7%). Throughout the late Campanian, there is a trend to lower abundances in Watznaueria spp. together with increasing abundances of C. ehrenbergii and Arkhangelskiella cymbiformis, which are considered in this basin as the main cool-water taxa. Our results reveal that, despite a diagenetic impact on calcareous nannoflora, a number of primary paleoe…

010506 paleontologybiologyδ13CPaleontologyStructural basin010502 geochemistry & geophysicsOceanographybiology.organism_classification01 natural sciencesCretaceousDiagenesisForaminiferaPaleontologyBorealBenthic zoneCalcareousEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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