Search results for "IGRA"

showing 10 items of 4940 documents

New fossil arthropods (Notostraca and Insecta: Syntonopterida) in the Continental Middle Permian of Provence (Bas-Argens Basin, France).

2009

9 pages; Apart frequent and relatively common ichnites, only a few body fossils (Ostracoda) have been mentioned in the Red Continental Permian formations of Provence till these last years. During 2006 and 2007 field researches, new arthropods have been discovered in the Pradineaux Formation of the Bas-Argens. They are Triopsidae (Crustacea, Notostraca) and an insect wing (Syntonopteridae) corresponding to a new genus and species Gallolithoneura butchlii gen. et sp. n. This latter is the first insect record in the Permian of Provence and the youngest one of this enigmatic Carboniferous paleopteran family. As in the other French Permian basins (Lodève, Saint-Affrique), these discoveries demon…

0106 biological sciences010506 paleontologyInsectaMiddle PermianPaleozoicPermianArthropodaBiostratigraphySyntonopterida010603 evolutionary biology01 natural sciencesPaleontologyNotostracaGenusCarboniferousPaleoclimatology0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologybiologyEcologyGeneral EngineeringMandibulataNotostracabiology.organism_classificationVarFrance[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
researchProduct

Eucynodont teeth from the Late Triassic of Krasiejów, Southern Poland

2021

Recent discoveries of Mammaliamorph teeth in the Keuper of southern Poland have extended the global record of eucynodonts in the Late Triassic and revealed a significant diversity of the group at that time. Here,we expand on this record with the description of new cynodont postcanine teeth from the Krasiejów bone bed. They show the dental morphology typical for Dromatheriidae, with a single root and crown without cingulum. We assigned them to Polonodon woznikensis, described from Woźniki. None of the 38 teeth from Krasiejów and Woźniki exhibit signs of serious wear, potentially indicating a very fast rate of tooth replacement in Polonodon.

0106 biological sciences010506 paleontologyKeuperZoologysocial sciencessclerobiont010603 evolutionary biology01 natural scienceshumanitiesstomatognathic diseasesGeographystomatognathic systemGroup (stratigraphy)Synapsidsheterochronymammals originGeneral Agricultural and Biological Scienceshuman activitiesHeterochronySclerobiontLate Triassic0105 earth and related environmental sciencesHistorical Biology
researchProduct

Étude paléobotanique d’une lentille argileuse cénomanienne de la carrière de Hucheloup, Maine-et-Loire, NO France : implications taxonomiques, strati…

2017

International audience; A Cenomanian clay lens in Hucheloup Quarry (Maine-et-Loire, north-western France) has yielded 82 foliar compressions and impressions, of which 62 were identified at several taxonomic levels. The plants are ascribed to diverse Pinales (27%), ferns (27%), Ginkgoales (26%), angiosperms (19%) and Cycadales (1%). The most abundant species in the assemblage are Frenelopsis alata (K. Feistmantel) E. Knobloch emend. J. Kvaček (Pinales) and Eretmophyllum obtusum (Velenovský) J. Kvaček (syn. E. andegavense Pons, Bourreau et Broutin) (Ginkgoales). Wood fragments, along with very well-preserved cuticles, have also been recovered and identified. The specimens are usually very fra…

0106 biological sciences010506 paleontologyMégasporesFluvial[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyLagune010603 evolutionary biology01 natural sciencesAnjouPaleontologyFrenelopsisEretmophyllumGenusCénomanienCenomanian0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyPalynologybiologyCuticlesPaleontologyBrackish lagoonPlant community15. Life on landMiosporesbiology.organism_classificationTaxon[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCuticulesCompressions foliairesLeaf compressionsCenomanianMegaspore[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyPinalesGeology
researchProduct

Variability of growth pattern observed in Metoposaurus krasiejowensis humeri and its biological meaning

2017

Purpose Histological studies on temnospondyl amphibian bones remain rare. A systematic revision of the histology was applied for the purpose of testing the histovariability in the humeri and becoming new information about the growth pattern. Methods The present study includes 12 humeri of Metoposaurus krasiejowensis, which originate from the Late Triassic clay pit near Krasiejo´w, southwestern Poland. The specimens were scanned with a microCT and the histological thin-sections have been obtained with the standard petrographic method. Results The evaluation of the studied bones shows a uniform growth series resulting in one morphotype. Strikingly, the histological analysis reveals a greater …

0106 biological sciences010506 paleontologyStratigraphyGeologyHistologyAnatomyBiologyMetoposaurusbiology.organism_classification010603 evolutionary biology01 natural sciencesBone remodelingSexual dimorphismMetoposaurus krasiejowensis Temnospondyli Krasiejo´w Bone histology Humeri Micro-CT0105 earth and related environmental sciencesJournal of Iberian Geology
researchProduct

New data on bat fossils from Middle and Upper Pleistocene localities of France

2011

We describe the bat fossils preserved in four sites from the middle and upper Pleistocene, three of them being well-known French localities: the rock shelter of Les Valerots, the caves of l’Escale at Saint Estève Janson and ‘‘du Prince’’ at Grimaldi (Italy), and the filling of Combe-Grenal, all of them containing microvertebrate assemblages with yet undescribed bat fossils. All species represented in these four localities are still presently distributed in France and had been previously recorded in other Pleistocene localities of central and western Europe, including France. The four assemblages differ both in the abundance of bat fossils as in species composition. The characteristics of ea…

0106 biological sciences010506 paleontologyTaphonomyMiddle PleistoceneWestern EuropeBiostratigraphy010603 evolutionary biology01 natural sciencesPaleontologíaTheriaPaleontologyEutheriaCaveLate PleistoceneChiroptera0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographygeography.geographical_feature_categorybiologyPaleontology15. Life on landbiology.organism_classificationArchaeologySpace and Planetary ScienceTaphonomyPaleoecologyPaleoecology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyCenozoicRock shelterGeology
researchProduct

Le site à ambre et plantes du Cénomanien de Neau (Mayenne, France)

2020

International audience; A new Cenomanian amber- and plant-bearing deposit has been discovered at Neau, in the Mayenne department (France). The Cenomanian fossiliferous lignites are located in karst filling in a substratum of Cambrian limestones. The amber corresponds mainly to tiny millimetric grains, devoid of arthropod inclusions, but rich in microorganisms, especially the sheated bacteria Leptotrichites resinatus , and containing pollen grains ( Classopollis ) and wood fibers (Araucariacae or Cheirolepidiaceae). The lignites provide abundant conifer and ginkgoale cuticle fragments ( Frenelopsis , Eretmophyllum ) and a lot of palynomorphs ( e.g. Gleicheniidites senonicu s, Cyathidites , D…

0106 biological sciences010506 paleontologyamberGeochemistryCondate-Eaumedicine.disease_causeGEOFcheirolepidiaceae010603 evolutionary biology01 natural sciencessheated bacteriaCénomanienAmbrePollenuticules de gymnospermesmedicinepalynologygymnosperm cuticles0105 earth and related environmental sciencesPalynologyChemical signaturegeographygeography.geographical_feature_categorybiology[SDV.BID.EVO]Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]lcsh:QE1-996.5Bactéries gainéescenomanianGeology15. Life on landbiology.organism_classificationKarstlcsh:GeologyCheirolepidiaceae[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPalynologie CArthropodMangroveCenomanian[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyfranceGeologyBSGF - Earth Sciences Bulletin
researchProduct

Revision of Permo-Carboniferous griffenflies (Insecta: Odonatoptera: Meganisoptera) based upon new species and redescription of selected poorly known…

2009

33 pages; International audience

0106 biological sciences010506 paleontologybiologyPermianStratigraphyOdonatopteraPaleontology15. Life on landbiology.organism_classification010603 evolutionary biology01 natural sciencesPaleontologyTaxonPhylogeneticsCarboniferousTaxonomy (biology)[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyMeganisopteraComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology
researchProduct

Middle-Late Triassic chondrichthyans remains from the the Betic Range (Spain)

2017

Purpose In the present study, we described, for first time, the chondrichthyan fauna from several Middle-Late Triassic sections in the Betic Domain and compare it with other recent described coeval faunas from the Iberian Ranges. Methods Specimens were retrieved after the dissolution (with 10% acetic acid) of carbonate rocks. Results The assemblage comprises of seven species belonging to six genera (Hybodus plicatilis, Omanoselache bucheri comb. nov., Omanoselache contrarius comb. nov., Lonchidion derenzii, Lissodus aff. L. lepagei, Pseudodalatias henarejensis and cf. Rhomaleodus budurovi), most of them non-nesoselachian. Chondrichthyans remains occur in levels dating from Ladinian to Carni…

0106 biological sciences010506 paleontologybiologyRange (biology)StratigraphyFaunaGeologyLadinianPaleontologiaRhomaleodusbiology.organism_classification010603 evolutionary biology01 natural sciencesHybodusPaleontologyLissodusLonchidionCarbonate rockGeology0105 earth and related environmental sciences
researchProduct

Athenacrinus n. gen. and other early echinoderm taxa inform crinoid origin and arm evolution

2020

AbstractIntermediate morphologies of a new fossil crinoid shed light on the pathway by which crinoids acquired their distinctive arms. Apomorphies originating deep in echinoderm history among early nonblastozoan pentaradiate echinoderms distinguish Tremadocian (earliest Ordovician) crinoid arms from later taxa. The brachial series is separated from the ambulacra, part of the axial skeleton, by lateral plate fields. Cover plates are arrayed in two tiers, and floor plates expressed podial basins and pores. Later during the Early Ordovician, floor plates contacted and nestled into brachials, then were unexpressed as stereom elements entirely and cover plates were reduced to a single tier. Inco…

0106 biological sciences010506 paleontologybiologyStereomPaleontologyCrinoidbiology.organism_classification010603 evolutionary biology01 natural sciencesTremadocianPaleontologyTaxonEchinodermGenusFloian[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOrdovician[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciences
researchProduct

Observations on the postcranial anatomy of Hoplitomeryx (Mammalia, Ruminantia, Hoplitomerycidae) from the Miocene of the Apulia Platform (Italy)

2016

The untypical ruminants of the Apulia Platform (central and southeastern Italy), originally accommodated in the genus Hoplitomeryx, have been recently revised. The Scontrone (Abruzzo, central Italy) representatives were included in a new genus, Scontromeryx, with the addition of a new species, Scontromeryx mazzai. In contrast, the Gargano ones were left in Hoplitomeryx, but also in this case with the addition of three new species, Hoplitomeryx devosi, H. macpheei, and H. kriegsmani, described on postcranial remains and based on body mass calculations and using a size class scoring technique. The results of the present study show that Scontromeryx is invalid, that S. mazzai is imperfectly de…

0106 biological sciences010506 paleontologybiologyStratigraphyHoplitomeryxPaleontologyPostcraniaSettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classification010603 evolutionary biology01 natural sciencesRuminantiaPaleontologyHoplitomeryx Artiodactyla Mammalia Miocene Abruzzo ItalyGeology0105 earth and related environmental sciencesPalaeontographica Abteilung A
researchProduct