Search results for "MAR"

showing 10 items of 24514 documents

Biometric and morphometric approaches on Lower Hettangian dinosaur footprints from the Rodez Strait (Aveyron, France).

2012

9 pages; International audience; Along the southern crystalline border of the Rouergue, the detrital Sandstones-variegated Mudstones Formation and the Dolomitic Formation yields numerous dinosaur footprints from the Earliest Hettangian. Among the 25 sites distributed along the 40 km-long transect between Marcillac-Vallon and Saint-Geniez-d'Olt, two of them, Puech de Castres and Le Bouyssou, have yielded abundant ichnites in various well-defined stratigraphic units. The combined analysis of these footprints with biometric and morphometric methods (Fourier analysis) warrants their identification to Grallator, Eubrontes and Dilophosauripus. The dual methodological approach also reveals two new…

010506 paleontologyEubrontesFluvialContext (language use)Structural basinRodez Strait010502 geochemistry & geophysicsTheropoda01 natural sciencesPaleontologyFloodplain0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyDinosauroid footprintsCoelophysoideabiologyGeneral Engineeringbiology.organism_classificationFourier analysisTheropodaTaxonLower HettangienFrance[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyMarine transgression
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High-resolution clay mineralogy as a proxy for orbital tuning: example of the Hauterivian-Barremian transition in the Betic Cordillera (SE Spain).

2012

11 pages; International audience; The response of clay mineral assemblages to potential orbital forcing is tested in Mesozoic hemipelagic marl- limestone rhythmites of the Río Argos section (Betic Cordillera, Southeastern Spain). Along the section, marls are pervasively enriched in kaolinite and illite, whereas limestones are enriched in smectite-rich illite/smectite mixed-layers, suggesting that marl-limestone alternations are produced by cyclic high-frequency fluctuations of continental runoff. Spectral analyses show that clay mineral assemblages evolve accordingly to precession, obliquity and eccentricity cycles. Durations of ammonite zones are assessed at 535 kyr for the Late Hauterivia…

010506 paleontologyOrbital forcingStratigraphyCyclostratigraphyengineering.material010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/StratigraphyPalaeoclimate01 natural sciencesPaleontologyGeologic time scaleHauterivianMarl0105 earth and related environmental sciencesRhythmiteGeologyCyclostratigraphyFaraoni Oceanic Anoxic EventCretaceousClay minerals13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringSedimentary rockBarremianGeology
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The end of the Messinian salinity crisis: Evidences from the Chelif Basin (Algeria).

2007

How did the Messinian Salinity Crisis end is a matter of intense debate between two opposite concepts i.e., the generalised dilution event, the so-called Lago–Mare, followed by the sudden restoration of the marine conditions at the base of the Zanclean, or the early partial or complete marine refill that would have happened earlier during the upper Messinian. The Chelif Basin of Northwestern Algeria, one of the greatest Messinian marginal basins of the Mediterranean, provides an exceptional opportunity to study in detail how this major paleoenvironmental change occurred through continuous sedimentary records of the Miocene–Pliocene boundary. Five sections representative of both the central …

010506 paleontologyOstracodSettore GEO/02 - Geologia Stratigrafica E Sedimentologicaδ18OForaminiferaStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaPaleontologyMessinianOstracodZanclean14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyStable IsotopesMediterranean basinPaleontologySedimentologySettore GEO/01 - Paleontologia E Paleoecologiabiology.organism_classificationSettore GEO/08 - Geochimica E VulcanologiaOceanographyBenthic zoneAlgeriaClastic rockLago–MareSedimentary rock[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyChelif basinGeologyMarine transgression
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Middle Triassic sharks from the Catalan Coastal ranges (NE Spain) and faunal colonization patterns during the westward transgression of Tethys

2020

Abstract Palaeogeographic changes that occurred during the Middle Triassic in the westernmost Tethyan domain were governed by a westward marine transgression of the Tethys Ocean. The transgression flooded wide areas of the eastern part of Iberia, forming new epicontinental shallow-marine environments, which were subsequently colonized by diverse faunas, including chondrichthyans. The transgression is recorded by two successive transgressive–regressive cycles: (1) middle–late Anisian and (2) late Anisian–early Carnian. Here, we describe the chondrichthyan fauna recovered from several Middle Triassic stratigraphic sections (Pelsonian-Longobardian) located at the Catalan Coastal Basin (western…

010506 paleontologyPalaeocurrentsFaunaPaleontologiaStructural basin010502 geochemistry & geophysicsOceanography01 natural sciencesCoastal chondrichthyansHybodusDispersal strategiesPaleontologyPeninsula14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorybiologyPaleontologyLadinianTethys Oceanbiology.organism_classificationLadinianAnisianTransgressiveGeologyMarine transgressionPalaeogeography, Palaeoclimatology, Palaeoecology
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Palynofacies and calcareous nannofossils in the Upper Kimmeridgian, southeastern Paris basin (France)

2005

AbstractThe Upper Kimmeridgian Members “Calcaires blancs supérieurs” and the “Marnes à exogyres supérieures” of the southeastern Paris basin were investigated for their palynofacies and calcareous nannofossils. These members display alternating limestone-marl lithotypes and represent shallow marine palaeoenvironments. The lower carbonate member is interpreted as a proximal palaeoenvironment (palaeobathymetry = 5 to 10 m), where storm and swell deposits were prevalent and the salinity was occasionally weak. The relative richness of brown phytoclasts in this part is favoured by good preservation related to restricted conditions. These conditions would explain the dominance of the nannofoss…

010506 paleontologyPalaeoenvironments010502 geochemistry & geophysics01 natural sciencesPalynofaciesSedimentary depositional environmentCoccolithPaleontologychemistry.chemical_compoundMarlCalcareous nannofossilsDominance (ecology)14. Life underwaterCoquina0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyPalynologyUpper KimmeridgianMarine shallow-water dépositsGeologyParis basinPalynofacieschemistryCarbonate[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Les ammonites du Pliensbachien du jebel Bou Rharraf (Haut Atlas oriental, Maroc).

2011

60 pages; International audience; L'originalité des dépôts sédimentaires et des faunes d'ammonites du jebel Bou Rharraf repose sur la présence de faciès « Ammonitico Rosso », les plus occidentaux connus pour le Pliensbachien, une forte diversité des Phylloceratida (Phylloceras, Calaiceras, Zetoceras, Partschiceras et Juraphyllites) et une disparité morphologique importante chez les Galaticeras, Miltoceras et les Tauromeniceras. Si quelques formes, telles que Miltoceras taguendoufi et Mauretaniaceras elmii nov. gen., nov. sp. ont un cachet endémique très affirmé, les faunes du Pliensbachien du Haut Atlas oriental sont classiques pour la marge sud de la Téthys occidentale. Trois genres (Callo…

010506 paleontologyPaleontologyJurassique inférieur010502 geochemistry & geophysicsPliensbachien01 natural sciencesMarocBiostratigraphieSpace and Planetary ScienceAmmonites[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyHaut AtlasPaléobiogéographie
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Rich fen development in CE Europe, resilience to climate change and human impact over the last ca. 3500 years

2017

Here, for the first time in SE Poland, we document the long-term development of a rich fen and assess its sensitivity to climate change and human impacts over the last ca. 3500 years. Our results are based on a high-resolution, continuous plant macrofossil remains, mollusc and pollen record, complemented by geochemical, mineral magnetic and physical characterisation, and radiocarbon dating from Bagno Serebryskie rich fen located in SE Poland. Based on the palaeoecological data we distinguished five stages of wet habitat conditions: 5000–3300, 2800–2150, 1600–1100, 750–230, 150–10 cal yr BP and five dry periods at ca. 3300–2800, 2150–1600, 1100–750, 230–150, 10 to − 64 cal yr BP. The pollen …

010506 paleontologyPeat010504 meteorology & atmospheric sciencesClimate changeOmbrotrophicOceanographymedicine.disease_cause01 natural scienceslaw.inventionlawPollenmedicineRadiocarbon datingBogEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categoryCladium mariscusbiologyEcologyPaleontologyMacrofossilbiology.organism_classificationGeologyPalaeogeography, Palaeoclimatology, Palaeoecology
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New Permian tetrapod footprints and macroflora from Turkey (Çakraz Formation, northwestern Anatolia): biostratigraphic and palaeoenvironmental implic…

2011

9 pages; International audience; New tetrapod footprints belonging to the ichnogenus Hyloidichnus have been discovered in Turkey for the first time, in the lower part of the Çakraz Formation (Northwestern Anatolia) and together with macrofloral imprints of Annularia and Stigmaria. These discoveries confirm the Permian age of the fossiliferous red beds in which the coniferophyte Walchia was previously recorded. Based on the stratigraphic range of Annularia, Stigmaria and Hyloidichnus known elsewhere, a Cisuralian age is proposed for these beds. These new ichno- and macrofloral remains, together with the sedimentological data (mudcracks, rain drops) suggest the presence of captorhinid reptile…

010506 paleontologyPermianPangaeaTurkeyIchnitesStigmaria010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyStigmariaMacrofloraTetrapod (structure)CaptorhinidMigration0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyRed bedsbiologyWalchiaGeneral Engineeringbiology.organism_classificationAnnulariaHyloidichnusLaurasia[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyAnnularia[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Early evidence of fire in south-western Europe: the Acheulean site of Gruta da Aroeira (Torres Novas, Portugal)

2020

The site of Gruta da Aroeira (Torres Novas, Portugal), with evidence of human occupancy dating to ca. 400 ka (Marine Isotope Stage 11), is one of the very few Middle Pleistocene localities to have provided a fossil hominin cranium associated with Acheulean bifaces in a cave context. The multi-analytic study reported here of the by-products of burning recorded in layer X suggests the presence of anthropogenic fires at the site, among the oldest such evidence in south-western Europe. The burnt material consists of bone, charcoal and, possibly, quartzite cobbles. These finds were made in a small area of the cave and in two separate occupation horizons. Our results add to our still-limited know…

010506 paleontologyPleistoceneOccupancyPrehistoric peopleslcsh:MedicinePlistocèContext (language use)01 natural sciencesArticleArqueologíaMarine Isotope Stage 11Homínids fòssilsCave0601 history and archaeologyFossil hominidsCharcoallcsh:Science0105 earth and related environmental sciencesgeography060101 anthropologyMultidisciplinarygeography.geographical_feature_categorylcsh:RPrehistoriaPaleontological excavations06 humanities and the artsArchaeologyPleistoceneArchaeologyvisual_artWestern europevisual_art.visual_art_mediumlcsh:QJaciments paleontològicsAcheulean
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Micro-PIXE/PIGE analysis of Palaeolithic mammoth ivory: Potential chemical markers of provenance and relative dating

2014

Abstract Micro-Proton Induced X-ray and Gamma-ray Emission (micro-PIXE/PIGE) provide non-destructive methods for the evaluation of the major, minor and trace element compositions of archaeological material. The current study applies micro-PIXE/PIGE analysis to mammoth ivory artefacts from four Palaeolithic sites (Abri Castanet, Vogelherd Cave, Grottes de la Verpilliere I and II) in France and Germany in order to assess the effectiveness of this approach to material older than 30,000 y BP. It has thus far not been established whether such methods of analysis can yield results of scientific and archaeological interest on ivory material that has undergone such extended periods of diagenesis. T…

010506 paleontologyProvenanceMicro pixe[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryMineralogyOceanography01 natural sciencesChemical markerCaveArchéologieEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesEarth-Surface ProcessesMammothgeographygeography.geographical_feature_category[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistorybiology010401 analytical chemistryTrace elementPaleontologybiology.organism_classificationArchaeology0104 chemical sciencesDiagenesis[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and PrehistoryRelative datingGeology
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