Search results for "mes"

showing 10 items of 23665 documents

The genomic history of the Iberian Peninsula over the past 8000 years

2019

We assembled genome-wide data from 271 ancient Iberians, of whom 176 are from the largely unsampled period after 2000 BCE, thereby providing a high-resolution time transect of the Iberian Peninsula. We document high genetic substructure between northwestern and southeastern hunter-gatherers before the spread of farming. We reveal sporadic contacts between Iberia and North Africa by ~2500 BCE and, by ~2000 BCE, the replacement of 40% of Iberia's ancestry and nearly 100% of its Y-chromosomes by people with Steppe ancestry. We show that, in the Iron Age, Steppe ancestry had spread not only into Indo-European-speaking regions but also into non-Indo-European-speaking ones, and we reveal that pre…

010506 paleontologyHumanidades::História e Arqueologia01 natural sciencesArticle03 medical and health sciencesAfrica NorthernPeninsulaPolitical scienceGeneticsHuman migrationHumansMigrationHistory Ancient030304 developmental biology0105 earth and related environmental sciences2. Zero hunger0303 health sciencesgeographyCiências Naturais::Ciências BiológicasScience & TechnologyMultidisciplinarygeography.geographical_feature_categoryChromosomes Human YPortugalHuman genomeGenome HumanExtramuralPrehistoriaAgricultureGenomicshumanitiesGene flowSpainHumanitiesgeographic locationsIberian Peninsula
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Fossiliferous Holocene tufa of Mende (Lozère, southern France): implication for the Atlantic vegetation of the Causses Basin

2016

International audience; Tufas bearing plant macroremains are uncommon in the Causses Basin (southern France). Here, we report anew fossiliferous tufa deposits at Mende, in Lozère. This palaeontological site is the first Quaternary tufa from thenorthern part of the Causses Basin that yields such an abundance of plant macroremains. The radiocarbon dating showsthat these Holocene deposits are related to the Atlantic period. Geomorphology and mineralogy show that theplant-bearing deposit is a calcareous tufa only composed by calcite, deposited near to an outlet of cool water, linked tothe karstic hydrological system of the Causse de Mende. The flora exposed in this article is dominated by angio…

010506 paleontologyLeavesAngiosperms010504 meteorology & atmospheric sciencesTilia cordataStructural basin01 natural sciencesTufslaw.inventionFeuillesPaleontologyLozèrelawRadiocarbon datingCausses BasinHolocene0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographygeography.geographical_feature_categoryBassin des CaussesHolocenebiologylcsh:QE1-996.5GeologyVegetationTufasbiology.organism_classificationKarstlcsh:GeologyTufaAngiospermesQuaternary[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyHolocène
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Early Pliocene continental vertebrate fauna at Puerto de la Cadena (SE Spain) and its bearing on the marine-continental correlation of the Late Neoge…

2017

In this paper, we synthesize sedimentological, magnetostratigraphic and paleontological data from the continental vertebrate site of Puerto de la Cadena (Murcia, SE Spain), in order to clarify its age. The study site is located on the northern edge of the Carrascoy mountain range, in the upper part of the Cigarrón Unit. The end-Messinian discontinuity has been detected at the base of this unit, which indicates it has an early Pliocene age. Abundant remains of small and large vertebrates, including rodents, lagomorphs, primates, carnivorans, perissodactyls, artiodactyls, proboscideans, testudines, squamats, and crocodiles, have been found in this area. Some of these elements are of African o…

010506 paleontologyMessinian salinity crisisFaunaEstratigrafíaLate MioceneBiostratigraphy010502 geochemistry & geophysicsOceanographyNeogene01 natural sciencesPaleontologybiology.animalSivatheriumEcology Evolution Behavior and SystematicsMagnetostratigraphy0105 earth and related environmental sciencesEarth-Surface ProcessesMammalsbiologyEcologyMagnetostratigraphyPaleontologyVertebrateReptilesBiostratigraphybiology.organism_classificationHipparionGeologyIberian Peninsula
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First shark record from the Upper Cretaceous of the Kuril Islands, Far East Russia

2020

Abstract The first find of a Late Cretaceous shark tooth, or of any cartilaginous fish for that matter, from the Kuril Islands in the Russian Far East is recorded as Carcharias sp. (Lamniformes, Carchariidae). The specimen originates from Maastrichtian strata on the island of Shikotan that are assigned to the Malokurilsk Formation. It constitutes an extremely rare find from rocks of this age in the northwest Pacific region. External and internal dental structures have been reconstructed by the use of computed tomography. The vasculature of this lamniform tooth is first modelled by CT scanning and shown under different angles, which allows an assessment of the spatial arrangement of hierarch…

010506 paleontologyNorthwest PacificCartilaginous fishComputed tomography010502 geochemistry & geophysics01 natural sciencesMaastrichtianPaleontologystomatognathic systemmedicineComputed tomography0105 earth and related environmental sciencesbiologymedicine.diagnostic_testPaleontologybiology.organism_classificationCretaceousCarchariasCarchariasstomatognathic diseasesVascular systemLamniformesVascular channelFar EastGeologyElasmobranchiiCretaceous Research
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Last Interglacial Iberian Neandertals as fisher-hunter-gatherers.

2020

Fruits of the sea The origins of marine resource consumption by humans have been much debated. Zilhão et al. present evidence that, in Atlantic Iberia's coastal settings, Middle Paleolithic Neanderthals exploited marine resources at a scale on par with the modern human–associated Middle Stone Age of southern Africa (see the Perspective by Will). Excavations at the Figueira Brava site on Portugal's Atlantic coast reveal shell middens rich in the remains of mollusks, crabs, and fish, as well as terrestrial food items. Familiarity with the sea and its resources may thus have been widespread for residents there in the Middle Paleolithic. The Figueira Brava Neanderthals also exploited stone pine…

010506 paleontologyOld WorldTaphonomy[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryIberian Neandertals01 natural sciences[SHS]Humanities and Social SciencesBirds03 medical and health sciencesCaveAnimal ShellsAnimalsNuts14. Life underwaterMiddle Stone AgeAtlantic OceanComputingMilieux_MISCELLANEOUSHoloceneMesolithic030304 developmental biology0105 earth and related environmental sciencesNeanderthalsMammals0303 health sciencesMultidisciplinarygeography.geographical_feature_categoryPortugalFishesSubsistence agriculturePinusArchaeologyDietTurtlesCavesGeographyArchaeologySeafoodInterglacialFisher-hunter-gatherersGruta da Figueira BravaScience (New York, N.Y.)
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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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Advances in Cretaceous palaeontology and stratigraphy – Christopher John Wood Memorial Volume; editors' preface

2018

Abstract In the last week of January 2016, the ‘Cretaceous community’ lost another of their prominent members, Chris Wood. During recent decades, Chris had been active in the United Kingdom as well as in mainland Europe, particularly in Germany and Poland. Several years ago he had been forced to leave the ranks of Associate Editors with Cretaceous Research , due to a severe illness that he was adamant to overcome. Later in 2016, two of us, fellow editors with that journal for a number of years, with the help of Rory Mortimore, approached former colleagues and friends of Chris's to contribute to a special issue. From the start, the idea has been to cover all aspects of Cretaceous stratigraph…

010506 paleontologyPaleontologyLate MesozoicNorthern ireland010502 geochemistry & geophysicsFull coverage01 natural sciencesCretaceousflorasEuropeKingdomPaleontologyBiozonationscorrelationsNorth AmericaMainlandStratigraphy (archaeology)faunasGeology0105 earth and related environmental sciencesCretaceous Research
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Evidence of an Early Triassic age (Olenekian) in Argana Basin (High Atlas, Morocco) based on new chirotherioid traces.

2010

8 pages; International audience; New chirotherioid traces (Synaptichnium, Chirotherium, Brachychirotherium, Isochirotherium), are described in the Argana Basin (High Atlas of Morocco). Seeing that these ichnotaxa are frequent in the Triassic, their occurrence in outcrops formerly mapped as Permian (T2 Member) has required detailed sedimentological and paleontological studies of the fossiliferous site. These studies clearly show that the ichnite-bearing strata belong actually to the T3 Member of the “regional Triassic”, i.e. lower member of the Timezgadiwine Formation, the age of which was, in fact, unknown up to now. The description of these ichnospecies and their statistical comparison wit…

010506 paleontologyPermianPaleozoicChirotheriumEarly TriassicArchosauriformesArgana BasinEarly Triassic010502 geochemistry & geophysics[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomy01 natural sciencesPaleontologyIchnotaxonPhanerozoicComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologybiology[SDV.BID.EVO]Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]General Engineeringbiology.organism_classificationMoroccoLepidosauriaLepidosauriaChirotherioid footprintsArchosauriformes[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyOlenekianGeology
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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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Electron Paramagnetic Resonance and petrographic analysis for dating Mesolithic and Neolithic pottery from Al Khiday (Sudan)

2016

Abstract Electron Paramagnetic Resonance (EPR) dating, like luminescence techniques, is based on the time-dependent accumulation of trapped charges at mineral defect centres. However, Fe(III) ions prevent the common Continuous Wave (CW-EPR) approach for dating pottery, which always contains iron. The Pulsed method (ED-EPR) allowed this limitation to be overcome, with recording of radiation-induced defect signals, as shown by increased signal intensity after artificial irradiation of samples. The method was applied to studying Mesolithic and Neolithic pottery from Al Khiday (Central Sudan), characterized by quartz-rich tempers and coming from dated contexts. As the occurrence of a natural ED…

010506 paleontologyRadiation060102 archaeologyAl Khiday; EPR dating; Prehistoric pottery; Quartz; Radiation; InstrumentationMineralogy06 humanities and the artsQuartz01 natural sciencesEPR datinglaw.inventionPetrographylawPrehistoric pottery0601 history and archaeologyPotterySignal intensityElectron paramagnetic resonanceAl KhidayQuartzInstrumentationGeologyMesolithic0105 earth and related environmental sciences
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