Search results for "SPECIES"

showing 10 items of 4255 documents

Pleistocene paleoenvironmental reconstructions and mammalian evolution in South-East Asia: focus on fossil faunas from Thailand.

2006

16 pages; International audience; Mammalian faunal studies have provided various clues for a better reconstruction of hominid Quaternary paleoenvironments. Inthis work, two methods were used: (1) the cenogram method, based on a graphical representation of the mammalian communitystructure, and (2) the species richness of murine rodents to estimate climatic parameters. These methods were applied to Middle andLate Pleistocene mammalian faunas of South-East Asia, from South China to Indonesia. Special emphasis was laid on a fauna fromnorth-east Thailand dated back to approximately 170,000 years (i.e. a glacial period). This Thai fauna seems characteristic of aslightly open forested environment …

010506 paleontologyArcheologyPleistocene[SDE.MCG]Environmental Sciences/Global ChangesFauna010502 geochemistry & geophysics01 natural sciencesQuaternaryPaleontology[ SDV.EE.BIO ] Life Sciences [q-bio]/Ecology environment/BioclimatologyMammalian communityGlacial periodEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyPaleoenvironmementPalynologyGlobal and Planetary ChangeEcology[SDV.BID.EVO]Life Sciences [q-bio]/Biodiversity/Populations and Evolution [q-bio.PE]Geology15. Life on landThailand[ SDE.MCG ] Environmental Sciences/Global ChangesGeographyTaxon13. Climate actionInterglacialCenogram methodSpecies richness[SDV.EE.BIO]Life Sciences [q-bio]/Ecology environment/Bioclimatology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyQuaternarySpecies richness
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Environmental responses of past and recent agropastoral activities on south Greenlandic ecosystems through molecular biomarkers

2016

Paleoenvironmental studies previously performed on Lake Igaliku revealed two agropastoral phases in south Greenland: the Norse settlement from AD 986 to ca. AD 1450 and the recent installation of sheep farmers, since the 1920s. To improve the knowledge of the timing and magnitude of the Greenlandic agropastoral activities, a lipid inventory was realized and compared with biological and geochemical data. During the 12th century, a major increase in deoxycholic acid (DOC) and coprophilous fungal spores revealed a maximum of herbivores. Synchronously, a minimum of the n-C29/ n-C31 alkane ratio and tree and shrub pollen and a maximum of triterpenyl acetates showed a reduction in the tree and s…

010506 paleontologyArcheologysouth Greenlandved/biology.organism_classification_rank.specieslake sediments010502 geochemistry & geophysicsmedicine.disease_cause01 natural sciencesShrubmolecular biomarkersPollenGrazingmedicine[ SDU.ENVI ] Sciences of the Universe [physics]/Continental interfaces environmentEcosystemRumex[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment0105 earth and related environmental sciencesEarth-Surface ProcessesGlobal and Planetary ChangeHerbivoreEcologybiologyEcologyved/biologyPaleontology15. Life on landbiology.organism_classificationMolecular biomarkersagropastoral activities13. Climate actionPlant speciesNorseGeologyecosystem responses
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SAPWOOD RINGS ESTIMATION FOR PINUS SYLVESTRIS L. IN LITHUANIA AND LATVIA

2019

Pinus sylvestris L. is the predominant tree species used for wooden constructions in the Baltic area. Accordingly, the timber of Pinus is the most important object for investigation and dating carried out by dendrochronologists of the Baltic countries. However, the dating of historical Pinus is often challenging when the outer sapwood rings are missing in the wood samples. In Pinus, sapwood rings increase in number as the tree ages, and therefore calculating the approximate number of missing outer rings from a set range, a technique used for oak, is not possible. In Norway, a simple method for estimating the number of sapwood rings has been developed for some native species of conifers. The…

010506 paleontologyAtmospheric Science010504 meteorology & atmospheric sciencesRange (biology)PaleontologyGeologyForestryForestry01 natural sciencesPinus <genus>GeographyDendrochronologyTree species0105 earth and related environmental sciencesTree-Ring Research
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Dental microwear texture analysis on extant and extinct sharks : Ante- or post-mortem tooth wear?

2020

Sharks are apex-predators that play an important role in past and present aquatic food webs. However, their diet - especially in extinct species - is often not well constrained. Dental microwear texture analysis (DMTA) has been successfully applied to reconstruct diet and feeding behaviours of different aquatic and terrestrial vertebrates. However, unlike in mammals, food-to-tooth contact in sharks is rather limited because only larger prey is manipulated before swallowing. Together with a fast tooth replacement rate, this reduces wear on individual teeth. Here, we present an explorative study of dental microwear texture on extant and extinct sharks to test whether ante-mortem wear is relat…

010506 paleontologyDental WearZoologyExtinct specieschemical and pharmacologic phenomenaShark teeth010502 geochemistry & geophysicsOceanography01 natural sciencesTexture (geology)DMTAZoologiPredationExtant taxonstomatognathic system14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesbiologyTumbling experimentPaleontologyGeologybiology.organism_classificationstomatognathic diseasesHabitatTooth wearCarcharhinusGeologiAlterationhuman activitiesZoologyGeologyElasmobranchii
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Permian-Triassic extinctions and rediversifications.

2015

Ammonoids were a major component of Permian marine faunas, but were on the verge of extinction during the Permian-Triassic crisis ~ 252 myr ago. Despite the severity of this extinction, their recovery was explosive in less than 1.5 myr. By Smithian time, they had already reached levels of taxonomic richness much higher than those of the Permian. The causes for the rapid Early Triassic diversification and proliferation of these organisms still remain elusive, but the evolution of their spatio-temporal diversity and disparity patterns closely correlates with the numerous environmental changes recorded during this time interval.

010506 paleontologyExtinctionPermianEarly Triassicmyrsocial sciences10125 Paleontological Institute and Museum010502 geochemistry & geophysics01 natural scienceshumanitiesPaleontologyGeography560 Fossils & prehistoric life14. Life underwaterSpecies richness[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology
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Revision of the genus Anasibirites Mojsisovics (Ammonoidea): An iconic and cosmopolitan taxon of the late Smithian (Early Triassic) extinction

2016

34 pages; International audience; The family Prionitidae Hyatt represents a major component of ammonoid faunas during the Smithian (Early Triassic), and the genus Anasibirites Mojsisovics is the most emblematic taxon of this family. Its stratigraphical range is restricted to the beginning of the late Smithian (Wasatchites distractus Zone). The genus is also characterized by an unusual cosmopolitan distribution, thus contrasting with most earlier Smithian ammonoid distributions that were typically restricted by latitude. Because the late Smithian witnessed an extinction of the nekton (e.g. ammonoids, conodonts) whose amplitude is equal to or larger than that of the end-Permian crisis, the nu…

010506 paleontologyFaunaAnasibiritesEarly Triassic10125 Paleontological Institute and Museum010502 geochemistry & geophysics[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomy01 natural sciencesTimorPaleontology0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyTaxonomybiologyPaleontologySpecies diversityAmmonoideabiology.organism_classification1911 Paleontology[SDV.BA.ZI]Life Sciences [q-bio]/Animal biology/Invertebrate ZoologyTaxon560 Fossils & prehistoric lifeintraspecific variationAnasibiritesCosmopolitan distributionTaxonomy (biology)late Smithian extinction[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology
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Terrestrial plants and marine algae from the Late Jurassic lithographic limestone of the Causse Méjean (Lozère, southern France)

2016

International audience; A new Late Jurassic flora was discovered in the fossiliferous lithographic limestone of the Causse Méjean, Lozère (southern France). It consists of the first Kimmeridgian/Tithonian plants from this area. Fossil plants are represented by megaremains preserved as impressions. This flora shows a co-occurrence of terrestrial plants and marine algae. The land plants include vegetative remains ascribed to bennettitaleans (Zamites Brongniart, 1828), conifers (Brachyphyllum Brongniart, 1828), and pteridosperms (Cycadopteris Zigno, 1853). Marine algae were ascribed to dasyclads (Goniolina D’Orbigny, 1850). Lithological and palaeontological features suggest preservation in a f…

010506 paleontologyFloraved/biology.organism_classification_rank.speciesLate JurassicContext (language use)010502 geochemistry & geophysics01 natural sciencesBennettitaleansBrachyphyllumPaleontologyAlgaeTerrestrial plant14. Life underwaterPteridospermsDasycladales0105 earth and related environmental sciencesZamites[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologybiologyved/biologyEcologyDasycladslcsh:QE1-996.5PtéridospermesGeologyVegetation15. Life on landbiology.organism_classificationConifèreslcsh:GeologyConifersHabitatJurassique terminalBennettitalesBassin des Causses.[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyCausses basin.GeologyCausses basin
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Pseudoskirroceras, a remarkable but poorly known Early Pliensbachian Tethyan ammonite genus: New data from the High Atlas (Morocco).

2007

13 pages; International audience; The discovery of new Early Pliensbachian ammonite faunas in Central High Atlas (Morocco) allows the re-examination of the taxonomic, stratigraphical and palaeogeographical framework of the genus Pseudoskirroceras, an intriguing but until now poorly known Tethyan taxon. For the first time, several specimens of Pseudoskirroceras mastodon (Fucini, 1935) the type species of the genus, have been collected in a well-known stratigraphical context. This material allows the evaluation of intra-specific variability and consequently the assessment of the taxonomical relevance of various geometrical and ornamental features. The best diagnostic features are the clearly …

010506 paleontologyPantropicalContext (language use)Biostratigraphy010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyPalaeobiogeographyStage (stratigraphy)GenusAmmonitesPalaeobiodiversity14. Life underwater0105 earth and related environmental sciencesEarth-Surface Processes[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyAmmoniteEarly JurassicBiostratigraphyGeologylanguage.human_languageType speciesTaxon[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphylanguage[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyWestern Tethys
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The Mid-Cenomanian Event in southeastern France: evidence from palaeontological and clay mineralogical data.

2013

16 pages; International audience; Reconstruction of main palaeoenvironmental conditions across the Mid-Cenomanian Event (MCE I) in the hemipelagic Tethyan section of Blieux (Southeast France, Vocontian Basin) is proposed. Quantitative analyses of calcareous nannofossil, ammonoid and clay mineral assemblages have been made and compared with respect to sea level changes and the carbon cycle perturbations. The nannofossil primary productivity, as recorded by nannofossil fluxes and relative abundances of meso-eutrophic taxa, is low just below and during the MCE Ia, then slightly increases in the interval including the MCE Ib. The clay assemblages mainly consist of illite/smectite mixed-layers w…

010506 paleontology[SDE.MCG]Environmental Sciences/Global Changesengineering.material[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesClimatic conditionsPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistrySchloenbachiaCalcareous nannofossilsKaoliniteRelative species abundanceSea level[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesMiddle CenomanianbiologyAmmonoidsPaleontology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrybiology.organism_classificationCretaceous[ SDE.MCG ] Environmental Sciences/Global ChangesVocontian Basin13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringPrimary productivityCenomanianClay minerals[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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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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