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showing 10 items of 26608 documents

The stable isotope composition of organic and inorganic fossils in lake sediment records: current understanding, challenges, and future directions

2018

This paper provides an overview of stable isotope analysis (H, C, N, O, Si) of the macro- and microscopic remains from aquatic organisms found in lake sediment records and their application in (palaeo)environmental science. Aquatic organisms, including diatoms, macrophytes, invertebrates, and fish, can produce sufficiently robust remains that preserve well as fossils and can be identified in lake sediment records. Stable isotope analyses of these remains can then provide valuable insights into habitat-specific biogeochemistry, feeding ecology, but also on climatic and hydrological changes in and around lakes. Since these analyses focus on the remains of known and identified organisms, they …

010506 paleontologyArcheologyTaphonomy010504 meteorology & atmospheric sciencesorganic remainsstable isotopessedimentit580 Plants (Botany)01 natural sciencesInorganic remainsäyriäisetIsotope fractionationpiilevätEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesIsotope analysisStable isotopesDiatomsGlobal and Planetary Changeinorganic remainsisotoopitEcologyStable isotope ratioLake ecosystemBiogeochemistryOstracodsGeologyselkärangattomatInvertebratespaleolimnologiaMacrophytelake sedimentLake sedimentostracodsOrganic remainsPaleoecologyEnvironmental science
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The influence of religious identity and socio-economic status on diet over time, an example from medieval France

2019

International audience; In Southern France as in other parts of Europe, significant changes occurred in settlement patterns between the end of Antiquity and the beginning of the Middle Ages. Small communities gathered to form, by the tenth century, villages organized around a church. This development was the result of a new social and agrarian organization. Its impact on lifestyles and, more precisely, on diet is still poorly understood. The analysis of carbon and nitrogen isotopes in bone collagen from the inhabitants of the well-preserved medieval rural site Missignac-Saint Gilles le Vieux (fifth to thirteenth centuries, Gard, France) provides insight into their dietary practices and enab…

010506 paleontologyArcheology[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistorymedia_common.quotation_subjectPopulation[SHS.ANTHRO-BIO]Humanities and Social Sciences/Biological anthropologyDiversification (marketing strategy)01 natural sciencesReligious identity0601 history and archaeologyMiddle AgesArqueologia MetodologiaeducationSocioeconomic status0105 earth and related environmental sciencesmedia_common2. Zero hungereducation.field_of_study060102 archaeology06 humanities and the arts15. Life on land6. Clean waterAgrarian societyGeographyAnthropologyEthnologyTerrestrial ecosystemDiversity (politics)
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Why should traceology learn from dental microwear, and vice-versa?

2019

Dental and artifact microwear analyses have a lot in common regarding the questions they address, their developmental history and their issues. However, few paleontologists and archeologists are aware of this, and even those who are, do not take into account most of the methodological insights from the other field. In this focus article, we briefly review the main developmental steps of both methods, highlight how similar their histories are and how combining methodological developments can improve both research fields. In both cases, the traditional analyses have been strongly criticized mainly because of their subjectivity and their lack of repeatability and reproducibility. Quantitative …

010506 paleontologyArtifact (archaeology)ArcheologyTeeth060102 archaeologyPaleontology06 humanities and the arts01 natural sciencesData scienceField (computer science)Confocal microscopyDental microwear texture analysisQuantitative surface texture analysis0601 history and archaeologyPsychologyArtifacts0105 earth and related environmental sciences
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Ammonoids and quantitative biochronology - A unitary association perspective

2015

Ammonoid evolutionary changes have long been recognized to be excellent time markers. They are the major macrofossil group to date and correlate Paleozoic and Mesozoic marine strata. Originations and extinctions of ammonoid species are commonly used to define GSSPs and build high resolution biozonations. Biochronology is now an advanced field with the recent development of computerized, quantitative methods yielding robust biochronological schemes. It has been demonstrated that such quantitative biochronological methods are very efficient to resolve (often complex) biostratigraphic contradictions and produce accurate and high resolution biozonations, thus enabling precise dating and correla…

010506 paleontologyAssociation (object-oriented programming)High resolutionGeometry10125 Paleontological Institute and MuseumBiostratigraphy010502 geochemistry & geophysics01 natural sciencesUnitary statePaleontology560 Fossils & prehistoric lifeBiochronology14. Life underwater[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyComputingMilieux_MISCELLANEOUS[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciences
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Marine Early Triassic Actinopterygii from Elko County (Nevada, USA): implications for the Smithian equatorial vertebrate eclipse

2017

AbstractThe Early Triassic vertebrate record from low paleolatitudes is spotty, which led to the notion of an ‘equatorial vertebrate eclipse’ during the Smithian. Here we present articulated ray-finned fishes (Actinopterygii), collected from the marine Lower Triassic Thaynes Group at three new localities in Elko County (Nevada, USA), which were deposited within the equatorial zone. From the Smithian of the Winecup Ranch, we describe two partial skulls of the predatory actinopterygianBirgeria(Birgeriidae), attributed toB.americananew species andBirgeriasp.Birgeria americanan. sp. is distinguished from other species by a less reduced operculogular series. With an estimated total length of 1.7…

010506 paleontologyEarly Triassic10125 Paleontological Institute and MuseumStructural basin010502 geochemistry & geophysics01 natural sciencesSaurichthysPaleontologyGroup (stratigraphy)biology.animal14. Life underwaterBirgeria[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyEcologyActinopterygiiPaleontologyVertebratebiology.organism_classification1911 Paleontology560 Fossils & prehistoric lifeRidge[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeologyJournal of Paleontology
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Transient metazoan reefs in the aftermath of the end-Permian mass extinction

2011

5 pages; International audience; Recovery from the devastating Permian-Triassic mass extinction about 252 million years ago is usually assumed to have spanned the entire 5 million years of the Early Triassic epoch1,2. The post-crisis interval was characterized by large-scale fluctuations of the global carbon cycle and harsh marine conditions, including a combination of ocean acidification, euxinia, and fluctuating productivity3. During this interval, metazoan-dominated reefs are thought to have been replaced by microbial deposits that are considered the hallmark of the Early Triassic4-7. Here we use field and microscopic investigations to document Early Triassic bioaccumulations and reefs f…

010506 paleontologyEarly Triassic10125 Paleontological Institute and Museum[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesCarbon cyclePaleontology14. Life underwaterReefPermian–Triassic extinction event[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesExtinction eventgeographygeography.geographical_feature_categoryExtinction1900 General Earth and Planetary SciencesfungiOcean acidificationsocial scienceshumanitiesOceanography560 Fossils & prehistoric life13. Climate actionBenthic zone[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeneral Earth and Planetary Sciences[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontologygeographic locationsGeologyNature Geoscience
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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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Trilobites from the Red Fauna (latest Emsian, Devonian) of Hamar Laghdad, Morocco and their biodiversity

2018

36 pages; International audience; Trilobites are widespread in Early Devonian deposits of north Gondwana; some of the most emblematic ones were collected from the famous latest Emsian (Early Devonian) mudmound locality Hamar Laghdad in south-eastern Morocco. This locality is famous for its trilobites, especially for the conspicuous red-coloured remains of phacopid trilobites with often greenish eyes. Here, we present a taxonomic revision of the previously described trilobites from the so-called Red Fauna of Hamar Laghdad. We introduce the new taxa Harpes hamarlaghdadensis n. sp. and Morocops davidbrutoni n. sp. Phacopids dominate the trilobite assemblage from the Red Cliff at Hamar Laghdad …

010506 paleontologyFaunaBiodiversity10125 Paleontological Institute and Museum[SDV.BID.SPT]Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomy010502 geochemistry & geophysics01 natural sciencesTafilaltDevoniandiversitytaxonomyPaleontology[SDV.BID.SPT] Life Sciences [q-bio]/Biodiversity/Systematics Phylogenetics and taxonomyCliff14. Life underwaterEmsian0105 earth and related environmental sciencesgeography.geographical_feature_categorybiologyvariabilityPalaeontologyTrilobitaPaleontologybiology.organism_classificationTrilobite1911 PaleontologyGondwanaTaxonGeography560 Fossils & prehistoric lifeeastern Anti-Atlas[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyNeues Jahrbuch für Geologie und Paläontologie - Abhandlungen
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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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