Search results for " palaeoenvironment"

showing 10 items of 12 documents

Lowermost Jurassic dinosaur ecosystem from the Bleymard Strait (southern France): sedimentology, mineralogy, palaeobotany and palaeoichnology of the …

2021

AbstractWe report the first Hettangian theropod tracksite (~200 Ma) yielding a rich accumulation of plant remains from the Bleymard Strait (southern France). It constitutes an excellent opportunity to reconstruct lowermost Jurassic ecosystems hosting dinosaurs and which are still poorly documented in this area. Two morphotypes of tridactyl tracks are distinguished. They share similarities with Grallator and Kayentapus. Plant-bearing beds yield abundant leafy axes (Pagiophyllum peregrinum), male cones (Classostrobus sp.), wood (Brachyoxylon sp.) and pollen of conifers (Classopollis classoides). Sedimentological, petrological and mineralogical analyses demonstrated that, in the Dolomitic Form…

010506 paleontologyFloraIntertidal zone010502 geochemistry & geophysics01 natural sciencesSupralittoral zoneparalic palaeoenvironmentsPaleontologytheropod footprintsLozereLittoral zone14. Life underwaterSedimentology0105 earth and related environmental sciencesHettangianbiologyGeology15. Life on landbiology.organism_classificationPagiophyllumCheirolepidiaceaeCheirolepidiaceae13. Climate actionconifers[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDE]Environmental SciencesPaleobotany[SDE.BE]Environmental Sciences/Biodiversity and Ecology[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Influence of dissolved organic matter on rare earth elements and yttrium distributions in coastal waters

2010

International audience; Data collected during this study indicate that dissolved Y and REE (rare earth element) behaviour can be monitored through shale-normalised ratios. Relationships occurring between these ratios suggest that leaching from lithogenic materials is the main source of REE in the studied area. This process involves riverine detrital matter in the inner area of the Gulf of Palermo. Features of shale-normalised patterns and the relationship recognised between dissolved Fe and Y/Ho suggest that REE are released from Fe-rich coatings of atmospheric dust. Observed similarities between dissolved Fe and chlorophyll- content suggest that leaching of Fe-rich atmospheric particulates…

010506 paleontologyMineralogyrare earth elementsMediterranean010502 geochemistry & geophysics01 natural sciencesMediterranean seaDissolved organic carbonMediterranean Sea[SDV.BBM]Life Sciences [q-bio]/Biochemistry Molecular BiologyOrganic matter14. Life underwaterScavengingEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGeneral Environmental Sciencechemistry.chemical_classificationEcologyRare-earth elementAuthigenicParticulatesREE; Mediterranean; Ce anomalyREESettore GEO/08 - Geochimica E VulcanologiachemistryCe anomaly13. Climate actionEnvironmental chemistryGeneral Earth and Planetary SciencesSeawaterchlorophyll-YREE Ce anomaly Central Mediterranean late Quaternary Palaeoenvironmental reconstructionGeologyChemistry and Ecology
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Oedenburg. Une agglomération d’époque romaine sur le Rhin supérieur : fouilles françaises, allemandes et suisses à Biesheim-Kunheim (Haut-Rhin)

2005

Die römische Fundstelle Oedenburg (Biesheim-Kunheim, Haut-Rhin, France) wird seit 1998 von einem international Team ausgegraben (Ecole pratique des hautes études, Paris, Universität Freiburg im Breisgau, Deutschland, Universität Basel, Schweiz). Gegenüber dem keltischen Oppidum von Breisach, nahe am heutigen Rhein gelegen, war die Siedlung in einer deutlich anderen Landschaft angelegt worden, die damals von verschiedenen Flussarmen durchzogen war. Nach dem bisherigen Stand der Erforschung scheint der Ort zu Beginn der tiberischen Zeit von einem Militärlager besetzt gewesen zu sein, das zum Kommandobereich von Vindonissa im Nordteil des Territoriums der Rauriker gehörte. Zur gleichen Zeit en…

Archeologysanctuaryagglomération secondaireRoman army ; church ; fortress ; palatium ; Valentinian ; archaeobotany ; archaeozoology ; palaeoenvironment ; sanctuary ; vicus ; military camp ; limes ; Rauraci ; Oedenburgchurch010502 geochemistry & geophysics01 natural sciencesmilitary campArchäozoologieRauraciforteresseBefestigungarmyOedenburgpalaeoenvironmentOedenburg ; Rauriker ; römische Armee ; Limes ; Militärlager ; Vicus ; Tempel ; antike Umwelt ; Archäozoologie ; Archäobotanik ; Valentinian ; Palatium ; Befestigung ; Kirchearmée romaineRaurikersanctuaireAlsacearchaeozoologyBiesheimKunheimPalatiumégliseantike Umwelt010506 paleontology[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistorypaléobotaniquecamparchéozoologiepaléoenvironnementTempelArchäobotanikéglise ; Oedenburg ; Rauraques ; armée romaine ; limes ; camp ; agglomération secondaire ; temples ; paléoenvironnement ; archéozoologie ; paléobotanique ; Valentinien ; palais ; forteressetemple0105 earth and related environmental sciencesRauraquesDépartement du Haut-Rhinrömische ArmeepalaisMilitärlagerValentinianagglomération13. Climate actionValentinienKirchefortressLimes[SHS.HIST]Humanities and Social Sciences/HistoryarchaeobotanyVicusGrand Est
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Chemostratigraphy of the early Pliocene diatomite interval from MIS AND-1B core (Antarctica): Palaeoenvironment implications

2013

The AND-1B drill core (1285m-long) was recovered, inside the ANDRILL (ANtarctic geological DRILLing) Program, during the austral summer of 2006/07 from beneath the floating McMurdo Ice Shelf. Drilling recovered a stratigraphic succession of alternating diamictites, diatomites and volcaniclastic sediments spanning about the last 14Ma. A core portion between 350 and 480mbsf, including a 80m-thick diatomite interval recording the early Pliocene warming event, was investigated in term of opal biogenic content and element geochemistry. Across the diatomite interval, in spite of the lithological uniformity, a fluctuating biogenic opal profile mirrors the δ18O record, testifying a decrease in prod…

Global and Planetary Changepalaeoenvironment010504 meteorology & atmospheric sciencesδ18OTerrigenous sedimentBiogenic opal; element geochemistry; palaeoenvironmentGeochemistryAuthigenic010502 geochemistry & geophysicsOceanographyMbsf01 natural sciencesBiogenic opalDiagenesisSedimentary depositional environmentPaleontology13. Climate actionChemostratigraphyGlacial periodelement geochemistryGeology0105 earth and related environmental sciencesGlobal and Planetary Change
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First xiphosuran traceway in the middle Muschelkalk facies (Middle Triassic) of the Catalan Basin (NE Iberian Peninsula)

2021

In the last decade, the first ichnoassamblages from the middle Muschelkalk facies (upper Anisian-middle Ladinian) of the Catalan Basin (NE Iberian Peninsula) have been discovered. Herein, the first xiphosuran trace fossils are described from the locality of Penya Rubí, a newly discovered ichnosite from the Catalan Basin. The finding opens a window into peri-Tethys ecosystems with coastal influence. The traceway is referred to the ichnogenus Kouphichnium, a locomotion trace attributed to xiphosurans. The traceway preserves telson grooves and different imprint morphologies from the various appendages. The traceway pattern and arrangement of the different traces suggest a crawling locomotion s…

Invertebrate ichnologyCoastal palaeoenvironmentgeographygeography.geographical_feature_categoryPaleontologyIntertidal zoneKouphichniumLadinianTrace fossilStructural basinMiddle TriassicQE701-760KouphichniumTelsonPaleontologyPeninsulaFaciesSedimentologyGeologySpanish Journal of Palaeontology
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8000 years of coastal changes on a western Mediterranean island: A multiproxy approach from the Posada plain of Sardinia

2018

Abstract A multi-proxy palaeoenvironmental investigation was conducted to reconstruct the Holocene history of coastal landscape change in the lower Posada coastal plain of eastern Sardinia. In the Mediterranean region, coastal modifications during the Holocene have been driven by a complex interplay between climate, geomorphological processes and human activity. In this paper, millennial-scale human-sea level-environment interactions are investigated near Posada, one of the largest coastal plains in eastern Sardinia. Biostratigraphic and palynological approaches were used to interpret the chrono-stratigraphy exhibited by a series of new cores taken from the coastal plain. This new study elu…

Mediterranean climate010506 paleontologyCoastal evolution010504 meteorology & atmospheric sciencesHUMAN IMPACTCoastal plainpalaeoenvironmental reconstructionsCLIMATE CHANGESPALEOENVIRONMENTAL RECONSTRUCTIONOceanographyPalaeoenvironmental reconstructions01 natural scienceseastern sardiniaPrehistoryGeochemistry and PetrologyMediterranean Seacoastal evolution; palaeoenvironmental reconstructions; sea-level changes; pollen; eastern sardinia; mediterranean seaBRONZE-AGEmediterranean seaHolocene0105 earth and related environmental sciencesSea-level changesShorePalynologygeographygeography.geographical_feature_categoryLAST 6000 YEARSSedimentGeologyEastern SardiniaRECONSTRUCTING PAST LANDSCAPESGEOARCHAEOLOGICAL EVIDENCEpollenTYRRHENIAN COASTPeriod (geology)PollenPhysical geographyALIMINI PICCOLOsea-level changesGeologycoastal evolution
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Middle Miocene foraminifera from Canals (Valencia, western Mediterranean). Biostratigraphic and palaeoenvironmental aspects

2020

The age and the palaeoenvironmental conditions of the tap marls outcroppings near the locality of Canals in the south of the Valencia Province (E Spain) are discussed. Based on the planktonic foraminifera assemblages, mainly the species Globorotalia praemenardii , these tap marls are dated as Serravallian in age (middle Miocene). The analysis of the foraminiferal assemblages suggests a relatively well-ventilated uppermiddle bathyal environment, with only a moderate oxygen deficiency throughout most of the studied section. The rather cool waters indicated by the planktonic foraminifera (e.g. Globigerina bulloides ) are compatible with the decreasing temperatures trend during the middle Mioce…

Mediterranean climatebiologyPaleontologyGlobigerina bulloidesbiology.organism_classificationQE701-760Bathyal zoneForaminiferaOceanographyforaminifera middle miocene biostratigraphy palaeoenvironment valencia spain.Benthic zoneMarlUpwellingGeologyRadiolariaSpanish Journal of Palaeontology
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Benthic foraminifera and environmental changes in the Quaternary of the western Mediterranean coast: the core of Xeraco, Valencia, Spain

2020

The evolution of the benthic foraminiferal assemblages from a 60 m core drilled in the Quaternary lagoon of Xeraco (Valencia, Spain) is studied. Two moments of warm climate, high sea-level and maximal marine influence in the lagoon have been identified. The first one at the base of the core, punctuated by highly frequent changes during the Upper Pleistocene, and the other one in the upper end of the series during the Holocene. The presence of a middle core section with low diversity and a nearly total absence of marine foraminifers is interpreted as a regressive interval of cold climate conditions linked to a glacial stage.

Mediterranean climatebiologyPleistocenePaleontologybiology.organism_classificationforaminifera quaternary palaeoenvironments xeraco valenciaQE701-760ForaminiferaPaleontologyOceanographyBenthic zoneStage (stratigraphy)Glacial periodQuaternaryGeologyHoloceneSpanish Journal of Palaeontology
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Geological context and micromammal fauna characterisation from the karstic infilling of La Pedrera (Albaida, Valencia, E Spain)

2020

La Pedrera is a new palaeontological site located south of the province of Valencia, between the Betic and Iberian Ranges, in a cavity filled with sediments inside a tufa formation. Roughly 260 fossil remains, corresponding to 14 taxa, have been recovered and studied from Unit III. Six rodents (Microtus sp., M. sp. gr. M. (Terricola) duodecimcostatus-lusitanicus, Microtus sp. gr. M. brecciensis-cabrerae, Arvicola sapidus, Eliomys quercinus, and Apodemus sp. gr. sylvaticusfl avicollis), one lagomorph (Oryctolagus cf. cuniculus), three insectivores (Soricinae indet., Crocidura sp., and Talpa cf. europaea) and four bats (Myotis blythii, Rhinolophus cf. ferrumequinum, Myotis bechsteinii, and Rh…

RhinolophusbiologyEcologyMyotis blythiibiochronology palaeoenvironment palaeoclimate mutual ecogeographic range method hitat weighting methodPaleontologyRhinolophus euryalebiology.organism_classificationQE701-760GeographyCrociduraApodemusArvicolaTalpaEliomys
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PALAEOECOLOGY AND TAPHONOMY OF THE STRAIGHT-TUSKED ELEPHANT LATE MIDDLE PLEISTOCENE SITE OF POGGETTI VECCHI (SOUTHERN TUSCANY, ITALY)

2018

Works for the construction of thermal pools at Poggetti Vecchi, near Grosseto (Tuscany, Italy) exposed an accumulation of fossil bones, largely belonging to the straight-tusked elephant Palaeoloxodon antiquus, mixed up with stone and wooden tools. The site is radiometrically dated to the late Middle Pleistocene, and the artefacts were thus created by early Neanderthals. Palaeobiological and taphonomic analyses of the fauna remains are part of a more general, multiproxy study of the site that provides new information on MIS 7-6 transition, as well as on human-animal interactions.

Settore GEO/01 - Paleontologia E PaleoecologiaPalaeoclimate palaeoenvironment reconstruction palaeobiology taphonomy elephants
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