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showing 10 items of 23740 documents

Wildcat scats: Taphonomy of the predator and its micromamal prey

2019

Small sized felids, such as wild and domestic cats, are one of the most common predators in the nature and in sites occupied by humans in archaeological and historical contexts. Wildcats have ingestion/ digestion traits highly destructive for their prey, i.e.: teeth to chew causing extreme breakage, and digestion along the entire digestive tract with low pH gastric juices causing extreme bone corrosion. Small sized cats are also well known to play with the prey and select skeletal parts to ingest. The present study is focused on the taphonomic analysis of micromammal remains recovered from scats produced by European wildcats (Felis silvestris silvestris) during several months and years. Exc…

010506 paleontologyArcheologyTaphonomy010504 meteorology & atmospheric sciencesZoologyMicromammals01 natural sciencesPredationFelis silvestris silvestris WildcatTaxonomic compositionAbundance (ecology)Taxonomic rankPredatorEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary ChangebiologyFelisGeologybiology.organism_classificationCarnivoresTaphonomyFelidsDigestionMontes do Invernadeiro Natural Park (Galicia Spain)
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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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Volcanic climate forcing preceding the inception of the Younger Dryas: Implications for tracing the Laacher See eruption

2021

Climatic warming from the last glacial maximum to the current interglacial period was punctuated by a similar to 1300 years long cold period, commonly referred to as the Younger Dryas (YD). Several hypotheses have been proposed for the mechanism triggering the abrupt inception of the YD, including freshwater forcing, an extra-terrestrial impact, and aerosols from volcanic eruptions. Here, we use synchronised sulphate and sulphur records from both Greenland and Antarctic ice cores to reconstruct volcanic forcing between 13,200-12,800 a BPGICC05 (years before 1950 CE on the Greenland Ice Core Chronology 2005; GICC05). This continuous reconstruction of stratospheric sulphur injections highligh…

010506 paleontologyArcheologyYounger Dryas010504 meteorology & atmospheric sciences530 PhysicsCIRCULATIONIce cores; Laacher See eruption; Sulphate; Volcanic radiative forcing; Younger DryasSULFURForcing (mathematics)01 natural sciencesVolcanic radiative forcingANTARCTIC ICE-CORESOCEANIce coreCHRONOLOGYYounger Dryas550 Earth sciences & geologyEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesGlobal and Planetary Changegeographygeography.geographical_feature_categoryGeologyLast Glacial MaximumRECORDWAIS DIVIDESulphateRadiative forcingGREENLANDLaacher See eruptionVolcano13. Climate actionIce coresClimatologySYNCHRONIZATIONInterglacialClimate modelSULFATEGeologyQuaternary Science Reviews
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Importation de grands animaux romains et amélioration du cheptel à la fin de l'Âge du Fer en Gaule Belgique

1996

Méniel Patrice. Importation de grands animaux romains et amélioration du cheptel à la fin de l'Âge du Fer en Gaule Belgique. In: Revue archéologique de Picardie, n°3-4, 1996. Table-ronde de Ribemont-sur-Ancre (Somme): la chronologie du second âge du fer en Gaule du Nord / La ferme laténienne de Jaux (Oise) et sa nécropole. pp. 113-122.

010506 paleontologyArcheology[SHS.ARCHEO] Humanities and Social Sciences/Archaeology and Prehistory[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory060102 archaeologygrand bœufimportation06 humanities and the artsgrand chevalostéométriearchéozoologie01 natural sciencesGaule BelgiqueLa Tène[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and Prehistory0601 history and archaeology0105 earth and related environmental sciencesPériodiques Scientifiques en Édition Électronique
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Analysis of stratigraphical sequences at Cocina Cave (Spain) using rare earth elements geochemistry

2021

This study investigates the stratigraphical sequence of Cocina Cave (Spain) employing and testing for the first time the capability of rare earth elements as markers of human activities in caves. Located in Dos Aguas (Valencian Community, Spain), Cocina Cave is characterized by the presence of several Holocene archaeological deposits from the final Mesolithic to the present day and is a pivotal site for understanding the socio‐ecological dynamics of the last hunter‐gatherer inhabitants of the Iberian Peninsula and the transition to pastoral and agricultural economies in the Western Mediterranean. However, the identification of strata from particular time‐periods in the cave is often difficu…

010506 paleontologyArcheologygeographygeography.geographical_feature_category060102 archaeologyRare earthGeochemistryGeology06 humanities and the arts15. Life on land01 natural scienceshumanitiesCave0601 history and archaeologyEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesBoreas
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New data about the landscape of the first occupation of Mallorca: Coval Simó (Escorca, Mallorca)

2020

The Coval Simó shelter provides some of the oldest evidence for settlement on the island of Mallorca and the Balearic archipelago. It also has the peculiarity of being a habitat in a mountain area, so that the human groups that settled there had to adapt their agricultural and farming sys­tem to this environment. The plant remains (wood charcoal and seeds) recovered in the occupation levels allow us to address these issues, since they are the result of the different activities developed in this cavity: fuel for domestic activities, food for livestock, etc. The results of this study show that between the III and II millennium cal BC, an agricultural system based on livestock and cereal farmi…

010506 paleontologyArcheologypaisaje de montañaMajorca Islandprehistoria recienteBell BeakerFirewood01 natural sciencesisla de mallorcaprimer poblamiento estableLate PrehistoryFirst settlementFarming system0601 history and archaeologysistema agropecuarioCharcoalmacrorrestos vegetales0105 earth and related environmental sciencesgeographygeography.geographical_feature_category060102 archaeologybiologybusiness.industryAgroforestry06 humanities and the artsbiology.organism_classificationcampaniformeHabitatArchaeologyAgriculturevisual_artArchipelagovisual_art.visual_art_mediumLivestockPlant macroremainsJuniperbusinessSettlement (litigation)Mountain landscapeCC1-960Trabajos de Prehistoria
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Astrochronology of the Valanginian Stage from reference sections (Vocontian Basin, France) and palaeoenvironmental implications for the Weissert Even…

2013

12 pages; International audience; High-resolution gamma-ray measurements performed on five biostratigraphically well-dated reference sections from the Vocontian Basin (south-eastern France) are used to develop a new astrochronology of the Valanginian Stage and its subdivisions (i.e. ammonite and calcareous nannofossil zones and subzones). Spectral analyses show a pervasive dominance of 405-kyr eccentricity cycles with the expression of 100-kyr eccentricity, obliquity and precession. Previous rough estimates of Valanginian Stage duration ranged from 3.9 to 6.5 myr but were generally based on less reliable or indirect methods. This study provides a precise duration of 5.08 myr, tuning the ser…

010506 paleontologyBiozone[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysicsOceanographyPalaeoclimate01 natural sciencesPaleontologyGeologic time scaleStage (stratigraphy)Ecology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesAmmoniteAstrochronologySeries (stratigraphy)High-resolution gamma-rayParaná-EtendekaPaleontologyCyclostratigraphylanguage.human_languageVocontian BasinStratigraphy13. Climate actionValanginian[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphylanguageGeologyWeissert Event
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Record of latest Barremian-Cenomanian environmental change in tectonically controlled depressions from the Jura-Burgundy threshold (Jura Mountains, e…

2019

Abstract The area of the western Jura Mountains constitutes the former Jura-Burgundy threshold between the Tethys Ocean and the epicontinental Paris Basin Sea. During the Barremian, the area was covered by a shallow-water Urgonian carbonate platform. Tectonic processes influenced the architecture of the Urgonian platform and were notably responsible for the formation of fault-related depressions on top of the Urgonian series, which were subsequently transformed into incised valleys and then to marine depocenters. Their sedimentary infills are mostly represented by the Perte-du-Rhone Formation and record stepwise environmental change on the innermost platform, which was strongly influenced b…

010506 paleontologyCarbonate platformPaleontologyStructural basin010502 geochemistry & geophysicsOceanographyTethys Ocean01 natural sciencesCretaceousPaleontology13. Climate actionMarlSedimentary rock14. Life underwaterCenomanianEcology Evolution Behavior and SystematicsGeologySea level0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Community replacement of neritic carbonate organisms during the late Valanginian platform demise: a new record from the Provence Platform.

2012

24 pages; International audience; The Valanginian is marked by amajor platform demise inducing a hiatus in the northern Tethyan neritic carbonate record from the top of the lower Valanginian to the lower Hauterivian. New biostratigraphic and chemostratigraphic data from the Ollioules section (Provence Platform, southern France) are presented here, demonstrating that a large part of the upper Valanginian is preserved in an inner platform environment. The thick, upper Valanginian, aggrading carbonate succession is observed in an aborted rift domain, implying relatively low subsidence. In this context, a relatively long-term sea-level rise was required to sustain a keep-up style of carbonate p…

010506 paleontologyCarbonate platformPlatform demiseContext (language use)010502 geochemistry & geophysicsOceanography[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural scienceschemistry.chemical_compoundPaleontology14. Life underwaterEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesRiftOllioules sectionTerrigenous sedimentCarbon isotopePaleontologySubsidencePhosphoruschemistryNeritic communitiesClastic rockValanginian[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyCarbonateGeologyMarine transgression
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Sr isotope variations in the Upper Triassic succession at Pizzo Mondello, Sicily: Constraints on the timing of the Cimmerian Orogeny

2018

Abstract The Late Triassic Cimmerian Orogeny was a result of the final closure of the Palaeotethys Ocean and the accretion of Gondwana-derived (Cimmerian) continents to southern Eurasia. Determining the timing of the Cimmerian Orogeny is crucial to our understanding of the large-scale climate changes driven by the uplift of the Cimmerian Mountains. Here we present stratigraphic variations in 87Sr/86Sr values of Upper Triassic pelagic limestone from the Pizzo Mondello section, Sicily, Italy, that constrain the timing of uplift of the Cimmerian Mountains. The 87Sr/86Sr values remain relatively constant in the lower part of the section, decreasing slightly in the Tuvalian (upper Carnian) and L…

010506 paleontologyCarnian; Cimmerian Mountains; Climate change; Limestone; Norian; Tethys; Oceanography; Ecology Evolution Behavior and Systematics; Earth-Surface Processes; PaleontologyEvolutionCimmerian MountainsClimate changeWeatheringEcological succession010502 geochemistry & geophysicsNorianOceanography01 natural sciencesPaleontologyBehavior and SystematicsClimate changeTethysEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesEarth-Surface ProcessesCarnianRadiogenic nuclideEcologyPaleontologyOrogenyTethys OceanLimestoneErosionAccretion (geology)Geology
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