Search results for "ef"

showing 10 items of 32085 documents

A mitogenome sequence of an Equus hydruntinus specimen from Late Quaternary site of San Teodoro Cave (Sicily, Italy)

2020

Abstract Equus hydruntinus was a small equid that ranged from the Iberian Peninsula to Middle East. In Italy it has been considered present from the Middle Pleistocene to its extinction in the Middle-Late Holocene. E. hydruntinus shares plesiomorphic traits with other known Pleistocene equids. As a consequence, its classification has always been problematic. Genetic analyses on few fossil remains from Iran and Crimea have revealed that E. hydruntinus was more closely related to extant hemiones. To further investigate its systematic position, using target-enrichment capture and next-generation sequencing, we reconstructed a near complete mitogenome of a specimen from San Teodoro Cave from Si…

010506 paleontologyArcheology010504 meteorology & atmospheric sciencesPleistoceneWestern EuropeSettore BIO/08 - Antropologia01 natural scienceslaw.inventionEquus hydruntinuSan Teodoro CaveQuaternaryPaleontologyGlaciationRefugium (population biology)CaveMitochondrial genomelawRadiocarbon datingGlacial periodEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesGlobal and Planetary Changegeography.geographical_feature_categoryAncient DNAGeologyLGMGeographyAncient DNAQuaternary
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A new method for the identification of archaeological soils by their spectral signatures in the vis-NIR region

2020

Abstract This paper introduces a statistical method to identify spectral signatures of buried archaeological remains and distinguish them from spectra of the background soil in the visible to near infrared region. The proposed method is based on the Principal Component Analysis (PCA). The difference between an archaeological spectrum and non-archaeological soil spectra is quantified by a so-called R value. R values larger than 1 indicate that the spectrum represents an archaeological material. The method is successfully applied to samples from five study sites in Italy and Hungary with special conditions. The reflection spectra are taken in a time-efficient way with a field spectrometer. Th…

010506 paleontologyArcheologySpectral signature060102 archaeologySpectrometerNear-infrared spectroscopy06 humanities and the artsCC01 natural sciencesArchaeologyField (geography)Spectral linePrincipal component analysisReflection (physics)0601 history and archaeologySpectral resolutionGeology0105 earth and related environmental sciencesJournal of Archaeological Science: Reports
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Through diachronic discontinuities and regionalization: The contribution of the analysis of the lithic industries from Grotta della Serratura (Strata…

2019

Abstract Within the evolutionary dynamics of post-Gravettian techno-complexes, one can observe an intense regionalization phenomenon, both on a European scale, with the creation of two main provinces, and within the Italian peninsula. To date, typological studies have led to the recognition of several Italian Epigravettian facies, identifying trends, similarities, and differences in the lithic complexes. An important contribution was made by the technological method which in recent years has allowed us to identify the evolutionary processes of the lithic industries in numerous deposits of northern Italy. It is the intent of this reporting to add information which contributes to the debate o…

010506 paleontologyArcheologygeography.geographical_feature_category060102 archaeologyPleistoceneEpigravettianReference site06 humanities and the arts01 natural sciencesArchaeologyNorthern italy[SHS]Humanities and Social SciencesGeographyPeninsulaFaciesUpper Paleolithic0601 history and archaeologyStratigraphy (archaeology)0105 earth and related environmental sciences
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The relationships between soft-sediment deformation structures and synsedimentary extensional tectonics in Upper Triassic deep-water carbonate succes…

2016

Abstract We describe soft-sediment deformation structures into the Upper Triassic cherty limestone outcropping in the Pizzo Lupo section (Central Sicily, Italy), pertaining to the deep-water palaeodomain of the Southern Tethyan margin. In the study section, mainly consisting of thin-bedded mudstone/marl alternations with bedded chert intercalations, some lithofacies have been separated on the basis of the abundance of the calcium carbonate/clay content and the overall textural features. The deformational structures, displaying different deformational styles as folded and faulted beds, disturbed layers, clastic dikes, and slumps occur mainly in the deformed horizons that involve marl-dominat…

010506 paleontologyDikegeographygeography.geographical_feature_categorySettore GEO/02 - Geologia Stratigrafica E SedimentologicaStratigraphyGeology010502 geochemistry & geophysics01 natural sciencesSeafloor spreadingSoft-sediment deformation structuresSoft-sediment deformation structures Synsedimentary tectonics Upper Triassic deep-water carbonates Central SicilyPaleontologyContinental marginClastic rockMarlExtensional tectonicsSedimentary rockGeology0105 earth and related environmental sciencesSedimentary Geology
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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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Structure and evolution of a Messinian mixed carbonate-siliciclastic platform: the role of evaporites (Sorbas Basin, South-east Spain).

2010

36 pages; International audience; The Sorbas Member is a late Messinian complex sedimentary systemthat formed immediately following deposition of the Messinian evaporites in the Sorbas Basin (South-east Spain). This work describes the sequence architecture and facies organization of a continuous kilometre long, alluvial fan to open platform transect near the village of Cariatiz in the north-east of the basin. The postevaporitic Cariatiz platform was a mixed carbonate-siliciclastic system composed of four intermediate-frequency, fifth-order depositional sequences (Depositional Sequences 1 to 4) arranged in an overall prograding trend. The intense fracturing and brecciation of these deposits …

010506 paleontologyEvaporiteStratigraphy[SDE.MCG]Environmental Sciences/Global Changeslate Messinian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentPaleontologyooidsooids.14. Life underwater0105 earth and related environmental sciencesmixed carbonate/siliciclastic platform[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryAlluvial fanmicrobialitesGeology[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/Tectonics15. Life on landEvaporite collapse and deformation[ SDE.MCG ] Environmental Sciences/Global Changes[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesOoidSiliciclasticSedimentary rockProgradationGeology
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Estimating “land use heritage” to model changes in archaeological settlement patterns

2016

International audience; In this paper, we present a method to calculate a “land use heritage map” based on the concept of “memory of landscape”. Such a map can be seen as one variable among others influencing site location preference, and can be used as input for predictive models. The computed values equate to an index of long-term land use intensity. We will first discuss the method used for creating the land use heritage map, for which kernel density estimates are used.We will then present the use of these land use heritage maps for site location analysis in two study areas in SE France. Earlier analyses showed that the influence of the natural environment on settlement location choice i…

010506 paleontologyIndex (economics)[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and Prehistory01 natural sciences[ SHS.GEO ] Humanities and Social Sciences/Geographysocio-cultural variablesOrder (exchange)memory of landscape0601 history and archaeologyRural settlement[ SHS.STAT ] Humanities and Social Sciences/Methods and statistics0105 earth and related environmental sciencesheritage map[SHS.STAT]Humanities and Social Sciences/Methods and statistics060102 archaeologyLand usePredictive modelling06 humanities and the arts[SHS.GEO]Humanities and Social Sciences/Geography15. Life on landArchaeologyPreferenceVariable (computer science)Geography[ SHS.ARCHEO ] Humanities and Social Sciences/Archaeology and Prehistorysettlement pattern analysisSettlement (trust)Predictive modelling
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Le système palatial franc: genèse et fonctionnement dans le nord-ouest du regnum

1990

Barbier Josiane. Le système palatial franc : genèse et fonctionnement dans le nord-ouest du regnum.. In: Bibliothèque de l'école des chartes. 1990, tome 148, livraison 2. pp. 245-299.

010506 paleontologyLinguistics and LanguageHistory060102 archaeologyCapitales et chefs-lieux06 humanities and the artsStructures administratives01 natural sciencesLanguage and LinguisticsRituels politiques[SHS.HIST] Humanities and Social Sciences/History0601 history and archaeology[SHS.HIST]Humanities and Social Sciences/History0105 earth and related environmental sciences
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Uneven Data Quality and the Earliest Occupation of Europe—the Case of Untermassfeld (Germany)

2017

AbstractThe database regarding the earliest occupation of Europe has increased significantly in quantity and quality of data points over the last two decades, mainly through the addition of new sites as a result of long-term systematic excavations and large-scale prospections of Early and early Middle Pleistocene exposures. The site distribution pattern suggests an ephemeral presence of hominins in the south of Europe from around one million years ago, with occasional short northward expansions along the western coastal areas when temperate conditions permitted. From around 600,000-700,000 years ago Acheulean artefacts appear in Europe and somewhat later hominin presence seems to pick up, w…

010506 paleontologyProvenance060101 anthropologyEarly PleistocenePleistoceneEphemeral keyExcavation06 humanities and the arts01 natural sciencesArchaeologyPaleontologyGeographyData qualityPeriod (geology)Hominin dispersal ; Early Pleistocene ; Europe ; Bone modifications ; Lower Palaeolithic ; Pseudo-artefacts0601 history and archaeologyAcheulean0105 earth and related environmental sciencesJournal of Paleolithic Archaeology
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Facies variations in response to Holocene sea-level and climate change on Bora Bora, French Polynesia: Unravelling the role of synsedimentary siderit…

2017

International audience; Five mixed carbonate-siliciclastic sedimentary facies were identified in the barrier-reef lagoon of Bora Bora using microfacies and statistical analyses of 70 sediment samples taken at high resolution from two vibrocores. Fades and fades successions were interpreted with respect to Holocene sea-level and climate changes. The windward lagoon core is characterized by sideritic marly wackestones and foraminifera-sideritic wackestones, deposited around 7700 years BP (years before present) during the early-mid Holocene transgression. At that time, extensive weathering and erosion of iron-bearing minerals from the volcanic island, due to a wetter climate, were expressed in…

010506 paleontology[SDU.STU]Sciences of the Universe [physics]/Earth Sciences010502 geochemistry & geophysicsOceanography01 natural sciencesForaminiferaSideritechemistry.chemical_compoundGeochemistry and Petrology14. Life underwaterLithificationReefComputingMilieux_MISCELLANEOUSHolocene0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyGeologybiology.organism_classification6. Clean waterOceanographychemistry13. Climate action[SDE]Environmental SciencesSiliciclasticProgradationGeologyMarine transgression
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