Search results for "Sect"

showing 10 items of 10622 documents

Arqueoentomología y arqueobotánica de los espacios de almacenamiento a largo plazo: el granero de Risco Pintado, Temisas (Gran Canaria)

2019

This contribution aims at understanding the storage techniques used in the past by means of studying the entomological and plant remains present in the pre-hispanic granary of Risco Pintado, dated between the IX and XV centuries cal AD.This type of granary groups together a large number of silos excavated in the volcanic tuff, situated on steep escarpments, difficult to access and easy to defend.The exceptional environmental conditions of these infrastructures have allowed the desiccated remains of the stored plant products and the pests associated with such storage to be preserved within the silos.The domestic species documented include cereals (barley and wheat), legumes (broad beans and …

010506 paleontologyArcheologyPlant remainsCanary IslandsGranary01 natural sciencesInsecticidasIslas CanariasAlimentos0601 history and archaeologyGraneros en cuevasGranaries in caveInsecticideRestos vegetales0105 earth and related environmental sciencesPrehispanicPrehispánico060102 archaeologybiologyWeevil06 humanities and the arts15. Life on landPlagas de insectosbiology.organism_classificationGeographyArchaeologyAgronomyBroad beansFoodInsects pestsCC1-960Trabajos de Prehistoria
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Ceramic raw materials: how to recognize them and locate the supply basins—mineralogy, petrography

2020

This tutorial paper is focused on the mineralogical-petrographic characterization of clayey raw materials with the purpose of sourcing supply basins and answering questions about the provenance of the corresponding archaeological ceramic artefacts. The first part gives general indications of how to profitably study archaeological ceramic thin sections through the polarizing microscope. Brief notes are provided on the theoretical basis of optical microscopy. A scheme is then provided for the petrographic description of ceramic samples, concerning the textural and compositional characteristics of aplastic inclusions and groundmass. Suggestions are also given for identifying any minero-petrogr…

010506 paleontologyArcheologyProvenance060102 archaeologyArchaeoceramics Clays analysis Polarizing optical microscopy Raw materials for ceramic production Thin section mineralogy and petrographyPlan (archaeology)06 humanities and the artsRaw materialField survey01 natural sciencesCharacterization (materials science)PetrographyMining engineeringAnthropologyvisual_artvisual_art.visual_art_medium0601 history and archaeologyCeramicGeology0105 earth and related environmental sciencesArchaeological and Anthropological Sciences
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Sierra del Colmenar 1A, a new late Messinian (Late Miocene) locality in the Bajo Segura Basin (SE Spain): biostratigraphic and palaeoenvironmental im…

2017

In this paper, we have studied a new micromammal site from the Sierra del Colmenar section (Elche, SE Spain), named Sierra del Colmenar 1A (SCO-1A), representing the uppermost levels of Messinian age of the Bajo Segura Basin. The sedimentary context of this locality corresponds to a costal lagoon with marine influence. The fossil site has yielded remains of Apodemus aff. gorafensis, Paraethomys meini, Apocricetus alberti, Occitanomys alcalai, Ruscinomys sp., Eliomys cf. truci, Muscardinus sp., Parasorex ibericus, Prolagus michauxi and Soricidae indet. Based on this assemblage, we propose a Late Miocene age (MN13) for the locality SCO-1A, matching the previously inferred age for the stratigr…

010506 paleontologyBajo Segura BasinEstratigrafíaRodentiaParaethomysLate MioceneStructural basin010502 geochemistry & geophysics01 natural sciencesPaleontologyMessinianSection (archaeology)TurolianGeneral Agricultural and Biological SciencesGeology0105 earth and related environmental sciencesHistorical Biology
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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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A new species ofPlesiodimylus(Dimylidae, Eulipotyphla, Mammalia) from the Early Miocene of Spain

2017

AbstractWe report a new dimylid species, Plesiodimylus ilercavonicus sp. nov., from the Early Miocene locality of Mas d’Antolino B-5 (Ribesalbes-Alcora, Castello, Spain). This new species of Plesiodimylus is an amblyodont form of the genus and exhibits some primitive characters. The phylogenetic and palaeoenvironmental implications of this southern occurrence of Plesiodimylus in Lower Miocene sediments are discussed.urn:lsid:zoobank.org:act:EB5435A4-EECE-4B88-B5AC-4B77E2E13029

010506 paleontologyLSIDPhylogenetic treeEcologyZoologyInsectivoreBiology010502 geochemistry & geophysicsSoricomorphabiology.organism_classification01 natural sciencesGenusGeneral Agricultural and Biological Sciences0105 earth and related environmental sciencesHistorical Biology
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The Borschovo section of the Gauja and Amata regional stages (Leningrad Region, Russia): sedimentology and biostratigraphy

2018

The results of the detailed sedimentological study and bed-by-bed collecting of fossils from the Borschovo section exposing the upper Givetian–lower Frasnian boundary beds are discussed. The succession consists of sandstones alternating with argillaceous and clayey packages that contain vertebrate and plant remains in the upper part. The grain size, sedimentary structures and cross-bed orientation considerably differ in the Oredezh Beds and the Staritsa Beds. Fine- to coarse-grained cross-stratified sandstones of the Oredezh Beds most probably are fluvial deposits, whereas the sandstones of the Staritsa Beds yielding tidal structures that show variable directions of the cross-bedding were a…

010506 paleontologyMiddle–Upper Devonianbiologylcsh:QE1-996.5Biostratigraphy010502 geochemistry & geophysicsbiology.organism_classification01 natural scienceslcsh:GeologyPaleontologyAmataSection (archaeology)sedimentary environmentGeneral Earth and Planetary Sciencessiliciclastic depositsSedimentologyvertebrate assemblage.Geology0105 earth and related environmental sciencesWater Science and TechnologyEstonian Journal of Earth Sciences
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Climatic fluctuations and seasonality during the Late Jurassic (Oxfordian–Early Kimmeridgian) inferred from delta18O of Paris Basin oyster shells.

2008

10 pages; International audience; Oxygen isotope data from biostratigraphically well-dated oyster shells from the Late Jurassic of the eastern Paris Basin are used to reconstruct the thermal evolution of western Tethyan surface waters during the Early Oxfordian–Early Kimmeridgian interval. Seventy eight oyster shells were carefully screened for potential diagenetic alteration using cathodoluminescence microscopy. Isotope analyses were performed on nonluminescent parts of shells (n=264). Intra-shell δ18O variability was estimated by microsampling along a transect perpendicular to the growth lines of the largest oyster shell. The sinusoidal distribution of the δ18O values along this transect …

010506 paleontologyOysterδ18O[SDE.MCG]Environmental Sciences/Global ChangesJurassic010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesIsotopes of oxygenPaleontologycarbonateGeochemistry and Petrology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrybiology.animalParis BasinEarth and Planetary Sciences (miscellaneous)medicinepaleotemperatureBathymetry14. Life underwaterTransect0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontologybiologyoxygen isotopesSeasonalitymedicine.disease[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryDiagenesisWaves and shallow water[ SDE.MCG ] Environmental Sciences/Global ChangesGeophysicsOceanography13. Climate actionSpace and Planetary Science[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphyoysters[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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Comments on: A review of the evolution, biostratigraphy, provincialism and diversity of Middle and early Late Triassic conodonts

2016

010506 paleontologyPaleontologySection (archaeology)media_common.quotation_subjectPaleontologyBiostratigraphy010502 geochemistry & geophysics01 natural sciencesGeology0105 earth and related environmental sciencesDiversity (politics)media_commonPapers in Palaeontology
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Stage boundaries, global stratigraphy, and the time scale: towards a simplification

2004

International audience; This paper examines four facets of stratigraphic terminology and usage considered faulty and proposes corrective measures. The four perfectible areas are: (1) The system of dual nomenclature requiring discrete terminologies for the superpositional and temporal aspects of rock units. (2) The premise that a GSSP establishes the base of a stage as being coincident with the top of the preceding stage rather than simply defining it as the boundary between stages. (3) The rejection of supplementary (auxiliary) sections that would broaden the knowledge of a GSSP and enlarge the area in which it is easily usable. (4) The current dual system of nomenclature for Precambrian an…

010506 paleontologyPrecambrian-Cambrian boundaryComputer scienceStratigraphyPhanerozoiccomputer.software_genre[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesCampanian-Maastrichtian boundaryBoundary (real estate)Terminologylcsh:StratigraphyStage (stratigraphy)Stages010503 geologyStratigraphy (archaeology)lcsh:QE701-7600105 earth and related environmental scienceslcsh:QE640-699GSSPChronostratigraphybusiness.industryScale (chemistry)Plio-Quaternarylcsh:QE1-996.5PaleontologyGeologyTerminologyPlio- QuaternaryCretaceous- Palaeogene boundaryDual (category theory)Global Boundary Stratotype Section and Pointlcsh:GeologyCretaceous-Palaeogene boundarylcsh:Paleontology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPremise[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyArtificial intelligencebusinessPrecambriancomputerNatural language processing
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Depositional environments and iron ooid formation in condensed sections (Callovian Oxfordian, South-eastern part of the Paris basin, France)

2005

Carbonate platforms across Western Europe were superseded at the Middle–Upper Jurassic (Callovian–Oxfordian) boundary either by alternating marl–limestone and widespread marl deposits or by condensed sections containing iron ooids. The characteristics of marine condensed sections in the south-eastern part of the Paris Basin (France) and their distribution pattern are examined here, and a model of iron ooid formation is developed. Iron ooids are found from the shoreface to the offshore zone. They are most abundant in the median-to-distal offshore transition zone, where they originally formed. They also occur commonly, albeit often as reworked grains, in the proximal offshore zone, to which t…

010506 paleontologyRecrystallization (geology)GoethiteStratigraphyCallovianiron ooidsGeochemistry[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesoxfordianSedimentary depositional environmentPaleontologychemistry.chemical_compoundcondensed sectionsMarlTransition zone14. Life underwater0105 earth and related environmental sciencesGeologyDiagenesischemistryvisual_art[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyOoidvisual_art.visual_art_mediumCarbonateGeologydepositional environments
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