Search results for "Cer"

showing 10 items of 24496 documents

The response of a shallow lake and its catchment to Late Glacial climate changes — A case study from eastern Poland

2015

In this study we investigate how climate fluctuation in the Late Glacial period influenced the development of a lake and its catchment located in the East European Plain. We analyzed the sediments of the lake for pollen, subfossil Cladocera, macrofossils and chemical composition. We aimed at disentangling: (1) the climate changes and their limno-ecological responses, (2) temperature dynamics with the use of Cladocera-based transfer function (MJT) and macrofossil-based reconstruction of mean minimum July temperature (MMJT), (3) timing of the response of different proxies to environmental changes. The results of multiproxy analyses explicitly suggest that the main driver for changes in aquati…

010506 paleontology010504 meteorology & atmospheric sciencesta1171lake sedimentsDrainage basinClimate change01 natural sciencesAllerød oscillationGlacial periodYounger Dryas0105 earth and related environmental sciencesEarth-Surface Processesgeographygeography.geographical_feature_categorySubfossilMacrofossil15. Life on landcatchment developmentsubfossil cladocera13. Climate actionClimatologylate glacialmulti-proxy analysista1181Terrestrial ecosystemPhysical geographyEast European plainGeology
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Environmental and climatic controls of the clay mineralogy of Albian deposits in the Paris and Vocontian basins (France)

2020

18 pages; International audience; High-resolution clay mineral analyses were performed on lower and middle Albian deposits from the Paris and Vocontian basins in order to specify the weathering conditions that prevailed at that time. The clay mineral assemblages are composed of small proportions of chlorite and vermiculitic clays associated with abundant illite, R0 type illite-smectite mixed-layers (smectite) and kaolinite. Clay minerals originated from the physical alteration and chemical weathering of rocks and soils outcropping on the Variscan massifs bordering the studied areas. In the Paris Basin, the covariation of illite and kaolinite suggests the reworking of these latter minerals f…

010506 paleontologyAptianOutcropGeochemistryWeatheringengineering.materialPalaeoclimate010502 geochemistry & geophysics01 natural sciencesParis BasinKaoliniteMortoniceras0105 earth and related environmental sciencesgeographygeography.geographical_feature_categorybiologyPaleontologyAlbianMassifbiology.organism_classificationClay mineralsVocontian Basin13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyIlliteengineeringClay mineralsGeologyCretaceous Research
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New results in ancient Maya rituals researches: The study of human painted bones fragments from Calakmul archaeological site (Mexico)

2020

Abstract The funeral chambers of the ancient city of Calakmul (Mexico) and the individuals who were buried in them have brought in recent decades new knowledge about the beliefs and funeral customs of the pre-Hispanic Maya. Tombs and bodies were prepared as part of the rituals that should favor the return of ch'ulel to the Underworld, known as Xibalba by the ancient Maya. The ch'ulel is one of the two anemic entities that inhabit the individual, equivalent to our concept of the soul. Bodies preparation included coloured scented body ointments application, with a deep symbolic connotation and probably also a conservative purpose. The aim of this research was to characterize pigments and bind…

010506 paleontologyArcheologyAncient citymedia_common.quotation_subjectCalakmulMortuary ceremoniesTransmitted lightClassic periodHuman bone01 natural sciencesNatural gumSEM-EDXMaya0601 history and archaeologyGC–MSSettore CHIM/12 - Chimica dell'Ambiente e dei Beni Culturali0105 earth and related environmental sciencesmedia_commonPainted dead bodies060102 archaeologyHevea Brasilliensis06 humanities and the artsArtArchaeologyPy-GC-MSOrganic fractionCinnabarMayaOrganic componentMaya Calakmul Classic period Painted dead bodies Mortuary ceremonies SEM-EDX GC–MS Py-GC-MS Natural gum Hevea BrasilliensisAncient maya
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The production of traditional building materials in Oristano (Sardinia, Italy)

2016

The study of ceramic-making communities which employ traditional practices can provide insights into the raw materials and techniques used over the centuries in a particular territory. The archaeometric study of ceramic products and of the raw materials used in their production is an effective complement to the existing ethnographic information. This paper focuses on the brick and tile making tradition of Oristano, a town in Central-Western Sardinia (Italy). Applying a combination of techniques, it includes an extensive analysis of traditional handmade and early industrial bricks and tiles, and a study of the local clays that may have been used as raw materials. Although we were unable to s…

010506 paleontologyArcheologyArchitectural engineeringEthnoarchaeologyBrick060102 archaeology06 humanities and the artsEthnoarchaeologySardinia01 natural sciencesArchaeologyOristanoClayey raw materialsGeographyEthnoarchaeometryAnthropologyvisual_artvisual_art.visual_art_mediumProduction (economics)0601 history and archaeologyTileBrick and tileTraditional ceramic manufactureSettore GEO/09 -Georis. Miner.e Appl.Mineral.-Petrogr. per l'Ambi.ed i B.Cult.0105 earth and related environmental sciencesArchaeological and Anthropological Sciences
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Late Weichselian and Holocene record of the paleoenvironmental changes in a small river valley in Central Poland

2016

Abstract: The developmental history, from the Oldest Dryas to the Late Holocene, of a paleolake and mire located in a river valley in Central Poland was studied using high-resolution records of pollen, macrofossils, Cladocera, sedimentology, and geochemistry from a 14 C dated sediment core. We inferred temperature and water level dynamics using cladocerans and palynological and geochemical methods were employed to investigate natural fluvial activity, particularly for these elements that are difficult to find through sedimentological methods. Our research demonstrates how climate fluctuation in the Late Glacial and Holocene periods influenced the development of a paleolake and mire in a sma…

010506 paleontologyArcheologyOldest Dryasta1171010502 geochemistry & geophysics01 natural sciencesAllerød oscillationPaleontologyIce corePaleoclimatologypaleoclimateYounger DryasGlacial periodEcology Evolution Behavior and SystematicsHolocene0105 earth and related environmental sciencesGlobal and Planetary ChangeHoloceneMacrofossilGeology15. Life on landCladoceraLate Glacial13. Climate actionmultiproxy analysisPhysical geographyGeologyQuaternary Science Reviews
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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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The global bio-events at the Cenomanian-Turonian transition in the reduced Bahloul Formation of Bou Ghanem (central Tunisia).

2010

In central Tunisia, the thickness of the Bahloul Formation varies generally between 20 to 40 m such as for example, respectively, at wadi Smara near Kalaat Senan and at wadi Bahloul near Maktar. The thickness is also of several tens metres at Koudiat el Azreg near Jerissa and at Tajerouine. In these sites where the thickness of the Bahloul Formation is dilated, in addition to five geochemical events (d13C), nine bio-events were defined near the Cenomanian-Turonian transition, successively in ascending order: 1. LO Rotalipora cushmani, 2. Heterohelix bio-event, 3. FO Pseudaspidoceras pseudonodosoides, 4. LO P. pseudonodosoides, 5. LO Thalmanninella multiloculata, 6. “filaments” bio-event, Ce…

010506 paleontologyBahloul Formationfood.ingredientTunisia010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyfoodStratotypeStage (stratigraphy)Cenomanian-Turonian boundaryCenomanianWadi0105 earth and related environmental sciencesgeographyLaminated faciesgeography.geographical_feature_categoryPaleontologyTuronianWatinocerasCretaceous[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyBio-eventsCenomanianGeology
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Changes of shell microstructural characteristics of Cerastoderma edule (Bivalvia) — A novel proxy for water temperature

2017

Abstract Shells of bivalves potentially provide an excellent archive for high-resolution paleoclimate studies. However, quantification of environmental variables, specifically water temperature remains a very challenging task. Here, we explore the possibility to infer water temperature from changes of microstructural characteristics of shells of the common cockle, Cerastoderma edule . The size and elongation of individual microstructural units, i.e., prisms, in the outer shell layer of seven three to five year-old, specimens collected alive from the intertidal zone of the North Sea near Texel, The Netherlands, and Schillig, Germany, were measured by means of automatic image processing. Grow…

010506 paleontologyCerastoderma edule010504 meteorology & atmospheric sciencesbiologyPaleontologyMineralogyIntertidal zoneOceanographyBivalviabiology.organism_classification01 natural sciencesIsotopes of oxygenSalinityOceanographyTurbidityCockleBivalve shellEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface Processes
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A North American ammonite fauna from the late Middle Turonian of Vaucluse and Gard, southern France: the Romaniceras mexicanum, Prionocyclus hyatti a…

2016

Abstract An unusual, exotic, ammonite fauna including Romaniceras mexicanum Jones, 1938, Prionocyclus hyatti (Stanton, 1894) and Coilopoceras cf. springeri Hyatt, 1903 is recorded from the late Middle Turonian of Vaucluse and Gard, southern France. It is the first record of this ammonite association outside the Gulf Coast region and the Western Interior of the United States of North America. Up to present, these species were considered as endemic to the Western Interior sea-way. The migration of numerous ammonites from North America to western Europe during the late Middle Turonian suggests it is linked to a transgressive event or to a short sea-level high.

010506 paleontologyCoilopocerasFauna010502 geochemistry & geophysics01 natural sciencesCretaceousAmmonitidaPaleontologyAmmonitesMigration[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesAmmonitebiologyTransgressive eventGeologyTuronianbiology.organism_classificationlanguage.human_languageCretaceousSouthern FranceWestern europeNorth AmericalanguageTransgressiveGeologyActa Geologica Polonica
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Report on the 4th International Meeting of the IUGS Lower Cretaceous ammonite working group, the "Kilian Group" (Dijon, France, 30th August 2010).

2011

8 pages; International audience; The 4th Kilian Group meeting (Dijon, France, 30th August 2010) focused on the Aptian and Albian Stages. For the Aptian, a two-fold division of the stage was adopted for the Mediterranean area with a boundary between the Dufrenoyia furcata and Epicheloniceras martini Zones. The main changes to the zonal scheme concern the Lower Aptian with: the introduction of a Deshayesites luppovi Subzone in the upper part of the Deshayesites oglanlensis Zone; the replacement of Deshayesites weissi by Deshayesites forbesi as new indexspecies of the second interval zone; the introduction of a Roloboceras hambrovi Subzone in the upper part of the D. forbesi Zone; and the subd…

010506 paleontologyKilian GroupAptian010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyStage (stratigraphy)AmmonitesGroup (stratigraphy)Lower CretaceousAptianMortoniceras0105 earth and related environmental sciences[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/PaleontologyAmmonitebiologyDouvilleicerasPaleontologyAlbianbiology.organism_classificationCretaceouslanguage.human_language[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyStandard zonationDipoloceraslanguage[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyGeology
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