Search results for "ck"

showing 10 items of 18632 documents

Intact seismic-scale platforms and ramps in the Lower to Middle Jurassic of Morocco: implications for stratal anatomy and lithofacies partitioning.

2017

9 pages; International audience; The Jurassic carbonate platforms of the central High Atlas in Morocco are well known for several high-quality outcrops. In the central High Atlas, there are two complementary locations that offer critical lessons for our understanding of Jurassic carbonate system evolution in extensional basins: a Lower Jurassic high-relief, carbonate platform with steep slopes that developed on the footwall of a rotating fault block in an active half-graben (Djebel Bou Dahar [DBD]) and an upper Lower to Middle Jurassic low-angle prograding carbonate ramp rich in ooids (Amellago ramp [AR]). The DBD and AR outcrops provide superbly exposed, structurally intact, and fully acce…

010506 paleontologyRiftCarbonate platformOutcropEnergy Engineering and Power TechnologyGeology010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesSedimentary depositional environmentchemistry.chemical_compoundPaleontologyFuel TechnologychemistryGeochemistry and Petrology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFaciesEarth and Planetary Sciences (miscellaneous)CarbonateFault blockHydrocarbon explorationGeology0105 earth and related environmental sciences
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Quaternary marine and continental unconformity-bounded stratigraphic units of the NW Sicily coastal belt

2017

In the coastal sector of NW Sicily, the regional correlation of relevant unconformities recognised within the Quaternary sedimentary successions allowed the mapping of seven unconformity-bounded stratigraphic units (UBSUs). The regional unconformities are marine or subaerial erosional surfaces, as well as non-depositional surfaces, locally marked by paleosoils. The erosional surfaces were produced from marine abrasion, surface water overland/concentrated flow, river erosion, karst solution, mass movement, or wind erosion. The main lithofacies of the Quaternary UBSUs consist of: (a) marine and coastal bioclastic calcarenites, (b) aeolian sandstones, (c) river deposits, (d) colluvial deposits…

010506 paleontologySettore GEO/02 - Geologia Stratigrafica E SedimentologicaNW Sicilyquaternary continental and marine depositsGeography Planning and DevelopmentGeochemistryquaternary continental and marine deposit010502 geochemistry & geophysics01 natural sciencesUnconformitylcsh:G3180-9980Earth and Planetary Sciences (miscellaneous)tectonicsclimateGeomorphologyUnconformity-bounded stratigraphic unit0105 earth and related environmental sciencesColluviumlcsh:Mapsgeographygeography.geographical_feature_categoryUnconformity-bounded stratigraphic unitsKarsttectonicsea-level changeTectonicsSubaerialErosionSedimentary rocksea-level changesQuaternaryGeologyUnconformity-bounded stratigraphic units; quaternary continental and marine deposits; tectonics; sea-level changes; climate; NW SicilyJournal of Maps
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Problems in the identity of "Crioceras" barremense Kilian, 1895 (Ancyloceratida, Late Barremian), and their proposed resolution

2010

17 pages; The study of "Crioceras" barremense KILIAN was undertaken as a part of the revision of the Hemihoplitidae. This species was considered "classic" and has been used as the index of an Upper Barremian subzone; this usage raises a number of problems. The type specimen from Tyrol was a fragment described and illustrated by UHLIG as Crioceras sp. ind. aff. roemeri. This specimen could not be retrieved, and a topotype could not be collected. Our study revealed that there is both a biostratigraphic hiatus and important differences between conceptions of this species: (1) that ascribed UHLIG's type specimen (Upper Barremian, Tyrol), (2) KILIAN's concept of the specimen he found and named "…

010506 paleontologyStratigraphyHiatusAmmonitinae[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesLower limitPaleontologylcsh:StratigraphyGenusmedicinelcsh:QE701-760Gassendiceras[ SDU.STU.PG ] Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesConfusionTaxonomylcsh:QE640-699Upper Barremianbiologylcsh:QE1-996.5PaleontologybiozonationGeologyAlpinum Subzonebiology.organism_classificationlcsh:GeologyBiohorizonlcsh:Paleontology[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyAlpinum Subzone / BiohorizonGassendiceratinae[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyType specimen[SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/PaleontologyVandenheckei Biozonemedicine.symptomsoutheastern France[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/PaleontologyCarnets de Géologie
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A little walk between Early Jurassic sponges and corals: a confusing morphological convergence.

2019

24 pages; International audience; Hispaniastraea Turnšek et Geyer, 1975 is a unique coral genus from the Early Jurassic Epoch (Liassic). Corals of this genus are characterised by a highly dominant major septum and a set of eleven minor septa that are very short or even abortive. Initially discovered in Spain, new samples of this genus were depicted from Morocco by Beauvais in 1980; however, this genus was interpreted as a synonym of Pseudoseptifer Fischer, 1970, a chaetetid sponge (i.e., a sponge with siliceous spicules embedded in a calcareous skeleton). The skeleton of Pseudoseptifer is composed of adjacent tubules that increase by fissiparity by means of a pseudoseptum. Based on the stud…

010506 paleontologySynonymPhylumEvolutionary convergenceCoralChaetetidsPaleontologyCT-scanBiology010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesHexanthiniariaLiassicPaleontologySpongeSponge spiculeSpace and Planetary ScienceGenusddc:550Key (lock)14. Life underwater[SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology0105 earth and related environmental sciencesTaxonomy
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Palaeoenvironmental interpretation of the Pliocene fan-delta system of the Vera Basin (SE Spain): Fossil assemblages, ichnology and taphonomy

2020

Abstract The marine fossil assemblages of the Pliocene of south Spain constitute the record of the marine fauna that colonised the western part of the Mediterranean after the Messinian Salinity Crisis. This work focuses on the analysis of lithofacies and fossil assemblages including trace fossils, invertebrates, and vertebrates with special attention to taphonomic features, for interpreting palaeoenvironmental conditions in the Vera Basin (SE Spain). The sedimentary sequences of the northern region of the Vera Basin display diverse stratigraphical, sedimentological, and palaeontological features that correspond to the evolution of a fan-delta in a narrow basin. The Vera Basin was characteri…

010506 paleontologyTaphonomyStratigraphyPaleontologyTrace fossilStructural basin010502 geochemistry & geophysics01 natural sciencesPaleontologyIchnologyFaciesMarlSedimentary rockProgradationEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesPalaeoworld
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Modern sedimentary analogues and integrated monitoring to understand varve formation in the Mediterranean Lake Montcortès (Central Pyrenees, Spain)

2018

Este artículo contiene 13 páginas, 6 figuras, 1 tabla.

010506 paleontologyVarve010504 meteorology & atmospheric sciencesModern analoguesPaleontologySedimentOceanography01 natural sciencesSediment trapsDeposition (geology)Calcite precipitationOceanographyWater columnBiogenic varvesSediment trapPhotic zoneSedimentary rockMediterranean regionSeasonal resolutionHypolimnionEcology Evolution Behavior and SystematicsGeology0105 earth and related environmental sciencesEarth-Surface ProcessesPalaeogeography, Palaeoclimatology, Palaeoecology
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Occurrence of organic-matter-rich beds in Early Cretaceous coastal evaporitic setting (Dorset, UK): a link to long-term palaeoclimate changes?

2009

11 pages; International audience; In Dorset (southern U.K.), the Durlston Bay and Lulworth Cove sections expose lowermost Cretaceous coastal marine and non-marine partly evaporitic sediments (the so-called Purbeckian facies). An interval with organic matter (OM)-rich layers is recognized in both sections. This OM-rich interval is 20 m thick in the middle of the Durlston Bay section. Within these beds, a large OM accumulation is recorded, with total organic carbon (TOC) of up to 8.5 wt%. High hydrogen index (HI) values (up to 956 mgHC/gTOC) point to a Type I OM, generally considered as derived from algal-bacterial biomass. This contrasts with the OM present in the underlying and overlying in…

010506 paleontology[SDE.MCG]Environmental Sciences/Global ChangesClimate changeJurassic[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesPalynofaciesDeposition (geology)CretaceousPaleontology[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry14. Life underwaterCoveSea level0105 earth and related environmental sciencesTotal organic carbonCretaceous.geographygeography.geographical_feature_categoryPaleontology15. Life on land[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/GeochemistryCretaceousPalynofaciesBotryococcus-type algae[ SDE.MCG ] Environmental Sciences/Global ChangesOceanography13. Climate action[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyPurbeckian faciesOrganic matterBayGeology
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<p><strong><em>Chilocoris</em> <em>serratus</em> n. sp., the first burrower bug species (Hemiptera: Heteroptera: …

2016

The first burrower bug species recorded in Guinea-Bissau, Chilocoris serratus n. sp., is described and compared with morphologically related species. Additionally, an annotated checklist of Afrotropical species of the genus Chilocoris is provided.

010506 paleontologybiologyHeteroptera010502 geochemistry & geophysicsbiology.organism_classification01 natural sciencesHemipteraChecklistGuinea bissauBotanyAnimal Science and ZoologyTaxonomy (biology)CydnidaeEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesZootaxa
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Carbonate slope re‐sedimentation in a tectonically‐active setting (Western Sicily Cretaceous Escarpment, Italy)

2020

Tectonic processes are widely considered as a mechanism causing carbonate platform margin instabilities leading to the emplacement of mass transport deposits and calciturbidites. However, only few examples establishing a clear link between tectonics and re-sedimentation processes are known from the lit- erature. The two-dimensional and three-dimensional wire-cut walls of hun- dreds of quarries extracting ornamental limestones (for example, Perlato di Sicilia) from the Western Sicily Cretaceous Escarpment in Italy expose a series of mass transport deposits. The depositional architecture, spatial facies distri- bution and sedimentary features of these deposits were studied in detail. Thin sec…

010506 paleontologygeographyPillow lavageography.geographical_feature_categoryCarbonate platformStratigraphyGeochemistryGeologyEscarpment010502 geochemistry & geophysics01 natural sciencesCretaceousSedimentary depositional environmentTectonicsFaciesGeneral Earth and Planetary SciencesSedimentary rockGeologyCarbonate slope Cretaceous mass transport deposits re-deposited facies tectonics0105 earth and related environmental sciencesGeneral Environmental ScienceSedimentology
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Ion fractionation in young sea ice from Kongsfjorden, Svalbard

2011

AbstractThe fractionation of major sea-water ions, or deviation in their relative concentrations from Standard Mean Ocean Water ratios, has been frequently observed in sea ice. It is generally thought to be associated with precipitation of solid salts at certain eutectic temperatures. the variability found in bulk sea-ice samples indicates that the fractionation of ions depends on the often unknown thermal history of sea ice, which affects the structure of pore networks and fate of solid salts within them. Here we investigate the distribution of ions in Arctic sea ice that is a few weeks old with a reconstructible thermal history. We separate the centrifugable (interconnected) and entrapped…

010506 paleontologygeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesBiogeochemistryMineralogyFractionation01 natural sciencesArctic ice packOceanographySea ice growth processes13. Climate actionSea iceSeawaterPrecipitationGeology0105 earth and related environmental sciencesEarth-Surface ProcessesEutectic systemAnnals of Glaciology
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