Search results for "Chronostratigraphy"

showing 8 items of 18 documents

The late Messinian "Lago-Mare" event and the Zanclean Reflooding in the Mediterranean Sea: New insights from the Cuevas del Almanzora section (Vera B…

2020

Abstract The return to normal marine conditions in the Mediterranean Sea after the end of the Messinian Salinity Crisis (MSC), that led to the deposition of thick evaporitic succession followed by settlement of brackish to freshwater conditions of the “Lago-Mare”, is still subject to extensive debate between two opposite scenarios. One scenario implies an abrupt reflooding through the Gibraltar gateway of the Mediterranean Sea previously disconnected from the world ocean and partly desiccated. The second scenario postulates that the Mediterranean Sea kept a high-water level throughout the Messinian Salinity Crisis and was connected continuously to the Atlantic Ocean and to the Paratethys. T…

Planktonic foraminifera010504 meteorology & atmospheric sciences[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]010502 geochemistry & geophysics01 natural sciencesLago-Mare event Mediterranean Sea Messinian-Zanclean transition Ostracods Oxygen and carbon stable isotopes of planktonic foraminifera Paleoenvironmental changes Planktonic foraminifera Zanclean refloodingForaminiferaPaleontologyMediterranean seaOstracodMediterranean SeaLago-Mare eventOxygen and carbon stable isotopes of planktonic foraminifera14. Life underwaterChronostratigraphyMessinian-Zanclean transitionGlobigerinoidesComputingMilieux_MISCELLANEOUS0105 earth and related environmental sciencesMilankovitch cyclesbiologyBrackish waterOstracodsGlobigerina bulloidesbiology.organism_classificationPaleoenvironmental changes13. Climate actionGeneral Earth and Planetary SciencesZanclean refloodingGeology
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Lithostratigraphy of Sicily

2018

This book offers as comprehensive an overview as possible of the lithostratigraphy of the Italian region of Sicily, taking into account the multiplicity of formational and terminological variability developed over more than a century of studies and publications. It presents stratigraphic terminology, the geological lexicon and the main stratigraphic subdivisions that are not familiar to Sicilian geologists. The new stratigraphic methods and the use of formations as mapping units have prompted the acquisition of new lithostratigraphic data, and a review of the previous units and their comparison with the new collected data, enabling the definition of a number of new lithostratigraphic units.…

Settore GEO/02 - Geologia Stratigrafica E SedimentologicaSedimentology Paleogeography Chronostratigraphy Stratigraphic Methods Plate-tectonic History Micropaleontology Facies Analysis Macro- and Micro-Facies Biostratigraphy Carbonate Deposits Evaporite Deposits
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Bio-chronostratigraphic calibration of the Upper Carnian-Lower Norian magnetostratigraphic scale at Pizzo Mondello (Sicani Mountains, Sicily).

2010

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicamagnetostratigraphy bio-chronostratigraphy Upper Carnian-Lower Norian Pizzo Mondello
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Integrated stratigraphy of the Norian GSSP candidate Pizzo Mondello section (Sicani Mountains, Sicily)

2008

Stratigraphy Triassic Chronostratigraphy Pizzo Mondello SicilySettore GEO/02 - Geologia Stratigrafica E Sedimentologica
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OSL dating of sediments from the Gobi Desert, Southern Mongolia

2010

Abstract The present study focuses on the chronological relationship between alternating dune sand and silty water-lain sediments in the central part of the Khongoryn Els dune field in the Gobi Desert, Southern Mongolia. The 23 m high section evolved from the construction of a natural dam by west–east moving sand dunes and fluvial inundation by a river system from the mountain ranges in the south. To resolve the chronology of events, optically stimulated luminescence (OSL) dating was applied and from sedimentological and geochemical analysis the depositional processes could be characterised. Quartz OSL dating of these sediments is hindered by feldspar contamination. Thus, dating of coarse-g…

StratigraphyFluvialGeologySand dune stabilizationSedimentary depositional environmentPaleontologyGeographieGeologic time scaleEarth and Planetary Sciences (miscellaneous)Aeolian processesChronostratigraphyGeomorphologyHoloceneGeologyChronologyQuaternary Geochronology
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Late Holocene erosion of the Canopic promontory (Nile Delta, Egypt)

2017

International audience; The mouths of the Nile Delta are sensitive coastal areas, their geomorphology primarily being mediated by relative sea-level rise and sediment supply. To further document the Holocene evolution of the Nile's Canopic mouth, a core was taken from the southern shores of Abu Qir Bay, close to the ancient Canopic channel. Core bio-sedimentology and chronostratigraphy highlight four stages of marine incursion which are juxtaposed upon the general progradation trend of the Nile coast in this area. Compiled age-depth points from sediment cores taken in Abu Qir Bay underscore two phases of negative sediment budget at the Canopic mouth: (1) a first period, between 3.5 and 2 ka…

geographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesGeoarchaeologySubmersion (coastal management)[SDU.STU]Sciences of the Universe [physics]/Earth SciencesGeology15. Life on land010502 geochemistry & geophysicsOceanography01 natural sciencesOceanography13. Climate actionGeochemistry and PetrologyRiver mouth14. Life underwaterProgradationChronostratigraphySedimentary budgetGeologySea levelHolocene0105 earth and related environmental sciencesMarine Geology
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Late Miocene sea surface salinity variability and paleoclimate conditions in the Eastern Mediterranean inferred from coral aragonite δ18O

2009

Abstract Coral skeletons are archives of chemical proxies which enable paleoenvironmental reconstructions to be made at subannual resolution. Stable oxygen isotope ( δ 18 O) ratios of these archives reflect sea surface temperature (SST) as well as the δ 18 O composition of ambient seawater. The δ 18 O seawater composition is not only controlled by global ice build-up, but river discharge and the hydrological balance of evaporation and precipitation, all influencing sea surface salinity (SSS), also play an important role in marginal seas. New sub-annually resolved coral δ 18 O data were measured and evaluated together with published data from reef coral communities of Late Miocene age from C…

geographygeography.geographical_feature_categorybiologyδ18OCoralPoritesGeologyLate Miocenebiology.organism_classificationPaleontologyMediterranean seaOceanographyGeochemistry and PetrologyPaleoclimatologyChronostratigraphyReefGeologyChemical Geology
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Calcareous Nannofossil Biostratigraphy and Chronostratigraphy of ODP Hole 964D (eastern Mediterranean Sea)

2008

Quantitative analyses of calcareous nannofossil were carried out on sediments from ODP Hole 964D succession, recovered in the Ionian Sea, Eastern Mediterranean. Results show that the sedimentary sequence, spanning from about 3.5 Ma (Early Pliocene) to the Present, has been investigated through an average sampling resolution of less than 30 kyr. The detailed subdivision into 11 biozones makes it possible to recognize chronostratigraphic the boundaries in the Early Pliocene-Middle Pleistocene interval. Finally, two sedimentary gaps, lasting at least 340 kyr and 120 kyr respectively, have been recognized between the Zanclean and Piacenzian and in the lower part of the Early Pleistocene. SHORT …

lcsh:GeologyCentral MediterraneanChronostratigraphylcsh:PaleontologyPlio-Quaternarylcsh:QE1-996.5Biostratigraphy Pliocene Pleistocene MediterraneanBiostratigraphyCalcareous nannofossilBiostratigraphy; Calcareous nannofossil; Plio-Quaternary; Central Mediterranean; Chronostratigraphylcsh:QE701-760
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