Search results for "Sea level"

showing 3 items of 123 documents

Sedimentation and tropical vegetation changes in Southern Benin (West Africa), carbon-13 tracing of organic matter dynamics and fluctuations of the s…

2007

12 pages; International audience

mangrovepaleoenvironment[SDE.MCG]Environmental Sciences/Global Changes[ SDV.SA.SDS ] Life Sciences [q-bio]/Agricultural sciences/Soil study13C/12C isotope ratio[SDV.SA.SDS]Life Sciences [q-bio]/Agricultural sciences/Soil study[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDE.MCG] Environmental Sciences/Global Changes[ SDE.MCG ] Environmental Sciences/Global ChangesOuémé-Sô[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyBeninsea level fluctuation[SDV.SA.SDS] Life Sciences [q-bio]/Agricultural sciences/Soil studydelta faciesComputingMilieux_MISCELLANEOUS
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Late Quaternary sedimentary evolution of the Castellammare Gulf (North-Western Sicily offshore)

2005

High-resolution seismic stratigraphy has been applied to the interpretation of the stratigraphic architecture of Late Pleistocene and Holocene successions on the continental shelf and upper slope of the Gulf of Castellammare, North-Western Sicily. The Late Quaternary type 1 depositional sequence is bounded by a regional unconformity and it is made up of four systems tracts, developed under fourth order relative sea level fluctuations, after the previous highstand of isotope Stage 5e. Systems tract are located in different parts of the basin, two being confined to the outer shelf and the upper slope, the other developed along the inner shelf. Facies associations, geomorphological elements, a…

offshore North-Western SicilyLate PleistoceneHolocenesequence stratigraphycontinental marginsea level changeSeismic stratigraphy
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Holocene sea level change in Malta

2013

A multidisciplinary approach has been applied to study sea level changes along the coast of Malta using data collected from underwater archaeological remains. The elevation of archaeological markers have been compared with predicted sea level curves providing new bodies of evidence that outline the vertical tectonic behaviour of this region, allowing estimation of the relative sea level changes that occurred in this area of the Mediterranean since the Bronze Age. During the Roman Age, sea level was at −1.36 ± 0.1 m, while in the Midde Age it was at −0.56 ± 0.2 m, in agreement with previous estimations for the Mediterranean region. Data indicate that Malta was tectonically stable during the …

vertical movementMediterranean climateClimatic changes -- MaltaSea level -- MaltaSettore GEO/02 - Geologia Stratigrafica E SedimentologicaPleistoceneMaltaSettore GEO/03 - Geologia StrutturaleSettore GEO/04 - Geografia Fisica E GeomorfologiaElevationLast Glacial Maximumrelative sea level changePaleoecology -- Maltarelative sea level change; Late Holocene; MaltaLate HoloceneTectonicsPaleontologyPalynology -- MaltaBronze Agesealevel changeHoloceneGeologySea levelEarth-Surface Processes
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