Search results for "Sea level change"

showing 10 items of 16 documents

Vertical movements in NE Sicily and its offshore: Outcome of tectonic uplift during the last 125 ky

2013

New data in the coastal area between Acquedolci and Patti (northeastern Sicily, Italy) have been collected to calculate vertical tectonic rates in a key sector between the Kabilian-Calabrian and the Sicilian-Maghrebian chain. The comparison among marine geology data (multibeam and seismic reflection profiles) on the continental shelf-slope system and the radiocarbon ages on geomorphological markers collected during a coastal survey, provided new stratigraphic, geomorphological and biological data, contributing to the knowledge of the geological evolution of this sector for the last 125 ky.This coastal area is framed between two main structural features active during the Pleistocene in north…

geographygeography.geographical_feature_categoryPleistoceneHoloceneLast Glacial MaximumSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia StrutturaleSettore GEO/04 - Geografia Fisica E GeomorfologiaMarine geologyLast Glacial MaximumFault (geology)Last Interglaciallaw.inventionTectonicsTectonic upliftlawRelative Sea level changeUplift rateLate Quaternary depositional sequenceRadiocarbon datingGeomorphologyGeologyHoloceneEarth-Surface Processes
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SEA-LEVEL AND CLIMATIC CHANGES DURING THELAST 41,000 YEARS IN THE OUTER SHELF OF THE SOUTHERN TYRRHENIAN SEA: EVIDENCE FROM FORAMINIFERA AND SEISMOST…

2012

Sea Level Changes QuaternarySettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/01 - Paleontologia E PaleoecologiaVariazioni del livello marino QuaternarioSettore GEO/08 - Geochimica E Vulcanologia
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Carbonate/evaporitic sedimentation during the Messinian salinity crisis in active accretionary wedge basins of the northern Calabria, southern Italy

2020

Abstract This work deals with Messinian deposits belonging to the Neogene infill of the Rossano and Belvedere Basins, respectively developed along the fore-arc and the back-arc areas of the north Calabria accretionary wedge. The main goal is to characterize the carbonate and evaporitic sedimentation during the Messinian Salinity Crisis, in the general framework of the basin architecture and the interplay between eustatic vs tectonic controlled sea-level variations. Fieldwork integrated with seismic lines and well logs interpretations led to the revision of the general stratigraphy of the basins and the proposal of a new sequential stratigraphic model driven by cyclic sea-level variations. E…

Accretionary wedgeSettore GEO/02 - Geologia Stratigrafica E SedimentologicaEvaporiteTerrigenous sedimentStratigraphyGeochemistryCalabriaGeologySettore GEO/01 - Paleontologia E PaleoecologiaStructural basinOceanographyNeogeneSea level changeschemistry.chemical_compoundTectonicsGeophysicschemistryMessinian salinity crisiCarbonateEconomic GeologyCarbonate sedimentEvaporitic sedimentGeologyMarine transgressionMarine and Petroleum Geology
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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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Millstones as indicators of relative sea-level changes in northern Sicily and southern Calabria coastlines, Italy

2011

Abstract New data are presented for late Holocene relative sea-level changes in two coastal sites of Sicily and Calabria, southern Italy. Reconstructions are based on precise measurements of submerged archaeological remains that are valuable indicators of past sea-level position. The archaeological remains are millstone quarries carved on sandstone coastal rocks and nowadays partially submerged which, to the authors’ knowledge, are used for the first time as sea-level markers. Millstones of similar typology are located on the coast of Capo d’Orlando (northern Sicily) and Capo dell’Armi (southern Calabria). When the archeologically-based sea-level position is compared with the shoreline elev…

BeachrockShoregeographygeography.geographical_feature_categoryHolocenePleistoceneSettore GEO/02 - Geologia Stratigrafica E SedimentologicaElevationtectonic movements; sea level changes; Holocene;tectonic movementArchaeologyMillstoneTectonicsgeoarcheologyPhysical geographysea level changeSicily and CalabriaSea levelHoloceneGeologyrelative sea-level changeEarth-Surface Processes
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Preservation of modern and mis 5.5 erosional landforms and biological structures as sea level markers: A matter of luck?

2021

The Mediterranean Basin is characterized by a significant variability in tectonic behaviour, ranging from subsidence to uplifting. However, those coastal areas considered to be tectonically stable show coastal landforms at elevations consistent with eustatic and isostatic sea level change models. In particular, geomorphological indicators—such as tidal notches or shore platforms—are often used to define the tectonic stability of the Mediterranean coasts. We present the results of swim surveys in nine rocky coastal sectors in the central Mediterranean Sea using the Geoswim approach. The entire route was covered in 22 days for a total distance of 158.5 km. All surveyed sites are considered to…

Marine isotope stageSettore BIO/07 - EcologiaErosion -- Mediterranean RegionBiological indicators; Coastal geomorphology; Geoswim; Landforms; Mediterranean Sea; MIS 5.5; Sea level change010504 meteorology & atmospheric sciencesGeography Planning and DevelopmentGeoswimAquatic ScienceCoastal geography010502 geochemistry & geophysicsBiological indicator01 natural sciencesBiochemistryNeotectonics -- Mediterranean RegionMediterranean seaMediterranean SeaSea level changeTD201-500Sea level0105 earth and related environmental sciencesWater Science and TechnologyShoregeographyPast sea levelgeography.geographical_feature_categorycoastal geomorphologyWater supply for domestic and industrial purposesCoast changes -- Mediterranean Region -- Case studiesSubsidenceHydraulic engineeringcoastal geomorphology MIS 5.5 landforms biological indicators sea level change Mediterranean Sea GeoswimSettore GEO/01 - Paleontologia E Paleoecologiabiological indicatorsCoastal geomorphologyMIS 5Sea level -- Mediterranean RegionMIS 5.5LandformInterglacialBeach erosion -- Mediterranean RegionPhysical geographyTC1-978landformssea level changeGeology
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Vermetid reefs in the Mediterranean Sea as archives of sea-level and surface temperature changes

2011

Vermetid reefs are among the most important bioconstructions in the Mediterranean Sea, with a distribution restricted to the warmest part of the basin. Their structure, and vertical and geographical distribution make them good biological indicators of changes in sea level and sea-surface temperature over the last two millennia.

Sea level changeSettore BIO/07 - Ecologiageographygeography.geographical_feature_categoryEcologyvermetid reef; sea-level change; sea-surface temperature; Mediterranean SeaStructural basinSea surface temperaturesea-level changeOceanographyMediterranean seaAquatic environmentsea-surface temperatureMediterranean SeaGeneral Earth and Planetary SciencesPhysical geographyReefEcology Evolution Behavior and SystematicsGeologySea levelvermetid reefGeneral Environmental Science
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A stalactite record of four relative sea-level highstands during the Middle Pleistocene Transition

2017

International audience; Ice-sheet and sea-level fluctuations during the Early and Middle Pleistocene are as yet poorly understood. A stalactite from a karst cave in North West Sicily (Italy) provides the first evidence of four marine inundations that correspond to relative sea-level highstands at the time of the Middle Pleistocene Transition. The speleothem is located ∼97 m above mean sea level as result of Quaternary uplift. Its section reveals three marine hiatuses and a coral overgrowth that fixes the age of final marine ingression at 1.124 ± 0.2, thus making this speleothem the oldest stalactite with marine hiatuses ever studied to date. Scleractinian coral species witness light-limited…

Marine isotope stageArcheology010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaSettore GEO/03 - Geologia Strutturale010502 geochemistry & geophysics01 natural sciencesSea level changeStable isotopesGlobal and Planetary Changegeography.geographical_feature_categoryEcologyArcheology (arts and humanities)Geology87Sr/86Sr ageSpeleothemStable isotopePleistocene87Sr/86Sr agesOceanographyArchaeology[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/ClimatologySr/Sr agesPaleogeographyCoralsGeologyStalactitePleistoceneEvolutionSpeleothemWestern Europecoastal/dk/atira/pure/sustainabledevelopmentgoals/life_below_water87Sr/86 41 Sr agesPaleontologyInterglacial(s)Behavior and Systematics14. Life underwaterSDG 14 - Life Below Water[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentSea levelEcology Evolution Behavior and Systematics0105 earth and related environmental sciencesU-Th datinggeographyGeomorphologySettore GEO/01 - Paleontologia E PaleoecologiaKarstEcology Evolution Behavior and SystematicSpeleothems87Sr/86Sr ages;Corals;U-Th dating;Pleistocene;Stable isotopes;Western Europe;Interglacial(s);Sea level changes;SpeleothemsSea level changesCoralQuaternaryGlobal and Planetary ChangeSettore ICAR/06 - Topografia E Cartografia
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Reply to comment by C. Morhange, C. Flaux, P.A. Pirazzoli, M.B. Carre on “Holocene Sea level Change in Malta”

2013

The pits of Birzebbugia are located near the present-day mean sea level, and some are partially submerged. They were dated using pottery discovered in an archaeological site close to the coast, dated to the Bronze Age (Zammit, 1928; Abela, 1999). As they have been interpreted as sites for the retting of flax, during their utilization they should have remained dry and the sea could not submerge them. This is the reason why these structures are not directly related to the sea level, as suggested by Biolchi et al. (2011), so they represent an upper limit.

Sea level changeClimatic changes -- MaltaSea level -- MaltaSettore GEO/02 - Geologia Stratigrafica E SedimentologicaMaltaSettore GEO/04 - Geografia Fisica E Geomorfologiasea level change; Malta;upliftPaleoecology -- MaltaGeographyOceanographyPalynology -- Maltaupliftsea level changeHoloceneEarth-Surface Processes
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Submerged speleothems and sea level reconstructions: a global overview and new results from the Mediterranean Sea

2021

This study presents a global overview of the submerged speleothems used to reconstruct paleo sea levels and reports new results from two stalactites collected in the Mediterranean Sea. Coastal cave deposits significantly contributed to the understanding of global and regional sea-level variations during the Middle and Late Quaternary. The studied speleothems cover the last 1.4 Myr and focused mainly on Marine Isotope Stages (MIS) 1, 2, 3, 5.1, 5.3, 5.5, 7.1, 7.2, 7.3 and 7.5. The results indicate that submerged speleothems represent extraordinary archives that can provide detailed information on former sea-level changes. The two stalactites collected in the central Mediterranean Sea, at Fa…

Sea level change010506 paleontologyStalactitevertical tectonic movementGeography Planning and DevelopmentAquatic Science010502 geochemistry & geophysics01 natural sciencesBiochemistryMediterranean seaCaveSea-level changeSea cave14. Life underwaterTD201-500Sea levelPhreatic[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/OceanographySea caves0105 earth and related environmental sciencesWater Science and Technology[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryWater supply for domestic and industrial purposesPhreatic speleothemHydraulic engineeringFavignana; Phreatic speleothem; Sea caves; Sea-level change; Submerged speleothem; Ustica; Vertical tectonic movementsFavignanaOceanographyUsticaQuaternaryFavignana Phreatic speleothem Sea caves Sea-level change Submerged speleothem Ustica Vertical tectonic movementsTC1-978Submerged speleothemVertical tectonic movementsGeology
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