0000000000354179

AUTHOR

Paolo Orrù

showing 2 related works from this author

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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New Evidence of MIS 3 Relative Sea Level Changes from the Messina Strait, Calabria (Italy)

2021

Investigation of sea-level positions during the highly-dynamic Marine Isotope Stage 3 (MIS 3: 29–61 kyrs BP) proves difficult because: (i) in stable and subsiding areas, coeval coastal sediments are currently submerged at depths of few to several tens of meters below the present sea level

Marine isotope stage010504 meteorology & atmospheric sciencesSettore GEO/02 - Geologia Stratigrafica E SedimentologicaOutcropSettore GEO/03 - Geologia StrutturaleGeography Planning and DevelopmentMarine Isotope Stage 3CalabriaAquatic Science010502 geochemistry & geophysics01 natural sciencesBiochemistryrelative sea levelPaleontologyGIAtectonics14. Life underwaterTD201-500Sea level0105 earth and related environmental sciencesWater Science and Technologygeographygeography.geographical_feature_categoryWater supply for domestic and industrial purposesTectonicsLast Glacial MaximumPost-glacial reboundHydraulic engineeringatmospheric_scienceRelative sea levelSedimentary rockIce sheetTC1-978GeologyMarine transgressionWater
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