6533b855fe1ef96bd12b0a3f
RESEARCH PRODUCT
New Evidence of MIS 3 Relative Sea Level Changes from the Messina Strait, Calabria (Italy)
Luigi FerrantiGianluca QuartaPaolo OrrùGiovanni ScicchitanoPaolo StocchiLucio CalcagnileFabrizio AntonioliMarco TavianiMarco TavianiMarco TavianiGiuseppe MastronuzziGiovanni ScardinoFabrizio PepeCarmelo MonacoCarmelo Monacosubject
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 transgressiondescription
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
year | journal | country | edition | language |
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2021-09-26 | Water |