6533b834fe1ef96bd129cb58
RESEARCH PRODUCT
MIS 5.5 highstand and future sea level flooding at 2100 and 2300 in tectonically stable areas of central mediterranean sea: Sardinia and the pontina plain (Southern Latium), Italy
Fabrizio AntonioliGiacomo DeianaValeria Lo PrestiPaolo E. OrrùLorenzo MorettiGiovanni Randazzosubject
Coastal plainGeography Planning and DevelopmentSubmersion (coastal management)Aquatic ScienceSardiniaBiochemistryMediterranean seaPast (MIS 5.5) and future sea level at 2100 and 2300TD201-500Sea levelWater Science and Technologygeographygeography.geographical_feature_categoryWater supply for domestic and industrial purposesFlooding (psychology)Last Glacial MaximumFuture sea levelHydraulic engineeringCentral Mediterranean coastal plainspast (MIS 5.5) and future sea level at 2100 and 2300 Sardinia Pontina Plain central Mediterranean coastal plainsPhysical geographyTC1-978Central Mediterranean coastal plains; Past (MIS 5.5) and future sea level at 2100 and 2300; Pontina Plain; SardiniaGeologyMarine transgressionPontina Plaindescription
Areas of the Mediterranean Sea are dynamic habitats in which human activities have been conducted for centuries and which feature micro-tidal environments with about 0.40 m of range. For this reason, human settlements are still concentrated along a narrow coastline strip, where any change in the sea level and coastal dynamics may impact anthropic activities. We analyzed light detection and ranging (LiDAR) and Copernicus Earth observation data. The aim of this research is to provide estimates and detailed maps (in three coastal plain of Sardinia (Italy) and in the Pontina Plain (southern Latium, Italy) of: (i) the past marine transgression occurred during MIS 5.5 highstand 119 kyrss BP
| year | journal | country | edition | language |
|---|---|---|---|---|
| 2021-09-21 |