Abstract Tectonically raised paleoshorelines have been recently identified along the southern fault scarps of Mt. Fellino and Roccarainola horst blocks, which are part northeastern border Campania Plain coastal basin (southern Apennines, Italy). Such blocks bounded to south by Polvica Fault, a roughly E‐W trending normal fault. The sequence uplifted has studied in detail integrating geomorphological, structural stratigraphical analyses assess Quaternary uplift blocks. Yet, staircase is still...

Abstract. We describe a database of Last Interglacial (Marine Isotopic Stage 5) sea-level proxies for the western Mediterranean region. The was compiled reviewing information reported in 199 published studies and contains 396 data points (sea-level index marine- or terrestrial-limiting points) 401 associated dated samples. follows standardized WALIS template is available as Cerrone et al. (2021b, https://doi.org/10.5281/zenodo.5341661).

Geological sea-level proxies (e.g., fossil intertidal or foreshore deposits) preserve crucial data that enable the reconstruction of historical fluctuations. This information is essential for assessing extension and volume ice sheets during previous warm periods.The work aims to present results a morpho-stratigraphic field campaign conducted along southern Brazilian coast, from Osório (Rio Grande do Sul) Paranaguá (Paraná). A classical geological geomorphological...

The Last Interglacial (125 ka) was the most recent period in Earth’s history when global temperatures were approximately 1°C higher than pre-industrial levels, with polar regions experiencing a warming of 3–5°C. This warmer climate led to smaller ice sheets, sea and significant shifts atmospheric oceanic patterns, including changes temperature seasonality. Such likely influenced coastal dynamics, altering prevailing winds, wave regimes, ecosystems like...

Quantitative analysis of drainage networks is one the most used approaches for investigation response landscape to tectonic forcing and crustal deformation in different geodynamic setting. Recently, river profile inversion has largely been reconstruction spatial temporal distribution uplift tectonically-active landscapes. The calibration erodibility coefficient particularly effective coastal landscapes, due diffuse presence independent geomorphic markers such as marine terraces. In this...

Understanding past sea-level variations is essential to constrain future patterns of rise in response warmer climate conditions.Due good preservation and the possibility use various geochemical methods date fossil index points, Last Interglacial (Marine Isotope Stage, MIS, 5e, 130-116 ka) often regarded as one best analogs for a climate.MIS 5e coastal stratigraphic sequences, such coral reefs, are characterized by abrupt shifts their geological facies, steps within reef topography or...

Capo Faro Promontory, located in Salina (Aeolian Islands, southern Italy), is a popular summer destination due to its volcanic morphologies, seaside, and enogastronomy. A flat area, right behind the scarp edge of coastal cliff, hosts Estate, one most renowned vineyards residences on Island. The promontory has been characterised terms geomorphological features. Remote sensing analysis, after nadir off–nadir UAV flights, supports field activities explore hazard which area subjected. In...

Understanding past sea-level variations is essential to constrain future patterns of rise in response warmer climate conditions. Due good preservation and the possibility use various geochemical methods date fossil index points, Last Interglacial (Marine Isotope Stage (MIS) 5e; 130-116 ka ago) often regarded as one best analogs for a slightly climate. Some MIS 5e coastal stratigraphic sequences, especially coral reefs tectonically stable areas, are characterized by abrupt shifts their...

Abstract. We describe a database of Last Interglacial (Marine Isotopic Stage 5) sea-level proxies for the Western Mediterranean region. The was compiled reviewing information reported in 179 published studies and contains 371 datapoints (sea-level index points marine or terrestrial limiting points) 304 associated dated samples. follows standardized WALIS template is available as Cerrone et al, 2021b (https://doi.org/10.5281/zenodo.4497365).

Understanding past sea-level variations is essential to constrain future patterns of rise in response warmer climate conditions. Due good preservation and the possibility use various geochemical methods date fossil index points, Last Interglacial (Marine Isotope Stage, MIS, 5e, 130-116 ka) often regarded as one best analogs for a climate. MIS 5e coastal stratigraphic sequences, such coral reefs tectonically stable areas, are characterized by abrupt shifts their geological facies, steps...

The degree to which the Last Interglacial (Marine Isotope Stage 5e; ~125,000 Before Present) can serve as an analog for future sea-level rise caused by anthropogenic climate change is a matter of great importance. Refining knowledge factors such glacio-hydro-isostatic conditions and ice-sheet histories leading up since will help resolve this question, well-constrained, well-dated indicators relative sea level provide crucial data towards end. We conducted stratigraphic surveys on several...

Geological sea-level proxies, such as fossil intertidal or foreshore deposits, store fundamental information that allow reconstructing past changes in sea level, which may be used to evaluate the volume of ice sheets during warm periods. Studies on Last Interglacial (LIG; Marine Isotope Stage 5e, ~ 125 ka) proxies are particularly important, this highstand is a process analogue for current interglacial, including warming caused by human greenhouse gas emissions. In fact, LIG was...

During past Interglacial periods, global ocean volume increased as a result of the higher temperatures and melting ice sheets, consequently leading to rise in sea levels. However, on timescales ranging from years few decades, regional level variability deviates pattern, due combination vertical land movements (earth’s crust viscoelastic response glacial sheet melting, tectonics), thermohaline circulation, wind forcing water storage. Therefore, decoding sea-level during periods is...

Abstract Rivers represent intricate geomorphological systems that exhibit sensitivity to even subtle base‐level changes. This study examines the response of Ribeira de Iguape River, located along southern coast São Paulo state, Brazil, hydrological changes and coastline migration resulting from Holocene climate pulses. Using a multidisciplinary approach, including stratigraphical analyses, optically stimulated luminescence dating, grain‐size interpretation satellite images, mapping...