Abstract The Last Interglacial (MIS 5e, 128–116 ka) is among the most studied past periods
in Earth's history. The climate at that time was warmer than today, primarily due to different …

The geomorphology and morphostratigraphy of numerous worldwide sites reveal the
relative movements of sea level during the peak of the Last Interglaciation (Marine Isotope …

We use numerical climate simulations, paleoclimate data, and modern observations to study
the effect of growing ice melt from Antarctica and Greenland. Meltwater tends to stabilize the …

During the last interglacial (LIG) period, global mean sea level (GMSL) was higher than at
present, likely driven by greater high-latitude insolation. Past sea-level estimates require …

In the last three years, there have been three large tsunamis in the Indian Ocean, most
notably the notorious one which struck on 26 December 2004 and killed more than 238,000 …

Large tsunamis are major geomorphic crises, since they imply extensive erosion, sediment
transport and deposition in a few minutes and over hundreds of kilometres of coast …

Carbonate eolianite forms distinctive coastal landforms on many mid-latitude continents and
islands. Numerous studies of extensive continental and smaller island deposits in both …

The Adriatic coast of southern Apulia (Italy) is marked by the presence of large boulder
accumulations. Boulders are up to 8 t in weight and arranged either in small groups or rows …

Several tracts of the Ionian coast of Apulia (southern Italy) are characterized by large
boulders, up to 80t in weight, scattered some meters above present sea level. The largest …

The occurrence of sedimentary storm deposits around the Tethys Ocean during the early
Toarcian hyperthermal (~ 183 Ma) suggests that intensified tropical cyclone (TC) activity …