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

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

This third edition of Reconstructing Quaternary Environments has been completely revised
and updated to provide a new account of the history and scale of environmental changes …

A compilation of the Marine Isotope Substage (MIS) 5.5 high stand (∼ 125Ka) sites
spanning the coastline of Italy allows a picture of the vertical displacement pattern affecting …

The specialist contributors to Geomorphological Techniques have thoroughly augmented
and updated their original, authoritative coverage with critical evaluations of major recent …

Dating the Quaternary, which covers approximately the last 2 million years, has experienced
considerable progress over the past few decades. On the one hand, this resulted from the …

Detailed geological map**, morphostratigraphic, palaeontological and geochronological
(uranium-series) analyses were undertaken on the raised marine terraces and interbedded …

In peninsular Italy, marine terraces and shorelines created during oxygen-isotope substage
5e, known historically as the Tyrrhenian highstand, provide a reliable and homogeneous …

The timing and duration of the Last Interglacial period have been controversial, with some
studies suggesting a relatively short duration that is orbitally forced and others suggesting a …

The sedimentary record of aeolian sand systems extends from the A rchean to the Q
uaternary, yet current understanding of aeolian sedimentary processes and product remains …