The Seine, Yonne and Somme are the main rivers draining northwestern France and flowing
into the Channel. During Pleistocene cold stages they were tributaries of the “Fleuve …

The study of drainage network response to uplift is important not only for understanding river
system dynamics and associated channel properties and fluvial landforms, but also for …

A comparison of fluvial terrace sequences from around the world, based on data collected
as part of International Geoscience Programme (IGCP) Project No. 449, has revealed …

The Evolution of Paleolithic Technologies provides a novel perspective on long-term
trajectories of evolutionary change in Paleolithic tools and tool-makers. Members of the …

The first arrivals of hominin populations into Eurasia during the Early Pleistocene are
currently considered to have occurred as short and poorly dated biological dispersions …

Abstract Late Cenozoic (and especially Quaternary) fluvial deposits and related landforms
provide valuable information about landscape evolution, not just in terms of changing …

Marine and ice-core records show that the Earth has experienced a succession of glacials
and interglacials during the Quaternary (last∼ 2.6 million years), although it is often difficult …

Climate impact on the fluvial processes led to morphological and sedimentological
differentiation of a terrace. This diversity in the fluvial environment determined how people …

Two clearly differentiated techno-complexes can be recognised in the Iberian Peninsula
during the second half of the Middle Pleistocene: the Acheulean and the Middle Palaeolithic …

The climatic signal of Marine Isotope Stage (MIS) 11 is well-documented in marine and ice-
sheet isotopic records and is known to comprise at least two major warm episodes with an …