The glacial-interglacial transitions of ice ages are associated with large, rapid changes in
climate, which potentially can be reconstructed from stratigraphic profiles of the chemical …

Ancient fluvial valley systems are long recognized as important features in the stratigraphic
record, but emerged as a specific focus of attention with publication of first-generation …

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 …

Channel fills are common elements of Holocene river systems and older fluvial sequences,
but surprisingly little is known about formation and their sedimentary buildup. Abandoned …

Fluvial deposits and landforms are important archives of river response to climate, tectonics
and base level change and are commonly associated with archaeological sites. Unlike …

Rivers self-organize their pattern/planform through feedbacks between bars, channels,
floodplain and vegetation, which emerge as a result of the basic spatial sorting process of …

Fennoscandia is the key area for glacial isostatic adjustment (GIA) research. Owing to its
long settlement and excellent infrastructure, ongoing land uplift in the north as well as …

We report the discovery of a 50,000-y-old birch tar-hafted flint tool found off the present-day
coastline of The Netherlands. The production of adhesives and multicomponent tools is …

Abstract Reconstructing Northern Hemisphere ice-sheet oscillations and meltwater routing
to the ocean is important to better understand the mechanisms behind abrupt climate …

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