Discharge variability is a key control on hydrological behavior in rivers, such as the
frequency and magnitude of floods. A better understanding of discharge variability and how …

The need to predict accurately the volume, timing and location of sediments that are
transported from an erosional source region into a basin-depocentre sink is important for …

Converging research in modern environments, stratigraphy, numerical modeling, and
physical experiments introduce new ideas and reinforce prior thinking on the complex and …

Downstream migration of point bars is an important process in meander belts. Inherent to
downstream migration is sediment accumulation in concave channel banks, immediately …

Depositional stratigraphy represents the only physical archive of palaeosediment routing
and this limits analysis of ancient sourcetosink systems in both space and time. Here, we …

The elemental composition of sediments in rivers is the product of physical and chemical
erosion of rocks, which is then transported across drainage networks. A corollary is that …

A wide range of key scaling relationships obtained from modern fluvial systems can be used
to estimate the drainage areas in ancient source-to-sink systems. In this study, these …

Namurian (Carboniferous) eustatic fluctuations drove the incision and backfill of shelf
crossing valley systems located in humid subequatorial regions, which are now preserved in …

Distinguishing trunk channels and delta-plain distributary channels in ancient systems can
be difficult due to poor or incomplete data (eg, limited outcrop or sparse well data). Accurate …

Rivers transport sediments in a source to sink system while responding to allogenic controls
of the depositional system. Stacked fluvial sandstones of the Middle Pennsylvanian …