The use of sedimentary structures as indicators of flow and sediment morphodynamics in
ancient sediments lies at the very heart of sedimentology, and allows reconstruction of …

The geometry of alluvial river channels both controls and adjusts to the flow of water and
sediment within them. This feedback between flow and form modulates flood risk, and the …

Understanding the dynamics of sediment transport and erosion-deposition patterns in the
locality of a coastal structure is vital to evaluating the performance of coastal structures and …

Sediment fluxes in aquatic environments are crucially dependent on bedform dynamics.
However, sediment-flux predictions rely almost completely on clean-sand studies, despite …

In aquatic habitats, micro‐organisms successfully adhere to and mediate particles, thus
changing the erosive response of fine sediments to hydrodynamic forcing by secreting glue …

Biologically active, fine‐grained sediment forms abundant sedimentary deposits on Earth's
surface, and mixed mud‐sand dominates many coasts, deltas, and estuaries. Our …

The differentiation of pure turbidites and contourites from mixed deposits—as the bottom
current reworked sands (BCRS)—in sedimentary cores and outcrops from the modern or …

Biofilm-coated microplastics are omnipresent in aquatic environments, carrying different
organic matter (OM) that in turn influences the flocculation and settling of microplastic …

The fringe of fine‐grained deep‐marine systems often exhibits complex sedimentary facies
and facies associations, because the presence of clay promotes the development of …

Clinoforms are ubiquitous depositional surfaces in sedimentary systems. The quintessential
shape, with a flat or gentle topset, sloping foreset, and gentle to flat bottomset, is …