Earth-surface processes operate across erosionally dominated landscapes and deliver
sediment to depositional systems that can be preserved over a range of timescales. The …

Sediment archives in the terrestrial and marine realm are regularly analyzed to infer
changes in climate, tectonic, or anthropogenic boundary conditions of the past. However …

Turbidity currents, and other types of underwater sediment density flow, are arguably the
most important flow process for moving sediment across our planet. Direct monitoring …

Climate, tectonics, and life influence the flux and caliber of sediment transported across
Earth's surface. These environmental conditions can leave behind imprints in the Earth's …

This cutting-edge summary combines ideas from several sub-disciplines including geology,
geomorphology, oceanography and geochemistry to provide an integrated view of Earth …

Early models of stratigraphic sequence development across continental margins predicted
terrigenous sediment delivery to the deep sea principally during periods of sea-level fall and …

Although the stratigraphy of sedimentary basins depends on the balance between the
magnitude and grain‐size characteristics of the sediment supply (Qs) and the spatial …

Advances in acoustic imaging of submarine canyons and channels have provided accurate
renderings of sea‐floor geomorphology. Still, a fundamental understanding of channel …

Recent studies show that paleoenvironmental (allogenic) signals preserved in the
stratigraphic record may be contaminated or overprinted by internally generated (autogenic) …

Infrequent extreme events such as large earthquakes pose hazards and have lasting
impacts on landscapes and biogeochemical cycles. Sediments provide valuable records of …