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 …

Abstract The Paleocene-Eocene thermal maximum (PETM) was the most extreme example
of an abrupt global warming event in the Cenozoic, and it is widely discussed as a past …

An appealing strategy for reconstructing the timing and tempo of paleoenvironmental
change from sedimentary strata is to linearly interpolate between marker beds of known age …

Environmental interpretations of subsurface fluvial successions are commonly based on
facies observations from core and are often attempted by generalist geologists by reference …

This study investigated the roles of variable daily discharges in controlling processes of
composite bank erosion in alpine meandering rivers located in the Zoige basin on the …

The stratigraphic record contains unique information about past landscapes and
environmental change. Whether landscapes faithfully transmit signals of environmental …

Overbank flooding is common along most rivers, and it influences the dispersal of sediment
to floodplains. While variable discharge is a critical aspect of fluvial landscape evolution, it is …

Alluvial fans form through primary and secondary geomorphic processes. Primary processes
comprise major geomorphic events that build the fan by transporting sediment from the …

Climate change is raising sea levels across the globe. On river deltas, sea‐level rise (SLR)
may result in land loss, saline intrusion into groundwater aquifers, and other problems that …

To simplify the complex hydrological variability of flow conditions, experiments on delta
evolution are often conducted using a representative channel‐forming flood flow and results …