The Palaeozoic evolution of land plants revolutionized river geomorphology. However, the
relationships between biotic forcing and channel dynamics are still debated and, as such …

Classical models developed for ancient fluvial point bars are based on the assumption that
meander bends invariably increase their radius as meander-bend apices migrate in a …

This study utilizes instruments from the Curiosity rover payload to develop an integrated
paleoenvironmental and compositional reconstruction for the 65‐m thick interval of …

Ephemeral fluvial systems are commonly associated with arid to semi‐arid climates.
Although their complex sedimentology and depositional settings have been described in …

Flume experiments and field observations show that bank vegetation promotes the formation
of narrow and deep single‐thread channels by strengthening riverbanks. Consistent with …

Proterozoic rivers flowed through barren landscapes, and lacked interactions with
macroscopic organisms. It is widely held that, in the absence of vegetation, fluvial systems …

The apparent increase in occurrence of meandering fluvial channel systems in the Middle
Palaeozoic has long been related to the effects of land-plant colonization. However …

The sedimentary products of forty-three Neoproterozoic fluvial-channel belts are superbly
exposed along the seaboard of Stoer Peninsula, Scotland, UK. The deposits belong to the …

The recognition of meandering rivers in Earth's prevegetation stratigraphic record is
hindered by an absence of depositional models specifically tailored to unvegetated single …

Assessments of depositional architecture and paleodrainage in planform are increasingly
recognized as critical for the reconstruction of ancient fluvial morphodynamics; however …