River-wetland corridors form where a high degree of connectivity between the surface
(rheic) and subsurface (hyporheic) components of streamflow creates an interconnected …

Alteration to the sediment supply of fluvial channels is well understood to trigger
morphological adjustment, but the particularities and peculiarities that arise in any specific …

We present a critical analysis of experimental findings on vegetation–flow–sediment
interactions obtained through both laboratory and field experiments on tidal and coastal …

The role of aquatic and riparian vegetation in driving morphodynamics of rivers is being
increasingly recognized across all river types. Here, we focus on gravel‐bed rivers, where …

The invasion of the land was a complex, protracted process, punctuated by mass extinctions,
that involved multiple routes from marine environments. We integrate paleobiology …

Sediment is the most valuable natural resource for deltaic environments because it is
required to build new land. For land building to occur, sediment must be retained in the delta …

We present here an integrated analysis of coastal deltaic floodplains in the active
Atchafalaya Coastal Basin coupled to downstream deltaic estuaries to review how …

Computational fluid dynamics was used to study the evolution of small patches of vegetation
into a vegetated landscape in a channel. The growth of new vegetation occurred in regions …

Abstract The Devonian Period was a crucial interval in the evolution of plants. During its 60
myr duration, it witnessed the successive evolution of roots, wood, trees and forests. In …

The evolution of trees and forests through the Devonian Period fundamentally changed the
Earth's land biosphere, as well as impacting physical environments and geomorphology by …