Natural levees are wedge-shaped morphological features developing along the boundaries
of mass flows. When they form in fluvial landscapes, they can have multiple implications for …

Abstract Changes in upstream land-use have significantly transformed downstream coastal
ecosystems around the globe. Restoration of coastal ecosystems often focuses on local …

Mangrove forests are valuable coastal ecosystems that have been shown to persist on
muddy intertidal flats through bio‐morphodynamic feedbacks. However, the role of coastal …

Worldwide, many tidal basins associated with barrier coasts have infilled over the past
millennia due to the combination of sediment supply, wave‐tidal sediment transport, and eco …

Coastal marsh loss is commonly attributed to changes in external forcings, such as an
increase in sea-level rise rate or a reduction in sediment supply. Here we show that …

The dynamics and morphological evolution of deltas and their channel networks involve
interactions between many factors, including water and sediment discharge and cohesion …

In the transformation from tidal systems to freshwater coastal landscapes, plants act as eco‐
engineering species that reduce hydrodynamics and trap sediment, but nature and timing of …

To save saltmarshes and their valuable ecosystem services from sea level rise, it is crucial to
understand their natural ability to gain elevation by sediment accretion. In that context, a …

A natural levee is a typical wedge-shaped deposit adjacent to a river channel. Given its
location and distinctive features, the levee can serve as a key to revealing depositional …

When sea‐level rise slowed down in the middle Holocene, fluvial and coastal sediments
filled the newly created accommodation, whilst others remained largely unfilled because of …