Vegetative cover was mapped annually, 1976–2022, in experimental plots in Great
Sippewissett Marsh, Cape Cod, USA, chronically fertilized at different doses, and subject to …

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 …

The survival of salt marshes depends on their ability to maintain vertical elevation and areal
extent. In the lateral direction, marsh edges can expand laterally or undergo edge erosion …

Coastal saltmarshes keep pace with sea-level rise through in-situ production of organic
material and incorporation of allochthonous inorganic sediment. Here we report rates of …

Tidal range is a key factor for flooding, mixing, and transport in estuaries. Sea level rise is
expected to change tidal range in the future. This change is complex, and has been showed …

Climate change is driving abiotic shifts that can threaten the conservation of foundation
species and the habitats they support. Directional range shifting is one mechanism of …

It is rational to assume that salt marshes in regions where sediment loads are high should
remain stable or prograde when facing a range of sea-level scenarios, whereas those in …

Marsh morphodynamics models are usually calibrated using sparse short-term
measurements. Hence, their ability to predict long-term trajectories (centuries to millennia) is …

The fate of mangroves and saltmarshes under conditions of accelerating sea-level rise is
dependent upon sedimentation and surface elevation gain that is sufficient to maintain …

Intertidal and subtidal environments occupy the land and sea interface and are highly
susceptible to the influence of human-induced climate change and other drivers of change …