This review discusses observed impacts from different climate change-driven pressures on
mangrove's role in modulating trace metal transfer at the land-ocean interface. It contributes …

Wetlands cover a small portion of the world, but have disproportionate influence on global
carbon (C) sequestration, carbon dioxide and methane emissions, and aquatic C fluxes …

Mangroves and saltmarshes are biogeochemical hotspots storing carbon in sediments and
in the ocean following lateral carbon export (outwelling). Coastal seawater pH is modified by …

Support for coastal wetland restoration projects that consider carbon (C) storage as a
climate mitigation benefit is growing as coastal wetlands are sites of substantial C …

Mangroves are known for large carbon stocks and high sequestration rates in biomass and
soils, making these intertidal wetlands a cost-effective strategy for some nations to …

We quantified whether pore‐water exchange flushes out saltmarsh sediment carbon, driving
carbon outwelling into the ocean and outgassing into the atmosphere. Radon‐derived pore …

Mangroves are carbon-rich ecosystems that store large quantities of carbon, mostly in soils.
Early carbon (C) budgets indicated that> 50% of mangrove C fixation was unaccounted for …

The intertidal zone is an important pathway for the transport of dissolved carbon across the
land–ocean interface. Quantifying carbon transformation and export from the intertidal zone …

Blue carbon ecosystems require conservation and restoration to maximize organic carbon
(CORG) sequestration to ameliorate greenhouse gas emissions. Salt marshes, mangrove …

The biogeochemical transformation of dissolved carbon in tidal beaches affects the coastal
carbon cycle and budget. Yet, the influence of groundwater flow on the behavior of dissolved …