Iron (Fe) oxides are widely recognized to prevent the degradation of organic matter (OM) in
environments, thereby promoting the persistence of organic carbon (OC) in soils. Thus …

Coastal wetlands host large and dynamic reservoirs of organic carbon (C) and are also
biogeochemical hotspots for a wide range of Fe (hydr-) oxides with different chemical …

Dissolved organic matter (DOM) plays a vital role in biogeochemical processes and in
determining the responses of soil organic matter (SOM) to global change. Although the …

Identifying controls on soil organic carbon (SOC) storage, and where SOC is most
vulnerable to loss, are essential to managing soils for both climate change mitigation and …

Despite the recognized organic carbon (OC) sequestration potential of mangrove forests, the
ongoing climate change and anthropogenic disturbances pose a great threat to these …

Association of organic carbon (C) with iron (Fe) minerals is one important mechanism for
long‐term terrestrial C storage. Yet, specific edaphic variables that directly contribute to Fe …

The greater number and activity of microorganisms in the rhizosphere than bulk soils is
expected to affect iron (Fe) and carbon (C) biogeochemical cycling. We investigated the …

Globally, a vast extent of tidal wetlands will be threatened by sea-level-rise-induced
salinization. Because ferric (hydro) oxides [Fe (III)] play a crucial role in soil organic carbon …

Subsoil carbon is generally older and decomposes more slowly than topsoil carbon. It has,
therefore, been suggested that carbon stocks could be increased by burying carbon-rich …

Salt marshes sit at the terrestrial–aquatic interface of oceans around the world. Unique
features of salt marshes that differentiate them from their upland or offshore counterparts …