Organic carbon in marine sediments is a critical component of the global carbon cycle, and
its degradation influences a wide range of phenomena, including the magnitude of carbon …

Goethite, hematite, ferrihydrite, and other iron oxides bind through various sorption reactions
with humic substances (HS) in soils creating nano-, micro-, and macro-aggregates with a …

Sedimentary organic matter provides carbon substrates and energy sources for
microorganisms, which drive benthic biogeochemical processes and in turn modify the …

Iron (Fe) plays a key role in sedimentary diagenetic processes in coastal systems,
participating in various redox reactions and influencing the burial of organic carbon. Large …

The abundant Fe (hydr-) oxides present in wetland sediments can form stable iron (Fe)-
organic carbon (OC) complexes (Fe-OC), which are key mechanisms contributing to the …

Preservation of organic carbon (C org) in marine sediments plays a major role in defining
ocean-atmosphere CO 2 levels, Earth climate, and the generation of hydrocarbons …

The protection of organic carbon through association with iron minerals (Fe R) is an
important factor in its stabilisation, long-term storage, and burial efficiency in marine …

In this study, we describe a novel high throughput, micro-macro approach for the
identification and efficient design of biopolymer stabilized soil systems. At the “microscopic” …

Purpose This field study aimed to guide the planning of iron amendments for phosphorus
retention by investigating the long-term fate of iron added to two urban lakes (Plötzensee …

The burial of organic carbon (OC) in sedimentary environments promotes long-term carbon
sequestration, which allows the release of oxygen in the atmosphere. Organo-mineral …