Iron (Fe) is an important micronutrient in soils, essential for bacterial growth and carbon
metabolism, serving as an enzymatic cofactor for many central carbon metabolic reactions. It …

Decreased biomass growth in iron (Fe)‐limited Pseudomonas is generally attributed to
downregulated expression of Fe‐requiring proteins accompanied by an increase in …

Iron is a metabolic requirement of living systems, yet iron is very insoluble in aerobic, neutral
environments. Therefore, the amount of iron in solution under these conditions is not …

Iron (Fe) is an essential nutrient to most microorganisms. Aerobic microorganisms exhibit
various strategies for acquiring Fe at near-neutral pH conditions, where Fe oxyhydroxides …

High-affinity iron (Fe) scavenging compounds, or siderophores, are widely employed by soil
bacteria to survive scarcity in bioavailable Fe. Siderophore biosynthesis relies on cellular …

What defines central carbon metabolism? The classic textbook scheme of central
metabolism includes the Embden-Meyerhof-Parnas (EMP) pathway of glycolysis, the …

Iron (Fe) is an essential micronutrient for the growth of all living organisms. However, Fe
availability in soil is limited due to its existing status as Fe oxides/hydroxides. Microbial …

Iron is important for bacterial growth and survival, as it is a common co-factor in essential
enzymes. Although iron is very abundant in the earth crust, its bioavailability is low in most …

This research investigated the potential role of siderophores in aerobic microbial Fe
acquisition from natural organic matter (NOM; XAD-8 isolate and reverse osmosis …

Iron is an essential micronutrient for plants and associated microorganisms. Iron nutrition of
these organisms relies on the soil supply. However, bioavailability of iron in cultivated soils …