We analyzed the carbon fluxes in the central metabolism of Geobacter metallireducens strain GS-15 using 13 C isotopomer modeling. Acetate labeled in the first or second position was the sole carbon source, and Fenitrilotriacetic acid was the sole terminal electron acceptor. The measured labeled acetate uptake rate was 21 mmol/g (dry weight)/h in the exponential growth phase. The resulting isotope labeling pattern of amino acids allowed an accurate determination of the in vivo global metabolic reaction rates (fluxes) through the central metabolic pathways using a computational isotopomer model. The tracer experiments showed that G. metallireducens contained complete biosynthesis pathways for essential metabolism, and this strain might also have an unusual isoleucine biosynthesis route (using acetyl coenzyme A and pyruvate as the precursors). The model indicated that over 90% of the acetate was completely oxidized to CO 2 via a complete tricarboxylic acid cycle while reducing iron. Pyruvate carboxylase and phosphoenolpyruvate (PEP) carboxykinase were present under these conditions, but enzymes in the glyoxylate shunt and malic enzyme were absent. Gluconeogenesis and the pentose phosphate pathway were mainly employed for biosynthesis and accounted for less than 3% of total carbon consumption. The model also indicated surprisingly high reversibility in the reaction between oxoglutarate and succinate. This step operates close to the thermodynamic equilibrium, possibly because succinate is synthesized via a transferase reaction, and the conversion of oxoglutarate to succinate is a rate-limiting step for carbon metabolism. These findings enable a better understanding of the relationship between genome annotation and extant metabolic pathways in G. metallireducens.Geobacter species are known to be one of the dominant groups of microorganisms mediating iron reduction in the environment (21). They have been found to be ubiquitous in a myriad of subsurface environments. Detailed studies of their metabolism have revealed them to be capable of bioremediation of several heavy metals, including uranium, plutonium, technetium, and vanadium, as well as biodegradation of several organic contaminants, including monoaromatic hydrocarbons (16,17,26). More recently, Geobacter species have been used to generate electricity from waste organic matter (2, 15, 19). These unique metabolisms make Geobacter species important players in the contaminated subsurface environment (18). Geobacter metallireducens was the first iron-reducing organism isolated that coupled complete oxidation of organic acids with reduction of iron oxides (20,21). It completely oxidizes organic carbons such as fatty acids, alcohols, and monoaromatic compounds via the tricarboxylic acid (TCA) cycle (3, 20) coupled with the reduction of iron. The genomes of several Geobacter species have been sequenced, and proteome data are also available (5, 24). While the genome sequence and proteome are important for understanding Geobacter, they are not necessarily accurate represe...