Comparison of 59Fe3+ uptake in vitro and in vivo by mouse duodenum

Initial rates of 59Fe3+ uptake by mouse duodenal fragments (in vitro) and tied-off duodenal segments (in vivo) have been characterised for control and hypoxic animals. 59Fe3+ uptake by duodenal fragments was rapid, selective and dependent on medium Fe3+-nitrilotriacetate concentration. Most of the 59Fe3+ uptake (70–75%) occurred via the mucosal route and was dependent on the metabolic state of the tissue. Mucosal uptake showed an adaptive increase following exposure of animals to 3 days hypoxia; the enhancement was due to a 2–3-fold increase in Vmaxapp, without any significant changes in the Kmapp. Studies of upper small intestine transit times showed a mean residence time of 4–5 min for 59Fe-labelled mouse chow, emphasising the importance of initial uptake measurements. Time courses for in vivo total mucosal uptake exhibited linearity over a wide variety of absorption rates after correction for the permeation by intact metal-chelate complex. The corrected uptake showed a hyperbolic dependence on medium Fe3+-nitrilotriacetate concentration. Kinetic studies revealed a 2–3-fold increase in total mucosal uptake in hypoxia. Mucosa-to-carcass transfer of 59Fe was also markedly increased by chronic hypoxia. The in vitro system exhibits similar qualitative and quantitative kinetics for Fe3+ transport via the mucosal membrane to those obtained in vivo. The results observed in vitro are thus valid and provide a convenient method for further studies on Fe3+ transport in animals and in man.