Erythropoietin (EPO) and soluble transferrin receptors (sTFR) are both sensitive indicators for erythropoietic activity. EPO is produced in the kidney by cells located between the tubuli in the interstitial space of the renal cortex. It is regulated at the level of its gene chiefly by tissue oxygenation. EPO triggers erythropoiesis via stimulating the proliferation, differentiation, and maturation of the erythroid precursors in bone marrow; that is, the burst-forming and colony-forming unit erythroid. About 120 million erythrocytes are destroyed every minute in the adult human body. To avoid anemia, an incredible fine balanced equilibrium between this destruction and the production of new red blood cells has to be ensured. About 500–1000 EPO receptors are present mainly on the surface of purified human erythroid precursor cells (4). Since hypoxia obviously plays a key role in stimulating EPO production and release, the biochemical mechanisms of oxygen sensing, in general, have been the target of intensive research during the last decades. It was found that a transcriptional factor, called the hypoxia-inducible factor (HIF), is essential in promoting cellular adaptation to changes in oxygen availability and regulating the hypoxic gene expression. Further studies revealed that in oxygenated and iron-repleted cells the HIF-alpha subunits are usually rapidly destroyed. This destruction involves ubiquitylation by the von Hippel-Lindau tumor suppressor (pHVL) E3 ligase complex. By hypoxia and iron chelation, in contrast, this process is suppressed and a transcriptional activation is induced. Most recently it could be shown that the interaction between pVHL and a specific domain of the HIF-1alpha subunit is regulated via hydroxylation of a proline residue (HIF-1alpha P564) by an enzyme termed HIF-alpha prolyl-hydroxylase (HIF-PH). This HIF-PH seems to function directly as a cellular oxygen sensor (2,3). TFR is a transmembrane glycoprotein that controls the uptake of transferrin-iron into premature red blood cells in a density of several hundred thousands per cell (1). Most important is that i) the soluble TFR reflects the total mass of tissue receptors and ii) the concentration of soluble TFR correlates directly with the erythropoietic activity and inversely with the amount of iron available for erythropoiesis (functional iron status). Therefore, if EPO increases, erythropoiesis increases and with an increased erythropoiesis the TFR receptor concentrations start to rise due to a concomitant increasing transfer of iron in the red blood precursor cells. From a physiological and pathophysiogical point of view, especially for exercise physiology and clinical medicine, it is very important to understand the time course of this process under various conditions (5). Therefore in this issue of Medicine & Science in Sports & Exercise®, Robach et al. (6) investigated the serum EPO and serum TFR concentrations in healthy humans during i) a progressive (31 d) decompression in a hypobaric chamber up to a simulated altitude of Mount Everest (8848 m) and ii) during and after a 1-wk stay at 4350 m. The first set-up was chosen to analyze the effect of step-by-step increasing hypoxia on both parameters, whereas the latter design focused on the acute effects during a shorter stay at a given altitude. The authors found that serum TFR mirrors the EPO response for a given level of hypoxia but clearly differs from EPO response during transitory phases. Therefore, Robach et al. conclude that the analysis of serum TFR may account for altitude-related erythropoiesis, at a time when EPO is blunted. That is why the measurement of TFR concentrations may be used i) as an index of altitude-related erythropoiesis, when EPO response is already blunted and ii) is helpful to detect a recent high erythropoietic activity due to high altitude exposure and/or exogenous administration (EPO doping) at a time when other parameters (EPO concentrations, hematocrit (Hct), hemoglobin (Hb), red cell volume) are not different from baseline values.
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