Control of erythropoiesis after high altitude acclimatization |
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Authors: | Gustave Savourey Jean-Claude Launay Yves Besnard Angélique Guinet Cyprien Bourrilhon Damien Cabane Serge Martin Jean-Pierre Caravel Jean-Marc Péquignot Jean-Marie Cottet-Emard |
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Affiliation: | (1) Centre de recherches du service de santé des armées, 38702, La Tronche cedex, France;(2) Institut de médecine aéronautique du service de santé des armées, BP 73, 91223, Brétigny sur Orge cedex, France;(3) Service de médecine nucléaire, Hôpital Michallon, CHU Grenoble, BP 217, 38043, Grenoble cedex 9, France;(4) UMR CNRS 5123, Université Claude Bernard–Lyon I, 43 Boulevard du 11 Novembre 1918, 69622 Villeurbanne Cedex, France;(5) Laboratoire de physiologie de lenvironnement, Faculté de médecine Grange Blanche, 8 avenue Rockefeller, 69373, Lyon cedex 08, France |
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Abstract: | Erythropoiesis was studied in 11 subjects submitted to a 4-h hypoxia (HH) in a hypobaric chamber (4,500 m, barometric pressure 58.9 kPa) both before and after a 3-week sojourn in the Andes. On return to sea level, increased red blood cells (+3.27%), packed cell volume (+4.76%), haemoglobin (+6.55%) (P<0.05), and increased arterial partial pressure of oxygen (+8.56%), arterial oxygen saturation (+7.40%) and arterial oxygen blood content (CaO2) (+12.93%) at the end of HH (P<0.05) attested high altitude acclimatization. Reticulocytes increased during HH after the sojourn only (+36.8% vs +17.9%, P<0.01) indicating a probable higher reticulocyte release and/or production despite decreased serum erythropoietin (EPO) concentrations (–46%, P<0.01). Hormones (thyroid, catecholamines and cortisol), iron status (serum iron, ferritin, transferrin and haptoglobin) and renal function (creatinine, renal, osmolar and free-water clearances) did not significantly vary (except for lower thyroid stimulating hormone at sea level, P<0.01). Levels of 2,3-diphosphoglycerate (2,3-DPG) increased throughout HH on return (+14.7%, P<0.05) and an inverse linear relationship was found between 2,3-DPG and EPO at the end of HH after the sojourn only (r=–0.66, P<0.03). Inverse linear relationships were also found between CaO2 and EPO at the end of HH before (r=–0.63, P<0.05) and after the sojourn (r=–0.60, P=0.05) with identical slopes but different ordinates at the origin, suggesting that the sensitivity but not the gain of the EPO response to hypoxia was modified by altitude acclimatization. Higher 2,3-DPG levels could partly explain this decreased sensitivity of the EPO response to hypoxia. In conclusion, we show that altitude acclimatization modifies the control of erythropoiesis not only at sea level, but also during a subsequent hypoxia. |
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Keywords: | Erythropoiesis Human High altitude acclimatization Erythropoietin 2,3-diphosphoglycerate |
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