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1 Dept of Internal Medicine and Medical Specialities, University of Catania, 2 Dept of Internal Medicine, and 5 Pathology, IRCCS S. Matteo and University of Pavia, Italy. 3 University Cayetano Heredia, Lima, Peru. 4 Dept of Anaesthesiology, University of Regensburg, Germany.
CORRESPONDENCE: L. Spicuzza, Dept of Internal Medicine and Medical Specialities, University of Catania, Catania, Italy. Fax: 39 0957594532. E-mail: luciaspicuzza@tiscalinet.it
Keywords: autonomic nervous system, chronic mountain sickness, erythropoietin, high altitude, polycythaemia, sleep disturbances
Received: January 3, 2003
Accepted August 21, 2003
| Abstract |
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Awake arterial oxygen saturation (Sa,O2) was significantly lower in patients with EEthan in controls (83.7±0.3% versus 85.6±0.4%). In both groups, the mean Sa,O2 significantly decreased during sleep (to 80.0±0.8% in EE and to 82.8±0.5% in controls). The mean Sa,O2 values remained significantly lower in patients with EE than in controls at all times of the night, and patients with EE spent significantly more time than the controls with an Sa,O2 of <80%. There were no differences between the two groups in the number and duration of the apnoeas/hypopnoeas. None of these variables were affected by O2 administration. In both groups the AHI positively correlated with the hypercapnic ventilatory response.
Andean natives undergo minor respiratory disorders during sleep. The reduction inoxygen saturation found in subjects with excessive erythrocytosis was small, yet consistent and potentially important, as it remained below the threshold known for theincrease in erythropoietin stimulation. This may be an important factor promoting erythropoiesis, but its relevance needs to be further explored.
Excessive erythrocytosis (EE) and hypoxaemia are the major features of a syndrome known as "chronic mountain sickness" (CMS) 1, 2 affecting millions of highlanders around the world and particularly common among Andean natives. The pathogenesis of EE is still unclear. In fact, while the increased erythropoiesis in highlanders is considered a mechanism of adaptation to the hypoxic environment, it is not clear why some of these subjects develop EE. One possible explanation is that a blunted hypoxic ventilatory response observed in highlanders with EE may induce a chronic hypoventilation that worsens the hypoxaemia 3. Other authors have suggested that sleep-related hypoxaemia may be the cause of EE 2, 4. This suggestion is based on the observation that hypoventilation is a physiological feature of the sleep state at sea-level as well 5. In addition, substantial nocturnal hypoxaemia has been reported in highlanders at 3,100 m and 3,658 m 6, 7 and sleep-disordered breathing (SDB) is a common finding in lowlanders ascending to high altitude 810. Coote and co-workers 11, 12 were the first toperform sleep studies in healthy Andean natives above 4,000 m and to determine the presence of nocturnal periodic breathing associated with a moderate fall in arterial oxygen saturation (Sa,O2). This finding led these authors to emphasise the importance of studying the nocturnal respiratory pattern in detail in these subjects. This should allow definitive conclusions to be drawn about the importance of nocturnal hypoventilation and/or SDB in the development of polycythaemia. However, to date, a comparison of the nocturnal respiratory profile between Andean highlanders with and without EE has never been performed.
Therefore, the frequency and duration of nocturnal apnoea/hypopnoea episodes, oxygen saturation, and sleep parameters in a group of patients with EE were compared with a group of controls that were permanent residents in the Andean town of Cerro de Pasco (Peru) at an altitude of 4,380 m.
The occurrence of SDB at altitude could be related to an altered hypoxic and/or hypercapnic ventilatory response 10, 13, 14. However, the ventilatory control of lowlanders during acute exposure to altitude is markedly different from that found in altitude natives 3, 15. Therefore, in order to investigate a possible correlation between the hypoxic/hypercapnic ventilatory response and the presence of SDB in the subjects, the ventilatory response to isocapnic hypoxia and to normoxic hypercapnia was assessed by classic rebreathing manoeuvres.
Finally, in a preliminary report, it was suggested, at least during wakefulness, that the depressed ventilation described in patients with EE may be reversed by the acute (1 h) administration of O2 15; similarly, a recent study showed an increase in ventilation during O2 administration in similar patients 16. These previous references thus provided a rationale for testing whether the 1-h administration of O2 prior to sleep could improve oxygen saturation (and consequently sleep parameters) during the night.
| Methods |
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64%. The sd of Ht and Hb in the healthy middle-aged male population in Cerro de Pasco is 3.13% and 1.21 g·dL1, respectively 19. Therefore, the EE group was comprised ofthose subjects with an Ht of
70% and Hb of
22.5 mg·dL1, and the control group of subjects with an Ht
60% and Hb
19.5 mg·dL1. Two groups of 10 subjects were established with these characteristics and provided a chance of
99% for detecting significant differences in these variables. All the subjects were selected from the male population of Cerro de Pasco among those who fulfilled these criteria. All subjects were Mestizos who were born and had lived their life at that altitude (no visit to a lower altitude in the last 12 months) and none of them was employed as a miner. The characteristics of the subjects are shown in table 1
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| Study protocol and polysomnography |
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or
frequency having a duration of >3 s associated with an increase in chin EMG 22. Arousal index was defined as the number of arousals·h sleep1. Apnoeas and hypopnoeas were defined as a complete cessation or a >50% decrease in airflow, respectively, for
10 s, associated with a decrease in Sa,O2 of
3%. Obstructive apnoeas were distinguished from central apnoeas by the presence of respiratory effort (thoracic/abdominal excursions). The apnoea/hypopnoea index (AHI) was defined as the number of apnoeas or hypopnoeas per hour of sleep according to standard definitions 20. The drop in Sa,O2 (
Sa,O2) during each apnoea/hyperpnoea episode was measured and averaged for the whole study period and is labelled m
Sa,O2. The mean Sa,O2 during 10 min of recording before sleep was defined as "awake Sa,O2". The average of the Sa,O2 during the whole sleep time is defined as "mean sleep Sa,O2".
Hypoxic and hypercapnic ventilatory response
On the first and second study day, in order to determine the hypoxic (HVR) and the hypercapnic ventilatory response (HCVR), the subjects were studied in the seated position (in the morning at rest for
2 h, and
2 h after a light breakfast with no tea or coffee), and connected to a rebreathing circuit through a mouthpiece, as previously described 2325. To assess the response to progressive hypoxia, end-tidal carbon dioxide (ETCO2) was kept constant by passing a portion of the expired air into a scrubbing circuit before returning it tothe rebreathing bag. Conversely, when the response to progressive hypercapnia was tested, O2 was continuously supplied to the rebreathing circuit in order to maintain Sa,O2 at sea-level normoxic levels (>95%). The rebreathing tests terminated when Sa,O2 reached 70% (hypoxic response) or when ETCO2 reached 7.3 kPa (55 mmHg; hypercapnic response). ETCO2 was continuously monitored by COSMOplus (Novametrix, Wallingford, CT, USA) connected to a mouthpiece, and Sa,O2 by a 3740 Ohmeda Pulse Oximeter (Ohmeda, Englewood, CO, USA). The COSMOplus was precalibrated against known gas mixtures. The airway flow was continuously measured by a Fleish pneumotachygraph (Metabo Epalinges, Lausanne, Switzerland), connected to a differential pressure transducer (RS part N395-257; RS Components Ltd, Corby, UK) connected in series in the expiratory part of the rebreathing circuit. The calibration ofthe pneumotachygraph was checked before and after eachrebreathing manoeuvre. All signals were acquired on a Macintosh personal computer (G3 model; Apple, Coupertino, CA, USA) at the frequency of 300 per sample channel. Therespiratory flow signal was integrated by software, and each breath was identified by an automatic and interactive program. Breathing rate, tidal volume, and minute ventilation (V'E) relative to each breath were recognised with their corresponding values of Sa,O2 and ETCO2. The chemoreflex sensitivity to hypoxia or hypercapnia was obtained from the slope of the linear regression of V'E versus Sa,O2 or ETCO2, respectively 2325.
Statistical analysis
Differences between groups were analysed using the unpaired t-test or the Mann-Whitney U-test. Differences between groups and sleep and respiratory variables in the two groups and by effects of O2 administration were also tested bymixed-design analysis of variance. Data are presented as mean±sd. Linear regression was used to assess correlations between parameters.
| Results |
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Sleep variables
During the first study night no significant differences were observed in the TST, sleep efficiency, stages II, III, IV and rapid eye movement (REM) sleep, and the arousal index between the EE and the controls (table 2
). Only stage I of sleep was slightly longer in the controls. The arousal index didnot correlate with any of the haematological, clinical, demographic or polysomnographic variables of the subjects. For both groups all sleep variables remained unchanged during the second night of the study, in which O2 was administered for 1 h before sleep (table 2
).
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38% of the night in the range 7680%). Since the TST was the same for both groups, the same findings would be observed if the data were evaluated in terms of actual time spent at each level of Sa,O2, rather than interms of percentage. Overall, the subjects with EE spent 10,343±1,856 s (i.e. nearly 3 h) between 7680% Sa,O2, whereas the controls spent 3,039±1,543 s (only
50 min) in the same Sa,O2 range (p<0.01).
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Sa,O2 were similar in the two groups (table 3
10, the severity of the sleep disorder could be defined as "mild", according to the standard criteria for sea level 26. The AHI showed a fair correlation with subjects' age (r2=0.22, p<0.05) and, more consistently, with the slope of HCVR (r2=0.59, p<0.05) but not with the slope of HVR. Administration of O2 prior to sleep in the second night of the study did not alter any of these respiratory parameters (table 3
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| Discussion |
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In contrast to the many studies on SDB in lowlander visitors to altitude, very few studies have addressed the question of breathing during sleep in high-altitude natives, particularly in those with EE. This study clearly indicates that in Andean natives the occurrence of SDB among patients with EE is similar to high-altitude natives with relatively normal haematocrit in terms of frequency and duration of the periodic breathing. However, although the absolute extent ofnocturnal desaturation was the same for EE and controls, EE subjects, who had lower Sa,O2 during the day, maintained a lower Sa,O2 during the night. This difference was small in absolute terms, but very consistent and prolonged during the entire period of the night, and, in addition, it allowed the EE group to spend a substantial period of the night with an Sa,O2 of <80%. Transient oxygen desaturations, even reaching very low values in Sa,O2, are not considered an important stimulus for the production of erythropoietin, whereas clinical conditions such as chronic obstructive pulmonary diseases and chronic respiratory failure, characterised by stable and prolonged hypoxaemia may be associated with polycythaemia 27. Therefore, it is likely that the percentage of sleep time spent below a specific given level of Sa,O2 may be a determinant of the haematopoietic response to hypoxia, even in theabsence of transient dramatic desaturations.
The authors found that EE patients spent one-half of the night with an Sa,O2 in the range of 8185%, and 38% of the night in the range of 7680%, whereas the healthy controls spent most of the time with an Sa,O2 of >81%. This points to apossible Sa,O2 cut-off value of
80%, below which the haematopoiesis may be stimulated. The presence of a threshold of 80% Sa,O2 for the stimulation of erythropoietin hasbeen clearly documented previously 28. Therefore, it is possible that a mean reduction of 34% in nocturnal Sa,O2, which has no effect in normal subjects, may drag patients with EE that have lower diurnal Sa,O2 below a value that is critical for erythropoiesis. This exactly crosses the difference between the controls and EE subjects (fig. 1
), and may thus explain at least in part why, even in the absence of major respiratory disorders some subjects develop polycythaemia, while others do not, despite intergroup small differences in Sa,O2. At an altitute of 3,100 m (Leadville, Colorado) and at 3,658 m (Lhasa), it has been found that nocturnal hypoxaemia in polycythaemic subjects is more marked compared with the EEgroup (although polycythaemia is less severe at lower altitude) 6, 7. One possible explanation is that there may be differences between ethnic groups. It is also possible that thedifferent altitude at which these studies were performed may have determined these different results. While at lower altitude a more severe SDB is necessary in order to induce excessive polycythaemia, at higher altitude even a mild SDB could induce moderate/severe polycythaemia, whereas a more severe SDB could be incompatible with life.
The finding that SDB, though not severe, occurs in the Andean population at 4,380 m is per se of interest. In fact periodic breathing was not reported in a small group of Himalayan Sherpas at an altitude of >5,000 m 13. If these differences were confirmed by larger studies on both populations, then nocturnal respiratory instability in the Andeans may be considered a sign of poor adaptation to altitude.
Both hypoxia and hypocapnia have been suggested as the stimuli that trigger and sustain periodic breathing at altitude 29, 30. In sea-level natives ascending to altitude, SDB isrelated to an increased HVR 13, 14 but in long-term residents at altitude the HVR is blunted 3, 31, therefore it is likely that other mechanisms may determine the nocturnal respiratory instability in these subjects. These findings support the hypothesis that the fall in arterial carbon dioxide tension (Pa,CO2) may be a determinant factor. The AHI did not correlate with basal ETCO2, in agreement with a previous report 32 but correlated significantly with the HCVR. Since a fall in Pa,CO2 below the apnoeic threshold depends on the individual chemoreflex sensitivity, it is not surprising that the AHI correlated with HCVR rather than with the ETCO2 level itself. The concept that a high gain of central chemoreflex response may lead to nocturnal periodic breathing has been evidenced from many studies in animal and humans 29. Briefly a low ETCO2 at basal condition may induce hyperventilation with further decrease in CO2 below the apnoeic threshold. The hyperventilation that occurs after each apnoea further decreases the CO2 level triggering the next apnoea andfinally leading to a vicious circle. In patients with high hypercapnic chemoreflex sensitivity these responses are enhanced and apnoeas more likely to occur. This mechanism is similar to what is shown at sea level in patients with chronic heart failure experiencing nocturnal (and also diurnal) periodic breathing; in addition, for these patients a clear correlation has been shown between HCVR and SDB 33.
Despite this, a significant difference in HCVR was not found in the two groups, in agreement with a recent study 34, and with the rest of the literature. This suggests that this factor may be able to explain the occurrence of sleep abnormalities (which in fact were present in both EE and controls to a similar extent), as it does in some patients at sealevel, but it does not necessarily play a partial role in the origin of EE, whose cause is probably more related to the lower Sa,O2. The lack of difference in HVR in the two groups could be due to the relatively small number of subjects studied, but again a normal or slightly reduced HVR may notbe necessarily the cause of the reduced Sa,O2. A depressed HVR is a common finding in Andean natives living at high altitude, regardless of the presence of EE 4, 16, 31, and even recent studies confirmed the presence of very small differences between these two groups of subjects 16. The age of the subjects also has some influence in the occurrence of nocturnal respiratory instability as a slight but significant positive correlation with the AHI was found. There is some evidence that age can be a risk factor for nocturnal periodic breathing also in lowlanders at sea level in the presence of some pathological conditions 35.
All sleep variables were similar in the two groups and this isin agreement with data reported at the same 11, 12 or at alower altitude 6. In contrast, lowlanders undergo profound changes in sleep pattern during the first days after ascending to altitude, then improve with acclimatisation 8, 36. Taken together these observations suggest that sleep is a physiological variable characterised by a fairly rapid adaptation to the environmental conditions and is not negatively influenced by chronic exposure to altitude.
This study indicates that Andean natives, with or without excessive erythrocytosis, undergo mild respiratory disorders during sleep, and that subjects with excessive erythrocytosis have a slightly (but highly significant) lower nocturnal arterial oxygen saturation and spend more time than controls with an arterial oxygen saturation below 80% during the night. Since an arterial oxygen saturation of 80% has been previously identified as a threshold for erythropoiesis, further studies are needed to establish whether or not a link exists between these changes in nocturnal arterial oxygen saturation and excessive erythrocytosis.
| Acknowledgements |
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