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Vol. 84, Issue 4, 1242-1251, April 1998
Departments of Physiology, Pathology, and Medicine, Dartmouth Medical School, Lebanon, New Hampshire 03756-0001; and Cardeza Foundation for Hematological Research, Department of Medicine, Thomas Jefferson University, Philadelphia, Pennsylvania 19107
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ABSTRACT |
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We examined erythropoietin (EPO) gene expression and EPO production during hypoxia in two Sprague-Dawley rat strains with divergent polycythemic responses to hypoxia. Hilltop (H) rats develop severe polycythemia, severe hypoxemia, and pulmonary artery hypertension. The H rats often die from a syndrome indistinguishable from chronic mountain sickness (CMS) in humans. Madison (M) rats develop polycythemia and pulmonary artery hypertension that is modest and suffer no excess mortality. We tested the hypothesis that these rat strains have different stimulus-response characteristics governing EPO production. Rats of each strain were exposed to hypoxia (0.5 atm, 73 Torr inspired PO2), and renal tissue EPO mRNA and EPO levels, plasma EPO, ventilation, arterial and renal venous blood gases, and indexes of renal function were measured at fixed times during a 30-day hypoxic exposure. During extended hypoxic exposure, H rats had significantly elevated renal EPO mRNA, renal EPO, and plasma EPO levels compared with M rats. Ventilatory responses and indexes of renal function were similar in the strains during the hypoxic exposure. H rats had greater arterial hypoxemia from the onset of hypoxia and more severe renal tissue hypoxemia and greater polycythemia after 14 days of hypoxic exposure. When EPO responses were expressed as functions of renal venous PO2, the two strains appeared to lie on the same dose-response curves, but the responses of H rats were shifted along the curve toward more hypoxic values. We conclude that H rats have significantly greater polycythemia secondary to poorer renal tissue oxygenation, but the stimulus-response characteristics governing EPO gene expression and EPO production do not seem to differ between M and H rats. Finally, the regulation of EPO levels during hypoxia occurs primarily at the transcriptional level.
erythropoietin; gene expression; renal oxygenation; renal work; tissue hypoxia; high altitude
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INTRODUCTION |
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POLYCYTHEMIA is a compensatory mechanism to sustain
O2 delivery during life at high
altitude, but excessive polycythemia is associated with chronic
mountain sickness (CMS). There is, on average, an increase in
hematocrit (Hct) after altitude exposure, but there is considerable
individual variation, and only a small number of high-altitude
residents develop CMS. The origin of the variation among individuals is
unknown, but variation in erythropoietin (EPO) responses to equivalent
hypoxic stress is a tenable hypothesis. EPO, a glycoprotein growth
factor, regulates the rate of red blood cell production by stimulating
the proliferation and differentiation of erythroid precursor cells
(12). EPO synthesis in adult mammals occurs primarily in the kidney
(19), and hypoxia in the kidney from a variety of causes (e.g.,
high-altitude exposure and anemia) stimulates the synthesis and release
of EPO, which are followed by increased production of red blood cells.
Recent molecular studies in vivo (2, 32-34) and in vitro (17)
showed that hypoxia or cobalt treatment led to rapid accumulation of
EPO mRNA in the kidney or in cultured hepatoma cell lines, and
detection of EPO mRNA preceded the appearance of EPO in plasma or in
cultured medium. Hence, accelerated EPO gene expression is the first
step in the polycythemic responses to hypoxic or cobalt treatment. The
location(s) of the hypoxic sensing mechanism is controversial. The
adequacy of renal tissue oxygenation at the EPO-producing sites is
thought to be the immediate signal regulating EPO production (22), but a more potent extrarenal sensing mechanism has also been postulated (31). Renal tissue oxygenation depends on the relationship between renal tissue O2 delivery, a
function of arterial O2 content
[CaO2, which depends on arterial
PO2
(PaO2) and Hct] and renal blood
flow, and renal tissue O2
consumption (
O2), a function of the excretory activity of the kidney. Therefore, there may be a link
between renal excretory function and the regulation of EPO production
(10, 11, 13). Polycythemia following EPO release ought to improve renal
tissue oxygenation and reduce EPO synthesis. However, changes in EPO
levels, renal tissue oxygenation, and Hct are not well correlated in
time, and the classic concept of a negative-feedback control of EPO
production by a polycythemic response remains debatable (3, 9, 28).
We have studied two Sprague-Dawley rat strains with marked differences in the propensity to develop CMS after chronic exposure to hypoxia: Hilltop (H) rats develop excessive polycythemia, accentuated hypoxemia, and severe pulmonary hypertension associated with a high mortality rate; Madison (M) rats develop only moderate polycythemia and pulmonary hypertension and no significant mortality (30). Excessive polycythemia apparent in H rats after 3 wk of exposure to a simulated altitude of 5,500 m was associated with persistent elevation of plasma and renal EPO (28). Metabolic degradation of EPO did not differ in the two rat strains, and the persistent elevation of EPO probably resulted from sustained EPO gene expression. In past experiments, high blood viscosity associated with excessive polycythemia in the H rats (Hct often >70%) may have compromised renal oxygenation and thereby enhanced EPO production (13, 28). In addition, there was a positive correlation between the extent of polycythemia and EPO production, which was not compatible with a negative-feedback control mechanism regulating EPO production. The purposes of the present study were to use the H and M rat strains 1) to characterize EPO gene expression and EPO production during chronic hypoxia, 2) to examine the relationships among the levels of EPO gene expression and EPO production and renal tissue oxygenation, and 3) to examine the notion of a negative-feedback control mechanism of EPO production.
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MATERIALS AND METHODS |
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Animals. Male Sprague-Dawley rats weighing 270-320 g were obtained from Hilltop (H), Scottsdale, PA (altitude-sensitive strain) and Madison, WI (M) breeding laboratories. There were two separate series of experiments: in one series of experiments, levels of EPO mRNA and EPO were measured; in the other, ventilatory and blood-gas responses, renal function, and renal oxygenation were measured. In each set of experiments, five groups of five to six rats from each strain were exposed to a simulated altitude of 0.5 atm (5,500 m, 73 Torr inspired PO2) for various durations (0, 6, and 24 h and 1, 3, 7, 14, 21, 28, and 30 days). Supplementary experiments were performed to test the effects of cobalt or combined cobalt and hypoxia treatment on EPO and EPO mRNA production.
Measurements of EPO mRNA and EPO.
Two methods were used to measure EPO mRNA: Northern and slot-blot
analyses using polyadenylated RNA
[poly(A)+ RNA] were
used in early experiments, and a highly sensitive RNase protection
assay was employed later in the study. EPO gene probes for Northern
blot studies were provided by Dr. E. Goldwasser (University of
Chicago). The probes were 1.0- and 1.2-kb
Pst I restriction fragments of the
cloned mouse EPO gene. The 1.2-kb fragment contained all of exons 2 and
3 and part of exon 4. The 1.0-kb fragment contained the remainder of
exon 4 and part of exon 5. The probes were labeled with
[32P]CTP (3,000 Ci/mmol; ICN, Costa Mesa, CA) to high specific activities (2 × 108 dpm/µg) using a nick
translation kit (BRL, Bethesda, MD) according to the manufacturer's
instructions. Probes were denatured by heating at 100°C for 10 min
and quenched on ice immediately before use. RNAs were isolated from
tissue homogenates by extraction with 4 M guanidine isothiocyanate and
sedimentation of RNA through 5.7 M cesium chloride (4).
Poly(A)+ RNA was isolated by
chromatography on oligo dT-cellulose. For electrophoresis, 6-30
µg of poly(A)+ RNA per lane were
loaded on formaldehyde-1.0% agarose gels. After electrophoresis, the
gels were blotted onto nitrocellulose filters and dried under vacuum at
80°C for 2 h. Northern and slot blots were hybridized with
32P-labeled probe at 42°C for
18 h and washed using standard methods. The blots were exposed to Kodak
XAR-5 X-ray film (Eastman Kodak, Rochester, NY) with an intensifying
screen at
70°C. The EPO mRNA was quantitated by scanning
densitometry. Results from Northern blots were expressed as
densitometric units per microgram of RNA loaded. As an internal control
for RNA loading, Northern and slot blots were probed with a mouse
-actin probe. Splenic poly(A)+
RNA was used as a negative control.
-32P]UTP (29.6 TBq/mM; Amersham, Arlington Heights, IL). Before hybridization, an
equal amount of each RNA sample was visualized by ethidium bromide-stained agarose gel electrophoresis to verify quantification and integrity of samples. RNA samples were hybridized overnight in 30 µl of hybridization buffer at 45°C with 0.5 × 106 cpm of labeled probe. RNase
digestion was performed at 30°C for 1 h using RNase T1
(Boehringer-Mannheim, Indianapolis, IN). The protected fragments were
separated on a denaturing 8% acrylamide-7 M urea gel and analyzed by
autoradiography. The autoradiographs were quantitated by scanning with
a BIO-Imaging analyzer (Fuji Medical System).
EPO was measured by radioimmunoassay using antiserum against human
recombinant EPO (Incstar, Stillwater, MN), as previously described
(28).
Measurements of ventilation, renal function, and renal tissue
oxygenation in fully awake and chronically instrumented rats.
Ventilation was measured in a whole body plethysmograph, as previously
described (28). The following renal variables were measured at each
designated time: urine output, sodium and potassium excretions, plasma
sodium and potassium concentrations, and sodium reabsorption. Potassium
and sodium concentrations were measured with a flame photometer (model
FLM3, Radiometer America, Cleveland, OH). The glomerular filtration
rate (GFR) was measured using polyfructosan (15), and renal plasma flow
was measured using p-aminohippurric acid by the method of Bratton and Marshall as modified by Smith et al.
(35). Urine flow and clearance rates are expressed per 100 g of body
weight. Hct was determined by a micromethod. Arterial and venous blood
gas samples were obtained anaerobically by withdrawing 300 µl from
the rat; only the last 160 µl were used for analysis. The residue was
returned to the rat. pH, PO2, and
PCO2 were measured with
microelectrodes at 37°C (model BMS 3 MK2, Radiometer America).
Hypoxic exposure did not affect the shape of the oxyhemoglobin dissociation curve in the H or M rats, and the
O2 content in arterial and venous
blood was estimated from a rat oxyhemoglobin dissociation curve after
correction for the blood pH measured in vivo (21). Renal blood flow was
calculated from renal plasma flow and the Hct. The renal coefficient of
O2 delivery (COD) was calculated by multiplying renal blood flow by CaO2,
and renal
O2 was calculated by multiplying renal blood flow by the renal arteriovenous
O2 content difference.
Surgical preparation. Four to 5 days before an experiment, catheters were implanted in each animal in the urinary bladder, femoral artery, and left renal and right external jugular veins under anesthesia using a combination of ketamine (60 mg/kg body wt im) and pentobarbital sodium (20 mg/kg body wt ip), as previously described (29). After surgery, each rat was treated with penicillin (100,000 U daily im for 5 days) and returned to the presurgical altitude immediately after recovery from anesthesia. All rats were allowed free access to water and laboratory rat chow. The animals were acclimated to a plastic restraining cage for 2 days before the renal function studies. The animals recovered from surgery uneventfully, and the majority gained weight by the time of measurements.
Experimental procedures. During the measurements, each rat was housed in a restraining cage. A Plexiglas hood was fitted over the front of the restraining cage so that the desired gas mixture could be flushed through the hood. Renal hemodynamic values were measured (29), and the exposed end of the bladder catheter was extended with a short length of polyethylene tubing to allow collection of urine under the restraining cage. Urine volume was measured by weight. After 30-40 min of equilibration, two to three samples of urine and arterial and renal venous blood were obtained from each animal under appropriate PO2 conditions. To avoid possible adverse effects of repeated blood sampling that might change the Hct, each rat was studied only once.
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RESULTS |
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Effect of extreme hypoxia and cobalt on EPO gene expression and EPO levels in H and M rats. Northern blot analysis failed to detect EPO mRNA in the kidney in either rat strain during exposure to a simulated altitude of 5,500 m, even though poly(A)+ RNA was used. To test the sensitivity of the Northern blot analysis, extreme stimuli, severe hypoxia alone (7,300 m simulated altitude or 65 Torr inspired O2) or combined severe hypoxia (7,300 m) and cobalt chloride (60 mg/kg sc) treatment, were used. The results are presented in Fig. 1. Under sea-level conditions, no EPO mRNA was detected in the kidney (Fig. 1B, lanes 3 and 4), and no strain difference in plasma EPO levels was detected (Fig. 1A, lanes 3 and 4). The EPO mRNA increased markedly in both rat strains during severe hypoxia (data not shown) and during combined hypoxia and cobalt injection (Fig. 1B, lanes 1 and 2), but there were no strain differences under these conditions. The combined stimuli elevated the plasma EPO levels from control values of 59.5 ± 12.7 to 2,234.4 ± 632.5 mU/ml in the H rats and from 56.6 ± 6.1 to 2,705.7 ± 451.3 mU/ml in the M rats. These findings indicate that the Northern blot analysis could detect EPO mRNA but was insensitive to the EPO mRNA changes during exposure to 10.5% inspired O2 (5,500 m). Therefore, a more sensitive RNase assay was used in subsequent experiments.
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Effect of 10.5% inspired O2 on EPO gene expression and EPO levels in H and M rats. The results of the EPO mRNA RNase protection analysis of total RNA from the kidney are summarized in Fig. 2A, and the quantitative relationships of renal EPO mRNA as estimated by phosphor image analysis are shown in Fig. 2B for each rat strain. At sea level, EPO mRNA levels were equivalent in the two rat strains. After 6 h of hypoxic exposure, EPO mRNA markedly increased in both rat strains, but the increase was at least 100% higher in the H than in the M rats. The EPO mRNA fell precipitously after 24 h of hypoxic exposure but remained significantly elevated above the control values in the H rats throughout the entire period of exposure. In contrast, EPO mRNA levels in the M rats fell toward the sea-level control values after 24 h of hypoxia. The results demonstrate exaggerated expression of the EPO gene in kidneys of H rats during hypoxic exposure. EPO mRNA was undetectable in the spleen, heart, or liver in H and M rats under control and hypoxic conditions. In contrast to the response to 10.5% inspired O2, cobalt injection (60 mg/kg sc) elicited equivalent accumulation of EPO mRNA in the kidney 6 h after treatment in both rat strains (Fig. 3). Thus RNase and Northern blot assays demonstrate no strain difference in EPO gene expression after cobalt treatment.
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Effect of 10.5% inspired O2 on renal
function in conscious H and M rats.
We examined a variety of aspects of renal function in H and M rats
under the hypoxic conditions. These results are summarized in Table
1. There were no strain differences in urine output, plasma sodium, sodium excretion, or GFR at sea level or at any point
during hypoxic exposure. Neither the plasma potassium (range 3.7-4.5 meq/l) nor potassium excretion (range 0.6-1.1
meq · l
1 · min
1)
differed between strains or across times of hypoxic exposure (data not
shown). Plasma sodium was significantly less than the sea-level value
on days 1 and
14, when data from H and M rats were
pooled (there was a significant main effect of the duration of altitude
exposure). Serum sodium on day 14 was
also less than sea-level control, but this failed to achieve
statistical significance (P = 0.054).
Plasma sodium was significantly less in the M than in the H rats on
day 14 only. The fractional sodium
reabsorption was significantly less than sea-level values on
day 1, when results from H and M rats
were pooled at each exposure time. Sodium excretion did not differ
between strains or among exposure times. However, the largest sodium
excretion occurred on day
1 in both strains, which is consistent with the lower
fractional sodium reabsorption at that time. A reduction in sodium
reabsorption often occurs in the first 24-48 h of acclimatization
to high altitude (18). The GFR was constant at all altitudes and
similar in the two strains. The changes in renal excretory function are
statistically significant but of small magnitude, and the work of the
kidney was maintained during hypoxic exposure.
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Effect of 10.5% inspired O2 on systemic
and renal tissue oxygenation in conscious H and M rats.
Table 2 summarizes
PaO2, renal venous
PO2
(PrvO2),
CaO2, renal venous
O2 content
(CrvO2), renal
O2, and COD measured or
calculated in H and M rats at sea level and during hypoxic exposure.
There were no strain differences in any of these variables at
sea level. PaO2 fell precipitously at
the onset of hypoxic exposure in both rat strains.
PaO2 in the H rats decreased as the
hypoxic exposure persisted, whereas PaO2
in the M rats remained relatively stable and even increased over the
remainder of the hypoxic exposure. As a result, the mean value of
PaO2 was ~41 Torr in the H rats and 48 Torr in the M rats at the end of 30 days.
PrvO2 was
similar at sea level in H and M rats and fell at the onset of
hypoxia. PrvO2
values paralleled the arterial values during hypoxia in both strains.
The initial hypoxic
PrvO2 values were similar, but
PrvO2 in H rats
fell after the initial hypoxic exposure and remained low throughout the
30-day hypoxic period. In contrast,
PrvO2 rose
steadily from the onset of hypoxia toward the sea-level value in M
rats. Although
PrvO2 remained significantly below sea-level values in both strains,
PrvO2 values were greater in M than in H rats by day 14, and this
persisted to the conclusion of the study. The hemoglobin concentration
was similar in the strains at sea level, rose in both strains, and was
significantly greater than the sea-level value from day 3 until the conclusion of the study. The increase in hemoglobin was
greater in H rats from day 14 onward.
CaO2 fell in both strains at the onset
of hypoxia but rose steadily until day 30, when
CaO2 had returned to the sea-level
range. The restoration of CaO2 to the
sea-level range was achieved by different mechanisms in each strain, as
discussed below.
CrvO2 was
similar at sea level in the two strains and fell at the onset of
hypoxia. CrvO2
rose in both strains, but the rise was more rapid in the M rats. Renal venous CO2 exceeded the sea-level value on day
14 in M rats and on day 30 in H rats. Renal blood flow
was a constant function of Hct in both strains and increased gradually
as the hypoxic exposure progressed and Hct rose (C. D. Thron, J. Chen,
J. C. Leiter, and L. C. Ou, unpublished observations). The renal COD, the product of renal blood flow and
CaO2, fell at the onset of hypoxic
exposure but increased steadily as Hct rose. The renal COD did not
differ between strains, and in both strains the renal COD was
significantly less than the sea-level value on days
1 and 3 and greater
than the sea-level value by day 30 of
hypoxic exposure. The mechanism whereby equivalent renal
O2 delivery was maintained
differed in the two strains: hemoglobin was greater and
PaO2 was lower in the H rats; the
reverse was true in the M rats. Renal
O2 was similar in H and M
rats at sea level and at each particular altitude, but when pooled
across all altitude conditions, renal
O2 was significantly lower in
the M rats (main effect of strain).
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Effect of 10.5% inspired O2 on
ventilatory response in conscious H and M rats.
To determine the cause of the accentuated hypoxemia in the H rats
during hypoxic exposure, minute ventilation
(
E) at sea level and at a variety of times during the hypoxic exposure was measured in H and M rats. The results of measurements of
E, PaO2, and arterial
PCO2
(PaCO2) are displayed in Fig. 6. There were no differences in
E and
PaCO2 in the two rat strains at
sea level.
E
increased and PaCO2 decreased similarly
in response to hypoxic exposure in the H and M rats, despite the marked
strain differences in PaO2.
E remained
similar in the H and M rats as the H rats became more hypoxemic late in
the hypoxic exposure period. However, we have never detected any
differences in hypoxic or hypercapnic ventilatory responses at sea
level or at any time during exposure to simulated high altitude (28).
Furthermore, we have seen in previous studies greater ventilatory
responses associated with more severe hypoxemia in the H than in the M
rats after chronic exposure to hypoxia (7) and after monocrotaline treatment (5).
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DISCUSSION |
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In the present study we examined the molecular and genetic mechanisms
of polycythemic responses to hypoxia in H and M rats during chronic
hypoxic exposure and the factors thought to stimulate a polycythemic
response to hypoxia: the balance between renal O2 delivery and renal
O2. Because hypoxic exposure
results in development of CMS with excessive polycythemia in the H rats
but elicits only moderate polycythemia and no apparent ill effects in
the M rats, the present results provide a spectrum of hypoxic responses
within which to analyze the mechanism(s) underlying the widely
different polycythemic responses in healthy and diseased states at high
altitude.
Molecular and genetic mechanisms of different polycythemic responses to hypoxia in H and M rats. The present study revealed, for the first time, the sequence of events, starting from enhanced expression of the EPO gene to elevated plasma and renal tissue EPO levels to, finally, the polycythemic responses in rats during chronic exposure to a simulated altitude of 5,500 m. The levels of EPO mRNA that accumulated with 10.5% inspired O2, as employed in this study, could not be detected by Northern blot analysis but were readily detectable by a more sensitive RNase protection analysis (33). RNase assays are more sensitive than Northern blot analysis, but a mouse probe was used for the Northern blot analysis in this study, which might further reduce the sensitivity of the particular Northern blot analysis we performed. The exaggerated EPO production and excessive polycythemia, which developed in the H rats during hypoxic exposure, originated from an inordinate and sustained expression of the EPO gene in the kidney (28, 30). Because no EPO mRNA was detectable in liver, heart, or spleen by Northern blot or RNase protection assays under sea-level control and hypoxic conditions in both rat strains, the kidney must be the primary site of EPO production in the adult animals exposed to 10% inspired O2. This conclusion is supported by the negligible increase in circulating EPO levels in nephrectomized rats of both strains when exposed to severe hypoxia (28). There were no strain differences in the rates of EPO degradation in these two rat strains under control and hypoxic conditions (28). Therefore, the rate of EPO gene expression in the kidney is the major factor determining the levels of EPO mRNA production and the polycythemic response to hypoxia in the H and M rats. This conclusion, however, is at variance with the work of Tan et al. (36). Using a similar RNase protection assay, these authors observed that EPO mRNA increased significantly in the liver and spleen in rats exposed to hypoxia. This discrepancy could be due to the difference in severity of the hypoxic stimulus used in the two studies: 7% O2 was used in the study of Tan et al., whereas 10.5% O2 was employed in the present study.
When the animals were exposed to severe hypoxia with or without cobalt treatment, circulating EPO and renal tissue EPO mRNA levels were elevated and similar in the H and M rats. M rats were capable of mounting an EPO response; there is no evidence that deficient EPO-generating capacity in the M rats accounted for the different EPO responses reported here. The different EPO responses in the two rat strains appear to be hypoxia specific. Treatment with cobalt, another erythropoietic stimulus, enhanced EPO gene expression and EPO production similarly in H and M rats. Moreover, elevated EPO mRNA and circulating EPO levels in the chronically hypoxic H rats fell abruptly to sea-level control values when the animals were brought down to sea-level conditions. Rather than strain-specific differences in EPO regulation, more severe renal tissue hypoxia in the H than in the M rats during equivalent hypoxic exposure seems to account for the divergent EPO responses observed in this study (Fig. 5, Table 2).Regulation of EPO gene expression and EPO production.
The physiological mechanism regulating EPO gene expression and EPO
production remains incompletely understood. Renal tissue oxygenation is
undoubtedly the single most important factor (12, 22). The balance
between renal O2 delivery and
renal
O2 determines the level
of renal tissue oxygenation. Renal
O2 depends on the work of the
kidney, particularly sodium reabsorption, which is the primary
energy-requiring renal process (22, 38). Inhibition of proximal sodium
reabsorption attenuates the EPO response to hypoxia, presumably as a
result of decreased renal work and elevated renal tissue oxygenation,
but the inhibition must be sufficient to prevent reabsorption of at
least 20% of the filtered load of sodium (10, 11). In the present
study, there were only minor changes in fractional sodium reabsorption
and, in general, renal function was preserved without strain
differences at sea level or under hypoxic conditions. Despite stable
excretory renal function under control and hypoxic conditions, hypoxic
exposure elicited distinctly different changes in EPO gene expression
and EPO production in the two rat strains. The dissociation between
measures of renal function and EPO production under hypoxic conditions
renders unlikely any significant regulatory role of renal function in
the EPO response to hypoxia.
Role of renal tissue hypoxia.
Carbon monoxide and anemia stimulate EPO gene expression and EPO
production in the absence of changes in
PaO2; therefore, the renal
hypoxia-sensing process is probably located near a venous or tissue
site (20). The hypoxia-sensing process probably occurs adjacent to the
EPO-generating sites in the kidney in adult mammals (22, 31). Because
PrvO2
approximates the average renal tissue O2 level (37),
PrvO2 is an
estimate of the primary hypoxic signal determining EPO production.
Renal O2 delivery and renal
O2 did not differ in the two
rat strains under sea-level control or hypoxic conditions (Table 2).
Systemic arterial hypoxemia was more severe in the H than in the M
rats, and the severity of hypoxemia increased in the H rats, but not in
the M rats, as the hypoxic exposure was prolonged (Fig. 6) (7, 28). Not
surprisingly,
PrvO2 was lower
in the H than in the M rats after 2 wk of hypoxic exposure (Table 2)
(28). There is no reason to believe that the EPO stimulus-response
characteristics differ between the rat strains during chronic (
24 h)
hypoxia: H rats simply experienced greater hypoxic stimulation during
equivalent altitude exposure. Furthermore, there can be no effective
polycythemic compensation for arterial hypoxemia in the H rats: the
arterial values were below the threshold of the EPO response (Fig. 5).
Thus more severe renal tissue hypoxia can account for the inordinate
EPO gene expression and EPO production and, thereby, the excessive
polycythemia in the H rats during chronic hypoxic exposure.
Role of negative-feedback control. The early finding that a humoral erythropoiesis-stimulating factor (EPO) increased rapidly on hypoxic exposure and declined toward control levels led to the notion of a negative-feedback control mechanism regulating erythropoiesis. According to this concept, hypoxia stimulates EPO production and erythropoiesis; the resulting polycythemia increases the O2-carrying capacity and O2 content of blood, and this improves tissue oxygenation and turns off further production of EPO (14). The idea of EPO-O2-carrying capacity feedback is inherent in all EPO dose-response curves published: the Hct is plotted as the independent variable (14, 23). Nevertheless, EPO measurements using sensitive radioimmunoassay for EPO and studies of EPO mRNA levels have made it clear that a negative-feedback control mechanism does not account for the regulation of the polycythemic response to environmental hypoxia (3, 9). The high levels of renal EPO mRNA and circulating EPO apparent at the onset of hypoxic exposure declined within the first 24 h of hypoxia before any detectable polycythemia or increased O2-carrying capacity developed in this and other studies (9). The rapid decline in EPO mRNA during continued hypoxic exposure in the kidney was also unrelated to the rising circulating EPO levels; there is no evidence of direct negative feedback in which EPO might inhibit its own production (9). Furthermore, evidence obtained in the present study does not support the concept of a negative-feedback mechanism, in which a polycythemic response to hypoxia suppresses EPO production. Rather, the data in Fig. 5 indicate that feedback control of EPO gene expression and EPO production operates in terms of PrvO2, and polycythemia is only one of multiple factors modifying PrvO2. The pattern of EPO production was biphasic. At the onset of the hypoxic exposure, there was a sharp increase in EPO production, but in <24 h, EPO levels fell substantially but remained above control values. EPO levels rose slowly in the late stages of the hypoxic exposure in the H rats. PrvO2 follows a similar pattern: an initial sharp drop, a rapid recovery to a stable level in M and H rats, and a slow decline after 2 wk of continued hypoxia in H rats (Table 2) (28). The parallel pattern of changes in PrvO2 and EPO levels during hypoxia is consistent with feedback control of EPO synthesis and release as a function of PrvO2. Polycythemia modifies PrvO2 only in M rats after 2 wk of hypoxia. The early changes in PrvO2 reflect ventilatory acclimatization, acute cardiovascular responses to hypoxia, and perhaps some benefit from the hemoconcentration after diuresis in the first days of acclimatization to high altitude (Table 2) (18). Only the late increase in PrvO2 in M rats demonstrates the beneficial effect of polycythemia. In contrast, the PrvO2 remained low in the H strain. This was not due to a lack of O2-carrying capacity (Hct rose above 70%) or low renal blood flow (renal COD was equivalent in the H and M rats and exceeded the sea-level value by day 30 of the hypoxic exposure) but to a low PaO2. Thus renal hypoxic stimulation persists when arterial hypoxemia is below the threshold of the EPO response and, therefore, beyond the capacity of polycythemia to restore renal tissue oxygenation to suprathreshold levels. The accentuated hypoxemia of the H rats, which originates in abnormal pulmonary vascular responses to hypoxia and associated gas exchange abnormalities, creates a situation in which polycythemia develops but has no significant effect on the level of EPO stimulation. Consequently, the signs of CMS develop: profound arterial hypoxemia, persistent production of EPO, and extraordinary polycythemia.
The EPO-PrvO2 response curves (Fig. 5), whether in terms of mRNA, renal EPO, or plasma EPO, have a shape resembling the ventilatory response to hypoxia and the pattern of carotid body discharge in response to hypoxia (24): there is little response until a threshold is reached, and below the threshold the response, ventilation or sinus nerve discharge or EPO production, rises steeply. The mechanism whereby declining O2 levels are sensed and transformed into ventilatory and EPO responses is unknown, but it is conceivable that the renal and carotid sensors share a common mechanism. For example, both may rely on heme proteins (1, 17, 26). In summary, the present study examined the genetic regulatory mechanisms as well as the physiological significance of the polycythemic response to environmental hypoxia in two rat strains with distinctly different susceptibility to CMS. The results suggest that the polycythemia of CMS derives from pulmonary abnormalities of gas exchange, vascular remodeling, and more severe arterial hypoxemia in the H rats rather than different patterns of EPO synthesis and release to a similar stimulus. EPO levels were appropriate for the levels of renal tissue hypoxia, but PaO2 and PrvO2 were below the EPO response threshold in the H rats, and no polycythemic response can restore renal tissue oxygenation in that setting.| |
ACKNOWLEDGEMENTS |
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This study was supported by National Heart, Lung, and Blood Institute Grant HL-21159. J. C. Leiter is a recipient of a Clinical Investigator Award from the American Lung Association.
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FOOTNOTES |
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Address for reprint requests: L. C. Ou, Dept. of Physiology, Dartmouth Medical School, Borwell Bldg., 1 Medical Center Dr., Lebanon, NH 03756-0001.
Received 14 May 1997; accepted in final form 3 December 1997.
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