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RED CELLS
From the Physiological Laboratory, University of
Cambridge, United Kingdom; and Department of Medicine, Albert Einstein
College of Medicine, Bronx, NY.
Interaction of hemoglobin S polymers with the red blood cell (RBC)
membrane induces a reversible increase in permeability ("Psickle") to (at least) Na+,
K+, Ca2+, and Mg2+. Resulting
changes in [Ca2+] and [H+] in susceptible
cells activate 2 transporters involved in sickle cell dehydration, the
Ca2+-sensitive K+ ("Gardos") channel
(KCa) and the acid- and volume-sensitive K:Cl cotransport.
We investigated the distribution of Psickle expression among deoxygenated sickle cell anemia (SS) RBCs using new experimental designs in which the RBC Ca2+ pumps were partially
inhibited by vanadate, and the cells' dehydration rates were detected
as progressive changes in the profiles of osmotic fragility curves and
correlated with flow cytometric measurements. The results exposed
marked variations in (sickling plus Ca2+)-induced
dehydration rates within populations of deoxygenated SS cells, with
complex distributions, reflecting a broad heterogeneity of their
Psickle values. Psickle-mediated dehydration
was inhibited by clotrimazole, verifying the role of KCa,
and also by elevated [Ca2+]o, above 2 mM.
Very high Psickle values occurred with some SS discocytes,
which had a wide initial density (osmotic resistance) distribution.
Together with its previously shown stochastic nature, the irregular
distribution of Psickle documented here in discocytes is
consistent with a mechanism involving low-probability, reversible interactions between sickle polymers and membrane or cytoskeletal components, affecting only a fraction of the RBCs during each deoxygenation event and a small number of activated pathways per RBC. A
higher participation of SS reticulocytes in
Psickle-triggered dehydration suggests that they form these
pathways more efficiently than discocytes despite their lower cell
hemoglobin concentrations.
(Blood. 2002;99:2578-2585) The permeability pathway generated by the
interaction of deoxygenated hemoglobin S polymers with the red blood
cell (RBC) membrane (Psickle) plays a major role in the
mechanism of dehydration of sickle cell (SS) anemia RBCs. The
functional properties of this pathway, however, have yet to be
determined. Psickle mediates changes in cell
Ca2+ and H+ concentrations, which activate the
2 main transporters involved in sickle cell dehydration, the
Ca2+-sensitive K+ ("Gardos") channel
(KCa), expressed in RBCs of all ages,1,2 and
an acid- and volume-sensitive K:Cl cotransport, expressed predominantly
in young RBC and reticulocytes,3-8 with both leading to a
net loss of KCl and water. In this sequence, Psickle
remains the most obscure link Early work established that Psickle is a poorly
selective permeability pathway for Na+, K+,
Ca2+, and Mg2+.9-15 In
reticulocytes, Psickle exhibits a peculiar heparin
sensitivity16 and is partially inhibited by
stilbenes.17 The Ca2+ and Mg2+
permeabilities through this pathway were shown to be similar in
different density fractions of sickle cells (light, normal discocytes,
and dense),15,16 suggesting that Psickle has
little correlation with those variations in sickling morphology
associated with different hydration states of the SS RBCs. A recent
study18 revealed 2 fundamental properties of
Psickle in SS discocytes: (1) Psickle remains
open or active for the duration of each deoxygenation (deoxy) episode
and therefore is the functional expression of a molecular structure
that forms on deoxygenation and remains stable within each deoxy
episode; and (2) consecutive deoxy pulses generate similar-sized
fractions of RBCs with similar Psickle values, even after
removal of high-Psickle cells from the previous pulse; this
indicated that Psickle is stochastic in nature, with a
conserved probability distribution in successive deoxy pulses. The
actual distribution of Psickle values among deoxygenated SS cell fractions, however, remained to be characterized.
To investigate the range of expression of Psickle, we
developed a new approach in which cell-to-cell differences in
Psickle intensity were converted into differences in
dehydration rates; these, in turn, were observed by following the
progressive shape changes of the RBC osmotic fragility curves. This
"profile migration method," which we described in detail
previously,19-21 is outlined below. In addition, a
smaller, ancillary series of experiments was performed in which SS RBC
dehydration was assessed by flow cytometric methods, as detailed below.
Together, these measurements exposed marked variations in (sickling
plus Ca2+)-induced dehydration rates within populations of
deoxygenated sickle cells that reflected a broad heterogeneity of their
Psickle values.
All chemicals were analytical reagent quality.
Ethyleneglycotetraacetic acid, HEPES, glucose, inosine,
Na-orthovanadate, and dimethyl sulfoxide (DMSO) were obtained from
Sigma Chemical (St Louis, MO). A23187 was obtained from
Calbiochem-Novabiochem (La Jolla, CA).
Composition of solutions
Preparation of RBCs
Experimental design To translate cell differences in Psickle into differences in cell dehydration rate, it was necessary to establish experimental conditions in which deoxygenation-induced sickle cell dehydration would be determined by Psickle. Because Psickle increases the Ca2+ permeability of the RBCs, their pump-leak [Ca2+]i level will increase when they are deoxygenated in the presence of external Ca2+. Elevated [Ca2+]i activates KCa channels and, in low-K+ media, mediates net KCl loss and RBC dehydration. This dehydration is usually rate-limited by the relatively low electrodiffusional Cl permeability
of the RBC membrane,20,22,23 but the limitation can be
bypassed by replacing a small fraction of the extracellular Cl by the more permeable anion
SCN .24 Previous studies22
established that at comparable [Ca2+]i
levels, all the RBCs would dehydrate via KCa channels at
comparable rates (except for the small fraction of high
Na+, low K+, "valinomycin-resistant"
[val-res] cells25). Therefore, in these conditions, the
dehydration rate in each RBC will be determined by the K+
permeability through its KCa channels, which will vary
directly with the value of Psickle. Thus, differences in
cell dehydration with time will reflect cell-to-cell differences in
Psickle.
Profile migration As the RBCs dehydrate, they become increasingly resistant to osmotic lysis, so that their osmotic hemolysis curves migrate toward progressively lower tonicities. Differences in the dehydration rate among the cells are reflected in the changing profile of the hemolysis curves in successive samples reflecting the distribution of Psickle values in the cell population. To avoid time-dependent artifacts and spontaneous hemolysis during profile migration measurements, we sought conditions for rapid RBC dehydration, preferably within 30 to 60 minutes. This was achieved by inhibiting the powerful Ca2+ pump by more than 99.5% using a high concentration of vanadate,26,27 thus magnifying the increase in [Ca2+]i and consequent level of KCa channel activation at each Psickle. The aim was to induce minimal cell dehydration in control oxy conditions (when passive Ca2+ influx proceeds through the intrinsically low permeability of the RBC membrane) but to expose easily detectable dehydration when Psickle was activated by deoxygenation. In such conditions, variations in RBC dehydration rates could be attributed to and correlated with the Psickle distribution among the cells.Based on the experimental design outlined above, the following protocol
was used to measure the population distribution of dehydration rates
with the profile migration method.19-21 Pairs of
correspondingly labeled 96-well plates were used, with one of each pair
having U-shaped well bottoms and the other being flat-bottomed for
optical density measurements. Each row of the U-bottomed plate
contained 250 µL each of 12 solutions with different osmolarities,
ranging from 1.0 to 0.01 relative tonicity (RT) units (lysis media).
These were prepared by mixing appropriate volumes of 2 solutions, one
containing 149 mM NaCl and 2 mM Na-HEPES (pH 7.5 at 20°C) and the
other only 2 mM Na-HEPES (pH 7.5 at 20°C). For each set of
measurements, 4 mL of a 2.5% (Hct) RBC suspension in solution C was
equilibrated for the designated time periods at 37° with
water-saturated O2 or N2 in a tonometer (model
237, Instrumentation Laboratory, Lexington, MA). NaSCN was added to the
suspension from a 1.5 M stock solution to a final concentration of 5 mM. Where indicated in "Results," the following were added: ionophore A23187, from a 2 mM stock solution in ethanol:DMSO (4:1), final concentration of 100 µM RBC; valinomycin, from 12 mM stock in
DMSO, final concentration 10 µM; orthovanadate, from 100 mM stock,
final concentration 1.0 mM; and calcium (from 1 M CaCl2 stock), between 0.5 and 5.0 mM, corrected for albumin binding. Fifteen
seconds before each sampling time, 0.6 mL cell suspension was
transferred from the tonometer to a plastic incubation tray (Accutran
disposable incubation tray, Schleicher & Schuell) at room temperature.
At the exact sampling time, a 12-channel pipette (Finnpipette, Thermo
Labsystems, Helsinki, Finland) was used to deliver 10 µL
samples of the suspension in the incubation tray to the row of 12 wells
on a U-bottomed 96-microwell plate containing the 250 µL of the lysis
media, and they were rapidly mixed by repeated vigorous squirts with
the multichannel dispenser. Each timed sample generated a full
hemolysis curve. To estimate the fraction of hemolysis in each well,
the plate was centrifuged for 5 minutes at 1100 rpm, 150 µL samples
of the supernatants were transferred with a 12-channel dispenser to the
correspondingly labeled row on the flat-bottomed plate, and
concentrations of hemoglobin were measured on a plate reader (Multiskan
Bichromatic type 348, Thermo Labsystems) by its absorption at 414 nm, the Sorette band, where its extinction coefficient is
optimal.20 Although the method proposed here was not used
previously with SS RBCs, it had been thoroughly tested, as noted above,
and shown to be reliable in various applications on normal human RBCs.
The hemolysis curves are shown in the standard format, plotting the percent hemolysis as a function of RT. Conserved profiles, ie, constant
shape of the migrating hemolysis curves, indicate uniformity of
dehydration rates, whereas changing profiles reflect heterogeneities of
dehydration rates among the cells. The population distribution of
hydration states may be appreciated more clearly from histograms representing the derivatives of the hemolysis curves. The histograms in
Figure 5 report the increment in hemolysis ( Flow cytometry experiments An aliquot of SS discocytes with density 1.091 < 1.106 was prepared and washed as described above and suspended at 1% Hct in 1.5 mL of solution D containing, in addition, CaCl2
to give a final concentration of between 1.0 and 2.0 mM
[Ca2+]o (corrected for albumin binding), as
indicated in "Results," and equilibrated in the tonometer with
water-saturated air for 10 minutes at 37°. After baseline sampling,
sodium vanadate was added from a stock solution to give a final
concentration of between 0.1 and 1.0 mM, as indicated. Further
equilibration was either with continuous air (oxy control) or with
cycles of 10 minutes of N2 gas followed by 5 minutes of air
(deoxy-oxy cycling), for up to 45 minutes.
As with the profile migration studies, preliminary experiments were done to determine the optimal conditions that would inhibit the RBC Ca2+ pumps enough to permit relatively rapid, easily detectable SS cell dehydration when Psickle was activated by deoxygenation but would result in minimal dehydration during control oxy conditions. With the very dilute RBC suspensions used in these studies, this balance of Ca2+ pump inhibition was generally observed with vanadate concentrations of about 0.1 mM and [Ca2+]o of about 1.0 mM but varied somewhat between samples from the same or different donors and had to be empirically determined for each experiment, as noted in "Results." RBCs from whole blood or density fractions were analyzed with a flow cytometry-based hematology analyzer, the Bayer-Technicon H*3 RTX (Bayer Diagnostics, Tarrytown, NY), as described previously.28 Briefly, the RBCs are isovolumetrically sphered and the volume and hemoglobin concentration (HC) of each cell is determined by analysis of low- and high- angle laser light scattering. The H*3 RTX instruments used in the present experiments differed from the commercial model of the H*3 (and later generations of this instrument) in having only a manual rather than automatic sampling mode. Using the manual mode, we could select the RBC conditions before H*3 sampling. As observed before in preliminary experiments,28 after the experimental manipulations used, the standard H*3 procedure of incubating for 15 minutes in the dye (oxazine) buffer solution, with or without the sphering detergent (TDAPS), resulted in RBC swelling, with broadening of HC distributions toward lower values. This swelling was avoided if the RBCs were read by the H*3 immediately after sampling and mixing with the sphering agent, without incubation with the dye. Therefore, all RBC samples were sampled 2 ways in the H*3: immediately after sphering (without RNA staining) and, then, to detect reticulocytes, after 15 minutes' incubation with the dye in the appropriate buffer for the experiment, immediately after adding the sphering agent.
Comparison of the dehydration response of SS discocytes and AA RBCs to deoxygenation and Ca2+ pump inhibition Preliminary experiments confirmed earlier work showing that, in the absence of Ca2+ pump inhibition, sustained short-term deoxygenation produced minimal dehydration of SS RBCs.16 Figure 1 shows the effects of vanadate on hemolysis curve migration in oxy and deoxy conditions in the presence of 2 mM [Ca2+]o. With AA RBCs there were negligible changes during the 1-hour incubation, oxy or deoxy (Figure 1A,B). With oxy SS discocytes (Figure 1C), addition of vanadate caused minor displacement of the hemolysis curves, apparently representing further dehydration of the relatively denser discocytes within this fraction whose osmotic resistance was highest initially. However, in deoxy conditions, addition of vanadate was associated with progressive migration of the hemolysis curves, ultimately affecting more than 95% of the RBCs (Figure 1D). The altered shape profile of the migrating curves, as compared with the control curve, indicated that there was substantial heterogeneity of dehydration rates.
Vanadate also inhibits the Na pump, which could result in RBC swelling and cause the hemolysis curve profiles to migrate to lower RTs. As seen in Figure 1, with both SS discocytes and AA RBCs this potential swelling effect was minimal within the time required to expose deoxy-induced dehydration. KCa channel mediation of deoxy-induced dehydration of SS RBC: effects of varying external Ca2+ concentrations and of clotrimazole The effects of varying external Ca2+ concentrations ([Ca2+]o) on vanadate-induced dehydration of deoxy SS discocytes are shown in Figure 2. In the absence of Ca2+ (Figure 2A) there was no dehydration and no difference between oxy and deoxy hemolysis curves. [Ca2+]o levels of 0.5 and 1 mM produced moderate dehydration of the oxy RBCs and large oxy-deoxy differential dehydration at both 10 and 25 minutes (Figure 2B,C). However, when [Ca2+]o was raised to between 2 and 5 mM, there was a progressive decrease in the extent of dehydration of the deoxy RBCs after 25 minutes' incubation, with a corresponding reduction in the oxy-deoxy differential (Figure 2D-F). Together, these results show that the dehydration of SS RBCs elicited by deoxygenation and vanadate is strictly Ca2+-dependent and that external Ca2+ has 2 opposing effects on the deoxy SS RBC: At low concentrations it elicits maximal dehydration, but at higher concentrations the rate of dehydration is reduced. Addition of a specific KCa channel inhibitor, clotrimazole,29 prevented vanadate-induced dehydration of deoxy SS discocytes (Figure 3), confirming that the dehydration following deoxygenation-induced Psickle formation was mediated by KCa channel activation.
Effects of Ca2+/K+ ionophores The observed differences in dehydration rates among SS discocytes could result either from (1) variations in their intracellular K+ concentrations, which would affect their driving gradients for dehydration, from (2) cell-to-cell differences in the number of KCa channels or (3) the extent of their activation. To help distinguish between these possible mechanisms, we compared the pattern of dehydration of a single batch of SS discocytes exposed to valinomycin, a K+-selective ionophore that produces uniform K+ permeabilization (Figure 4A), with that induced by deoxygenation plus vanadate (Figure 4D). Valinomycin caused maximal and uniform cell dehydration in more than 85% of the SS discocytes within 20 minutes, indicating that most of the SS RBCs in this density fraction retained normal driving K+ gradients for dehydration.
Addition of appropriate concentrations of the Ca2+ ionophore A23187 in the presence of external Ca2+ produces uniform Ca2+ loads in all the RBCs and induces maximal activation of their KCa channels.24 The dehydration pattern of the SS discocytes induced by A23187 plus Ca2+ (Figure 4B) was similar to that elicited by valinomycin, indicating that fully activated KCa channels produce rapid and uniform dehydration in more than 85% of these SS RBCs, as seen previously with AA RBCs.30 The results with both the K+ and Ca2+ ionophores indicate that the grossly heterogeneous dehydration rates exhibited by SS discocytes deoxygenated in the presence of vanadate (Figure 4D) must reflect differences in their individual RBC [Ca2+]i levels, which in turn must result from variations in either their Psickle or their residual Ca2+ pumping. Psickle distributions Figure 5D-I illustrates the dynamic distribution of dehydration states of SS discocytes deoxygenated in the presence of Ca2+, with their Ca2+ pumps inhibited by vanadate. Figure 5A,B reports the initial and final distributions in the oxy controls. Over the 45 minutes of deoxygenation, there is a progressive migration of RBCs into the fraction with maximal osmotic resistance. During the first 10 minutes of deoxy incubation, about 15% of the RBCs have dehydrated rapidly, newly appearing in the 0 to 15 RT columns (Figure 5F); these rapidly dehydrating RBCs appear to migrate from a wide range of initial RT columns (RT lytic ranges between 15-35 RT), excluding only the lightest RBCs (RT > 35). Over the next 45 minutes, portions of all but the lightest RBCs become progressively dehydrated, at apparently different rates, with some lagging behind or failing to dehydrate. About 8% to 10% of the lightest RBCs (RT lytic range 40 to 65) fail to dehydrate altogether (Figure 5I) unless K+-permeabilized with valinomycin (Figure 5C). Thus, dehydration rates appear to be distributed in a continuous gradation. To the extent that the heterogeneity of dehydration rates reflects the population variation in Psickle, the Psickle distribution follows a complex pattern with 2 major groups: a large group of intermediate to (relatively) high-density discocytes with a widely graded distribution of Psickle and an intermediate to very light group of RBCs in which Psickle is minimally or not activated and which is likely to contain most of the hemoglobin F cells present in this cell fraction.
Flow cytometric observations of the dehydration response of SS discocytes For comparison with the results using the profile migration method, density-fractionated light SS discocytes were deoxygenated in the presence of vanadate and external Ca2+ and the distribution of their HCs and volumes were followed with the Bayer-Technicon H*3 flow cytometry system.28 As shown in Figure 6, it was possible to achieve a balance between the extent of inhibition of the Ca2+ pump by vanadate and deoxygenation-induced Psickle that resulted in little or no detectable RBC dehydration in the oxygenated control condition but distinct dehydration, with a markedly heterogeneous distribution, among the deoxygenated SS discocytes. In the conditions of that particular experiment, about half of the SS discocytes failed to shrink, while the other cells showed a wide range of dehydration responses in the first 30 minutes of incubation, with only small further changes over time. These results are qualitatively consistent with those obtained using the profile migration method: They show a fraction of SS discocytes that did not dehydrate in these test conditions and show a broadly distributed dehydration response among those RBCs that did dehydrate. No quantitative consistency is expected between these 2 methods, because they both depend on the balance achieved in each experiment between Ca2+ pump inhibition by vanadate and the increased Ca2+ influx generated by Psickle, and the effects of that balance among the RBC population.
Whereas the Hct of the cell suspensions used for the profile migration experiments was about 10%, the flow cytometry experiments were carried out at an Hct of about 1%. Preliminary experiments indicated that, to achieve the balanced level of Ca2+ pump inhibition described above, the concentration of vanadate in the cell suspension had to be adjusted downward to preserve vanadate/cell ratios comparable to those in the 10% Hct suspensions. Therefore, in experiments with the same or different donors, it was found necessary to vary the concentration of vanadate empirically between 0.05 and 0.2 mM, but in each of 4 experiments, when that balance was achieved, the results were equivalent to those shown in Figure 6. Deoxygenation-induced dehydration in reticulocyte-rich SS cell fractions Using the same protocol as that applied to the SS discocyte fractions, we examined the effects of deoxygenation of light, reticulocyte-rich SS cell fractions ( 1.091) on the profile migration of hemolysis curves. As shown in the experiment of Figure 7 (representative of 3 similar
experiments), the hemolysis curves of these light SS cell fractions
extended over a much wider RT range than those of the SS discocytes.
Importantly, in this low-density, low-mean-cell HC RBC fraction,
initially high osmotic resistance is based not only on a high-density
dehydration state, as in the SS discocytes, but also on the increased
surface area/volume ratio of the reticulocytes. Because the
reticulocytes must gain relatively more water to reach their critical
hemolytic volume, they require lower RT values for hemolysis.
Upon K+ permeabilization with valinomycin (Figure 7A), more than 80% of the cells in this light, reticulocyte-rich fraction dehydrated rapidly and maximally, indicating that they retained normal K+ gradients for dehydration. However, about 18% of the light SS cell fraction used in this experiment and 30% and 22% in 2 similar experiments (not shown) showed no dehydration following exposure to valinomycin. These nondehydrating SS cells correspond to a recently discovered subpopulation of light, high-Na, low-K "valinomycin-resistant" RBCs that compose about 4% of the total SS cell population; their properties were described elsewhere25 and are not considered further here. In oxy conditions (Figure 7B), the net effect of vanadate was rapid swelling of a substantial fraction of cells, attributable to inhibition of the reticulocytes' Na pumps, which are more than 10-fold more active than those of mature RBCs.31 Swelling occurred in more than 80% of the cells but was much more prominent in about 35% of the cells that were most susceptible to osmotic lysis (other than val-res cells). Deoxygenation reversed the swelling in all the cells, countering the substantial differences in right-shift displacements. These shifts highlight patterns of Psickle heterogeneity unique to reticulocyte-rich cell fractions. However, the superposition of opposite effects with this method, together with the marked heterogeneity of osmotic resistance levels, limits further analysis of Psickle-induced dehydration responses in reticulocyte-rich SS cell fractions. The vanadate-induced right shift observed in the hemolysis curves of the reticulocyte-rich cell fractions was either absent (Figure 1C) or minimal (Figure 4C) in oxy discocytes. Therefore, the pump-leak Na/K traffic in discocytes must have been too small to generate the counterbalancing, swelling effect observed with the reticulocyte-rich fraction and could not contribute significantly to the heterogeneity of the discocytes' Psickle response.
The results of the present experiments show that the Psickle distribution generated within each deoxy episode is complex, often with sharp discontinuities between subpopulations (Figure 6), confirming earlier suggestions of unequal Psickle permeabilization of SS cell subpopulations during each deoxygenation episode.18 Among the SS discocytes, there appeared to be some RBCs with particularly high Psickle values; within this fraction, these RBCs were initially distributed over a broad range of densities (osmotic resistances), excluding only the lightest discocytes (Figure 5D-I). Interpretation of the present results in terms of uneven distribution of Psickle values among sickle discocytes is consistent with our earlier observation on the stochastic nature of Psickle.18 As shown in Figure 1D, in vanadate-free controls in Cl medium (medium C), no significant dehydration of deoxy sickle cells was detected within 45 minutes. Using a high vanadate concentration to inhibit the Ca2+ pump,27 it was possible to expose measurable patterns of Psickle-induced dehydration. The results demonstrate subpopulation differences in Ca2+-dependent, deoxy-induced dehydration rates, suggesting a wide distribution of Psickle values. The relative decrease in the dehydration rate of SS discocytes observed when [Ca2+]o was increased above 1 mM (Figure 2) is consistent with our earlier observations that external Ca2+ inhibited Psickle in SS reticulocytes, particularly the Na+ component. Further studies by Joiner et al32 demonstrated that in the lightest 15% to 25% of SS RBCs, Ca2+ and other divalent cations inhibited the Na+ component of Psickle more than the K+ component, resulting in a net K+ loss that occurred even in the absence of KCa channel activation. Taken together, these observations indicate that Psickle is inhibited by external divalent cations and that the inhibitory effect has a low affinity, increasing from 1 mM to 5 mM for external Ca2+ (Figure 2). The mechanism underlying these Ca2+ (divalent cation) effects on Psickle remains to be determined. The inhibitory effects of clotrimazole on Psickle-triggered dehydration of SS discocytes (Figure 3) confirm KCa mediation of the dehydration response. Valinomycin elicited uniform and maximal dehydration of more than 90% of discocytes and up to 80% of cells from the reticulocyte-rich fraction (Figures 4A and 7A), indicating that the slower and much more irregular dehydration pattern induced by Psickle could not be attributed to variations in K+ driving gradient among the cells. The known stochastic nature of Psickle,18 together with its heterogeneous distribution as documented here among the discocytes, are consistent with the view that the permeability pathway is generated by low-probability, direct or indirect interactions between hemoglobin S polymers and membrane or cytoskeletal components, affecting only a fraction of cells within each deoxy event, as if the number of activated pathways per cell was very small.
Submitted August 1, 2001; accepted November 20, 2001.
Supported by National Institutes of Health grants HL-28018 and HL-58512 and by the Wellcome Trust (United Kingdom).
The publication costs of this article were defrayed in part by page charge payment. Therefore, and solely to indicate this fact, this article is hereby marked "advertisement" in accordance with 18 U.S.C. section 1734.
Reprints: Robert M. Bookchin, Dept of Medicine, Albert Einstein College of Medicine, 1300 Morris Park Ave, Rm 913U, Bronx, NY 10461; e-mail: bookchin{at}aecom.yu.edu.
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© 2002 by The American Society of Hematology.
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