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Quantitation of transmembrane O 2 flux via RhAG in a neutral‐buoyancy assay
Author(s) -
Moss Fraser,
Zeise Brian,
Boron Walter
Publication year - 2021
Publication title -
the faseb journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.709
H-Index - 277
eISSN - 1530-6860
pISSN - 0892-6638
DOI - 10.1096/fasebj.2021.35.s1.01698
Subject(s) - chemistry , membrane , buoyancy , biophysics , transmembrane protein , chromatography , aquaporin , biochemistry , biology , thermodynamics , physics , receptor
The central dogma of transmembrane gas flux had been that all gases cross all membranes by dissolving in the lipid phase of the membrane. Contradicting this simple view are three discoveries: (1) CO 2 ‐impermeable membranes; (2) CO 2 ‐permeable membrane proteins or “gas‐channels”, namely, certain aquaporins (AQPs) and rhesus (Rh) proteins; and (3) a reduction in CO 2 ‐permeability when incorporating the CO 2 ‐impermeable Nicotiana tabacum AQP NtPIP2;1, into artificial membranes. The characterization of the CO 2 and NH 3 permeabilities of AQPs 0‐9 and several rhesus (Rh) proteins shows that they can exhibit gas selectivity. Our laboratory has found that, during O 2 ‐offloading, ~55% of O 2 exits mouse red blood cells (RBCs) via AQP1 and the Rh complex (i.e., RhAG + mRh). To characterize the mechanism by which RhAG and other proteins conduct O 2 , and to screen for novel O 2 channels in a heterologous expression system, we have modified of our Neutral Buoyancy Assay (NBA), originally developed to assess transmembrane N 2 fluxes. We inject a precise volume of N 2 gas (number of gas molecules = n Gas ) into a Xenopus oocyte, which we place into a saline‐containing pressure‐resistant tube. We then impose sufficient pressure in the air phase above the air‐water interface to collapse the injected bubble enough to maintain the oocyte at a depth of 5 cm. As N 2 gas dissolves in the cytosol and ultimately diffuses into the extracellular fluid (ECF), the bubble shrinks, cell density increases, and the oocyte sinks. A camera/computer combination detects the sinking and decreases air‐phase pressure enough to maintain neutral buoyancy at 5 cm depth. Calibration exercises allow us to compute the time course of Δn Gas , and thus gas efflux. Here we modify the NBA to quantify gas influx. When we raise [N 2 ] in the ECF from [N 2 ] o = 0.56 mM (room air at 1×ATA) to [N 2 ] o = 2.06 mM (pre‐equilibrating saline with 93% N 2 /7% O 2 at 3×ATA) at constant [O 2 ] o = 0.26 mM, N 2 enters the cell during the NBA and n Gas rises. If we now hold [N 2 ] o constant at 2.06 mM but selectively increase [O 2 ] o from 0.26 mM to 0.91 mM (pre‐equilibrating saline with 78.96% N 2 /21% O 2 /0.04% CO 2 at 3.5×ATA), n Gas rises faster. Compared to control oocytes (injected with H 2 O rather than cRNA encoding RhAG), RhAG‐expressing oocytes exhibit no significant difference in Δn Gas over 1000 s when [N 2 ] o = 2.06 mM/[O 2 ] o = 0.26 mM. Thus, RhAG appears not to be an N 2 channel. However, when [N 2 ] o = 2.06 mM/[O 2 ] o = 0.91 mM, Δn Gas over 1000 s is significantly greater in RhAG vs control oocytes. Thus, RhAG is selective for O 2 over N 2 . When we repeat the low‐to‐high [O 2 ] o experiment with oocytes expressing NtPIP1;3 (reported to facilitate O 2 flux in a spectrophotometric assay when expressed in yeast protoplasts), we also observe substantial increases in Δn Gas over 1000 s vs control oocytes. These data are consistent with our previous findings in RBCs that the Rh complex constitutes a major pathway for O 2 flux across the plasma membrane, and also supports the NtPIP1;3 report from another laboratory. Although we specifically developed the NBA for N 2 fluxes, here we demonstrate the versatility of the assay for measuring transmembrane fluxes of other gases.

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