Significance of affinity and cooperativity in oxygen binding to hemoglobin of horse fetal and maternal blood

The physiological significance of the position and shape of the oxygen equilibrium curve (OEC) of horse hemoglobin (Hb) is considered from the viewpoint of oxygen (O2) transport efficiency and the effectiveness of the Bohr effect. In horse fetal and maternal bloods, their physiological O2 affinities are nearly optimized with respect to the effectiveness of the Bohr shift occurring at the O2 release site, when it is measured by the change in O2 saturation per unit change in P50. With relatively low cooperativity (n=2.69) of horse Hb under physiological conditions, the effectiveness of the Bohr shift for fetal blood at O2 uptake site and maternal blood at O2 release site is high. These facts imply that the position and the cooperativity of horse Hb OEC are optimized to receive maximal benefit from the double Bohr shift. Before exercise, the position of the OEC for adult mares is nearly optimized for the effectiveness of the Bohr shift occurring at the O2 release site, whereas, at maximal exercise, the position of the OEC tends to become advantageous for O2 transport efficiency.     

A truncated mutant of the extrinsic 23-kDa protein that absolutely requires the extrinsic 17-kDa protein for Ca2+ retention in photosystem II

One function of the extrinsic 23-kDa protein in photosystem II (OEC23) is to retain Ca(2+ )and Cl(-), two essential cofactors for photosynthetic oxygen evolution. A truncated mutant of OEC23 (OEC23 Delta19) revealed that 19 residues of the N-terminus of OEC23 were necessary for Ca(2+ )retention but not for its proper interaction with OEC17, the extrinsic 17-kDa protein in photosystem II. The lost ability of OEC23 Delta19 to reconstitute the oxygen-evolving activity was partially restored by OEC17 binding, suggesting the involvement of OEC17 in Ca(2+ )retention in photosystem II.     

Effects of hyperchloremia on blood oxygen binding in healthy calves

Three different levels of hyperchloremia wereinduced in healthy Friesian calves to study the effects of chloride onblood oxygen transport. By infusion, the calves received either 5 ml/kg of 0.9% NaCl (low-level hyperchloremia; groupA), 5 ml/kg of 7.5% NaCl (moderate hyperchloremia;group B), or 7.5 ml/kg of 7.5% NaCl(high-level hyperchloremia; groupC). Blood was sampled from the jugular vein and thebrachial artery. Chloride concentration, hemoglobin content, arterialand venous pH, PCO₂, and PO₂ were determined. At each timepoint (0, 15, 30, 60, and 120 min), the whole blood oxygen equilibriumcurve (OEC) was measured under standard conditions. Ingroups B andC, hyperchloremia was accompanied by asustained rightward shift of the OEC, as indicated by the significantincrease in the standard PO₂ at 50%hemoglobin saturation. Infusion of hypertonic saline also inducedrelative acidosis. The arterial and venous OEC were calculated, withbody temperature, pH, and PCO₂ valuesin arterial and venous blood taken into account. The degree of blooddesaturation between the arterial and the venous compartments[O₂ exchange fraction(OEF%)] and the amount of oxygen released at tissue level by 100 ml of bovine blood (OEF vol%) were calculated from the arterial andvenous OEC combined with the PO₂ andhemoglobin concentration. The chloride-induced rightward shift of theOEC was reinforced by the relative acidosis, but the alteredPO₂ values combined with the lowerhemoglobin concentration explained the absence of any significantdifference in OEF (% and vol%). We conclude that infusion ofhypertonic saline induces hyperchloremia and acidemia, which canexplain the OEC rightward shift observed in arterial and peripheralvenous blood.

     

Study on the Binding State of Calcium in Photosystem ⅡOxygen-Evolution Complex

Washing spinach PSII oxygen-evolution complex (OEC) with 2 mmol/L EGTA or extraction medium caused a 28.4% and 25.0% loss of oxygen evolution activities respectively, but the loss of polypeptide components of OEC did not take place, whereas washing with 1 mol/L NaCI caused both a 90.0% loss of oxygen evolution activity and loss of 17, 23kD polypeptides. Adding 5–10 mmol/L CaC12 could restore oxygen evolution activities of OEC by various washing to a great extent, but had no effect on control OEC, whereas adding 5–10 mmol/L EGTA had no effect on the OEC by various' washing, but caused the loss of oxygen evolution mixtures, which could induce the release of of 17, 23kD polypeptides from OEC, caused 54.3% loss of oxygen evolution activity, under this circumstance, adding 2 mmol/L of EGTA could only maintain a weak oxygen evolution activity of OEC, but adding 10 mmol/L of CaCl2 could restore oxygen evolution activity of OEC to the control level. These findings' suggest a two way loose binding of Ga2+ to PSⅡ OEC in one way Ca2+ is loose bound to the surface of PSⅡOEC and in other, the Ca2+-binding site is wrapped by 17, 23kD polypeptides. Both of them have effect on oxygen evolution activity of PSⅡ OEC. By way, Mn2+ can antagonize the restoration of oxygen evolution activity by Ca2+ to the NaCl-washing PSⅡ OEC.     

Carbonic anhydrase activity of the photosystem II OEC33 protein from pea

The purpose of this study was to identify the location of one of the two sources of carbonic anhydrase (CA) activity associated with the PSII complex in chloroplast membranes. We tested the hypothesis that the extrinsic 33 kDa protein, OEC33, associated with the oxygen-evolving complex (OEC), is one source of CA activity. We found that precursor OEC33 expressed in Escherichia coli exhibits CA activity, but the expressed precursors of OEC24 or OEC17 do not. The CA activity of OEC33 remained after treatment at 90 degrees C for 15 min. Additional biochemical evidence supports the hypothesis. Only those wash treatments that remove the OEC33 from PSII also remove CA activity. Both immunoblot and CA activity show that the CA tracks the OEC33, in parallel, when PSII undergoes washing at different CaCl2 concentrations. The OEC33 protein purified by HiTrap Q anion exchange chromatography has CA activity that is inhibited by an antibody against OEC33. PSII membranes washed with 1 M CaCl2 to remove OEC33 can be reconstituted either with extracted, purified, OEC33 or with the E. coli-expressed precursor OEC33. Reconstitution partially restores both oxygen evolution and CA activity. For maximal CA activity, OEC33 requires manganese as a cofactor.     

X-ray spectroscopy-based structure of the Mn cluster and mechanism of photosynthetic oxygen evolution

The mechanism by which the Mn-containing oxygen evolving complex (OEC) produces oxygen from water has been of great interest for over 40 years. This review focuses on how X-ray spectroscopy has provided important information about the structure of this Mn complex and its intermediates, or S-states, in the water oxidation cycle. X-ray absorption near-edge structure spectroscopy and high-resolution Mn Kbeta X-ray emission spectroscopy experiments have identified the oxidation states of the Mn in the OEC in each of the intermediate S-states, while extended X-ray absorption fine structure experiments have shown that 2.7 A Mn-Mn di-mu-oxo and 3.3 A Mn-Mn mono-mu-oxo motifs are present in the OEC. X-ray spectroscopy has also been used to probe the two essential cofactors in the OEC, Ca2+ and Cl-, and has shown that Ca2+ is an integral component of the OEC and is proximal to Mn. In addition, dichroism studies on oriented PS II membranes have provided angular information about the Mn-Mn and Mn-Ca vectors. Based on these X-ray spectroscopy data, refined models for the structure of the OEC and a mechanism for oxygen evolution by the OEC are presented.     

Importance of the N-terminal sequence of the extrinsic 23 kDa polypeptide in Photosystem II in ion retention in oxygen evolution

The function of the extrinsic 23 kDa polypeptide (OEC23) in Photosystem II (PS II) is to retain Ca(2+) and Cl(-) during the S-state turnover of the Mn cluster in photosynthetic oxygen evolution. Recombinant OEC23s from several plant species were produced in Escherichia coli to characterize the molecular mechanism of the OEC23 function then used in reconstitution experiments. One tobacco isoform, OEC23 (2AF), had much less oxygen-evolving activity than the spinach and cucumber OEC23s when PS II activities were reconstituted in salt-washed spinach PS II particles. The fact that the OEC23s had similar binding affinities for PS II particles suggests different ion-retention capacities for the individual OEC23s: The chimeric OEC23s produced between spinach and 2AF and those produced between cucumber and 2AF show that 58 N-terminal amino acid residues are important for PS II activity. Further dissection of the sequence and site-directed mutagenesis indicated the importance of 20 N-terminal amino acid residues for activity, in particular the asparagine at the 15th position. In spinach the N15D mutation decreased PS II activity, whereas in 2AF the D15N mutation increased it. This shows the importance of the N-terminal sequence of OEC23 in ion retention during the water-splitting process.     

The oxygen-evolving complex of chloroplast membranes

The oxygen-evolving complex (OEC) of plants is the main energy-transforming structure of chloroplast membranes, in which light energy is used for photosynthetic oxidation of intracellular water and oxygen formation. The conducted research has resulted in isolation of functionally active OEC of higher plants and elucidation of its molecular composition, photochemical properties and structural organization. The OEC has been revealed to represent the dimer of the pigment-lipoprotein complexes of photosystem 2 (PLPC PS-2) associated in a chloroplast membrane according to the mirror symmetry rule into an integrate structure based on hydrophobic bonds. The model has been developed for the structure of the dimeric complex of PS-2 that has the function of oxygen formation. This model was confirmed by the X-ray analysis of crystals of the dimeric complex of PS-2. The concept about the fact that the “hydrophobic boiler” determining the formation of the water-oxidizing center of the OEC is formed in the area of association of the reaction centers of monomeric PLPCs PS-2 was advanced based on the regularities of change in the functional activity of the OEC under the action of stress-factors. The new scheme has been advanced for the two-anode organization of the water-oxidizing center as the main condition for realizing the process of molecular oxygen formation. The mechanism of the process of photosynthetic water oxidation and molecular oxygen formation has been developed based on the experimental data about the structural organization of the OEC and its water-oxidizing center. The quantum-chemical modeling of the process showed that its course corresponds to the mechanism suggested.     

Light-induced FTIR difference spectroscopy as a powerful tool toward understanding the molecular mechanism of photosynthetic oxygen evolution

The molecular mechanism of photosynthetic oxygen evolution remains a mystery in photosynthesis research. Although recent X-ray crystallographic studies of the photosystem II core complex at 3.0-3.5 A resolutions have revealed the structure of the oxygen-evolving center (OEC), with approximate positions of the Mn and Ca ions and the amino acid ligands, elucidation of its detailed structure and the reactions during the S-state cycle awaits further spectroscopic investigations. Light-induced Fourier transform infrared (FTIR) difference spectroscopy was first applied to the OEC in 1992 as detection of its structural changes upon the S(1)-->S(2) transition, and spectra during the S-state cycle induced by consecutive flashes were reported in 2001. These FTIR spectra provide extensive structural information on the amino acid side groups, polypeptide chains, metal core, and water molecules, which constitute the OEC and are involved in its reaction. FTIR spectroscopy is thus becoming a powerful tool in investigating the reaction mechanism of photosynthetic oxygen evolution. In this mini-review, the measurement method of light-induced FTIR spectra of OEC is introduced and the results obtained thus far using this technique are summarized.     

IMPACT OF BLEACHING STRESS ON THE FUNCTION OF THE OXYGEN EVOLVING COMPLEX OF ZOOXANTHELLAE FROM SCLERACTINIAN CORALS1

Global climate change is leading to the rise of ocean temperatures and is triggering mass coral bleaching events on reefs around the world. The expulsion of the symbiotic dinoflagellate algae is believed to occur as a result of damage to the photosynthetic apparatus of these symbionts, although the specific site of initial impact is yet to be conclusively resolved. Here, the sensitivity of the oxygen evolving complex (OEC) to bleaching stress was studied as well as its natural variation between seasons. The artificial electron donor, diphenyl carbazide (DPC), was added to cultured, freshly isolated and expelled (bleaching treatments only) zooxanthellae suspensions. Chl a fluorescence and oxygen production measurements showed that upon addition of DPC, no restoration of diminished photochemical efficiency occurred under control or bleaching conditions. This result was consistent between 12 h and 5 d bleaching treatments on Pocilloporadamicornis, indicating that the OEC is not the primary site of damage, and that zooxanthellae expulsion from the host is a nonselective process with respect to the functioning of the OEC. Further experiments measuring fast induction curves (FICs) revealed that in both summer and winter, the temperature when OEC function was lost occurred between 7°C and 14°C above the sea surface temperature. FIC and oxygen production measurements of P. damicornis during exposure to bleaching stress demonstrated that the thermotolerance of the OEC increased above the temperature of the bleaching treatment over a 4 h period. This finding indicates that the OEC has the capacity to acclimate between seasons and remains functional at temperatures well above bleaching thresholds.     

An expanded two-state allosteric model for interactions of human hemoglobin A with nonsaturating concentrations of 2,3-diphosphoglycerate

Oxygen binding curves (OEC) for red cell suspensions have a biphasic shape and reduced n50 values when the concentration of 2,3-diphosphoglycerate (DPG) is lowered by aging or experimental procedures. The mechanism for the abnormal shape of the OEC has been related to variations in the activity of free DPG. DPG binds to tetrameric Hb at a single site, and in red cells its normal concentration is equivalent to that of tetrameric Hb. This equivalence renders the oxygen affinity of Hb and the shape of the OEC very sensitive to small changes in the activity of DPG. The OEC for stripped Hb solutions in the presence of nonsaturating concentrations of DPG also exhibit a biphasic shape but with much larger changes in the n values than observed for red cells. Upon addition of chloride, a known competitor of DPG binding to Hb, the shape of the OEC becomes similar to that of red cell suspensions with the same DPG/Hb ratio. Studies on Hb solutions in the presence of varying concentrations of DPG, but without chloride, have revealed that the cofactor shifts the entire OEC to the right, including both its upper and lower asymptotes. This finding indicates that DPG lowers the intrinsic oxygen affinity for both the T and R states. Theoretical considerations leading to a successful modeling of OEC obtained under varying conditions of DPG and chloride require an expanded two-state allosteric model in which allowance is made for DPG-dependent variations in the dissociation constants of oxygen for both the T and R conformations.     

Effects of lanthanide substitution at Ca2+-site on the properties of the oxygen evolving center of photosystem II

Functional calcium present in a photosynthetic oxygen evolving center (OEC) was replaced by lanthanides. To this end, sample membranes depleted of Ca2+ as well as 16 and 24 kDa extrinsic proteins were prepared and the effects of lanthanides substitution on OEC were studied. The lanthanides inhibited Ca2+-dependent restoration of oxygen evolution but the presence of Ca2+ during the treatment protected OEC from this inhibition, which occurred within 1 min at 20 degrees C but required much longer time at 0 degrees C. Kinetic analysis suggests that lanthanides function as a mixed-type competitor for Ca2+. Lanthanides with ionic radii smaller than Ca2+ show higher affinity for the Ca2+ site than those with larger radii. A lanthanide-substituted OEC displayed a thermoluminescence (TL) band arising from S2Q(A)- charge recombination, indicating that the Mn cluster is oxidized to the S2 state. However, the peak temperature of the TL band varied depending on lanthanide species. The results indicate that the oxidation potential of the Mn cluster is modified in various ways in a substituted OEC. Furthermore, the threshold temperature for the S1 to S2 transition in the lanthanide-substituted OEC was markedly upshifted to the temperature coincident with that found in Ca2+-depleted but 24 kDa protein preserved OEC. Changes in the OEC induced by the binding of lanthanides to the Ca2+-site are discussed based on these results.     

Molecular dynamics simulations reveal highly permeable oxygen exit channels shared with water uptake channels in photosystem II

Photosystem II (PSII) catalyzes the oxidation of water in the conversion of light energy into chemical energy in photosynthesis. Water delivery and oxygen removal from the oxygen evolving complex (OEC), buried deep within PSII, are critical requirements to facilitate the reaction and minimize reactive oxygen damage. It has often been assumed that water and oxygen travel through separate channels within PSII, as demonstrated in cytochrome c oxidase. This study describes all-atom molecular dynamics simulations of PSII designed to investigate channels by fully characterizing the distribution and permeation of both water and oxygen. Interestingly, most channels found in PSII were permeable to both oxygen and water, however individual channels exhibited different energetic barriers for the two solutes. Several routes for oxygen diffusion within PSII with low energy permeation barriers were found, ensuring its fast removal from the OEC. In contrast, all routes for water showed significant energy barriers, corresponding to a much slower permeation rate for water through PSII. Two major factors were responsible for this selectivity: (1) hydrogen bonds between water and channel amino acids, and (2) steric restraints. Our results reveal the presence of a shared network of channels in PSII optimized to both facilitate the quick removal of oxygen and effectively restrict the water supply to the OEC to help stabilize and protect it from small water soluble inhibitors.     

Oxygen-organophosphate linkage in hemoglobin A. The double hump effect.

At low concentrations of chloride ions, and in the presence of nonsaturating concentrations of organophosphates, the oxygen equilibrium curves (OEC) for solutions of human adult hemoglobin exhibit a biphasic shape conveniently revealed by graphical analysis of the first derivative of the Hill equation with a characteristic form that we call "the double hump effect." This shape, observed for sub-saturating concentrations of organophosphates, stands in marked contrast to the simple lateral shifts of the OEC represented largely by scaling factors when pH or chloride are varied. In the case of protons or chloride, there is a self-buffering effect due to the presence of a large reservoir of proton or chloride binding sites not necessarily linked to oxygen, whereas such sites do not exist in the case of organophosphates. In addition, in the former case, we are dealing with curves measured at constant activity of the effector, while in the latter, at constant concentration. In the presence of saturating concentrations of inositol hexaphosphate (IHP), at low chloride concentration, the entire OEC is shifted to the right, including both its upper and lower asymptotes, indicating a decrease in the intrinsic oxygen affinities of both the T and R states. Theoretical considerations leading to a successful modeling of OEC obtained under nonsaturating and saturating concentrations of IHP required an expanded two-state allosteric model in which IHP-dependent variations in oxygen association constants for both the T and R conformations are taken into account.     

A ligand field chemistry of oxygen generation by the oxygen-evolving complex and synthetic active sites

Oxygen-oxygen bond formation and O2 generation occur from the S4 state of the oxygen-evolving complex (OEC). Several mechanistic possibilities have been proposed for water oxidation, depending on the formal oxidation state of the Mn atoms. All fall under two general classifications: the AB mechanism in which nucleophilic oxygen (base, B) attacks electrophilic oxygen (acid, A) of the Mn4Ca cluster or the RC mechanism in which radical-like oxygen species couple within OEC. The critical intermediate in either mechanism involves a metal oxo, though the nature of this oxo for AB and RC mechanisms is disparate. In the case of the AB mechanism, assembly of an even-electron count, high-valent metal-oxo proximate to a hydroxide is needed whereas, in an RC mechanism, two odd-electron count, high-valent metal oxos are required. Thus the two mechanisms give rise to very different design criteria for functional models of the OEC active site. This discussion presents the electron counts and ligand geometries that support metal oxos for AB and RC O-O bond-forming reactions. The construction of architectures that bring two oxygen functionalities together under the purview of the AB and RC scenarios are described.     

Influence of age and breed on the binding of oxygen to red blood cells of bovine calves

Gustin, P., B. Detry, A. Robert, M. L. Cao, F. Lessire, C. Cambier, V. Katz, M. Ansay, A. Frans, and T. Clerbaux.Influence of age and breed on the binding of oxygen to red bloodcells of bovine calves. J. Appl.Physiol. 82(3): 784-790, 1997.The influence ofsomatic growth and genetic selection on the whole blood oxygen equilibrium curve (OEC) was measured under standard conditions indouble-muscled and dairy calves during their first 3 mo of life.Crossbreed animals were also investigated. Hemoglobin,2,3-diphosphoglycerate (DPG), Cl, andP_i concentrations were alsomeasured. The percentage of fetal hemoglobin (HbF) was determined. Theinfluence of exogenous Cl, P_i, andpH on the OEC was also assessed. ThePO₂ at 50% hemoglobin saturation(P₅₀) increased during somaticgrowth, probably because of the increase in DPG recorded indouble-muscled neonates and to the progressive disappearance of HbF inboth breeds. The oxygen exchange fraction (OEF%) was used to assessthe combined influence of the OEC shift and OEC shape changes on bloodoxygen desaturation under standard conditions, when thePO₂ decreases within a physiologicalrange. The OEF% showed an increase during the first month, then astabilization. The effects of Cl, P_i, and pH in Friesian calves weresimilar as in adult cattle. Double-muscled neonates had alower P₅₀, OEF% values, and DPG concentrations and higher hemoglobin and Cl concentrations than Friesian neonates. The P_iconcentration and the percentage of HbF were similar in both breeds.The pH and the Cl concentration had significantly less effect on theOEC in double-muscled than in Friesian calves. Crossbreed animalsexhibited intermediate parameter values, between those recorded fordouble-muscled and Friesian calves. All differences between breedsprogressively disappeared during the first month. These data show thatblood function changes markedly in calves during the first month of life and that genetic selection can alter blood function.

     

Damage to the oxygen-evolving complex by superoxide anion, hydrogen peroxide, and hydroxyl radical in photoinhibition of photosystem II

Under strong illumination of a photosystem II (PSII) membrane, endogenous superoxide anion, hydrogen peroxide, and hydroxyl radical were successively produced. These compounds then cooperatively resulted in a release of manganese from the oxygen-evolving complex (OEC) and an inhibition of oxygen evolution activity. The OEC inactivation was initiated by an acceptor-side generated superoxide anion, and hydrogen peroxide was most probably responsible for the transportation of reactive oxygen species (ROS) across the PSII membrane from the acceptor-side to the donor-side. Besides ROS being generated in the acceptor-side induced manganese loss; there may also be a ROS-independent manganese loss in the OEC of PSII. Both superoxide anion and hydroxyl radical located inside the PSII membrane were directly identified by a spin trapping-electron spin resonance (ESR) method in combination with a lipophilic spin trap, 5-(diethoxyphosphoryl)-5-phenethyl-1-pyrroline N-oxide (DEPPEPO). The endogenous hydrogen peroxide production was examined by oxidation of thiobenzamide.     

Evidence against bicarbonate bound in the O2-evolving complex of photosystem II

The oxidation of water to molecular oxygen by photosystem II (PSII) is inhibited in bicarbonate-depleted media. One contribution to the inhibition is the binding of bicarbonate to the non-heme iron, which is required for efficient electron transfer on the electron-acceptor side of PSII. There are also proposals that bicarbonate is required for formation of O 2 by the manganese-containing O 2-evolving complex (OEC). Previous work indicates that a bicarbonate ion does not bind reversibly close to the OEC, but it remains possible that bicarbonate is bound sufficiently tightly to the OEC that it cannot readily exchange with bicarbonate in solution. In this study, we have used NH 2OH to destroy the OEC, which would release any tightly bound bicarbonate ions from the active site, and mass spectrometry to detect any released bicarbonate as CO 2. The amount of CO 2 per PSII released by the NH 2OH treatment is observed to be comparable to the background level, although N 2O, a product of the reaction of NH 2OH with the OEC, is detected in good yield. These results strongly argue against tightly bound bicarbonate ions in the OEC.     

Molecular mechanism of action of Pb and Zn on water oxidizing complex of photosystem II

Pb²⁺ and Zn²⁺ inhibition of photosystem II (PSII) activity was reported to be mediated via displacement of native inorganic cofactors (Cl⁻, Ca²⁺ and Mn²⁺) from the oxygen evolving complex, OEC [Rashid and Popovic (1990) FEBS Lett. 271, 181–184; Rashid et al. (1991) Photosynth. Res. 30, 123–130]. Since the binding sites of these cofactors are protected by a shield of three extrinsic polypeptides (17, 23 and 33 kDa), we investigated whether these metal ions affect the extrinsic polypeptide shield of OEC. By immunoblotting with antibodies recognizing the 23 and 33 kDa polypeptides, we showed that both the metal ions significantly dissociated the 23 kDa (+17 kDa) polypeptide, and partially dissociated the 33 kDa. Ca²⁺, one of the important inorganic cofactors of oxygen evolution, strongly prevented the dissociating action of Pb²⁺ but did not prevent the action of Zn²⁺. The probable molecular mechanism of action of Pb²⁺ and Zn²⁺ on PSII OEC is discussed.