Specific helix stabilization of poly(L-glutamic acid) in mixed counterion systems

The coil–helix transitions of poly (L -glutamic acid) in aqueous alcohol solutions have been investigated for mixed counterion systems. It has been found that coexistence of two kinds of counterion species, i.e., two alkali metal counterions, alkali and alkaline earth metal, and two alkaline earth metals, specifically stabilizes or destabilizes the helix conformation depending upon the combination of the counterion species. The most striking enhancement of the helix content was observed for the combination of Li⁺ and K⁺ counterions. It has been suggested that the helix stabilization is attributed to the reduction of the free energy in the contact ion pair formation between the polymer charges and the counterions in the mixed counterion systems. © 1993 John Wiley & Sons, Inc.     

De-icers derived from corn steep water

Corn steep water (CSW) and other byproducts derived from fermentations and sugar productions are presently forming the base of compositions for de-icing and anti-icing materials. Since the de-icing and anti-icing values are in part a colligative property, increase in the molar concentration of ionic species has been frequently necessary to decrease further the freezing point of this byproducts stream. In the present study this has been achieved by the generation of biodegradable organic acid salts in situ, without the use of chloride or other inorganic salts, by the alkaline degradation of reducing sugars added to corn steep water, which alone is not an efficient de-icer. Reducing sugars, such as glucose, react with alkali metal hydroxides to produce principally hydroxy carboxylic acids that react with the alkali metal hydroxide to form a mixture of organic acid salts. The ionic strength of the resulting solution is increased since each sugar molecule produces nearly two acid molecules upon degradation. The ionic strength necessary to achieve the desired freezing point depression is determined by the amount and concentration of the alkali metal hydroxide used, with the necessary counter anions being derived from the degradation of the reducing sugar. The amount of the sugar used is that required to result in a near to neutral final solution. The well-known anti-corrosive property of CSW is used in the de-icer preparations, either by conducting the alkaline degradation of the sugar in this medium, or by using water for the degradation of the sugar followed by dilution of the resulting solution with CSW to adjust the viscosity of the final solution to meet the requirements for spraying. The monovalent metal hydroxides are more efficient in producing de-icer solutions than the divalent metal hydroxides.     

The permeability of endplate channels to monovalent and divalent metal cations

The relative permeability of endplate channels to monovalent and divalent metal ions was determined from reversal potentials. Thallium is the most permeant ion with a permeability ratio relative to Na+ of 2.5. The selectivity among alkali metals is weak with a sequence, Cs+ greater than Rb+ greater than K+ greater than Na+ greater than Li+, and permeability ratios of 1.4, 1.3, 1.1, 1.0, and 0.9. The selectivity among divalent ions is also weak, with a sequence for alkaline earths of Mg++ greater than Ca++ greater than Ba++ greater than Sr++. The transition metal ions Mn++, Co++, Ni++, Zn++, and Cd++ are also permeant. Permeability ratios for divalent ions decreased as the concentration of divalent ion was increased in a manner consistent with the negative surface potential theory of Lewis (1979 J. Physiol. (Lond.). 286: 417--445). With 20 mM XCl2 and 85.5 mM glucosamine.HCl in the external solution, the apparent permeability ratios for the alkaline earth cations (X++) are in the range 0.18--0.25. Alkali metal ions see the endplate channel as a water-filled, neutral pore without high-field-strength sites inside. Their permeability sequence is the same as their aqueous mobility sequence. Divalent ions, however, have a permeability sequence almost opposite from their mobility sequence and must experience some interaction with groups in the channel. In addition, the concentrations of monovalent and divalent ions are increased near the channel mouth by a weak negative surface potential.     

9-Amino-acridine as a probe of the electrical double layer associated with the chloroplast thylakoid membranes

Chloroplasts washed with monovalent cations are found to quench 9-amino-acridine fluorescence after resuspension in a cation-free medium. This quenching occurs in the absence of a high energy state and can be reversed by the addition of salts. The effectiveness of these salts is related to the charge carried by the cations and appears to be essentially independent of the associated anions. The order of effectiveness is polyvalent > divalent > monovalent, and virtually no variation is found within the groups of monovalent cations and divalent cations tested. Furthermore, choline and lysine are as effective as alkali metal cations, and lysyl-lysine is almost as effective as alkaline earth metal cations. These results are consistent with an effect mediated by the electrical double layer at the membrane surface rather than chemical bonding, and can be qualitatively explained in terms of the Gouy-Chapman theory.It appears that 9-amino-acridine acts as a diffusible monovalent cation which increases its fluorescence when displaced from the diffuse layer adjacent to the negatively charged membrane surface. The 9-amino-acridine fluorescence changes have been experimentally correlated with the cation-induced chlorophyll a fluorescence changes also observed with isolated chloroplasts.     

Probing cationic selectivity of cardiac calsequestrin and its CPVT mutants

CASQ (calsequestrin) is a Ca2+-buffering protein localized in the muscle SR (sarcoplasmic reticulum); however, it is unknown whether Ca2+ binding to CASQ2 is due to its location inside the SR rich in Ca2+ or due to its preference for Ca2+ over other ions. Therefore a major aim of the present study was to determine how CASQ2 selects Ca2+ over other metal ions by studying monomer folding and subsequent aggregation upon exposure to alkali (monovalent), alkaline earth (divalent) and transition (polyvalent) metals. We additionally investigated how CPVT (catecholaminergic polymorphic ventricular tachycardia) mutations affect CASQ2 structure and its molecular behaviour when exposed to different metal ions. Our results show that alkali and alkaline earth metals can initiate similar molecular compaction (folding), but only Ca2+ can promote CASQ2 to aggregate, suggesting that CASQ2 has a preferential binding to Ca2+ over all other metals. We additionally found that transition metals (having higher co-ordinated bonding ability than Ca2+) can also initiate folding and promote aggregation of CASQ2. These studies led us to suggest that folding and formation of higher-order structures depends on cationic properties such as co-ordinate bonding ability and ionic radius. Among the CPVT mutants studied, the L167H mutation disrupts the Ca2+-dependent folding and, when folding is achieved by Mn2+, L167H can undergo aggregation in a Ca2+-dependent manner. Interestingly, domain III mutants (D307H and P308L) lost their selectivity to Ca2+ and could be aggregated in the presence of Mg2+. In conclusion, these studies suggest that CPVT mutations modify CASQ2 behaviour, including folding, aggregation/polymerization and selectivity towards Ca2+.     

Kinetic and thermodynamic analysis of the interaction of cations with dialkylglycine decarboxylase

Dialkylglycine decarboxylase (DGD) is a tetrameric pyridoxal phosphate (PLP)-dependent enzyme that catalyzes both decarboxylation and transamination in its normal catalytic cycle. Its activity is dependent on cations. Metal-free DGD and DGD complexes with seven monovalent cations (Li(+), Na(+), K(+), Rb(+), Cs(+), NH(4)(+), and Tl(+)) and three divalent cations (Mg(2+), Ca(2+), and Ba(2+)) have been studied. The catalytic rate constants for cation-bound enzyme (ck(cat) and ck(cat)/bK(AIB)) are cation-size-dependent, K(+) being the monovalent cation with the optimal size for catalytic activity. The divalent alkaline earth cations (Mg(2+), Ca(2+), and Ba(2+)) all give approximately 10-fold lower activity compared to monovalent alkali cations of similar ionic radius. The Michaelis constant for aminoisobutyrate (AIB) binding to DGD-PLP complexes with cations (bK(AIB)) varies with ionic radius. The larger cations (K(+), Rb(+), Cs(+), NH(4)(+), and Tl(+)) give smaller bK(AIB) ( approximately 4 mM), while smaller cations (Li(+), Na(+)) give larger values (approximately 10 mM). Cation size and charge dependence is also found with the dissociation constant for PLP binding to DGD-cation complexes (aK(PLP)). K(+) and Rb(+) possess the optimal ionic radius, giving the lowest values of aK(PLP). The divalent alkaline earth cations give aK(PLP) values approximately 10-fold higher than alkali cations of similar ionic radius. The cation dissociation constant for DGD-PLP-AIB-cation complexes (betaK(M)z+) was determined and also shown to be cation-size-dependent, K(+) and Rb(+) yielding the lowest values. The kinetics of PLP association and dissociation from metal-free DGD and its complexes with cations (Na(+), K(+), and Ba(2+)) were analyzed. All three cations tested increase PLP association and decrease PLP dissociation rate constants. Kinetic studies of cation binding show saturation kinetics for the association reaction. The half-life for association with saturating Rb(+) is approximately 24 s, while the half-life for dissociation of Rb(+) from the DGD-PLP-AIB-Rb(+) complex is approximately 12 min.     

Some observations on the structure, cation content and possible evolutionary status of dinoflagellate chromosomes

SICEE, D. C., 1984. Some observations on the structure, cation content and possible evolutionary status of dinoflagellate chromosomes. Dinoflagellate chromosomes have a well-ordered structure, as observed in living cells, glutaraldehyde/osmium tetroxide-fixed cells, ultrathin cryosections and freeze-etch preparations. It is suggested that the stabilization of this chromatin in the living cell is largely mediated by divalent cations, acting as bridging molecules between the DNA superstructure and the protein matrix. Studies using X-ray micro-analysis and autoradiography have shown that these chromosomes have high levels of bound Ca and transition metals, and that these are associated with both the DNA and surrounding proteins.
The organization and stabilization of chromatin in dinoflagellate chromosomes is quite different from that of the cells of other eukaryotes, but shows some resemblance to the dispersed chromatin of bacteria. The evolution of dinoflagellate chromosomes from a prokaryote-like ancestral genome is attributed to two main factors–the retention of a primitive cationic non-histone stabilization system, and a pronounced evolutionary trend towards high DNA values. On this theory, dinoflagellate chromosomes are phylogenetically distinct from all other eukaryote chromosomes, and provide a separate evolutionary route for the attainment of high DNA levels and increased cell size.     

Neuromuscular transmission in Ca<Superscript>2+</Superscript>-free extracellular solution

The review brings together the data on neuromuscular transmission upon substitution of different alkaline earth metals for Ca²⁺ ions. It is known that due to the low selectivity of calcium channels and their ability to conduct other divalent cations, a considerable presynaptic current carried by strontium or barium may develop, which under certain conditions may lead to the neuromuscular transmission. The review illustrates how the equimolar substitution of external Ca²⁺ by other polyvalent cations affects the parameters of nonquantum, spontaneous, and induced quantum exocytosis of the neuromediator, as well as endocytosis and the activities of acetylcholinesterase and postsynaptic receptors. The effects of the modulators of synaptic transmission under these conditions are also considered.     

Divalent Metal Cations upon Coordination to the N7 of Purines Differentially Stabilize the PyPuPu DNA Triplex due to Unequal Hoogsteen-type Hydrogen Bond Enhancement

Abstract

The PyPuPu triplexes consisting of CG*G triads are stabilized by alkaline earth cations (Ca²⁺, Mg²⁺) and transition metal cations (Mn²⁺, Co²⁺, Ni²⁺, Zn²⁺, Cd²⁺), while similar triplexes including TA*A triads are stabilized only by transition metal cations. We hypothesize that such a differential triplex stabilization by divalent metal cations can be the consequence of their coordination to the N7 of the third strand purines with concomitant polarization effects on the bases resulting in unequal Hoogsteen-type hydrogen bond enhancement.     

Equilibria between ionophore A23187 and divalent cations: stability of 1:1 complexes in solutions of 80% methanol/water

The cation complexation equilibria between ionophore A23187 and several alkaline earth and first transition series divalent cations have been investigated. Absorption and fluorescence spectroscopy were used to monitor the reactions which were studied in solutions of 80% methanol/water, at 25 degrees C, and under conditions of controlled ionic strength and pH. Titration of the ionophore with divalent cations results first in formation of the dimeric species MA2 and subsequently in the formation of MA+ by disproportionation of the first product. With Zn2+, Ni2+, and Co2+ (above pH approximately 6), a third species is detected which is postulated to be MA.OH. The existence of this species with Mn2+ and alkaline earth cations is uncertain. For formation of MA2, the second stepwise stability constant is similar to or exceeds the first value with all cations studied. However, it is possible to isolate the first reaction and determine accurate stability constants by working at an ionophore concentration of 3 X 10(-8) M or less and by employing pH values which preclude interference by the mixed ionophore/hydroxide species. Under these conditions, the relationship between log KMA' and pH is linear and displays a slope of 1.0. pH-independent stability constants were calculated by using pH-dependent stability constants and the known value of the ionophore's protonation constant in this solvent. The logarithms of the values obtained ranged from 7.54 +/- 0.06 for Ni2+ to 3.60 +/- 0.06 for Ba2+. The selectivity sequence and relative affinities (in parentheses) for the species MA+ are as follows: Ni2+ (977) greater than Co2+ (331) greater than Zn2+ (174) greater than Mn2+ (34) greater than Mg2+ (1.00) approximately equal to Ca2+ (0.89) greater than Sr2+ (0.20) greater than Ba2+ (0.11). Data are discussed in comparison to other studies on the complexation properties of A23187 and in terms of their significance to interpreting the transport properties of this ionophore.     

ON THE RECONSTITUTION OF THE CRYSTALLINE COMPONENTS OF THE SEA URCHIN FERTILIZATION MEMBRANE

The characteristics of the reconstitution of a crystalline component of the sea urchin fertilization membrane are presented. The reassembly of large aggregates of cylindrical or tubular components is effected by the addition of calcium or other divalent cations. The reassembly requires a slightly alkaline pH and is little affected by increasing ionic strength. Reassembly is strongly inhibited by treatment with reducing agents such as dithiothreitol. The role of this protein in the formation of the fertilization membrane and its possible relation to the calcium-insoluble proteins of the mitotic apparatus are discussed.     

Sodium and chloride ions contribute synergistically to salt toxicity in wheat

The effects of supplying excess mineral salts, involving sodium as a cation and a range of counteranions, including chloride, on the growth and photosynthetic capacity of a salt susceptible bread wheat were studied. Plant performance was much more affected by the NaCl treatment than by the same concentration of either of the two component ions. With the exception of K⁺, other alkali metal chlorides also greatly inhibit plant growth and the electron flow through photosystem 2. The ranking of toxicity of these cations is Li⁺>Na⁺>K⁺. The synergistic effect of sodium (and other alkali and alkaline earth metals) and chloride shows that neither of these ions alone is responsible for salt stress induced damage.     

Chromosome bands and the subunit structure of Chinese hamster metaphase chromosomes

Isolated Chinese hamster chromosomes dissociate into a series of specific chromatin subunits approximately the size of stainable chromosome bands upon reduction of the divalent ion concentration during or after isolation. At high pH the chromatin in some bands is differentially removable during chromosome isolation, leaving a banded chromosome with a pattern typical of most G-band procedures. This provides an alternate molecular mechanism to explain the production of banded chromosomes by a variety of staining procedures. These results also suggest an approach to chromatin fractionation, using metaphase chromosomes as a starting material.     

Raman spectroscopy of DNA-metal complexes. I. Interactions and conformational effects of the divalent cations: Mg, Ca, Sr, Ba, Mn, Co, Ni, Cu, Pd, and Cd.

Interactions of divalent metal cations (Mg2+, Ca2+, Ba2+, Sr2+, Mn2+, Co2+, Ni2+, Cu2+, Pd2+, and Cd2+) with DNA have been investigated by laser Raman spectroscopy. Both genomic calf-thymus DNA (> 23 kilobase pairs) and mononucleosomal fragments (160 base pairs) were employed as targets of metal interaction in solutions containing 5 weight-% DNA and metal:phosphate molar ratios of 0.6:1. Raman difference spectra reveal that transition metal cations (Mn2+, Co2+, Ni2+, Cu2+, Pd2+, and Cd2+) induce the greatest structural changes in B-DNA. The Raman (vibrational) band differences are extensive and indicate partial disordering of the B-form backbone, reduction in base stacking, reduction in base pairing, and specific metal interaction with acceptor sites on the purine (N7) and pyrimidine (N3) rings. Many of the observed spectral changes parallel those accompanying thermal denaturation of B-DNA and suggest that the metals link the bases of denatured DNA. While exocyclic carbonyls of dT, dG, and dC may stabilize metal ligation, correlation plots show that perturbations of the carbonyls are mainly a consequence of metal-induced denaturation of the double helix. Transition metal interactions with the DNA phosphates are weak in comparison to interactions with the bases, except in the case of Cu2+, which strongly perturbs both base and phosphate group vibrations. On the other hand, the Raman signature of B-DNA is largely unperturbed by Mg2+, Ca2+, Sr2+, and Ba2+, suggesting much weaker interactions of the alkaline earth metals with both base and phosphate sites. A notable exception is a moderate perturbation by alkaline earths of purine N7 sites in 160-base pair DNA, with Ca2+ causing the greatest effect. Correlation plots demonstrate a strong interrelationship between perturbations of Raman bands assigned to ring vibrations of the bases and those of bands assigned to exocyclic carbonyls and backbone phosphodiester groups. However, strong correlations do not occur between the Raman phosphodioxy band (centered near 1092 cm-1) and other Raman bands, suggesting that the former is not highly sensitive to the structural changes induced by divalent metal cations. The structural perturbations induced by divalent cations are much greater for > 23-kilobase pair DNA than for 160-base pair DNA, as evidenced by both the Raman difference spectra and the tendency toward the formation of insoluble aggregates. In the presence of transition metals, aggregation of high-molecular-weight DNA is evident at temperatures as low as 11 degrees C.(ABSTRACT TRUNCATED AT 400 WORDS)     

Raman spectroscopy of DNA-metal complexes. II. The thermal denaturation of DNA in the presence of Sr2+, Ba2+, Mg2+, Ca2+, Mn2+, Co2+, Ni2+, and Cd2+.

Differential scanning calorimetry, laser Raman spectroscopy, optical densitometry, and pH potentiometry have been used to investigate DNA melting profiles in the presence of the chloride salts of Ba2+, Sr2+, Mg2+, Ca2+, Mn2+, Co2+, Ni2+, and Cd2+. Metal-DNA interactions have been observed for the molar ratio [M2+]/[PO2-] = 0.6 in aqueous solutions containing 5% by weight of 160 bp mononucleosomal calf thymus DNA. All of the alkaline earth metals, plus Mn2+, elevate the melting temperature of DNA (Tm > 75.5 degrees C), whereas the transition metals Co2+, Ni2+, and Cd2+ lower Tm. Calorimetric (delta Hcal) and van't Hoff (delta HVH) enthalpies of melting range from 6.2-8.7 kcal/mol bp and 75.6-188.6 kcal/mol cooperative unit, respectively, and entropies from 17.5 to 24.7 cal/K mol bp. The average number of base pairs in a cooperative melting unit (<nmelt>) varied from 11.3 to 28.1. No dichotomy was observed between alkaline earth and transition DNA-metal complexes for any of the thermodynamic parameters other than their effects on Tm. These results complement Raman difference spectra, which reveal decreases in backbone order, base unstacking, distortion of glycosyl torsion angles, and rupture of hydrogen bonds, which occur after thermal denaturation. Raman difference spectroscopy shows that transition metals interact with the N7 atom of guanine in duplex DNA. A broader range of interaction sites with single-stranded DNA includes ionic phosphates, the N1 and N7 atoms of purines, and the N3 atom of pyrimidines. For alkaline earth metals, very little interaction was observed with duplex DNA, whereas spectra of single-stranded complexes are very similar to those of melted DNA without metal. However, difference spectra reveal some metal-specific perturbations at 1092 cm-1 (nPO2-), 1258 cm-1 (dC, dA), and 1668 cm-1 (nC==O, dNH2 dT, dG, dC). Increased spectral intensity could also be observed near 1335 cm-1 (dA, dG) for CaDNA. Optical densitometry, employed to detect DNA aggregation, reveals increased turbidity during the melting transition for all divalent DNA-metal complexes, except SrDNA and BaDNA. Turbidity was not observed for DNA in the absence of metal. A correlation was made between DNA melting, aggregation, and the ratio of Raman intensities I1335/I1374. At room temperature, DNA-metal interactions result in a pH drop of 1.2-2.2 units for alkaline earths and more than 2.5 units for transition metals. Sr2+, Ba2+, and Mg2+ cause protonated sites on the DNA to become thermally labile. These results lead to a model that describes DNA aggregation and denaturation during heating in the presence of divalent metal cations; 1) The cations initially interact with the DNA at phosphate and/or base sites, resulting in proton displacement. 2) A combination of metal-base interactions and heating disrupts the base pairing within the DNA duplex. This allows divalent metals and protons to bind to additional sites on the DNA bases during the aggregation/melting process. 3) Strands whose bases have swung open upon disruption are linked to neighboring strands by metal ion bridges. 4) Near the midpoint of the melting transition, thermal energy breaks up the aggregate. We have no evidence to indicate whether metal ion cross-bridges or direct base-base interactions rupture first. 5) Finally, all cross-links break, resulting in single-stranded DNA complexed with metal ions.     

Remarkable affinity and selectivity for Cs+ and uranyl (UO22+) binding to the manganese site of the apo-water oxidation complex of photosystem II.

The size and charge density requirements for metal ion binding to the high-affinity Mn2+ site of the apo-water oxidizing complex (WOC) of spinach photosystem II (PSII) were studied by comparing the relative binding affinities of alkali metal cations, divalent metals (Mg2+, Ca2+, Mn2+, Sr2+), and the oxo-cation UO22+. Cation binding to the apo-WOC-PSII protein was measured by: (1) inhibition of the rate and yield of photoactivation, the light-induced recovery of O2 evolution by assembly of the functional Mn4Ca1Clx, core from its constituent inorganic cofactors (Mn2+, Ca2+, and Cl-); and by (2) inhibition of the PSII-mediated light-induced electron transfer from Mn2+ to an electron acceptor (DCIP). Together, these methods enable discrimination between inhibition at the high- and low-affinity Mn2+ sites and the Ca2+ site of the apo-WOC-PSII. Unexpectedly strong binding of large alkali cations (Cs+ > Rb+ > K+ > Na+ > Li+) was found to smoothly correlate with decreasing cation charge density, exhibiting one of the largest Cs+/Li+ selectivities (>/=5000) for any known chelator. Both photoactivation and electron-transfer measurements at selected Mn2+ and Ca2+ concentrations reveal that Cs+ binds to the high-affinity Mn2+ site with a slightly greater affinity (2-3-fold at pH 6.0) than Mn2+, while binding about 10(4)-fold more weakly to the Ca2+-specific site required for reassembly of functional O2 evolving centers. In contrast to Cs+, divalent cations larger than Mn2+ bind considerably more weakly to the high-affinity Mn2+ site (Mn2+ > Ca2+ > Sr2+). Their affinities correlate with the hydrolysis constant for formation of the metal hydroxide by hydrolysis of water: Me2+aq --> [MeOH]+aq + H+aq. Along with the strong stimulation of the rate of photoactivation by alkaline pH, these metal cation trends support the interpretation that [MnOH]+ is the active species that forms upon binding of Mn2+aq to apo-WOC. Further support for this interpretation is found by the unusually strong inhibition of Mn2+ photooxidation by the linear uranyl cation (UO22+). The intrinsic binding constant for [MnOH]+ to apo-WOC was determined using a thermodynamic cycle to be K = 4.0 x 10(15) M-1 (at pH 6.0), consistent with a high-affinity, preorganized, multidentate coordination site. We propose that the selectivity for binding [MnOH]+, a linear low charge-density monocation, vs symmetrical Me2+ dications is functionally important for assembly of the WOC by enabling: (1) discrimination against higher charge density alkaline earth cations (Mg2+ and Ca2+) and smaller alkali metal cations (Na+ and K+) that are present in considerably greater abundance in vivo, and thus would suppress photoactivation; and (2) higher affinity binding of the one Ca2+ ion or the remaining three Mn2+ ions via coordination to form mu-hydroxo-bridged intermediates, apo-WOC-[Mn(mu-OH)2Mn]3+ or apo-WOC-[Mn(mu-OH)Ca]3+, during subsequent assembly steps of the native Mn4Ca1Clx core. In contrast to more acidic Me2+ divalent ion inhibitors of the high-affinity Mn2+ site, like Ca2+ and Sr2+, Cs+ does not accelerate the decay of the first light-induced intermediate, IM1, formed during photoactivation (attributed to apo-WOC-[Mn(OH)2]+). The inability of Cs+ to promote decay of IM1, despite having comparable affinity as Mn2+, is consistent with its considerably weaker Lewis acidity, resulting in the reprotonation of IM1 by water becoming the rate-limiting step for decay prior to displacement of Mn2+. All four different lines of evidence provide a self-consistent picture indicating that the initial step in assembly of the WOC involves high-affinity binding of [MnOH]+.     

Low angle x-ray diffraction studies of chromatin structure in vivo and in isolated nuclei and metaphase chromosomes

Diffraction of x-rays from living cells, isolated nuclei, and metaphase chromosomes gives rise to several major low angle reflections characteristic of a highly conserved pattern of nucleosome packing within the chromatin fibers. We answer three questions about the x-ray data: Which reflections are characteristic of chromosomes in vivo? How can these reflections be preserved in vitro? What chromosome structures give rise to the reflections? Our consistent observation of diffraction peaks at 11.0, 6.0, 3.8, 2.7 and 2.1 nm from a variety of living cells, isolated nuclei, and metaphase chromosomes establishes these periodicities as characteristic of eukaryotic chromosomes in vivo. In addition, a 30-40- nm peak is observed from all somatic cells that have substantial amounts of condensed chromatin, and a weak 18-nm reflection is observed from nucleated erythrocytes. These observations provide a standard for judging the structural integrity of isolated nuclei, chromosomes, and chromatin, and thus resolve long standing controversy about the “tru” nature of chromosome diffraction. All of the reflection seen in vivo can be preserved in vitro provided that the proper ionic conditions are maintained. Our results show clearly that the 30-40-nm maximum is a packing reflection. The packing we observe in vivo is directly correlated to the side-by-side arrangement of 20- 30-nm fibers observed in thin sections of fixed and dehydrated cells and isolated chromosomes. This confirms that such packing is present in living cells and is not merely an artifact of electron microscopy. As expected, the packing reflection is shifted to longer spacings when the fibers are spread apart by reducing the concentration of divalent cations in vitro. Because the 18-, 11.0-, 6.0-, 3.8-, 2.7-, and 2.1-nm reflections are not affected by the decondensation caused by removal of divalent cations, these periodicities must reflect the internal structure of the chromaticn fibers.     

Bacteriorhodopsin Is a Powerful Light-Driven Proton Pump

The activity of bacteriorhodopsin was investigated with Halobacterium halobium cell envelopes, which lack cytoplasmic constituents. It was found that the physiological concentration of magnesium ion greatly enhanced the light-induced pH change; under optimal conditions, the pH change of the external medium was as large as 3.5 pH units, even though the volume fraction of the envelope vesicles was as low as 0.01. This pH change is about three times larger than the largest change reported thus far. This same effect was observed with transition metal ions, but not with other alkaline divalent cations. That is, divalent cations that formed hydroxides below pH 10 were effective in enhancing the light-induced pH change. This result suggests that some divalent cations acted as buffers against a large increase in the internal pH, and that the internal pH was an important factor in determining the activity of bacteriorhodopsin. It was also shown that a high level of the proton-pump activity was maintained in a wide range of external pHs, at least between 4.5 and 9.4.     

General features in the stoichiometry and stability of ionophore A23187-cation complexes in homogeneous solution

Existing literature describing the stoichiometry and stability of complexes between A23187 and divalent cations in solution has been extended to include additional transition series cations, the heavy-metal cations Cd2+ and Pb2+, plus seven lanthanide series trivalent cations. Stability constants of 1:1 complexes between the ionophore and the divalent cations vary by 6.2 orders of magnitude between Cu2+ and Ba2+ which are the strongest and weakest complexes, respectively. Considering alkaline-earth and first-series transition cations together, the pattern of stability constants obeys the extended Irving-Williams series as is seen with many nonionophorous liganding agents. Cd2+ and Pb2+ are bound with an affinity similar to those of Mn2+ and Zn2+, whereas the lanthanides are bound with little selectivity and slightly higher stability. Titration of the ionophore in the 10(-5) M concentration range with di- and trivalent cations gives rise first to complexes of stoichiometry MA2 and subsequently to MA as the metal concentration is increased. The second stepwise stability constants for formation of the MA2 species exceeds the first constant by approximately 10-fold. With lanthanides, heavy metals, and transition-metal cations, OH-, at near physiological concentrations, competes significantly with free ionophore for binding to the 1:1 complexes. This competition is not apparent when Ca2+ or Mg2+ are the central cations. Possible implications of the 1:1 complex selectivity pattern, the ionophore-hydroxide competitive binding equilibria, and potential ternary complexes involving 1:1 ionophore:cation complexes and other anions present in biological systems are discussed with respect to the ionophore's transport selectivity and biological actions.