Erik B. Smaal

Localization of the pathway of the penicillin biosynthesis in Penicillium chrysogenum.

The localization of the enzymes involved in penicillin biosynthesis in Penicillium chrysogenum hyphae has been studied by immunological detection methods in combination with electron microscopy and cell fractionation. The results suggest a complicated pathway involving different intracellular locations. The enzyme delta‐(L‐alpha‐aminoadipyl)‐L‐cysteinyl‐D‐valine synthetase was found to be associated with membranes or small organelles. The next enzyme isopenicillin N‐synthetase appeared to be a cytosolic enzyme. The enzyme which is involved in the last step of penicillin biosynthesis, acyltransferase, was located in organelles with a diameter of 200–800 nm. These organelles, most probably, are microbodies. A positive correlation was found between the capacity for penicillin production and the number of organelles per cell when comparing different P. chrysogenum strains.

Involvement of microbodies in penicillin biosynthesis

Penicillium chrysogenum strains were constructed which express a mutant acyltransferase lacking the putative targeting signal for microbody proteins. The mutated enzyme was located in vacuoles and in neighbouring cytoplasm. Although acyltransferase was expressed in vivo and was active in vitro, the mutants did not produce penicillin. The results demonstrate the involvement of microbodies in penicillin production.

2H-NMR, 31P-NMR and DSC characterization of a novel lipid organization in calcium-dioleoylphosphatidate membranes. Implications for the mechanism of the phosphatidate calcium transmembrane shuttle

2H-NMR, 31P-NMR and DSC investigations are presented on the structure and dynamics of the Ca2+-dioleoylphosphatidate complex which is formed upon addition of calcium to dispersions of pure dioleoylphosphatidate or of dioleoylphosphatidate in mixtures with dioleoylphosphatidylcholine (DOPC). It is concluded that the phosphate region in the polar headgroup of dioleoylphosphatidate is immobilized, while the oleate chains remain liquid and have increased disorder. In mixtures of dioleoylphosphatidate and DOPC in the presence of calcium a dioleoylphosphatidate-rich phase is segregated, in which the molecular behaviour of phosphatidate is rather similar to that of the pure Ca2+-dioleoylphosphatidate complex. A hypothetical model is proposed for the structure of this complex and this is correlated with the dioleoylphosphatidate-mediated transmembrane transport of calcium (Smaal, E.B., Mandersloot, J.G., De Kruijff, B. and De Gier, J. (1986) Biochim. Biophys. Acta 860, 99-108). Data indicate that this transmembrane shuttle is an inverted organization of phosphatidate molecules enclosing calcium ions in an anhydrous core.

Consequences of the interaction of calcium with dioleoylphosphatidate-containing model membranes: calcium-membrane and membrane-membrane interactions

Calcium binds to dioleoylphosphatidate/dioleoylphosphatidylcholine (DOPA/DOPC) (20:80, mol%) multilamellar vesicles in the presence of a calcium ionophore with stoichiometry of about 0.6 nmol calcium per nmol phosphatidate and an apparent dissociation constant of about 1.7 mM. Experiments on the behaviour of monomolecular films at an air/water interface show that calcium-phosphatidate binding results in a decrease in the area of the polar region of the phosphatidate molecule, probably caused by headgroup dehydration and partial charge neutralization. At calcium concentration higher than about 3 mM calcium neutralizes the negatively charged membrane surface of DOPA/DOPC (20:80, mol%) large unilamellar vesicles, and vesicle aggregation is observed. At 10 mM of calcium this results in a low level of vesicle fusion. These observed processes are not attended with calcium-induced phosphatidylcholine transbilayer movement in the membranes of DOPA/DOPC (20:80, mol%) large unilamellar vesicles. When these findings are compared with the results of a previous study on the permeability behaviour of large unilamellar vesicles of the same phospholipid composition under comparable conditions (Smaal, E.B., Mandersloot, J.G., De Kruijff, B. and De Gier, J. (1986) Biochim. Biophys. Acta 860, 99-108) the following conclusions can be drawn. At low millimolar calcium concentrations (less than 2.5 mM) calcium does not occupy all the binding sites of the membrane, no membrane-membrane interactions are observed and a selective translocation of calcium and calcium-chelating anions is appearing. The mechanism of this translocation may be explained by the formation of uncharged dehydrated complexes of calcium, phosphatidate and calcium chelator, which can pass the membrane via transient occurring non-bilayer structures. Between 3 and 10 mM of calcium an a selective permeability increase of the vesicular membrane is found, which is not a consequence of vesicle fusion but apparently of vesicle aggregation, possibly causing packing defects in the membrane.

Essential adaptation of the calcium influx assay into liposomes with entrapped arsenazo III for studies on the possible calcium translocating properties of acidic phospholipids

An adapted version of the Ca2+-influx assay of Weissmann et al. (Weissmann, G., Anderson, P., Serhan, C., Samuelson, E. and Goodman, E. (1980) Proc. Natl. Acad. Sci. USA 77, 1506-1510) is presented for studies on the possible ionophoretic properties of acidic phospholipids. This method is based on the use of the metallochromic dye arsenazo III enclosed in liposomal vesicles, to indicate the Ca2+ influx. An essential control is introduced to discriminate between Ca2+-arsenazo III complex formation inside the vesicles, as a consequence of Ca2+ influx, and outside the vesicles, as a consequence of arsenazo III leakage from the vesicles. Furthermore, some minor improvements are added, like the use of large unilamellar vesicles instead of multilamellar vesicles, and the use of dual wavelength spectrophotometry. Using this method, it was found that dioleoylphosphatidylcholine vesicles, containing 20 mol% dioleoylphosphatidylglycerol, were impermeable to Ca2+. In this system a selective Ca2+ permeability could be induced by the addition of the fungal Ca2+ ionophore A23187. In contrast, dioleoylphosphatidylcholine vesicles, containing 20 mol% dioleoylphosphatidic acid, incubated in the presence of Ca2+ were permeable to both Ca2+ and arsenazo III.

Calcium-induced changes in permeability of dioleoylphosphatidylcholine model membranes containing bovine heart cardiolipin

At calcium concentrations up to about 4 mM a selective permeability increase of cardiolipin/dioleoylphosphatidylcholine (50:50, mol%) membranes for calcium and its chelator arsenazo III is observed. Under these conditions calcium does not occupy all the binding sites of cardiolipin at the membrane interface and no vesicle-vesicle interactions are found. Lowering of the cardiolipin content of the vesicles to 20 mol% extends the calcium concentration range in which a selective permeability for calcium and arsenazo III is appearing up to about 12 mM. We suggest that the observed selective permeability increase is caused by transient formation of inverted micellar structures in the membrane with cardiolipin as translocating membrane component for calcium and arsenazo III. At calcium concentrations of 4 mM and higher for 50 mol% cardiolipin-containing vesicles a general permeability increase is found together with calcium-cardiolipin binding in a 1:1 stoichiometry, vesicles aggregation and, above 8 mM of calcium, vesicle fusion. The loss of barrier function of the membrane under these conditions is correlated with vesicle aggregation and may be explained by a transition from a bilayer into a hexagonal HII organization of the phospholipids.

Consequences of the interaction of calcium with dioleoylphosphatidate-containing model membranes: changes in membrane permeability

The permeability behaviour of dioleoylphosphatidate/dioleoylphosphatidylcholine (20:80, mol%) large unilamellar vesicles at low millimolar calcium concentrations is different for various solutes. Between 0.5 mM and 2.5 mM of calcium a selective influx of calcium and efflux of enclosed calcium chelating anions is observed. At higher calcium concentrations the membrane loses its barrier function for a large variety of solutes. These permeability increases are a specific consequence of calcium phosphatidate interactions, because control experiments in which calcium was replaced by magnesium or in which dioleoylphosphatidate was replaced by dioleoylphosphatidylglycerol showed under the same conditions no permeability changes. These results are discussed on the basis of various putative mechanistic models for phosphatidate-mediated calcium translocation across membranes. Furthermore a kinetical model is presented by which the observed selective calcium and calcium-chelator translocation can be explained.

Ethylene glycol causes acyl chain disordering in liquid-crystalline unsaturated phospholipid model membranes, as measured by 2H-NMR

2H NMR has been used to probe the effects of ethylene glycol at the level of the acyl chains in liposomes prepared from dioleoylphosphatidic acid or dioleoylphosphatidylcholine, labeled with 2H at the 11‐position of both oleic acid chains. Increasing concentrations of ethylene glycol lead to a proportional and substantial decrease in the quadrupolar splittings, measured from the 2H NMR spectra of both liposomal systems, indicative of acyl chain disordering.

Differences in permeability of dioleoylphosphatidylcholine model membranes containing saturated or unsaturated phosphatidic acids

Abstract At low millimolar Ca2+ concentrations, large unilamellar dioleoylphosphatidylcholine vesicles containing dimyristoylphosphatidate (20 mol%) release enclosed solutes like sulphate, but influx of Ca2+ is not demonstrable. Coincident with the permeability change, vesicle aggregation and membrane fusion are observed. These results contrast with those for dioleoylphosphatidate-containing vesicles under the same conditions, which show Ca2+ influx and Ca2+ chelator efflux, but no sulphate efflux, vesicle aggregation or membrane fusion. The observed differences in permeability behaviour of membranes containing these two phosphatidate molecular species are discussed with respect to the differences in their phase behaviour.

Structural and Functional Aspects of the Chemical and Physical Diversity of Membrane Lipids

Current concepts on the structure of biological membranes depict such a membrane as a liquid crystalline bilayer of lipid molecules in which penetrating protein structures are embedded. It is often assumed that the proteins are responsible for the specific properties of the membrane such as signal transduction and membrane transport, whereas the bilayer is there to provide a fluid matrix and to form an impermeable barrier. In view of such concepts the complexity of the lipid composition of a membrane is a striking fact. Although one suitable type of lipid could accomplish the requirements of a fluid matrix, most biological membranes appear to be built with complex mixtures of lipid species, showing many variations in size and charge of the polar headgroups, in length and unsaturation of the paraffin chains, and in cholesterol content [1]. For a given membrane the lipid composition is characteristic, but between membranes with different functions, large differences in composition can be noticed. This raises the question whether such a complex lipid composition is a functional requirement and provokes the hypothesis that lipids contribute in more specific ways to membrane functions than by just forming a fluid impermeable matrix.