Abstract

The membranes of extremely halophilic Archaea are characterized by the abundance of a diacidic phospholipid, archaetidylglycerol methylphosphate (PGP-Me), which accounts for 50-80 mol% of the polar lipids, and by the absence of phospholipids with choline, ethanolamine, inositol, and serine head groups. These membranes are stable in concentrated 3-5 m NaCl solutions, whereas membranes of non-halophilic Archaea, which do not contain PGP-Me, are unstable and leaky under such conditions. By x-ray diffraction and vesicle permeability measurements, we demonstrate that PGP-Me contributes in an essential way to membrane stability in hypersaline environments. Large unilamellar vesicles (LUV) prepared from the polar lipids of extreme halophiles, Halobacterium halobium and Halobacterium salinarum, retain entrapped carboxyfluorescein and resist aggregation in the whole range 0-4 m NaCl, similarly to LUV prepared from purified PGP-Me. By contrast, LUV made of polar lipid extracts from moderately halophilic and non-halophilic Archaea (Methanococcus jannaschii, Methanosarcina mazei, Methanobrevibacter smithii) are leaky and aggregate at high salt concentrations. However, adding PGP-Me to M. mazei lipids results in gradual enhancement of LUV stability, correlating with the PGP-Me content. The LUV data are substantiated by the x-ray results, which show that H. halobium and M. mazei lipids have dissimilar phase behavior and form different structures at high NaCl concentrations. H. halobium lipids maintain an expanded lamellar structure with spacing of 8.5-9 nm, which is stable up to at least 100 degrees C in 2 m NaCl and up to approximately 60 degrees C in 4 m NaCl. However, M. mazei lipids form non-lamellar structures, represented by the Pn3m cubic phase and the inverted hexagonal H(II) phase. From these data, the forces preventing membrane aggregation in halophilic Archaea appear to be steric repulsion, because of the large head group of PGP-Me, or possibly out-of-plane bilayer undulations, rather than electrostatic repulsion attributed to the doubly charged PGP-Me head group.

Highlights

  • To elucidate the role of PGP-Me, we performed a comparative study on the stability of large unilamellar vesicles (LUV) made of polar lipid extracts from several archaeal strains including extreme halophiles, moderate halophiles, and non-halophiles, which strongly differ by PGP-Me content (Table 1)

  • Because our aim was to elucidate the effect of PGP-Me on the membrane stability, we compared the properties of LUV made of polar lipid extracts from extremely halophilic, moderately halophilic, and non-halophilic Archaea, which strongly differ by PGP-Me content

  • The CF leakage is minimal for LUV prepared from the polar lipids of the extreme halophiles H. halobium and H. salinarum, which have highest PGP-Me content, as well as for LUV prepared from purified PGP-Me

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Summary

Introduction

To elucidate the role of PGP-Me, we performed a comparative study on the stability of large unilamellar vesicles (LUV) made of polar lipid extracts from several archaeal strains including extreme halophiles, moderate halophiles, and non-halophiles, which strongly differ by PGP-Me content (Table 1). H. halobium lipids, typified by a very high PGP-Me content of ϳ78% (Table 1), maintained an expanded lamellar structure stable up to least 4 M NaCl in broad temperature ranges about the physiological temperatures, whereas M. mazei lipids, which have no PGP-Me, formed non-lamellar structures, represented by the Pn3m cubic phase and the inverted hexagonal HII phase, at high NaCl concentrations In this way, both the LUV and the x-ray diffraction data sets consistently demonstrate a critical role of PGP-Me for the bilayer stabilization in hypersaline environments

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