Akihiko Sugai

Variation in molecular species of polar lipids from Thermoplasma acidophilum depends on growth temperature

Five types of molecular species of C40 isoprenoid chains, having different numbers of cyclopentane rings, were detected in the ether core lipid of Thermoplasma acidophilum. The average cyclization number of the hydrocarbon chains in the lipids increased with increasing growth temperatures.

Sulfurisphaera ohwakuensis gen. nov., sp. nov., a novel extremely thermophilic acidophile of the order Sulfolobales

Three spherical thermoacidophilic archaea (strains TA-1T, TA-13, TA-14) were obtained from acidic hot springs located in Ohwaku Valley, Hakone, Japan. All the isolates are facultatively anaerobic, and grew optimally at around 85 degrees C, pH 2.0. Isolate TA-1T was characterized further. The G + C content of DNA from TA-1T is 33 mol%. Although these properties resemble those of the genus Acidianus, the sequence of the 16S rRNA gene from strain TA-1T was more similar to that of species of Stygiolobus than of Acidianus. DNA-DNA hybridization experiments also indicated that strain TA-1T is clearly distinguished phylogenetically from the members of Acidianus, Sulfolobus and Metallosphaera. On the basis of the distinct physiological and molecular properties, we describe the new strains as members of the new genus Sulfurisphaera. The type species of the genus is Sulfurisphaera ohwakuensis, and the type strain of the species is TA-1T (= IFO 15161T).

The structure of the core polyol of the ether lipids fromSulfolobus acidocaldarius

The major ether-type lipid structures ofSulfolobus acidocaldarius (ATCC33909) were composed of caldarchaeol and calditoglycerocaldarchaeol. However, the characterization by nuclear magnetic resonance spectroscopy and mass spectrometry showed that the structure of calditol in calditoglycerocaldarchaeol is not nonitol, 2-(1′,2′,3′-trihydroxypropyl)1,2,3,4,5,6-hexahydroxyhexane, but 2-hydroxymethyl-1-(2,3-dihydroxypropoxy),2,3,4,5-cyclopentanetetraol with an ether linkage in the molecule. Such an intermolecular ether linkage was resistant, to BCl3 treatment, but nonresistant to 57% HI degradation treatment conducted at 100°C for 60 h, producting 2-hydroxymethyl-1,2,3,4,5-cyclopentanepentaol from calditol as reaction product. Further, it was confirmed that the structure of calditol is essentially a derivative of glycerol, and hydrocarbon chains were conjugated to the glycerol-like site in the structure. The calditol with an ether linkage in the molecule suggested an important role regarding the properties of heat-resistance and acid-resistance observed inSulfolobales.

Sulfolobus hakonensis sp. nov., a Novel Species of Acidothermophilic Archaeon

We characterized a microbial strain that was isolated from a hot spring at a geothermal area in Hakone, Japan. This isolate, whose lobed-shaped cells were about 1.0 micron in diameter, was a facultative chemolitho-autotroph that required aerobic conditions for growth. The optimum pH was 3.0 (pH range, 1.0 to 4.0), and the optimum temperature was 70 degrees C (temperature range, 50 to 80 degrees C). Lithotrophically, this strain grew on elemental sulfur and reduced sulfur compounds. The G+C content of the genomic DNA was 38.4 mol%. This organism contained calditoglycerocaldarchaeol, which is characteristic of members of the Sulfolobaceae. The levels of 16S rRNA sequence similarity between the new isolate and Sulfolobus acidocaldarius, Sulfolobus solfataricus, and Sulfolobus shibatae were less than 89.8%. Unlike S. acidocaldarius, S. solfataricus, and S. shibatae, the new isolate utilized sugars and amino acids poorly as sole carbon sources, and the levels of DNA-DNA hybridization between the new isolate and these Sulfolobus species were very low. Phenotypically, the new isolate was also distinct from the obligately lithotrophic organism Sulfolobus metallicus. We concluded that the new organism belongs to a new Sulfolobus species, for which we propose the name Sulfolobus hakonensis.

Effect of Growth Temperature and Growth Phase on the Lipid Composition of the Archaeal Membrane from Thermococcus kodakaraensis

Archaea have unique membrane lipids typified by ether linkages of the glycerol-to-isoprenoid chains with sn-2,3 stereochemistry that runs against the naturally occurring sn-1,2 stereochemistry of the glycerophospholipids of Bacteria and Eukarya. Membrane lipids were extracted and analyzed from the hyperthermophilic archaeon, Thermococcus kodakaraensis, cultivated at various temperatures. At all growth temperatures examined, both the diphytanylglycerol diether (archaeol, C20) and diphytanyldiglycerol tetraether (caldarchaeol, C40) were identified as saturated forms, and no other lipids could be identified. The ratio of caldarchaeol to archaeol increased with increasing growth temperature, particularly at 93 °C. A larger amount of archaeol was detected from cells in the logarithmic phase than from those in the stationary phase at all temperatures examined. These results indicate that T. kodakaraensis modulated the membrane lipid composition depending on both the growth phase and the growth temperature, and suggest that the membrane fluidity to environmental change was maintained by altering the length of the hydrocarbon chains, and not by side-chain saturation such as double-bond hydrogenation nor by such a modification as cyclopentane ring formation.

Isolation and Characterization of Novel Neutral Glycolipids from Thermoplasma acidophilum

Several novel neutral glycolipids (GL-1a, GL-1b, GL-2a, GL-2b and GL-2c) were isolated from Thermoplasma acidophilum by high-performance liquid chromatography using phenylboronic acid-silica and preparative thin-layer chromatography. The tentative structures of these lipids were characterized by the combination of gas-liquid chromatography, the methylation procedure, and (1)H-NMR and FAB-mass spectrometries. The lipophilic portion of the neutral glycolipids was composed of a simple molecular species named caldarchaeol (dibiphytanyl-diglycerol tetraether). The sugar moieties of these glycolipids were composed of gulose and glucose which formed monosaccharide residues on one side or both sides of the core lipids. Gulose was attached to the terminal glycerol OH group of the core lipid with a beta-configuration and glucose being attached with an alpha-configuration. The proposed structure of GL-1a was gulosylcaldarchaeol and that of GL-1b was glucosylcaldarchaeol. The structures of GL-2a, GL-2b, and GL-2c were the analogs of the caldarchaeol derivatives attached by a variety of gulosyl residues or glucosyl residues on both sides of the terminal OH groups.

The evolution of lipids.

Living organisms on the Earth which are divided into three major domains--Archaea, Bacteria, and Eucarya, probably came from a common ancestral cell. Because there are many thermophilic microorganisms near the root of the universal phylogenetic tree, the common ancestral cell should be considered to be a thermophilic microorganism. The existence of a cell is necessary for the living organisms; the cell membrane is the essential structural component of a cell, so its amphiphilic property is vital for the molecule of lipids for cell membranes. Tetraether type glycerophospholipids with C40 isoprenoid chains are major membrane lipids widely distributed in archaeal cells. Cyclization number of C40 isoprenoid chains in thermophilic archaea influences the fluidity of lipids whereas the number of carbons and degree of unsaturation in fatty acids do so in bacteria and eucarya. In addition to the cyclization of the tetraether lipids, covalent bonding of two C40 isoprenoid chains was found in hyperthermophiles. These characteristic structures of the lipids seem to contribute to their fundamental physiological roles in hyperthermophiles. Stereochemical differences between G-1-P archaeal lipids and G-3-P bacterial and eucaryal lipids might have occurred by the function of some proteins long after the first cell was developed by the reactions of small organic molecules. We propose that the structure of lipids of the common ancestral cell may have been similar to those of hyperthermophilic archaea.

Glucosylcaldarchaetidylglycerol, a Minor Phosphoglycolipid from Thermoplasma acidophilum

A novel phosphoglycolipid (GPL-K) was isolated from Thermoplasma acidophilum (ATCC 27658). The chemical components of GPL-K were analyzed by gas liquid chromatography and GC-MS. The sugar moiety of GPL-K and its anomeric region were analyzed by NMR assignment. The core lipid of GPL-K was caldarchaeol, and its main hydrocarbon chains were acyclic and monocyclic C(40) biphytanyl. The polar head groups were alpha-glucose and glycerophosphate. The negative FAB-MS spectrum of GPL-K confirmed that the lipid peak of m/z 1614 consists of a caldarchaeol (including one cyclopentane ring), a hexose sugar, and a glycerophosphate. We have proposed the tentative structure of GPL-K.

Thermosipho globiformans sp. nov., an anaerobic thermophilic bacterium that transforms into multicellular spheroids with a defect in peptidoglycan formation

An anaerobic rod-shaped thermophile was isolated from a hydrothermal vent at Suiyo Seamount, Izu-Bonin Arc, western Pacific Ocean, and was named strain MN14(T). The rods were gram-negative-staining, non-motile without flagella, 2-4 µm long and 0.5 µm wide, and divided by binary fission in the mid-exponential phase. The cells were surrounded by a sheath-like structure (toga) and occurred singly or in chains. Spheroids containing multiple cells were observed not only in the stationary phase, as previously observed for species of the order Thermotogales, but also from the early exponential phase. Transmission electron microscopy revealed that the peptidoglycan in rods partly disintegrated in the early growth phases and that the outer membrane of the spheroids was not completely lined with peptidoglycan. These findings suggested that the spheroids were formed from rods by the disintegration of peptidoglycan and subsequent inflation of the outer membrane. The spheroids eventually generated tiny cells in the periplasmic space, indicating a viviparous mode of proliferation in addition to binary fission. Strain MN14(T) grew at 40-75 °C, pH 5.0-8.2 and with 0.25-5.20 % (w/v) NaCl, with optimal growth occurring at 68 °C, pH 6.8 and with 2.5 % NaCl. The shortest doubling time was 24 min, assuming that the strain propagated only by binary fission. Elemental sulfur enhanced growth, but was not essential. Thiosulfate was not an electron acceptor for growth. The strain was a chemo-organotroph that grew on yeast extract as the sole growth substrate. Tryptone and starch supported its growth in the presence of yeast extract. The G+C content of the genomic DNA was 31.7 mol%. Phylogenetic analysis based on the 16S rRNA gene sequence indicated that this strain belonged to the genus Thermosipho. No significant DNA-DNA hybridization was observed between the genomic DNA of strain MN14(T) and phylogenetically related species of the genus Thermosipho. Based on this evidence, strain MN14(T) is proposed to represent a novel species, named Thermosipho globiformans sp. nov. The species epithet globiformans reflects the formation of multicellular and reproductive spheroids by the novel strain. The type strain of this species is MN14(T) ( = JCM 15059(T) = DSM 19918(T)).

Characterization of caldarchaetidylglycerol analogs, dialkyl-type and trialkyl-type, from Thermoplasma acidophilum

The structures of three kinds of phospholipids (PL-X, PL-Y, and PL-T) isolated from Thermoplasma acid-ophilum have been characterized. The core lipid of PL-Y was caldarchaeol, and that of PL-X was archaeol. The composition of the hydrocarbon chains of the PL-T core lipid was C20 phytane and C40 isoprenoid in a molar ratio of 2 to 1. The major molecular species of the C40 isoprenoid was acyclic without the cyclopentane ring. These three kinds of intact phospholipids commonly had glycerophosphate residues as polar head groups. The structure of PL-T was characterized as trialkyl-type caldarchaetidylglycerol, PL-Y as caldarchaetidylglycerol, and PL-X as archaetidylglycerol.