The order Thermoplasmales includes the wall-less strains in the Archaea. The genus Thermoplasma (two species), the genus Picrophilus (two species), and the genus Ferroplasma (one species) are present. The strains of Thermoplasma include the thermophilic acidophile (T. acidophilum grows between 45 and 62 , optimum 59 , pH 1~4, optimum 1~2 (1); T. volucanium does between 33 and 67 , optimum 60 , pH 1~4, optimum 2 (2)) and the cells are surrounded by a single triple-layer membrane, 5~10 nm thick. The family Picrophilaceae is the thermophilic hyperacidophile growing between 47 and 65 and between pH 0 and 3.5. This family is separated from the family Thermoplasmaceae based on their base sequence of the 16S rRNA gene, DNA-dependent RNA polymerase, and the presence of an S-layer (3). In contrast to these families, the family Ferroplasmaceae, also a wall-less Eur-yarchaeon, grows in the quite different temperature range between 15 and 45 , optimum 35 , pH 1.3~2.2, optimum 1.7 (4). Among these wall-less representatives, only the structure of the membrane lipids of T. acidophilum has been well investigated. The structure of the main membrane lipids of T. acidophilum is caldarchaeol (2, 2 , 3, 3-tetra-O-di(biphytanyl)-sn-diglycerol) (5, 6), one of the ether core lipids of the archaeal strains. Five types of molecular species of the C 40 isoprenoid chain, classified by the number of cyclopentane rings, have been detected in the caldarchaeol of the extreme thermophilic Crenarchaeon such as Sulfolobus solfataricus. These are acyclic-, monocyclic-, bicyclic-, tricyclic-, and tetracyclic-C 40 isoprenoid chains (7). It has been observed that a decrease in the number of double bond in the membrane depends on lowering the environmental temperature for controlling the membrane fluidity in Eucarya and Bacteria. In S. solfataricus, it has been