A novel strictly anaerobic bacterium designated strain SSD-17BT was isolated from the hypersaline brinesediment interface of the Shaban Deep, Red Sea. Cells were pleomorphic but usually consisted of a central coccoid body with one or two "tentacle-like" protrusions. These protrusions actively alternated between a straight, relaxed form and a contracted, corkscrew-like one. A peptidoglycan layer was not detected by electron microscopy. The organism forms "fried-egg"-like colonies on MM-X medium. The organism is strictly anaerobic and halophilic and has an optimum temperature for growth of about 30 to 37°C and an optimum pH of about 7. Nitrate and nitrite are reduced; lactate is a fermentation product. The fatty acid profile is dominated by straight saturated and unsaturated chain compounds. Menaquinone 4 is the major respiratory quinone. Phylogenetic analysis demonstrated strain SSD-17B T represents a novel and distinct lineage within the radiation of the domain Bacteria. The branching position of strain SSD-17BT was equidistant to the taxa considered to be representative lineages of the phyla Firmicutes and Tenericutes (with its sole class Mollicutes). The phenotypic and phylogenetic data clearly show the distinctiveness of this unusual bacterium, and we therefore propose that strain SSD-17BT ؍( DSM 18853 ؍ JCM 14575) represents a new genus and a new species, for which we recommend the name Haloplasma contractile gen. nov., sp. nov. We are also of the opinion that the organism represents a new order-level taxon, for which we propose the name Haloplasmatales.The divergent movement of the African and Arabian tectonic plates, which is associated with deposition of new oceanic crust, led to the formation of several isolated topographical depressions within the Red Sea basin (4). Redissolution of buried Miocenic evaporites and/or hydrothermal phase separation, followed by upward migration to the seafloor and later accumulation in enclosed depressions, filled as many as 25 such deeps with highly saline water (13,15). In addition to their common extreme salinity (up to 27% [wt/vol] NaCl), all of these brines are anoxic, are enriched in metals and hydrocarbons, and have temperatures higher than 21.7°C, which is the mean deep-seawater temperature of the Red Sea (13, 29).The brine-filled deeps of the Red Sea represent a rare type of extreme environment and were considered to be sterile as recently as the late 1960s (34). Few studies have focused on the microbiology of these biotopes, resulting in only a few microbial isolates (1, 2, 10). Phylogenetic studies have, however, revealed an unexpectedly high microbial diversity (10, 11). Parallel studies, focusing on the microbiology of analogous deep-sea brines located in the eastern Mediterranean Sea further corroborate the extensive microbiological diversity in such biotopes (8).Samples for geochemical and microbiological studies were retrieved from the northernmost brine-filled deeps of the Red Sea during the RV Meteor Cruise 52/3 in 2002. Isolation attempts with a samp...