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Additional info for Adaptation to Life at High Salt Concentrations in Archaea, Bacteria, and Eukarya (Cellular Origin, Life in Extreme Habitats and Astrobiology) (Cellular ... Life in Extreme Habitats and Astrobiology)
2. Chemical and Physical Properties of the Dead Sea The Dead Sea is a terminal desert lake. Its water level is the lowest exposed surface on Earth and is currently 417 m below sea level. At its deepest place, the lake is over 300 meters deep. Its main source of water input was the river Jordan. With a total dissolved salt content of about 342 g l-1, the Dead Sea is one of the most hypersaline environments on Earth. The unique ionic composition of its waters is dominated by divalent cations. 21 M K+.
89-96. , Ventosa, A. H. (1996). Halobacillus gen. , with descriptions of Halobacillus litoralis sp. nov. and Halobacillus trueperi sp. , and transfer of Sporosarcina halophila to Halobacillus halophilus comb. nov. Int. J. Syst. Bacteriol. 46, 492-496. W. (1997) Changes in lake levels, salinity and the biological community of Great Salt Lake (Utah, USA), 1847-1987. Hydrobiologia 197, 139-146. W. M. (1976) Phytoplankton production in the Great Salt Lake, Utah, and a laboratory study of algal response to enrichment.
A. System. Appl. Microbiol. 11, 94-96. D. J. (1990) A chemotaxonomic study of member of the family Halomonadaceae. System. Appl. Microbiol. 13, 142-147. W. ) (2002) Great Salt Lake, An Overview of Change. Special Publication of the Utah Department of Natural Resources, Salt Lake City, Utah. T. (1981) Primary production in saline lakes. A review. Hydrobiolgia 81, 47-57. R. G. (1993) The Great Salt Lake. General Interest Publications of the U. S. Geological Survey. Salt Lake City, Utah, USA, 24 pp.