THE presence of common salt in water, in any considerable quantity, renders it unfit for the development of the eggs and larvae of amphibians. Marine waters have consequently proved a strong barrier to the distribution of this group of animals. A very few amphibians have eggs and larvae capable of development in waters having some quantity of sodium chloride in solution, while many species appear to develop in alkaline waters of varying concentration. A. S. Pearse (1911) found tadpoles in water in crab holes which were covered daily by the tide water from Manila Bay. In consequence the water had a fairly strong salt concentration. Pearse does not mention the species, but I presume it to be Rana moodiei Taylor, since I have found its tadpoles near Manila, in brackish water in crab holes, though above the tidemark. On one occasion I captured an adult on the edge of the beach, from under a piece of coral, where it sat partially submerged. One might suspect that certain species with a wide archipelagic distribution might be more tolerant of sodium chloride concentrations than continental forms. The presence of larval newts in brackish water was recently reported in England (Spurway, 1943, and Hardy, 1943). Weismann (1878) was under the impression that the habitat of Siredon mexicana is brackish water. I believe that this is an error, since both Lake Xochomilco and Chalco are fresh water lakes (Chalco is now almost entirely drained and cultivated). It is true that there are bodies of brackish water in the Valle de Mexico but Siredon mexicana is not to be found in them. I do not believe any of these bodies of brackish water have other ambystomids. The discovery by Mr. Dyfrig McHattie Forbes of a salamander living in the saline waters of Lake Alchichica, Puebla, Mexico, is thus of especial interest and importance. It proves to be a species differing from other known forms, and is described below. Laguna Alchichica is one of a series of three small lakes in the high plateau region lying to the northwest of the great volcano Citlaltepetl (Orizaba). The region about them is flat and all seem to have been formed by a sinking of the surface crust. They do not seem to be crater lakes. The lakes differ in level, in the salt content of their waters, and in their fauna and flora. The actual depth of the water is not known in any of them. Laguna Quecholac and Laguna de la Mina Preciosa contain potable fresh water. They support a heavy growth of rushes about their edges, with many algae in the water. Each lake has, at least, one species of fish, and one salamander. Laguna Alchichica, with water distinctly salty to the taste, has no fresh water rushes or algae, and only submerged seaweedlike plants were observed, growing on rocks. There is a single species of fish,1 and the salamander here described.
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