Hydrotherosaurus

The first remains of Hydrotherosaurus to be found were several vertebrae discovered by Frank C. Paiva on his own property in the Panoche Hills of Fresno County, California, which were taken to Berkeley in the spring of 1937 by W. M. Tucker, who was the Chairman of the Department of Geology of Fresno State College. Afterwards, Fresno State College and the University of California Museum of Paleontology organized a joint expedition which would uncover a nearly complete fossilized skeleton of the animal, with only parts of the skull, shoulder girdle, flippers and certain vertebral elements missing. This specimen, designated UCMP 33912, was collected in a ravine on the property of the Sun Ray Gypsum Mine, about 22 miles west of Mendota, California, and the deposits from which it originates are part of the Moreno Formation. then at the University of California Berkeley, where it remained until being put into storage in the 1960s. In 1943, American paleontologist Samuel Paul Welles found that the specimen was notably different from other known plesiosaurs and declared it as the type specimen of a new genus and species which he named Hydrotherosaurus alexandrae. The generic name means "fisherman lizard", while the specific name honors Annie Montague Alexander, who has done plenty of research on the vertebrates of the western United States. ==Description==

Hydrotherosaurus was a medium-sized plesiosaur, with an estimated body length of long and body mass of around . It has one of the longest necks relative to total length among elasmosaurids, with 60 vertebrae in total. It had a small head that measured about long, a streamlined body, and four large flippers that were specially designed to help the huge animal balance, move, and accelerate itself. ==Classification==

The following cladogram shows the phylogenetic position of Hydrotherosaurus within Elasmosauridae: }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} }} ==See also==