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The Phrynosomatidae are a diverse family of lizards, sometimes classified as a subfamily (Phrynosomatinae), found from Panama to the extreme south of Canada.Many members of the group are adapted to life in hot, sandy deserts, although the spiny lizards prefer rocky deserts or even relatively moist forest edges, and the short-horned lizard lives in prairie or sagebrush environments.
Tropidosaura montana, also known commonly as the common mountain lizard and the green-striped mountain lizard, is a species of lizard in the family Lacertidae. The species is endemic to South Africa .
The Italian three-toed skink or the cylindrical skink (Chalcides chalcides) is a species of lizard found from Italy (including Sicily, Sardinia and Elba), to northern Algeria, Libya, Morocco and Tunisia and in india.
The "rock-paper-scissors" mating strategy is a genetically-based male polymorphism that has been maintained over millions of years throughout many populations of side-blotched lizard in the United States and Mexico. However, speciation has resulted from the formation of reproductive isolation between populations when a population loses of one ...
Pedioplanis lineoocellata, known commonly as the common sand lizard, the ocellated sand lizard, and the spotted sand lizard, is a species of lizard in the family Lacertidae. The species is endemic to Southern Africa. There are three recognized subspecies.
The smooth helmeted iguana is a medium-sized lizard with long slim legs and very long toes. It can be grey, olive, brown, black or reddish-brown with irregular blotches. [6] The smooth helmeted iguana can change the color of its skin as a method of camouflage. As indicated by its name, the smooth helmeted iguana has a prominent crest on its ...
Print/export Download as PDF; Printable version; In other projects ... The Herero girdled lizard (Namazonurus pustulatus) is a species of small, spiny lizard in the ...
Obamadon is known from two lower jaw fragments, each less than a centimeter in length. One was found in the collections of the University of California Museum of Paleontology after having been collected from the Hell Creek Formation in Montana, and the other collected from the Lance Formation in Wyoming.