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Encyclopedia Britannica - Main :: PER-PIG |
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PHENACODUS , one of the earliest and most primitive of the ungulate mammals, typifying the family Phenacodontidae and the sub-order Condylarthra. The typical Phenacodus primaevus, of the Lower or Wasatch Eocene of North America, was a relatively small ungulate, of slight build, with straight limbs each terminating in five complete toes, and walking in the digitigrade fashion of the modern tapir. The middle toe was the largest, and the weight
body
extinct
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series of forty
In the Puerco, or Lowest Eocene of North America the place of the above species was taken by Euprotogonia puercensis, an animal only half the size of Phenacodus primaevus, with the terminal joints of the limbs intermediate between hoofs and claws, and the first and fifth toes taking their full share in the support of the weight
body
As ancestors of the Artiodactyle section of the Ungulata, we may look to forms more or less closely related to the North American Lower Eocene genera Mioclaenus and Pantolestes, respectively typifying the families Mioclaenidae and Pantolestidae. They were five-toed, bunodont Condylarthra, with a decided approximation to the perissodactyle type in the structure of the feet. A third type of Condylarthra from the North American Lower Eocene is represented by the family Meniscotheriidae, including the genera Meniscotherium and Hyracops. These, it is suggested, may have been related to the ancestral Hyracoidea. Teeth and jaws probably referable to the Condylarthra have been obtained in European early Tertiary formations. All Ungulata probably originated from Condylarthra. See H. F. Osborn, Skeleton of Phenacodus primaevus; comparison with Euprotogonia, Bull . Amer. Mus. x. 159. (R. L.*) PHENANTHRENE, C14HIo, a hydrocarbon isomeric with anthracene, with which it occurs in the fraction of the coal tar distillate boiling between 2700400 C. It may be separated from the anthracene oil by repeated fractional distillation
condition of phenanthrene in alcoholic solution see R. Behrend, Zeit. phys. Chem., 1892, 9, p. 405; 10, p. 265. Chromic acid oxidizes phenanthrene, first to phenanthre..;:-4uinone, and then to diphenic acid, HO2CC6H4C6H4CO2H.Phenanthrene-quinone, [C6H412[CO]2, crystallizes in orange needles which melt at 1980 C. It possesses the characteristic properties of a diketone, forming crystalline derivatives with sodium bisulphite and a dioxime with hydroxylamine
On the constitution of phenanthrene see CHEMISTRY: Organic. End of Article: PHENACODUS If you wish, you can link directly to this article.
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