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 the Miocene to the Pleistocene, and was also represented during the latter epoch in North America. It serves to connect the Bradypodidae with Myrmecophagidae. The alleged occurrence of an allied form in Madagascar is somewhat doubtful (see and ).

Of Dasypodidae numerous representatives occur in the South American Tertiaries. From the higher beds many of the species are referable to existing genera, such as Dasypus and Tatusia, although some are much larger than any living forms, the skull in one case being nearly a foot in length. In other instances, when lower formations are reached, the genera are also distinct, Eutatus having the whole armour divided into movable bands, and the allied Stegotherium representing the group in the Santa Cruz formation of Patagonia. Even in the Argentine Pleistocene there is an extinct genus, Chlamydotherium, represented by a species of the size of a rhinoceros, with grooved teeth approximating to those of the glyptodonts. The latter represent a family (Glyptodontidae) by themselves, and typically may be described as giant solid-shelled armadillos, although some of their smaller Santa Cruz representatives (Propalaeohoplophorus) approximate in some degree to true armadillos (see ).

A very remarkable Santa Cruz armadillo, Peltephilus, has an altogether peculiar type of head-shield, developed into horns in front of the eyes; and, what is still more noteworthy, teeth in the front of the jaws, thereby rendering the ordinary definition of the order Edentata incorrect. It has been made the type of a distinct family, Peltephilidae.

The past history of the armadillo group does not, however, by any means end here. True armadillos, it should be observed, are known in North America as far north as Texas, from the Pleistocene onwards; but in formations of middle Tertiary age are unrepresented. Recent discoveries apparently indicate, however, the occurrence of armadillos of a primitive type in the lower Tertiary or Eocene formations of Wyoming. The first evidence of these Eocene armadillos was afforded by portions of the jaws, which, together with a leg-bone of a totally different animal, were believed to indicate creatures nearly allied to the aye-aye (Chiromys) of Madagascar, and for which the name Metachiromys was consequently proposed. According to modern usage, this name, in spite of its inappropriate nature, is retained for the armadillos, although in the writer’s opinion it ought to be replaced. According to Professor H. F. Osborn, by whom their remains have been described, the North American fossil armadillos were closely related to the existing members of the group, from which they differ chiefly by the armour, or shield, having probably been formed of tough leathery skin instead of bony plates, by the presence of a single pair of large enamel-capped tusk-like teeth in each jaw, and by the degeneration of the other teeth. If these determinations are trustworthy, the question arises whether we should regard the armadillos of South America as the descendants of North American forms which migrated southwards before that separation of the two continents was established, which lasted for a large portion of the Tertiary period, or whether a migration took place at the same early epoch in the opposite direction.

More interesting still is the occurrence of remains of reputed armadillos (Necrodasypus) from the Oligocene of France and Germany. In the opinion of Dr F. Ameghino these Oligocene armadillos, which had bony shields on both the head and body, were near akin to some of the modern South American forms.

Passing on to the aard-varks (Orycteropodidae), we find these represented by a species closely allied to the existing ones in the Lower Pliocene formations of Spain, France, Hungary, Samos and Asia Minor. A single tibia from the French Oligocene is identified by Dr Ameghino with the present family, and the genus Archaeorycteropus established for its reception; this genus, in its founder’s opinion, being also represented in the Santa Cruz beds of Patagonia. As regards the pangolins, the only fossils referred to this group (apart from a few discovered in a cave in India) appear to be certain limb-bones from the Oligocene of France and Germany, for which the names Necromanis and Teutomanis have been proposed. The occurrence of the characteristic cleft terminal toe-bones among these remains seems to leave little doubt as to the correctness of the determination.

The alleged occurrence of remains of giant pangolins in the upper Tertiary of Europe is due to misidentification (see ). By some authorities the Eocene group of Ganodonta has been affiliated to the Edentata, but this reference is not accepted by Prof. W. B. Scott.

 EDENTON, a town and the county-seat of Chowan county, North Carolina, U.S.A., on Edenton Bay, an estuary of Albemarle sound, near the mouth of Chowan river, in the N.E. part of the state. Pop. (1890) 2205; (1900) 3046 (2090 negroes); (1910) 2789. It is served by the Norfolk & Southern railway, and by the Albemarle Steam Navigation Co. In 1907 the former projected a great bridge across Albemarle sound near the city. Edenton is an old and interesting town, has a number of fine old homesteads, and has broad and well-shaded streets. Lumbering and the shad and herring fisheries are the most important industrial interests, and the town is a shipping point for fish, truck and other farm products, cotton and peanuts. There is a Fish Cultural Station here, established by the Federal government. The court-house was built about 1750.

Edenton was settled about 1658, and was for some time known as the “Towne on Queen Anne’s Creek” or the “Port of Roanoke”; in 1722 the present name was adopted in honour of Governor Charles Eden (1673–1722), whose grave is in St Paul’s churchyard here. Throughout the 18th century Edenton was a place of considerable social and political importance; the legislative assembly of North Carolina met here occasionally, and here lived the royal governors and various well-known citizens of the province, among them: Joseph Hewes (1730–1779), a signer of the Declaration of Independence; James Iredell, Sr. (1750–1799), a Federalist leader and after 1790 a justice of the United States Supreme Court, and his son James Iredell, Jr. (1788–1853), a prominent lawyer, for many years a member of the state legislature, governor of North Carolina in 1827–1828, and a member of the United States Senate in 1828–1831. Near Edenton lived Samuel Johnston (1733–1816), a prominent leader of the American Whigs preceding and during the War of American Independence, a member of the Continental Congress in 1780–1782, governor of North Carolina in 1787–1789, and a Federalist member of the United States Senate in 1790–1793. In 1907 the Hewes, Iredell and Johnston homesteads were still standing. In a house facing the court-house green the famous “Edenton Tea Party” of fifty-one ladies met on the 24th of October 1774 and signed resolutions that they would not conform “to that Pernicious Custom of Drinking Tea” and would not “promote the wear of any manufacture from England” until the tax on tea should be repealed. Near Edenton the Confederate ram “Albemarle,” on emerging from the Roanoke river, was met by the Union “double-enders,” “Sassacus,” “Mattabesett,” and “Miami,” on the 5th of May 1864; the battle, which resulted in favour of the Confederates, was a duel between the Confederate ironclad and the Union wooden side-wheeler, the “Sassacus,” which rammed the “Albemarle” and had her bows, fitted with a three-ton bronze beak, twisted off and carried away.

 EDESSA (mod. Vodena), the ancient capital of Macedonia, previously known as Aegae, situated 46 m. W. of Thessalonica