probably a mere variety of one of the others, and Elephas priscus of Goldfuss, founded partly on specimens of the African elephant, assumed by mistake to be fossil, and partly on some aberrant forms of E. antiquus.
The first effect of the intercalation of so many intermediate forms between the two most divergent types, has been to break down almost entirely the generic distinction between Mastodon and Elephant. Dr. Falconer, indeed, observes that Stegodon (one of several subgenera which he has founded) constitutes an intermediate group, from which the other species diverge through their dental characters, on the one side into the Mastodons, and on the other into the Elephants.[1] The next result is to diminish the distance between the several members of each of these groups.
Dr. Falconer has discovered that no less than four species of elephant were formerly confounded together under the title of Elephas primigenius, whence its supposed ubiquity in post-pliocene times, or its wide range over half the habitable globe. But even when this form has been thus restricted in its specific characters, it has still its geographical varieties; for the mammoth's teeth brought from America may in most instances, according to Dr. Falconer, be distinguished from those proper to Europe. On this American variety Dr. Leidy has conferred the name of E. Americanus. Another race of the same mammoth (as determined by Dr. Falconer) existed, as we have seen, before the glacial period, or at the time when the buried forest of Cromer and the Norfolk cliffs (see above, p. 216) was deposited; and the Swiss geologists have lately found remains of the mammoth in their country, both in pre-glacial and post-glacial formations.
Since the publication of Dr. Falconer's monograph, two other
- ↑ Geological Quarterly Journal, vol. xiii. p. 314, 1857.
