The Voyage Of The Beagle By Charles Darwin





































































 -   The Siberian
salt-lakes are inhabited by small crustaceous animals; and
flamingoes (Edin. New Philos. Jour., Jan 1830) likewise
frequent - Page 65
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The Siberian Salt-Lakes Are Inhabited By Small Crustaceous Animals; And Flamingoes (Edin.

New Philos.

Jour., Jan 1830) likewise frequent them. As these circumstances, apparently so trifling, occur in two distant continents, we may feel sure that they are the necessary results of a common cause - See Pallas's Travels, 1793 to 1794, pp. 129 - 134.

[5] I am bound to express in the strongest terms, my obligation to the government of Buenos Ayres for the obliging manner in which passports to all parts of the country were given me, as naturalist of the Beagle.

[6] This prophecy has turned out entirely and miserably wrong. 1845.

[7] Voyage dans l'Amerique Merid. par M. A. d'Orbigny. Part. Hist. tom. i. p. 664.

CHAPTER V

BAHIA BLANCA

Bahia Blanca - Geology - Numerous gigantic Quadrupeds - Recent Extinction - Longevity of species - Large Animals do not require a luxuriant vegetation - Southern Africa - Siberian Fossils - Two Species of Ostrich - Habits of Oven-bird - Armadilloes - Venomous Snake, Toad, Lizard - Hybernation of Animal - Habits of Sea-Pen - Indian Wars and Massacres - Arrow-head, antiquarian Relic.

The Beagle arrived here on the 24th of August, and a week afterwards sailed for the Plata. With Captain Fitz Roy's consent I was left behind, to travel by land to Buenos Ayres. I will here add some observations, which were made during this visit and on a previous occasion, when the Beagle was employed in surveying the harbour.

The plain, at the distance of a few miles from the coast, belongs to the great Pampean formation, which consists in part of a reddish clay, and in part of a highly calcareous marly rock. Nearer the coast there are some plains formed from the wreck of the upper plain, and from mud, gravel, and sand thrown up by the sea during the slow elevation of the land, of which elevation we have evidence in upraised beds of recent shells, and in rounded pebbles of pumice scattered over the country. At Punta Alta we have a section of one of these later-formed little plains, which is highly interesting from the number and extraordinary character of the remains of gigantic land-animals embedded in it. These have been fully described by Professor Owen, in the Zoology of the voyage of the Beagle, and are deposited in the College of Surgeons. I will here give only a brief outline of their nature.

First, parts of three heads and other bones of the Megatherium, the huge dimensions of which are expressed by its name. Secondly, the Megalonyx, a great allied animal. Thirdly, the Scelidotherium, also an allied animal, of which I obtained a nearly perfect skeleton. It must have been as large as a rhinoceros: in the structure of its head it comes according to Mr. Owen, nearest to the Cape Anteater, but in some other respects it approaches to the armadilloes. Fourthly, the Mylodon Darwinii, a closely related genus of little inferior size. Fifthly, another gigantic edental quadruped. Sixthly, a large animal, with an osseous coat in compartments, very like that of an armadillo.

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