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The Voyage of the Beagle

Charles Darwin · 1831-1836 (journal of the voyage; later edited/condensed for publication) primary

passage 104 of 397 · CHAPTER I > CHAPTER VII (6/15)

in brief
From the Bajada area opposite St. Fe, Darwin crosses the Paraná, studies geology at cliff bases and the Pampas sequence of estuary deposits, and uses microscopic infusoria evidence to argue ancient brackish water conditions during Pampas elevation.

was brackish. Below Buenos Ayres there are upraised beds of sea-shells of existing species, which also proves that the period of elevation of the Pampas was within the recent period.

In the Pampaean deposit at the Bajada I found the osseous armour of a gigantic armadillo-like animal, the inside of which, when the earth was removed, was like a great cauldron; I found also teeth of the Toxodon and Mastodon, and one tooth of a Horse, in the same stained and decayed state. This latter tooth greatly interested me, [3] and I took scrupulous care in ascertaining that it had been embedded contemporaneously with the other remains; for I was not then aware that amongst the fossils from Bahia Blanca there was a horse's tooth hidden in the matrix: nor was it then known with certainty that the remains of horses are common in North America. Mr. Lyell has lately brought from the United States a tooth of a horse; and it is an interesting fact, that Professor Owen could find in no species, either fossil or recent, a slight but peculiar curvature characterizing it, until he thought of comparing it with my specimen found here: he has named this American horse Equus curvidens. Certainly it is a marvellous fact in the history of the Mammalia, that in South America a native horse should have lived and disappeared, to be succeeded in after-ages by the countless herds descended from the few introduced with the Spanish colonists!

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topics: the earth and its formation · weather, storms, and the seasons

The Voyage of the Beagle · Charles Darwin · 1831–1836