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sistibly hurried into the belief of some great catastrophe; but
thus to destroy animals, both large and small, in Southern Pata-
gonia, in Brazil, on the Cordillera of Peru, in North America
up to Behring's Straits, we must shake the entire framework of
the globe
An examination, moreover, of the geology of La
Plata and Patagonia, leads to the belief that all the features of
the land result from slow and gradual changes. It appears from
the character of the fossils in Europe, Asia, Australia, and in
North and South America, that those conditions which favour
the life of the larger quadrupeds were lately co-extensive with
the world: what those conditions were, no one has yet even
conjectured. It could hardly have been a change of tempera-
ture, which at about the same time destroyed the inhabitants of
tropical, temperate, and arctic latitudes on both sides of the
globe. In North America we positively know from Mr. Lyell,
that the large quadrupeds lived subsequently to that period, when
boulders were brought into latitudes at which icebergs now never
arrive from conclusive but indirect reasons we may feel sure,
that in the southern hemisphere the Macrauchenia, also, lived
long subsequently to the ice-transporting boulder-period. Did
man, after his first inroad into South America, destroy, as has
been suggested, the unwieldy Megatherium and the other Eden-
tata? We must at least look to some other cause for the destruc-
tion of the little tucutuco at Bahia Blanca, and of the many
fossil mice and other small quadrupeds in Brazil. No one
will imagine that a drought, even far severer than those which
cause such losses in the provinces of La Plata, could destroy
every individual of every species from Southern Patagonia to
Behring's Straits. What shall we say of the extinction of the
horse? Did those plains fail of pasture, which have since been
overrun by thousands and hundreds of thousands of the descend-
ants of the stock introduced by the Spaniards? Have the subse-
quently introduced species consumed the food of the great ante-
cedent races? Can we believe that the Capybara has taken the
food of the Toxodon, the Guanaco of the Macrauchenia, the ex-
isting small Edentata of their numerous gigantic prototypes?
Certainly, no fact in the long history of the world is so startling
as the wide and repeated exterminations of its inhabitants.
Nevertheless, if we consider the subject under another point of

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1834.]

CAUSES OF EXTINCTION.

176

view, it will appear less perplexing. We do not steadily bear in mind, how profoundly ignorant we are of the conditions of exist ence of every animal; nor do we always remember, that some check is constantly preventing the too rapid increase of every organized being left in a state of nature. The supply of food, on an average, remains constant; yet the tendency in every animal to increase by propagation is geometrical; and its surprising effects have nowhere been more astonishingly shown, than in the case of the European animals run wild during the last few centuries in America. Every animal in a state of nature regularly breeds; yet in a species long established, any great increase in numbers is obviously impossible, and must be checked by some means. We are, nevertheless, seldom able with certainty to tell in any given species, at what period of life, or at what period of the year, or whether only at long intervals, the check falls; or, again, what is the precise nature of the check. Hence probably it is, that we feel so little surprise at one, of two species closely allied in habits, being rare and the other abundant in the same district; or, again, that one should be abundant in one district, and another, filling the same place in the economy of nature, should be abundant in a neighbouring district, differing very little in its conditions. If asked how this is, one immediately replies that it is determined by some slight difference in climate, food, or the number of enemies: yet how rarely, if ever, we can point out the precise cause and manner of action of the check! We are, therefore, driven to the conclusion, that causes generally quite inappreciable by us, determine whether a given species shall be abundant or scanty in numbers.

In the cases where we can trace the extinction of a species through man, either wholly or in one limited district, we know that it becomes rarer and rarer, and is then lost it would be difficult to point out any just distinction between a species destroyed by man or by the increase of its natural enemies. The evidence of rarity preceding extinction, is more striking in the successive tertiary strata, as remarked by several able observers; it has often been found that a shell very common in a tertiary stratum is now most rare, and has even long been thought to be See the excellent remarks on this subject by Mr. Lyell, in his Prin ciples of Geology.

extinct.

If then, as appears probable, species first become rare and then extinct-if the too rapid increase of every species, even the most favoured, is steadily checked, as we must admit, though how and when it is hard to say—and if we see, without the smallest surprise, though unable to assign the precise reason, one species abundant and another closely-allied species rare in the same district-why should we feel such great astonishment at the rarity being carried a step further to extinction? An action going on, on every side of us, and yet barely appreciable, might surely be carried a little further, without exciting our observation. Who would feel any great surprise at hearing that the Megalonyx was formerly rare compared with the Megatherium, or that one of the fossil monkeys was few in number compared with one of the now living monkeys? and yet in this comparative rarity, we should have the plainest evidence of less favourable conditions for their existence. To admit that species generally become rare before they become extinct-to feel no surprise at the comparative rarity of one species with another, and yet to call in some extraordinary agent and to marvel greatly when a species ceases to exist, appears to me much the same as to admit that sickness in the individual is the prelude to death-to feel no surprise at sickness-but when the sick man dies to wonder, and to believe that he died through violence.

1834.1

EXPLORING THE SANTA CRUZ.

177

CHAPTER IX.

Santa Cruz-Expedition up the River-Indians--Immense streams of basaltic lava-Fragments not transported by the River-Excavation of the valley-Condor, habits of-Cordillera-Erratic boulders of great size -Indian relics-Return to the ship-Falkland Islands-Wild horses, cattle, rabbits-Wolf-like fox-Fire made of bones-Manner of hunting wild cattle-Geology-Streams of stones-Scenes of violence-PenguinGeese Eggs of Doris-Compound animals.

SANTA CRUZ, PATAGONIA, AND THE FALKLAND ISLANDS.

April 13th, 1834.-The Beagle anchored within the mouth of the Santa Cruz. This river is situated about sixty miles south of Port St. Julian. During the last voyage Captain Stokes proceeded thirty miles up it, but then, from the want of provisions, was obliged to return. Excepting what was discovered at that time, scarcely anything was known about this large river. Captain Fitz Roy now determined to follow its course as far as time would allow. On the 18th three whale-boats started, carrying three weeks' provisions; and the party consisted of twenty-five souls a force which would have been sufficient to have defied a host of Indians. With a strong flood-tide and a fine day we made a good run, soon drank some of the fresh water, and were at night nearly above the tidal influence.

The river here assumed a size and appearance which, even at the highest point we ultimately reached, was scarcely diminished. It was generally from three to four hundred yards broad, and in the middle about seventeen feet deep. The rapidity of the current, which in its whole course runs at the rate of from four to six knots an hour, is perhaps its most remarkable feature. The water is of a fine blue colour, but with a slight milky tinge, and not so transparent as at first sight would have been expected. It flows over a bed of pebbles, like those which compose the beach and the surrounding plains. It runs in a winding course through a valley, which extends in a direct line westward. This

valley varies from five to ten miles in breadth; it is bounded by step-formed terraces, which rise in most parts, one above the other, to the height of five hundred feet, and have on the opposite sides a remarkable correspondence.

April 19th.—Against so strong a current it was, of course, quite impossible to row or sail: consequently the three boats were fastened together head and stern, two hands left in each, and the rest came on shore to track. As the general arrangements made by Captain Fitz Roy were very good for facilitating the work of all, and as all had a share in it, I will describe the system. The party, including every one, was divided into two spells, each of which hauled at the tracking line alternately for an hour and a half. The officers of each boat lived with, ate the same food, and slept in the same tent with their crew, so that each boat was quite independent of the others. After sunset the first level spot where any bushes were growing, was chosen for our night's lodging. Each of the crew took it in turns to be cook. Immediately the boat was hauled up, the cook made his fire; two others pitched the tent; the coxswain handed the things out of the boat; the rest carried them up to the tents and collected firewood. By this order, in half an hour everything was ready for the night. A watch of two men and an officer was always kept, whose duty it was to look after the boats, keep up the fire, and guard against Indians. Each in the party had his one hour every night.

During this day we tracked but a short distance, for there were many islets, covered by thorny bushes, and the channels between them were shallow.

April 20th.--We passed the islands and set to work. Our regular day's march, although it was hard enough, carried us on an average only ten miles in a straight line, and perhaps fifteen or twenty altogether. Beyond the place where we slept last night, the country is completely terra incognita, for it was there that Captain Stokes turned back. We saw in the distance a great smoke, and found the skeleton of a horse, so we knew that Indians were in the neighbourhood. On the next morning (21st) tracks of a party of horse, and marks left by the trailing of the chuzos, or long spears, were observed on the ground. It was generally thought that the Indians had reconnoitred us during

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