Part 4

"I found the Mammoth," observes this gentleman, "still in the same place, but altogether mutilated ... the Jakutski of the neighbourhood having cut off the flesh, with which they fed their dogs during the scarcity. Wild beasts, such as white bears, wolves, wolverines, and foxes, also fed upon it, and the traces of their footsteps were seen around. The skeleton, almost entirely devoid of its flesh, remained whole, with the exception of one fore-leg. The head was covered with a dry skin; one of the ears, well preserved, was furnished with a tuft of hairs. All these parts have necessarily been injured in transporting them a distance of 7330 miles (to St Petersburg); but the eyes have been preserved, and the pupil of one can still be distinguished.

"The Mammoth was a male, with a long mane on the neck. The tail and proboscis were not preserved. The skin, of which I possess three-fourths, is of a dark-grey colour, covered with reddish wool and black hairs; but the dampness of the spot, where it had lain so long, had in some degree destroyed the hair. The entire carcase, of which I collected the bones on the spot, was nine feet four inches high, and sixteen feet four inches long, without including the tusks, which measured nine feet six inches along the curve. The distance from the base or root of the tusk to the point is three feet seven inches. The two tusks together weighed three hundred and sixty pounds, English weight, and the head alone four hundred and fourteen pounds.

"I next detached the skin of the side on which the animal had lain, which was well preserved. This skin was of such extraordinary weight that ten persons found difficulty in transporting it to the shore. After this I dug the ground in different places, to ascertain whether any of its bones were buried, but principally to collect all the hairs which the white bears had trod into the ground while devouring the flesh. Although this was difficult from the want of instruments, I succeeded in collecting more than a pood (thirty-six pounds) of hair. In a few days the work was completed, and I found myself in possession of a treasure which amply recompensed me for the fatigues and dangers of the journey, and the considerable expenses of the enterprise.... The escarpment of ice was thirty-five to forty toises high; and, according to the report of the Tungusians, the animal was, when they first saw it, seven toises below the surface of the ice, &c. On arriving with the Mammoth at Borchaya, our first care was to separate the remaining flesh and ligaments from the bones, which were then packed up. When I arrived at the Jakutsk, I had the good fortune to repurchase the tusks, and from thence expedited the whole to St Petersburg. The skeleton is now in the Museum of the Academy, and the skin still remains attached to the head and feet. A part of the skin, and some of the hair of this animal were sent by Mr Adams to Sir Joseph Banks, who presented them to the Museum of the Royal College of Surgeons. The hair is entirely separated from the skin, excepting in one very small part, where it still remains attached. It consists of two sorts, common hair and bristles, and of each there are several varieties, differing in length and thickness. That remaining fixed on the skin is of the colour of the camel, an inch and a-half long, very thick-set, and curled in locks. It is interspersed with a few bristles about three inches long, of a dark-reddish colour. Among the separate parcels of hair are some rather redder than the short hair just mentioned, about four inches; and some bristles nearly black, much thicker than horse hair, and from twelve to eighteen inches long. The skin, when first brought to the Museum, was offensive; it is now quite dry and hard, and where most compact, is half-an-inch thick. Its colour is the dull black of the living elephants."

To me this narrative possesses an intense interest, and I have gazed with great curiosity on the bit of dried and blackened leather that is preserved in the Museum in Lincoln's-Inn-Fields, knowing it to have presented the primal freshness of life within the present century. I cannot help thinking that both the rhinoceros and this elephant roamed over the plains of Siberia, not only since the creation of man, but even since the Deluge. The freshness of their state shews that the freezing up of their carcases must have been sudden, and immediate upon death. What supposition so natural as that, perhaps in a blinding snowstorm, they slipped into a crevice in the ice-cliff, were snowed up instantly, and thus preserved by the antiseptic power of frost to this age? The glaciers of the north may hold multitudes more of these and kindred creatures, some of which may yet be disinterred, or thawed out, and may lift yet more the curtain which so tantalisingly covers the conditions of their life-history. These two huge Pachyderms are certainly extinct now; yet their remains, scattered over so vast an area, are everywhere associated with those of other animals which were indubitably contemporary with them, and whose species-life is continued to our own times. Some of these, as the great bear and the musk-ox of the sub-polar regions, we know to be in the habit of migrating northward in spring, and southward in autumn. That no lack of suitable food would be found, even in such high latitudes, for browsing quadrupeds, appears from the fact that, even beyond the parallel of 75° north, large birch-trees are found embedded in the cliffs, in abundance sufficient to be largely used as common fuel, and still retaining their woody fibre, their bark, branches, and roots. The climate then was not greatly different from what it is now, when the birch, as a tree, reaches to about 70°.

It is interesting to observe that both this elephant and this rhinoceros were inhabitants of England also; and that at the same period as the cavern bear, the hyena, the lion, and the machairode, the baboon, the bison, and the urus, the Irish elk, and the extinct horse; at the same time too, as the reindeer, the stag, the black bear, the wolf and fox, the beaver, the wild cat, the hare, and rabbit, the otter and badger, the wild hog, the rat and mouse, all our present shrews, the mole, the stoat and polecat, the noctule and the horse-shoe bats. And curious it is to note, as we go over this list, how some of the creatures enumerated are long extinct everywhere, some have been long extinct in England, but are still found elsewhere, some have more recently become extinct here, but at different eras, some are nearly extinguished, and some are yet abundant in different degrees.

I do not attach much importance to the traditions of the Siberians, that the tusks and skeletons which they find belonged to a large subterraneous animal, which could not bear the light; nor to those of the Chinese, respecting a similar burrowing quadruped of prodigious bulk, which they call, by a sort of irony, tyn-schu, or the mouse that hides himself. The fables may have easily been formed from the observation of the fossil bones, and do not necessarily imply any memory of the living original.

The two examples of the exhumation of Pachydermata in a fresh state, which I have given in detail, are by no means the only cases that have occurred. It is the universally-received belief throughout Siberia, that Mammoths have been found with the flesh quite fresh and filled with blood; probably meaning that the animal juices flowed when thawed. Isbrand Ides mentions a head on which the flesh, in a decaying state, was present; and a frozen leg, as large as the body of a man; and Jean Bernhard Müller speaks of a tusk, the cavity of which was filled with a substance which resembled coagulated blood.

Again, in the voyage of Sarytschew, particulars are given of the discovery of a Mammoth on the banks of the Alaseia, a river which flows into the Arctic Ocean, beyond the Indigirska. It had been dislodged by a flood, and somewhat injured; but the carcase was still almost entire, and was covered with the skin, to which in some places long hair remained attached.

These statements might reasonably have been esteemed either fables or gross exaggerations, but for the subsequent discovery of the rhinoceros and elephant whose remains have been brought to Europe. Read in the light of these accounts, the earlier stories take the dignity of authentic history; and it is interesting to note how well these details agree with those observed by the accurate Adams;--the long hair, for example, with which the Alaseia carcase was clothed being the very counterpart of that upon the Lena elephant; though à priori we should have looked for a very different condition in the integument of these huge Pachyderms.

If we look now at the great Mastodon, that elephantine beast, which with a stature equal to that of the tallest African elephant combined a much greater length of body and bulk of limb, we shall see some reason for concluding that the period of its decease is not indefinitely removed from our own era. Its remains occur in greatest abundance in North America; and it is interesting to observe that among several of the aboriginal tribes of Red men there were extant traditions of the Mastodon as a living creature. Dim, vague, and distorted these traditions are; but so far from our rejecting them in toto on that account, we ought rather to consider these characters as evidence of their antiquity. When semi-savage nations present us with orally-preserved accounts of very remote objects or actions, we look, as a matter of course, for a considerable element of the wild, and extravagant, and absurd in them. If we found nothing but what was reasonable, and consistent, and intelligible, we should say in a moment, this account cannot have been transmitted very far. The question, in the case before us, is not, we must remember, the precise habits and instincts of the Mastodon, but whether the Indians knew anything at all of the Mastodon having ever been a living animal. Now, as I have observed, they had. M. Fabri, a French officer who had served in Canada, informed Buffon that the Red men spoke of the great bones which lay scattered in various parts of that region as having belonged to an animal which, after their oriental style, they named Le Père aux B{oe}ufs. The Shawnee Indians believed that with these enormous animals there existed men of proportionate development, and that the Great Being destroyed both with thunderbolts. Those of Virginia stated that, as a troop of these terrible quadrupeds were destroying the deer, the bisons, and the other animals created for the use of the Indians, the Great Man slew them all with His thunder, except the big bull, who, nothing daunted, presented his enormous forehead to the bolts, and shook them off as they fell, till, being at last wounded in the side, he fled towards the great lakes, where he is to this day.

Evidence of the comparatively-recent entombment of these remains exists, however, of another character. They do not in general appear to have been rolled, but to have lived where they are now found; in some instances, as along the Great Osage River, being imbedded in a vertical position, as if the animals had been suddenly bogged in the swampy soil. Nor is there any great accumulation of earth upon them generally. All along the edges of that great saline morass called, from the abundance of these animal relics, Big Bone Lick, and on the borders, the skeletons are found sunk in the soft earth, many of them not more than a yard or two below the surface, and some even scarcely covered. With them are found in large numbers the bones of the existing bison, the wapiti-stag, and other herbivores, which still throng to the same place, for the same reasons, and meet the same fate.

Comparative anatomy determines, from the structure of the bones of the head in the Mastodon, that it must have carried a proboscis like that of the elephant. This, though wholly fleshy, has left traces of its existence. Barton reports that, in 1762, out of five skeletons which were seen by the natives, one skull still possessed what they described as a "long nose" with the mouth under it. And Kalm, in speaking of a skeleton, discovered by the Indians in what is now the State of Illinois, says that the form of the trunk was still apparent, though half decomposed. The preservation of these perishable tissues in this case must doubtless be attributed to the salt with which the bog-earth is saturated. Still more recently a skeleton was found in Virginia, which contained a very interesting proof of the food of the animal: a mass of twigs, grass, and leaves, in a half-bruised state, enclosed in a sort of sac, lay within the cavity of the body, doubtless the contents of the stomach. Some of the twigs could be identified as those of existing species of trees and shrubs, among them a species of rose, still common in the region.

All this is very strong evidence that the deposition of these remains cannot have taken place in a very remote era,--that, in fact, it must have been since the general deluge recorded in the Word of God.

Hugh Miller has an interesting observation concerning the actual date of geologic phenomena in North America, compared with that of their counterparts in the Old World. He says, "The much greater remoteness of the mastodontic period in Europe than in America is a circumstance worthy of notice, as it is one of many facts that seem to indicate a general transposition of at least the later geologic ages on the opposite sides of the Atlantic. Groups of corresponding character on the eastern and western shores of this great ocean were not contemporaneous in time. It has been repeatedly remarked that the existing plants and trees of the United States, with not a few of its fishes and reptiles, bear in their forms and constructions the marks of a much greater antiquity than those of Europe. The geologist who set himself to discover similar types on the eastern side of the Atlantic, would have to seek for them among the deposits of the later tertiaries. North America seems to be still passing through its later tertiary ages; and it appears to be a consequence of this curious transposition, that while in Europe the mastodontic period is removed by two great geologic eras, from the present time, it is removed from it in America by only one."

Professor Agassiz has expressed opinions of the same character, adducing the present existence in America of several forms of animals, which are known in this hemisphere only in a fossil state.

I cannot refrain from adding the following combination of fact and speculation, from the pen of an accomplished traveller in Mexico. It opens up a new train of ideas:--

"Some time before our visit, a number of workmen were employed on the neighbouring estate of Chapingo, to excavate a canal over that part of the plain from which the waters have gradually retired during the last three centuries. At four feet below the surface, they reached an ancient causeway, of the existence of which there was of course not the most remote suspicion. The cedar piles, by which the sides were supported, were still sound at heart. Three feet below the edge of this ancient work, in what may have been the very ditch, they struck upon the entire skeleton of a Mastodon, embedded in the blue clay. Many of the most valuable bones were lost by the careless manner in which they were extricated; others were ground to powder on their conveyance to the capital, but sufficient remained to prove that the animal had been of great size. My informant measured the diameter [qu. circumference?] of the tusk, and found it to be eighteen inches.

"Though I should be very glad to take shelter under the convenient Quien sabe? the use of which I have suggested to you, I could not avoid, at the time I was in Mexico, putting my isolated facts together, and feeling inclined to believe that this country had not only been inhabited in extremely remote times, when the valley bore a very different aspect from that which it now exhibits, or which tradition gives it, but that the extinct race of enormous animals, whose remains would seem, in the instance I have cited, to be coeval with the undated works of man, may have been subjected to his will, and made instrumental, by the application of their gigantic force, to the transport of those vast masses of sculptured and chiselled rock which we marvel to see lying in positions so far removed from their natural site.

"The existence of these ancient paved causeways also, not only from their solid construction over the flat and low plains of the valley, but as they may be traced running for miles over the dry table-land and the mountains, appears to me to lend plausibility to the supposition; as one might inquire, to what end the labour of such works, in a country where beasts of burden were unknown?

"But I leave this subject to wiser heads and bolder theorists. Had the Mammoth of Chapingo been discovered with a ring in his nose, or a bit in his mouth, a yoke on his head, or a crupper under his tail, the question would have been set at rest. As it is, there is plenty of room for conjecture and dispute."

With respect to the great extinct Mammalia of South America, we find Mr Darwin, to whom we are indebted for our knowledge of so many of them, continually expressing his wonder at the comparatively modern era of their existence. After having enumerated nine vast beasts, which he found imbedded in the beach at Bahia Blanca, within the space of 200 yards square, and remarked how numerous in kinds the ancient inhabitants of the country must have been, he observes that "this enumeration belongs to a very late tertiary period. From the bones of the Scelidotherium, including even the kneecap, being entombed in their proper relative positions, and from the osseous armour of the great armadillo-like animal being so well preserved, together with the bones of one of its legs, we may feel assured that these remains were fresh and united by their ligaments when deposited in the gravel with the shells. Hence we have good evidence that the above-enumerated gigantic quadrupeds, more different from those of the present day than the oldest of the tertiary quadrupeds of Europe, lived whilst the sea was peopled with most of its present inhabitants."

Of the remains of the Mylodon, and of that strange semi-aquatic creature the Toxodon, he says, they appeared so fresh that it was difficult to believe they had lain buried for ages under ground. The bones were so fresh, that they yielded, on careful analysis, seven per cent. of animal matter, and when heated in the flame of a spirit-lamp, they not only exhaled a very strong animal odour, but actually burned with a small flame.

Mr Darwin's interest was excited by the evidences everywhere present of the immensity of this extinct population. "The number of the remains imbedded in the great estuary-deposit which forms the Pampas, and covers the gigantic rocks of Banda Oriental, must be extraordinarily great. I believe a straight line drawn in any direction through the Pampas would cut through some skeleton or bones.... We may suppose that the whole area of the Pampas is one wide sepulchre of these extinct gigantic quadrupeds."

The whole plain of South America from the Rio Plata to the Straits of Magellan has been raised from the sea within the species-life of the existing sea-shells, the old and weathered specimens of which, left on the surface of the plain, still partially retain their colours! Darwin infers, as certain, from data which he has adduced, that the Macrauchen, that strange giraffe-necked pachyderm, lived long after the sea was inhabited by its present shells, and when the vegetation of the land could not have been other than it is now. And if the Macrauchen, then the Toxodon, the Scelidothere, the Megathere, the Mylodon, the Glyptodon, the Glossothere, and all the rest of the quaint but mighty host of gone giants, that once thronged these austral plains.

Evidence for the recent existence of the colossal ostrich-like birds of New Zealand is stronger still. It is about twenty-one years since the first intimation was given to scientific Europe of the remains of such animals, through some bones sent by the Rev. W. Williams to Dr Buckland. From these, and a collection soon afterwards sent home, Professor Owen established the genus Dinornis, identifying five species, the largest of which, D. giganteus, he concluded to have stood about ten feet in height. The remains have since been obtained in great profusion, and the result of further investigations by the Professor has been the establishment of three other genera, viz., Palapteryx, Nestor, and Notornis,--the latter a large bird allied to the Rails and Coots.

A very interesting communication from Mr Williams accompanied one of the consignments, extracts of which I will quote. It bears date "Poverty Bay, New Zealand, 17th May 1842." "It is about three years ago, on paying a visit to this coast, south of the East Cape, that the natives told me of some extraordinary monster, which they said was in existence in an inaccessible cavern on the side of a hill near the river Wairoa; and they shewed me at the same time some fragments of bone taken out of the beds of rivers, which they said belonged to this creature, to which they gave the name of Moa. When I came to reside in this neighbourhood I heard the same story a little enlarged; for it was said that this creature was still existing at the said hill, of which the name is Wakapunake, and that it is guarded by a reptile of the Lizard species, but I could not learn that any of the present generation had seen it. I still considered the whole as an idle fable, but offered a large reward to any who would catch me either the bird or its protector." These offers procured the collection of a considerable number of fossil bones, on which Mr Williams makes the following observations:--

"1. None of these bones have been found on the dry land, but are all of them from the banks and beds of fresh-water rivers, buried only a little distance in the mud.... All the streams are in immediate connexion with hills of some altitude.

"2. This bird was in existence here at no very distant time, though not in the memory of any of the inhabitants: for the bones are found in the beds of the present streams, and do not appear to have been brought into their present situation by the action of any violent rush of waters.