If it is a scene of painful interest, as surely it is to a well-constituted mind, to stand by and watch the death-struggles of one of the nobler brutes,—a dog or an elephant, for example,—to mark the failing strength, the convulsive throes, the appealing looks, the sobs and sighs, the rattling breath, the glazing eye, the stiffening limbs—how much more exciting is the interest with which we watch the passing away of a dying species. For species have their appointed periods as well as individuals: viewed in the infinite mind of God, the Creator, from the standpoint of eternity, each form, each race, had its proper duration assigned to it—a duration which, doubtless, varied in the different species as greatly as that assigned to the life of one individual animal differs from that assigned to the life of another. As the elephant or the eagle may survive for centuries, while the horse and the dog scarcely reach to twenty years, and multitudes of insects are born and die within a few weeks, so one Certain it is, that not a few species of animals have died during the present constitution of things. Races, which we know on indubitable evidence to have existed during the dominion of man, have died out, have become extinct, so that not a single individual survives. The entire totality of individuals which constituted the species, have, in these cases, ceased to be. Some of these seem to have died at a very early era of human history; but others at a comparatively recent period, and some even within our own times. Even within the last twenty years several animals have been taken, of which it is highly probable that not a single representative remains on the earth; while there are others yet again, which we know to be reduced to a paucity so extreme, that their extinction can scarcely be delayed more than a few years at most. Thus we may consider ourselves as standing by the dying-beds of these creatures, with the consciousness that we shall On that prochronic hypothesis, by which alone, as I conceive, the facts revealed by geological investigation can be reconciled with the unerring statements of Scripture,—every word of which is truth, the truth of a "God that cannot lie,"—we may assume the actual creation of this earth to have taken place at that period which is geologically known as the later Tertiary Era, or thereabout. When, on the third day, "the waters under the heaven were gathered together into one place, and the dry land appeared," it is not necessary to suppose that the form assumed by the emerging land was immediately that which it now has; we may, on the other hand, I think, assume as likely, that successive or continuous changes of elevation followed, which have been protracted, perhaps constantly decreasing in extent and force, to the present hour. Perhaps between the six days' work of Creation and the Noachic Flood, Europe became much altered in outline, and in elevation. It may have been, at first, a great archipelago, agreeing with the epithet by which it is Probably changes very similar were coevally taking place in Asia and North America, while the vast flat alluvial regions of South America were, perhaps, even still more recently formed, and a great Pacific continent was in course of subsidence, of which Australasia and Polynesia are the existing remains. Such changes of elevation, and of the continuity of land, must effect considerable alterations of climate; and, therefore, it is not surprising to know that, in earliest ages, animals and plants flourished in regions to which they would now be altogether unfitted, and that many In the great swamps of emerging Germany, and in the, as yet, only half-drained valleys of Switzerland, lurked then the heavy Dinothere. Huger than the hugest elephant, he carried an enormous body of twenty feet in length, vast and barrel-like, which even his columnar limbs of ten feet long scarcely sufficed to raise from the ground. His uncouth head, elephantine in shape, was furnished with a short proboscis; and two tusks, short and strong, projected from the lower jaw, not curving upward, as in the elephant, but downward, as in the walrus. In the teeming marshes lurked this ungainly beast, half immersed, digging out with his mighty pickaxe-tusks the succulent roots that permeated the soft soil, which his sensitive trunk picked up, and conveyed to his mouth. On the southern slopes of the slowly-rising Himalayas, already clothed with forests of teak, and palm, and bamboo, revelled the Sivathere, another heavy creature, of the bulk of a rhinoceros, and therefore not more than half equalling the German colossus. He too was a strange subject. With a proportionally enormous head, in form somewhat between that of the elephant and of the rhinoceros, minute sunken piggish eyes, and a short proboscis like that of the tapir, he carried two pairs of dissimilar horns. On the forehead were placed one pair, seated upon bony cores, not unlike those of our short-horn oxen. Behind these there rose another pair, large and massive, In the same regions a land Tortoise of enormous bulk, far vaster than the vastest of now existing species, to which that ponderous one which will march merrily away with a ton weight on its back, is a mere pigmy, shook the earth with its waddle, and the forests with its hoarse bellowing. Broad roads, like our highways, were beaten by it through the jungle, along which it periodically travelled to the cool springs, leisurely sauntering, and tarrying to munch the fleshy gourds and cactuses that bordered its self-made track. The plains of Siberia, stretching away towards the Arctic Ocean, sheltered countless hosts of huge pachydermatous quadrupeds. A species of Rhinoceros, not less bulky than those of the present age, roamed to the very verge of the Icy Sea; its hide, tough and leathery, was destitute of folds, but was clothed with tufts of rigid gray hair,—an ornament which is denied to our existing degenerates. Two horns, the front one of unusual massiveness and length, were seated, as in several of the African kinds, one behind the other, and were wielded by a head of great strength and development. More remarkable still was that great hairy Elephant, There was, at the same time, a quadruped, nearly allied to the elephants, but differing from them in some technical characters. With a body equally bulky, but considerably longer, it had shorter limbs, a broader head, small tusks in the lower, as well as large curving ones in the upper jaw, and probably a trunk intermediate between the elephant's and the tapir's. Truly cosmopolite as this great Mastodon was, for we dig up his bones from all parts of the world, he had his head-quarters in North America, where, from his dimensions and his numbers, he must have formed a very characteristic feature of the primeval swamps and forests. There, with his tusks, he grubbed up the young trees, whose juicy roots he ground down with his great mammillary molar teeth, or chewed up to a pulp the sapwood of the recent branches and spicy twigs. And ever and anon he would resort to the broad saline marshes,—the "Licks," as they are now called,—to lick up the crystallised salt on their margins, so grateful to all herbivorous quadrupeds. Here, in his eagerness to gratify his palate with the pungent condiment, he would press farther and farther into the treacherous quagmire, But let us look at South America, where, as the great back-bone chain of the Andes is being elevated out of the sea, the torrents and cataracts are pouring down from its sides immense quantities of crumbled rock and pasty mud, which, deposited upon the vast tabular field, brought by the upheaving just to the level of the sea, forms that grand alluvial plain unequalled on the face of the globe for extent, which is clothed with the mighty forests of Guiana and Brazil, or with the tall grass and thistles of the Pampas. The torrents still fall; and, meandering through this glorious plain, unite and form the most majestic of rivers, ever depositing the rich alluvium, and thus sensibly augmenting, to this day, the breadth of their noble continent, and their own length. Strange creatures riot here in these primal ages. The young land, hot and moist,—moist with the unevaporated water of the depositing rivers, and hot with the influence of the submarine volcano which is lifting it, as well as with the beams of the tropical sun,—brings forth from its steaming bosom, the most gigantic trees in the most profuse luxuriance. And animal life teems too, in this riant But lo! here are mightier creatures yet! See the vast Mylodon, the Scelidothere, and the still more colossal Megathere. Ponderous giants these! The very forests seem to tremble under their stately stride. Their immense bulk preponderates behind, terminating in a tail While the heavy giant is absorbed in his juicy breakfast, see, there lounges along his neighbour, the Macrauchen. Equally massive, equally heavy, equally vast, equally peaceful, the stranger resembles a huge rhinoceros elevated on much loftier limbs; but his most remarkable feature is an enormously long neck, like that of the camel, but carried to the altitude of that of the giraffe. Thus he thrusts his great muzzle into the very centre of the leafy trees, and gathering with his prehensile and flexible lip the succulent twigs and foliage, he too finds abundance of food for his immense body, in the teeming vegetation, without intruding upon the supply of his fellows. And what enormous mass is suddenly thrust up out of the quiet water of yonder igaripÉ? A hoarse, hollow Away to the great Austral land—in our day minished to the insular Australia and New Zealand and a few satellite isles—but then, in the morning of creation, possibly stretching far to the north and on either hand, so as to include the scattered groups of Polynesia in one great But what of our own land? What of these distant isles of the Gentiles in that early day, when the enterprising sons of Cain, migrating from the already straitened land of Nod, were pushing their advancing columns, with arts And the beasts that already tenanted this fair land were for bulk and power worthy of the domain. The Dinothere and the Mastodon wallowed and browsed where great London now crowds its princely palaces. Through the greenwood shades of the forests of oak wandered hippopotamuses and rhinoceroses of several kinds, the long-tusked mammoth, and two or three species of horses. Two gigantic oxen—a bison and a urus—roamed over the fir-clad hills of Scotland, and a curious flat-headed ox, of small size and minute horns, made Ireland its peculiar home. That island, too, was the metropolis of a colossal fallow-deer, whose remains, ticketed as those of the Irish All these herbivores, and numberless smaller genera, some now extinct, some surviving, were kept in check by powerful predatory tyrants, for whose representatives we must now look to the jungles of India or the burning karroos of Southern Africa. The Lion and the Tiger stalked over these isles, and a terrible tiger-like creature, the Machairode, of even superior size and power to the scourge of the Bengal jungle, with curved and saw-edged canine-teeth, hung upon the flanks of the cervine and bovine herds, and sprang upon the fattest of them. Then, too, there was a vast Bear, huger and mightier than the Thus I have endeavoured to draw a picture, vague and imperfect, I know, of some of the more remarkable and prominent features of the primeval earth, limiting the sketch to those forms which we know only by their fossil remains. In endeavouring to paint their contour and general appearance, and still more their habits and instincts, conjecture must be largely at work—a conjecture, however, which takes for its basis the anatomical exigencies of the osseous structure, and the analogy of existing creatures the most nearly related to the fossil. These forms, many of them so huge and uncouth, are well known as having tenanted various regions of the earth during what is known as the Tertiary Era, in its later periods. They certainly do not exist in those regions I do not pretend to offer positive evidence concerning the synchronism of all the animals I have been describing with man; but, as there is no doubt that they were all contemporaneous, inter se, if we can attain to good grounds for concluding his co-existence with some of them, it may be no unfair presumption that the case was so with the others. And first, with respect to the Colossochelys Atlas, that vast fossil land tortoise of the Sewalik hills, in the north of India, whose carapace may have covered an area of twelve or fifteen feet in diameter, and whose entire length, as in walking, when head and tail were protruded, could not have been much less than thirty feet. The discoverers of this interesting relic, Dr Falconer and Major Cauntley, have discussed the question of its probable cessation of existence with some care; and they have come to the conclusion "that there are fair grounds for entertaining the belief, as probable, that the Colossochelys Atlas may have lived down to an early period of the human Elian, the Greek naturalist, quoting Megasthenes, a still older authority, who resided several years in India, and who collected a good deal of interesting information concerning the country, reports that in the sea around Ceylon there were found tortoises of such enormous dimensions that huts were made of their shells, each shell being fifteen cubits (or twenty-two feet) long; so that several people were able to find comfortable shelter under it from the rain and sun. The circumstances attending the discovery of the rhinoceros and elephant of Siberia are very curious and interesting; since of them we have not the fossilised skeletons, but the carcases preserved in a fresh state, as if just dead, with (in one case) the flesh upon the bones in an eatable state, and actually forming the food of dogs and wolves, the skin entire, and covered with fur, and even the eyes so perfectly preserved that the pupils could be distinctly seen. In 1771, in the frozen gravelly soil of Wilhuji, in the northern part of Siberia, an animal was found partially exposed. It was twelve feet in length; its body was enveloped in a skin which had the thickness and firmness of sole-leather, but was destitute of folds. Short hair, strongly planted in the pores of the skin, grew on the face in tufts; it was rigid in texture, and of a grey hue, with here and there a black bristle, larger and stiffer than the rest. Short ash-grey hair was observed to clothe the legs, in moderate profusion. The eyelids and eyelashes were still visible; the remains of the brain were still in the cavity of the skull, and the flesh of the body, in a putrefying condition, was still beneath the skin. On the nose there were indications of a horn having been seated, around which the integument had formed a sort of fold. Thus the creature was known to be a Rhinoceros, and the head and feet were lifted, and conveyed to St Petersburg, where they are still preserved in the Imperial Nearly thirty years afterwards a still more interesting revelation occurred. The shores of the Icy Ocean had yielded a vast number of tusks, not distinguishable from those of the known elephants, and capable of being worked up by ivory-manufacturers, so that they occupied a well-recognised place in the commercial markets, and they constitute to this day the principal supply of the Russian ivory-turners. A fisherman living at the mouth of the Lena, being one day engaged in collecting tusks, saw among some ice-blocks an uncouth object. The next year he observed it still further exposed, and in the following season, 1801, he saw that it was an enormous animal, having great tusks, one of which, with the entire side of the carcase, projected from the frozen mass. He knew it to be a Mammoth, for so the fossil elephants were called, and observed it with interest. The next season was so cold that no change took place; but in 1803, the melting of the ice proceeded so far that the gigantic animal fell down from the cliff entire, and was deposited on the sand beneath. The following season the fisherman, Schumachoff, cut out the tusks, which he sold for fifty rubles, and two years after this the scene was visited by Mr Adams, in the service of the Imperial Court, who "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 "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 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 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 rein-deer, 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 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 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 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. 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. "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 ques 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 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- 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 pre "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. "3. They existed in considerable numbers,—(an observation which has since been abundantly confirmed.) "4. It may be inferred that this bird was long-lived, and that it was many years before it attained its full size. (The writer grounds this inference on the disparity in dimensions of the corresponding bones, supposing that they all belonged to one and the same species; which, however, was an erroneous assumption.) "5. The greatest height of the bird was probably not less than fourteen or sixteen feet. The leg-bones now sent give the height of six feet to the root of the tail. "Within the last few days I have obtained a piece of information worthy of notice. Happening to speak to an "This incident might not have been worth mentioning, had it not been for the extraordinary agreement in point of the size of the bird [with my deductions from the bones]. Here are the bones which will satisfy you that such a bird has been in existence; and there is said to be the living bird, the supposed size of which, given by an independent witness, precisely agrees." The story told of the whaler appears to me to bear marks of truth. The bold essay to explore, the terror inspired by the gigantic figure, especially in the solemnity of night, the description of the manners of the bird running and striding, so like those of the Apteryx, with which its bones shew the Moa to have been closely allied, and the inglorious return of the party without achieving any And well may the colossus have inspired fear. The bones sent to London greatly exceed in bulk those of the largest horse. The leg-bone of a tall man is about one foot four inches in length, and the thigh of O'Brien, the Irish giant, whose skeleton, eight feet high, is mounted in the Museum of the Royal College of Surgeons, is not quite two feet. But the leg-bone (tibia) of the Dinornis we know measured as much as two feet ten inches, and we have no reason to suppose, considering the disparity that exists in the specimens examined, that we have seen by any means the largest. Additional reason for supposing these magnificent birds to have existed not long ago, is found in the fact that specimens of their eggs have been preserved. The circumstances attendant on the discovery and identification of these possess a remarkable interest. In the volcanic sand of New Zealand Mr Walter Mantell found a gigantic egg, which we may reasonably infer to be that of either Dinornis or Palapteryx, of the magnitude of which he gives us a familiar idea by saying that his hat would have been but just large enough to have served as an egg-cup for it. This is the statement of a man of science, and therefore we may assume an approximate degree of precision in the comparison. I do not know the size of Mr Mantell's hat, but I find that the transverse diameter of my own is six inches or a little more. If we may take this as the shorter diameter But about the same time as Mr Mantell's discovery, one of equal interest was made in Madagascar. The master of a French ship obtained, in 1850, from natives of the island, three eggs, of far greater size, and fragments of the leg-bones of an immense bird. These, on their arrival at Paris, formed the subjects of valuable investigations by M. Isidore Geoffroy St Hilaire The native statement was, that one of the eggs had been found entire in the bed of a torrent, among the debris of a land-slip; that a second egg, with some frag These two, though nearly alike in size, differed considerably in their relative proportions and shape, the one being shorter and thicker, with more equal ends than the other. The following table shews the dimensions of both compared with those of an ostrich's egg:—
M. Geoffroy St Hilaire estimates the larger of the two to contain 10? quarts, or the contents of nearly six eggs of the Ostrich, or sixteen of the Cassowary, or a hundred and forty-eight of the Hen, or fifty thousand of the Humming bird. The fragments of bone indicated a bird of the same natural affinities as the New Zealand colossi, and of dimensions not widely remote from theirs. Professor Owen thinks that it did not exceed in height or size Dinornis giganteus, and that there is a probability that it was slightly smaller. The Madagascar bird has been named Æpyornis maximus. The fragments of the egg of the New Zealand bird (still uncertain as to the species to which it is to be referred) shew that the shell was absolutely thinner, and therefore relatively much thinner than that of the Ostrich's egg; the air-pores, too, have a different form, being linear, instead of round, and the surface is smoother. In these qualities, the New Zealand egg resembles that of the Apteryx; in the thickness and roughness of the egg of Æpyornis there is more similarity to those of the Ostrich and Cassowary. The colour of the Madagascar egg is a dull greyish yellow; but it is possible that this may be derived from the soil in which it has long been imbedded. The fragments of the New Zealand egg are white, like the eggs of the Apteryx and Ostrich: those of the Emu and Cassowary are light green. The willing fancy suggests the possibility that, in an island of such immensity as Madagascar, possessing lofty mountain-ranges, covered with the most magnificent forests, where civilised man has only yet touched one or two spots on the seaward borders, but where these slight explorations have educed so many wondrous animals, so many strange forms of vegetable life, the noble Æpyornis may yet be stalking with giant stride along the fern-fringed hill-sides, or through the steaming thickets; though in the more contracted area of New Zealand its equally ponderous cousins, the Dinornis and the Palapteryx, may have sunk beneath the persevering persecutions of man. Yet another item of evidence bearing on the recent if At a meeting of the Zoological Society of London, held on the 13th November 1850, Dr Mantell made the following communication relative to this discovery:— "It was in the course of last year, on the occasion of my son's second visit to the south of the middle island, that he had the good fortune to secure the recent Notornis, which I now submit, having previously placed it in the hands of the eminent ornithologist Mr Gould, to figure and describe. This bird was taken by some sealers who were pursuing their avocations in Dusky Bay. Perceiving the trail of a large and unknown bird on the snow, with which the ground was then covered, they followed the footprints till they obtained a sight of the Notornis, which their dogs instantly pursued, and, after a long chase, caught alive in the gully of a sound behind Resolution Island. It ran with great speed, and on being captured uttered loud screams, and fought and struggled violently. It was kept alive three or four days on board the schooner, and then killed, and the body roasted and eaten by the crew, each partaking of the dainty, which was declared to be delicious. The beak and legs were of a bright red colour. My son secured the skin, together with very fine specimens of the Kapapo or ground parrot (Strigops), a pair of Huias (Neomorpha), and two species of Kiwikiwi, "Mr Walter Mantell states, that, according to the native traditions, a large Rail was contemporary with the Moa, and formed a principal article of food among their ancestors. It was known to the North Islanders by the name 'Moho,' and to the South Islanders by that of 'Takahe;' but the bird was considered by both natives and Europeans to have been long since exterminated by the wild cats and dogs; not an individual having been seen or heard of since the arrival of the English colonists. On comparing the head of the bird with the fossil cranium, and mandibles, and the figures and descriptions in the 'Zoological Transactions' (Plate lvi.), my son was at once convinced of their identity. It may not be irrelevant to add, that in the course of Mr Walter Mantell's journey from Banks's Peninsula along the coast to Otago, he learned from the natives that they believed there still existed in that country the only indigenous terrestrial quadruped, except a species of rat, which there are any reasonable grounds for concluding New Zealand ever possessed. While encamping at Arowenua, in the district of Timaru, the Maoris assured them that about ten miles inland there was a quadruped which they called KÁureke, and that it was formerly abundant, and often kept by their ancestors in a domestic state as a pet animal. It was described as about two feet in length, with coarse grizzly hair; and must have more nearly resembled the Mr Gould then read a paper pointing out the zoological characters of the bird discovered by Mr Mantell, which he had no hesitation in identifying as the species formerly characterised, from its osseous remains, by Professor Owen, under the name of Notornis Mantelli. Mr Gould, in adverting to the extreme interest with which the present existence of a species which was certainly contemporary with the Moa must be regarded, pointed out, from the preserved skin, which was on the table, how accurate a prevision of its character had been made by Professor At length I come home to Great Britain and Ireland—the "nice little, tight little islands" where so many of our sympathies properly centre, where natural-history facts and all other facts interest us so much more than parallel facts elsewhere, and where, above all, there are so many more lights streaming into the darkness, and bringing out truth. Let us again look back to the period of the Bison, and Reindeer, and Elk, of the Elephant, and Hippopotamus, and Rhinoceros, of the Lion and the Hyena, and the great Cave Bear, and search among the vanishing traces of the far past for glimpses of evidence when their age ceased to be. Some dim light falls on the obscurity from the discovery of the fossil remains of man himself—the human bones found by Dr Schmerling in a cavern near Liege, the remains mentioned by M. Marcel de Serres and others in several caverns in France, associated with fossil relics of this period. But more from the occurrence of flints, apparently fashioned by human art, in superficial deposits, together with the same extinct fossils of the tertiary. Even at the very moment that I write this sheet, my eye falls on the report These flints, which seem indubitably to have been chipped into the forms of arrow-heads, lance-heads, and the like, have been found in France in large numbers, as also in other parts of the continent, and in England. They resemble those still used by some savage tribes. In this very neighbourhood, as in the cavern called Kent's Hole near Torquay, and in one more recently examined at Brixham, they are found mixed up with the bones of the Rhinoceros, of the Cave Bear, and the Hyena, At Menchecourt, near Abbeville, they occur in a deposit of sand, sandy clay, and marl, with bones of the same animals, and others, their contemporaries. Concerning this bed, Mr Prestwich, in a paper read before the Royal Society, May 26, 1859, says that it must be referred to those usually designated as post pliocene, but that the period of its deposit was anterior to that of the surface assuming its present outline, so far as some of its minor features are concerned. "He does not, however, consider that the facts of necessity carry man back in past time more than they bring forward the great extinct mammals towards our own time, the evidence having reference only to relative, and not to absolute time; and he is of opinion that many of the later geological changes may have been sudden, or of shorter duration than generally considered. In fact, from the evidence here exhibited, and from all that he At the meeting of the Ethnological Society just held, there seems to have been an increasing tendency to admit the hypothesis of the continuance of the Mammalia of the Tertiary into the human era. Mr Evans, who exhibited specimens taken at a depth of twenty to thirty feet, from a stratum of coarse fresh-water gravel, lying on chalk, and containing an entire skeleton of an extinct Rhinoceros, and overlaid by sandy marl containing existing shells, shewed that the deposit had certainly not been disturbed till the present time, so that the gravel, the bones, and the flints had been deposited coetaneously. He suggested "that the animals supposed to have become extinct before man was created might have continued to exist to more recent periods than had been admitted." And this opinion found support from other leading geologists. That this conclusion would throw the existence of man to an era far higher than that assigned to him by the inspired Word, is, I know, generally held; and certain investigations, made in the alluvial deposit of the Nile, So, doubtless, concerning other deposits containing fossil remains, whose extreme antiquity is assumed from the known rate of surface-increase now, we ought to remember that we have not a tittle of proof that the rate of increase has not at certain remote periods been suddenly and immensely augmented. There are many facts on record which tend to shew that the rate at which geologic changes take place in certain localities affords no reliable data whatever to infer that at which phenomena apparently quite parallel have occurred in other localities. An upheaval or a subsidence of one part of a country may rapidly effect a great change in the amount of soil or gravel precipitated by streams, without destroying or changing their channels, and yet the deposit may be The degradation of a cliff, either suddenly or gradually, might throw a vast quantity of fragments into a rapid stream, and cause a deposit of gravel of considerable breadth and thickness in a comparatively short period of time,—say a century or two. Sir Charles Lyell has adduced examples of very rapid formation of certain stony deposits, which should make us cautious how we assert that such and such a thickness must have required a vast number of years. In one of them there is a thickness of 200 or 300 feet of travertine of recent deposit, while in another, a solid mass thirty feet thick was deposited in about twenty years. There are countless places in Italy where the formation of limestone may be seen, as also in Auvergne and other volcanic districts. From these and similar considerations it seems to me by no means unreasonable that the four thousand years which elapsed between the Creation and the commencement of Western European history should have been amply sufficient for many of those geological operations whose results are seen in what are known as the later Tertiary deposits,—the crag, the drift, the cavern-accumu But have we nothing better for this conclusion than an assumption of the possibility, and a more or less probable conjecture? Yes; we have some facts of interest to warrant it, or I should not have ventured to introduce the subject in this work. There are facts,—besides the admixture of human workmanship with the animal remains in undisturbed deposits—direct evidence, not altogether shadowy, of the co-existence of the extinct animals with living men. And first, I would mention some circumstances bearing analogy to the exhumation of the fresh Pachyderms of Siberia. Some years ago, a portion of the leg of an Irish Elk, so-called, (Megaceros hibernicus,) with a part of the tendons, skin, and hair upon it, was dug up with other remains from a deposit on the estate of H. Grogan Morgan, Esq., of Johnstown Castle, Wexford, and is now in that gentleman's possession. This leg was exhibited, and formed the subject of a lecture at the time by Mr Peile, veterinary surgeon, Dublin. It has been ascertained that the marrow in some of the bones blazes like a candle; that the cartilage and gelatine, so far from having been destroyed, were not appar Pepper, in his "History of Ireland," states that the ancient Irish used to hunt a very large black deer, the milk of which they used as we do that of the cow, and the flesh of which served them for food, and the skin for clothing. This is a very remarkable record; and is confirmed by some bronze tablets found by Sir William Betham, the inscriptions on which attested that the ancient Irish fed upon the milk and flesh of a great black deer. According to the "Annals of the Four Masters," Niel Sedamin, a king of Ireland before the Christian era, was so called because "the cows and the female deer were alike milked in his reign." The art of taming the wild deer and converting them into domestic cattle is said to have been introduced by Flidisia, this monarch's mother. Deer are said to have been used to carry stones and wood for Codocus when his monastery was built, as also to carry timber to build the castle of a king of Connaught. These An interesting letter from the Countess of Moira, published in the "ArchÆologia Britannica," gives an account of a human body found in gravel under eleven feet of peat, soaked in the bog-water; it was in good preservation, and completely clothed in antique garments of deer-hair, conjectured to be that of the Giant Elk. A skull of the same animal has been discovered in Germany in an ancient drain, together with several urns and stone-hatchets. And in the museum of the Royal Dublin Society there exists a fossil rib bearing evident token of having been wounded by some sharp instrument which remained long infixed in the wound, but had not penetrated so deep as to destroy the creature's life. It was such a wound as the head of an arrow, whether of flint or of metal, would produce. In the year 1846, a very interesting corroboration of the opinion long held by some that the great broad-horned Deer was domesticated by the ancient Irish, was given by the discovery of a vast collection of bones at Lough GÛr, near Limerick. The word GÛr is said to mean "an assemblage," so that the locality is "the Lake of the Assemblage," commemorating perhaps the gathering of an army or some other host at the spot. In the midst of the lake is an island, which is described as being so completely surrounded with bones and skulls of animals "that one The skulls are described as belonging to the following animals:—The giant deer (females); a deer of inferior size; the stag; another species of stag; the fallow deer; the broad-faced ox; the hollow-faced ox; the long-faced ox; another species of ox; the common short-horned ox; the goat; and the hog. The principal points of interest centred in the Giant Deer or so-called Irish Elk. The skulls of these, as of all the larger animals, "were broken in by some sharp and heavy instrument, and in the same manner as butchers of the present day slaughter cattle for our markets, and in many cases the marrow-bones were broken across, as if to get at the marrow." Of course, if this was indubitable, the conclusion was inevitable, that the Giant Deer was not only contemporary with man, but was domesticated by him with other quadrupeds, and used for food. Professor Owen, however, contended that the skulls of the Giant Deer were not females but males, from which the horns had been forcibly removed, and that the holes in the foreheads were made by the violent wrenching off of the horns tearing away a portion of the frontal bone from which they grew. In reply to this opinion, Mr H. D. Richardson of Dublin, whose personal acquaintance with the relics of this noble species is peculiarly extensive, shewed that certain variations of proportion on which the learned Professor relied to prove the skulls to be male, were of To put the matter to test, Mr Richardson experimented on two perfect male skulls. In the one instance the force was applied to the beam of the horns, and the result was their fracture where they are united to the peduncles. In the other case the force was applied to the peduncles themselves, to ascertain whether it was possible to wrench them and the ridge away from the face, when the consequence was, that the skull was completely riven asunder. Indeed to any one who looks at the position of the horns in this animal, and their implantation, it must be self-evident that their violent removal must tear away the entire forehead, and not leave a central hole. Mr Edward Newman who subsequently examined the specimens speaks decidedly on this point:—"I have not the least hesitation in expressing my firm conviction that the fractures were the result of human hands, and were the cause of the death of the animals. These two fractured skulls correspond too exactly with each other, and with that of a bullock with which I compared them, to have resulted from accident: the edges of the fractures wore the appearance of having been coeval with the interment or A circumstance of much importance is that these skulls were found in company with those of many well-known domestic animals, as the ox, the goat, and the hog. These skulls were similarly fractured. As it is evident that their demolition was produced by the butcher's pole-axe, why not that of the elk-skulls? "At the first cursory glance, it may appear somewhat strange that the skulls of the males should invariably have been found entire, and that even the recent discovery at Lough GÛr should form no exception. "I do not, however, find any difficulty here. In the first place, we may fairly suppose that males, like our bulls, were not equally prized as food. In the second place, the size, as well as the position of the antlers, would render it next to an impossibility to give the desired blow with the pole-axe. In the third place, the greater strength and thickness of the skull would almost to a certainty render the blow unavailing; and in the fourth place, supposing the females domesticated, and the occasional tenants of sheds and other buildings, we may well imagine that the males were excluded from such buildings by the enormous size of their antlers. Perhaps a few only of the males, as in In a communication subsequently made to the Zoologist by Mr Richardson, he gives the following additional evidence:—"In the collection of the late Mr Johnston, of Down, which had been left by his uncle, an attorney, and in which everything was labelled with the accuracy and precision of that profession, is a small brass spear, with a piece of wood still in the socket, with a label, stating it to have been found in a marl-pit, among the bones of a deer. An excise-officer told me that he saw, found in a marl-pit, at Mentrim in Meath, the skeleton of a deer, and a man, and a long knife: the latter, I believe, is rather a short sword, now, I think, in the collection of Mr Petrie, of Dublin, who told me that some such tradition had accompanied it into his possession.... Dr Martin informs me that on the banks of the river Suir, near Portland, Waterford, and on nearly every farm, are found, near springs, spaces of frequently seventy feet in diameter, consisting of stones, broken up as if for roads, and lying together in a mass. These stones were evidently purposely broken, From all these testimonies combined, can we hesitate a moment in believing that the Giant Deer was an inhabitant of Ireland since its colonisation by man? It seems to me that its extinction cannot have taken place more than a thousand years ago. Perhaps at the very time that CÆsar invaded Britain the Celts in the sister isle were milking and slaughtering their female elks, domesticated in their cattlepens of granite, and hunting the proud-antlered male with their flint arrows and lances. It would appear, that the mode of hunting him was to chase and terrify him into pools and swamps, such as the marl-pits then were; that, having thus disabled him in the yielding bogs, and slain him, the head was cut off, as of too little value to be worth the trouble of dragging home; that the under jaws and tongue were cut off; and that frequently the entire carcase was disjointed on the spot, the best parts only being removed. This would account for the so frequent occurrence of separate portions of the skeleton, and especially of skulls, in the bog-earth. No doubt so large an animal would not long survive in a state of freedom, after an island so limited in extent as Ireland became "I then went forth to search the lands, To see if I could redeem my chief, And soon returned to noble Tara, With the ransom that Cormac required. "I brought with me the fierce Geilt, And the tall Grib And the two Ravens of Fid-dÁ-Beann, And the two Ducks of Loch Saileann. "Two Foxes from Sliabh Cuilinn, Two Wild Oxen Two Swans from the dark wood of Gabhran, And two Cuckoos from the wood of Fordrum. "Two Toghmalls Which is by the side of the two roads, And two Otters after them, From the brown-white rock of Dobhar. "Two Gulls from Tralee hither, Two Ruilechs Four Snags Two Plovers from the rock of DunÁn. "Two Echtachs Two Thrushes from Letter Longarie, Two Drenns The two Cainches "Two Herons from the hilly Corann, The two Errfiachs The two Eagles of Carrick-na-Cloch, Two Hawks from the wood of Caenach. "Two Pheasants from Loch Meilge, Two Water-hens from Loch Eirne, Two Heath-hens from the Bog of Mafa, Two Swift Divers from Dubh Loch. "Two Cricharans Two Titmice from Magh Tualang, Two Choughs from Gleann Gaibhle, Two Sparrows from the Shannon. "Two Cormorants from Ath Cliath, Two Onchus Two Jackdaws from Druim Damh, Two Riabhogs "Two Rabbits from Dumho Duinn, Two wild Hogs from circular Cnoghbha, Two wild Boars "Two Pigeons out of Ceis Corann, Two Blackbirds out of Leitir Finnchoill, Two black Birds (?) from the strand of Dabhan, Two Roebucks from Luachair Deaghaidh. "Two Fereidhins Two Fawns from Moin mor, Two Bats out of the Cave of Cnoghbha, Two Pigs "Two Swallows out of Sidh Buidhe, Two Iaronns Two Geisechtachs Two charming Robins from Cnamh Choill. "Two Woodcocks from Coillruadh, Two Crows from Lenn Uar, Two Bruacharans Two Barnacle-Geese from Turloch Bruigheoil. "Two Naescans Two Yellow-ammers from the brink of Bairne, Two Spireogs Two Grey Mice from Limerick. "Two Corncrakes from the Banks of Shannon, Two Wagtails from the brinks of Birra, Two Curlews from the Harbour of Galway, Two SgreachÓgs "Two Geilt Glinnes Two Jackdaws from great Ath Mogha, Two fleet Onchus Two Cats out of the Cave of Cruachain. "Two Goats from Sith Gabhran, Two Pigs A Ram and Ewe both round and red, I brought with me from Aengus. "I brought with me a Stallion and a Mare, From the beautiful stud of Manannan, A Bull and a white Cow from Druim Cain, Which were given me by Muirn Munchain." No known allusion occurs in this poem to the Giant Deer. The enumeration of nearly a hundred and sixty quadrupeds and birds either indigenous to or naturalised in Ireland at so early a period, possesses, I say, a peculiar interest. If the editor's suggestion is correct, that the Echtach was a bovine animal, then we have three distinct mentions of this family in the poem,—the Wild Oxen, the Echtachs, and the Bull and White Cow. The second and third of these were probably domesticated animals; the first one expressly "Wild." Now at least five distinct species of Oxen are known to have inhabited Europe and the British Isles during the later periods of the Tertiary era, which have been named respectively, Bison priscus, Bos primigenius, frontosus and longifrons, and Ovibos moschatus. Of these, skulls of Bos frontosus and B. longifrons have been dug up in some numbers in Ireland. Some of these bear, in the perforation of the forehead, evident proof of having been slaughtered secundum artem, and therefore of having been domesticated. But one large skull of the longifrons type, now in the Museum of the Royal Irish Academy, has a cut in the forehead, into which can be accurately fitted several of the narrow bronze "celts," or arrow-heads so frequently dug up in Ireland; a pretty fair proof that this animal was killed by the hunter's arrow, and was therefore wild. No bovine animals of the true taurine race are now known to exist in an aboriginally wild state; but at the It is probable that this race extended widely over Europe, and even into Asia. Herodotus mentions Macedonian wild oxen, with exceedingly large (?pe?e?a??a) horns; and Philip of Macedon killed a wild bull in Mount Orbela, which had made great havoc, and produced much terror among the inhabitants; its spoils he hung up in the Temple of Hercules. The Assyrian artists delighted to sculpture on the royal bas-reliefs of Nineveh the conquest of the wild bull by the prowess of their Nimrod monarchs, and the figures, in their minute anatomical characters, well agree with the descriptions and remains of the European Urus. The large forest that surrounded ancient London was infested with boves sylvestres among other What has become of the terrible Uri which lived in Europe at the commencement of the Christian era? Advancing civilisation has rooted them out, so that no living trace of them remains, unless the cream-white breed which is preserved in a semi-wild state in some of our northern parks be their representatives; or, as is not improbable, their blood may still circulate in our domestic oxen. Yet there is no doubt of the identity of a species found abundantly in Britain in the Tertiary deposits, and named by Owen Bos primigenius, with the Urus of CÆsar. This fossil bull was as certainly contemporary in this island with the elephant, and the hyena, and the baboon, and, strange to say, with the reindeer, and the musk-ox, too—thus combining a tropical, a temperate, and an arctic fauna in our limited island at the same period! What a strange climate it must have been to suit them all! Professor Nilsson, who has paid great attention to fossil oxen, mentions a skull of this species which must have belonged to an animal more than twelve feet in length from the nape to the root of the tail, and six feet and That this ancient fossil bull was really contemporary with man in Scandinavia is proved by evidence which is irrespective of the question of its identity with CÆsar's Urus. For one of Professor Nilsson's specimens "bears on its back a palpable mark of a wound from a javelin. Several celebrated anatomists and physiologists, among whom," he says, "I need only mention the names of John MÜller, of Berlin, and Andreas Retzius, of Stockholm, have inspected this skeleton, and are unanimous in the opinion that the hole in question upon the backbone is the consequence of a wound, which, during the life of the animal, was made by the hand of man. The animal must have been very young, probably only a calf, when it was wounded. The huntsman who cast the javelin must have stood before it. It was yet young when it died, probably not more than three or four years old." We may, then, assume as certain that the vast Bos primigenius of Western Europe lived as a wild animal contemporaneously with man; and as almost certain (assuming its identity with the Urus) that it continued to be abundant as late as the Christian era. The Bos frontosus is a middling-sized bovine. "Its This species occurs in a fossil state in some numbers in Ireland; it has also been found in England. It is by some supposed to be the origin of, or, at least, to have contributed blood to, the middling Highland races with high occiput, and small horns. There is more certainty of the co-existence of the small B. longifrons with man. Some of the evidence I have already adduced. "Within a few years," says a trustworthy authority, "we have read in one of the scientific periodicals,—but have just now sought in vain for the notice,—of a quantity of bones that were dug up in some part of England, together with other remains of what seemed to be the relics of a grand feast, held probably during the Roman domination of Britain, for, if we mistake not, some Roman coins were found associated with them. There were skulls and other remains of Bos longifrons Professor Owen conjectures that this species may have contributed to form the present small shaggy Highland and Welsh cattle,—the kyloes and runts; and a similar breed in the northern parts of Scania may have had a similar origin. In the Bison priscus, the fossil remains of which occur in many parts of Europe, and more sparsely in Great Britain, It is a formidable beast, standing six feet high at the shoulders, where it is protected by a thick and profuse mane. Specimens have been known to reach a ton in weight. It manifests an invincible repugnance to the ox. There are several other animals of note which, like the Bison, were once common inhabitants of these islands, but have long been extinct here, though more genial circumstances have preserved their existence on the continent of Europe. Of the great Cave Bear, no evidence of its period exists, that I know of, except that which may be deduced from the commixture of its remains with those of other animals of whose recent date we have proof. But there is another kind of Bear, whose relics in a fossil state are not uncommon in the Tertiary deposits, viz., the common Black Bear (Ursus arctos) of Europe. This savage animal must have early succumbed to man. In Ireland it seems to have become extinct even yet earlier. Bede says the only ravenous animals in his day were the wolf and the fox; Donatus, who died in A.D. 840, distinctly says it was not a native of the island in his time; and Geraldus Cambrensis does not enumerate it as known in the twelfth century. Neither is it included in The wolf, however, survived in both islands to a much later era. In the days of the Heptarchy it was a terrible pest; King Edgar commuted the punishment of certain offences into a requisition for a fixed number of wolves' tongues; and he converted a heavy tax on one of the Welsh princes into an annual tribute of three hundred wolves' heads. These laws continued to the time of Edward I., when the increasing scarcity of the animal doubtless caused them to fall into disuse. Mr Topham, in his Notes to Somerville's "Chase," says, that it was in the wolds of Yorkshire that a price was last set on a wolf's head. The last record of their occurring in formidable numbers in England is in 1281; but for three centuries after this, the mountains and forests of Scotland harboured them; for Hollinshed reports that in 1577 the wolves were very troublesome to the flocks of that country. Nor were they entirely destroyed out of this island till about a century afterwards, when the last wolf fell in Lochaber, by the hand of Sir Ewen Cameron of Lochiel. In Ireland the last wolf was slain in 1710. Thus here we are able to lay our finger on the exact dates when a large and rapacious species of animal actually became extinct so far as the British Isles are concerned. And if the species had been confined in its geographical limits, as many other species of animals are, to one group of islands, we should know the precise date of its absolute extinction. The Beaver was once an inhabitant of British rivers. Its remains are found in Berkshire, Cambridgeshire, Yorkshire, and elsewhere, associated with the other Mammalia of the fresh-water deposits and caves, but not in any abundance. No record of its actual existence, however, in these counties exists, nor anywhere else but in Wales and Scotland, whose mountain streams and rugged ravines afforded it shelter till after the Norman Conquest. It was very rare even then, and for a hundred years before; for the laws of Howel Dda, the Welsh king, who died in 948, in determining the value of peltry, fix the price of the beaver's skin at a hundred and twenty pence, when the skins of the stag, the wolf, the fox, and the otter, were worth only eightpence each, that of the white weasel or ermine at twelvepence, and that of the marten, at twenty-four pence. The appropriate epithet of Broad-tail (Llostllyddan) was given it by the Welsh. Giraldus Cambrensis, who travelled through Wales in 1188, gives, in his Itinerary, a short account of the beaver, but states that the river Teivy in Cardiganshire, and one other river in Scotland, were the only places in Great Britain, where it was then found. In all probability it did not long survive that If, as naturalists of the highest eminence believe, there is specific difference between the beaver of Europe and that of America, then we may say that our species is fast passing away from the earth. A few colonies yet linger along the banks of the Danube, the Weser, the Rhone and the Euphrates, but they consist of few individuals, ever growing fewer; and the value of their fur exciting cupidity, they cannot probably resist much longer the exterminating violence of man. The causes which led to the extinction of these animals in our islands are then obvious, and are thus playfully touched by the late James Wilson:—"The beaver might have carried on business well enough, in his own quiet way, although frequently incommoded by the love of peltry on the part of a hat-wearing people; but it is clear that no man with a small family and a few respectable farm servants, could either permit a large and hungry wolf to be continually peeping at midnight through the keyhole of the nursery, or allow a brawny bruin to snuff Perhaps the example of recent extinction most popularly known is that of the Dodo, a very remarkable bird, which about two centuries ago existed in considerable abundance, in the isles of Mauritius, Bourbon, and Rodriguez. It was a rather large fowl, incapable of rising from the ground, by reason of the imperfect development of its wings, of massive, uncouth figure, predisposed to fatness, and noted for the sapidity of its flesh. Two skulls and two unmatched feet of this strange bird are preserved in European museums; and these shew that its nearest affinities were with the pigeon-tribe, of which we know some species of terrestrial habits, but none approaching this bird in its absolute confinement to the earth. In the reports of numerous voyagers who visited these islands from the end of the fifteenth century to the middle of the seventeenth, we have many accounts of the appearance and habits of this bird, evidently sketched from the life. Some of the descriptions, as also the figures by which "The Dodo," he says, "comes first to our description. Here and in Dygarrois (and nowhere else that I cd ever see or heare of) is generated the Dodo. (A Portuguize name it is, and has reference to her simplenes) a bird which for shape and rareness might be call'd a Phoenix (wer't in Arabia); her body is round and extreame fat, her slow pace begets that corpulencie; few of them weigh lesse than fifty pound: better to the eye than the stomack: greasie appetites may perhaps commend them, but, to the indifferently curious, nourishment, but prove offensive. Let's take her picture: her visage darts forth melancholy, as sensible of nature's injurie in framing so great and massive a body to be directed by such small and complementall wings, as are unable to hoise her from the ground, serving only to prove her a bird; which otherwise might be doubted of: her head is variously drest, the one halfe hooded with downy blackish feathers; the other perfectly naked; of a whitish hue, as if a transparent lawne had covered it; her bill is very howked and bends downwards, the thrill or breathing place is in the midst of it; from which part to the end, the colour is a light greene mixt with a pale yellow; her eyes be round and small, and bright as diamonds; her cloathing is of finest downe, such as ye see in goslins; her trayne is (like a China beard) of three or foure It is pretty certain that a living specimen was about the same time exhibited in England. Sir Hamon L'Estrange tells us distinctly that he saw it. His original MS. is preserved in the British Museum, and with some blanks caused by the injury of time, of no great consequence, reads as follows:— "About 1638, as I walked London streets, I saw the picture of a strange fowl hong out upon a cloth. vas and myselfe with one or two more Gen. in company went in to see it. It was kept in a chamber, and was a greate fowle somewhat bigger than the largest Turky Cock and so legged and footed but stouter and thicker and of a more erect shape, coloured before like the breast of a yong Cock Fesan and on the back of dunn or deare coulour. The keeper called it a Dodo and in the ende of a chimney in the chamber there lay an heap of large pebble stones whereof hee gave it many in our sight, some as bigg as nutmegs and the keeper told us shee eats them conducing to digestion and though I remember not how farre the keeper was questioned therein yet I am confident that afterwards shee cast them all agayne." It is probable that this very specimen passed into the museum of Tradescant, who, in the Catalogue of "The Collection of Rarities preserved at Lambeth," dated 1656, mentions the following: "Dodar from the Island Mauritius: it is not able to flie being so bigg." Willoughby the ornithologist, a most unexceptionable testimony, says that he saw this specimen in Tradescant's museum: it is mentioned also by others;—as by Llhwyd in 1684, and by Hyde in 1700. It passed, with the rest of the Tradescant Collection, to Oxford, and thus became part of the Ashmolean Museum,—and being in a decayed condition, was ordered to be destroyed by the authorities, who had no apprehension of its value, in 1755. The skull and one foot, however, were preserved, and are still in the Museum at Oxford. Remains of the Dodo have been dug up in the Mauritius, and are in the Paris Museum, and in that of the Zoological Society of London. The bird certainly does not exist there now, nor in either of the neighbouring islands. In the British Museum there is a fine original painting, once the property of George Edwards, the celebrated bird painter, representing the Dodo surrounded by other minor birds and reptiles. Edwards states that "it was drawn in Holland, from a living bird brought from St Maurice's Island, in the East Indies. It was the property of Sir Hans Sloane at the time of his death, and afterwards becoming my property, I deposited it in the British Museum as a great curiosity." Professor Owen has discovered another original figure It is possible that there were two species of Dodo; which would explain certain discrepancies in the descriptions of observers. At all events we have here one, if not more, conspicuous animal absolutely extinguished within the last two hundred years. Just about a century ago a great animal disappeared from the ocean, which, according to Owen, was contemporary with the fossil elephant and rhinoceros of Siberia and England. Steller, a Russian voyager and naturalist, discovered the creature, afterward called Stelleria by Cuvier, in Behring's Straits; a huge, unwieldy whale-like animal, one of the marine pachyderms, allied to the Manatee, but much larger, being twenty-five feet long, and twenty in circumference. Its flesh was good for food, and from its inertness and incapacity for defence, the race was extirpated in a few years. Steller first discovered the species in 1741, and the last known specimen was killed in 1768. It is believed to be quite extinct, as it has never been met with since. Nearly a century ago, Sonnerat found in Madagascar, a curious animal, (Cheiromys,) which in structure seems to connect the monkeys with the squirrels. So rare was it there that even the natives viewed it with curiosity as an animal altogether unknown to them; and, from their Species are dying out in our own day. I have already cited the interesting case of the Moho, that fine Gallinule of New Zealand, of which a specimen—probably the last of its race,—was obtained by Mr Walter Mantell; and that of the KÁureke, the badger-like quadruped of the same islands, which was formerly domesticated by the Maoris, but which now cannot be found. The Samoa Isles in the Pacific recently possessed a large and handsome kind of pigeon, of richly-coloured plumage, which the natives called Manu-mea, but to which modern naturalists have given the name of Didunculus strigirostris. It was, both by structure and habit, essentially a ground pigeon, but not so exclusively but that it fed, and roosted too, according to Lieut. Walpole, among the branches of tall trees. Mr T. Peale, the naturalist of the U. S. Exploring Expedition, who first described it, informs us that according to the tradition of the natives, it once abounded; but some years ago these persons, like more civilised folks, had a strong desire to make pets of cats, and found, by means of whale-ships, opportunities of procuring a supply; but the consequence of the introduction of "pussy,"—for under this familiar old-country title were the exotic tabbies introduced—was the rapid When Norfolk Island,—that tiny spot in the Southern Ocean since so stained with human crime and misery—was first discovered, its tall and teeming forests were tenanted by a remarkable Parrot with a very long and slender hooked beak, which lived upon the honey of flowers. It was named Nestor productus. When Mr Gould visited Australia in his researches into the ornithology of those antipodeal regions, he found the Nestor Parrot absolutely limited to Philip Island, a tiny satellite of Norfolk Island, whose whole circumference is not more "I have seen the man who exterminated the Nestor productus from Philip Island, he having shot the last of that species left on the island; he informs me that they rarely made use of their wings, except when closely pressed; their mode of progression was by the upper mandible; and whenever he used to go to the island to shoot, he would invariably find them on the ground, except one, which used to be sentry on one of the lower branches of the Araucaria excelsa, and the instant any person landed, they would run to those trees and haul themselves up by the bill, and, as a matter of course, they would there remain till they were shot, or the intruder had left the island. He likewise informed me that there was a large species of hawk that used to commit great havoc amongst them, but what species it was he could not tell me." I have before mentioned that Professor Owen had recognised the species in fossil skulls from New Zealand, associated with remains of Dinornis, Palapteryx, and Notornis. Thus it appears that the long-billed Parrot is an ancient race, whose extreme decrepitude has just survived to our time;—that it first became extinct from New Mr Yarrell, in his "History of British Birds," This fine bird, which was larger than a goose, is believed to be extinct. Mr Bullock's specimen was taken in 1812; another was captured at St Kilda in 1822, another was picked up dead near Lundy Island in 1829, and yet another was taken in 1834, off the coast of Waterford. On the north coast of Europe the bird is equally rare; Two centuries ago, the Great Auk was not uncommon on the shores of New England; and, off the great fishing-banks of Newfoundland, it appears to have been very abundant. "Its appearance was always hailed by the mariner approaching that desolate coast as the first indication of his having reached soundings on the fishing-banks. During the sixteenth and seventeenth centuries these waters, as well as the Iceland and Faroe coasts, were annually visited by hundreds of ships from England, France, Spain, Holland, and Portugal; and these ships actually were accustomed to provision themselves with the bodies and eggs of these birds, which they found breeding in myriads on the low islands off the coast of Newfoundland. Besides the fresh birds consumed by the ship's crew, many tons were salted down for further use. In the space of an hour, these old voyagers tell us, they could fill thirty boats with the birds. It was only necessary to go on shore, armed with sticks to kill as many "In 1841, a distinguished Norwegian naturalist, (too early, alas! lost to science,) Peter Stuwitz, visited Tunk Island, or Penguin Island, lying to the east of Newfoundland. Here, on the north-west shore of the island, he found enormous heaps of bones and skeletons of the Great Auk, lying either in exposed masses or slightly covered by the earth. On this side of the island the rocks slope gradually down to the shore; and here were still standing the stone fences and enclosures into which the birds were driven for slaughter." It is just possible that the bird may yet haunt the inaccessible coast of East Greenland, but ships sailing between that country and Iceland never meet with it at sea. Nor did Graah observe it during his toilsome researches east of Cape Farewell. The numerous fishing craft that every season crowd the shores of Newfoundland and Labrador forbid the notion that it yet lingers there; for the great market-value set upon the bird and its eggs for collections would prevent its existence there from being overlooked. The numerous Polar voyages of dis The interest attached to this now extinct bird has induced some correspondents of the Zoologist to attempt an enumeration of the specimens, both of the bird and of its eggs, (which from their great size, as well as from their rarity, have always had a value with collectors,) known to be preserved in cabinets. The result is that English collections contain 14 birds and 23 eggs; those of continental Europe, 11 birds and 20 eggs; the United States, 1 bird and 2 eggs:—the total being 26 birds and 45 eggs. It would appear that the rock off the south of Iceland which was the chief breeding resort of the Great Auk, and which from that circumstance bore the name or "Geir-fulga Sker," sank to the level of the sea during a volcanic disturbance in or about the year 1830. "Such disappearance of the fit and favourable breeding-places of the Alca impennis," observes Professor Owen, "must form an important element in its decline towards extinction." One might think that there would be rocks enough left for the birds to choose a fresh station; but Mr Darwin speaks of a large wolf-like Fox (Canis antarcticus) which at the time of his voyage was common to both the Falkland Islands, but absolutely confined to them. He says, "As far as I am aware, there is no other instance in any part of the world, of so small a mass of broken land, distant from a continent, possessing so large an aboriginal quadruped peculiar to itself. Their numbers have rapidly decreased; they are already banished from that half of the island which lies to the eastward of the neck of land between St Salvador Bay and Berkeley Sound. Within a very few years after these islands shall have become regularly settled, in all probability this fox will be classed with the Dodo, as an animal which has perished from the face of the earth." The Musk Ox (Ovibos moschatus), a long-haired ruminant, resembling what you would suppose a cross between a bull and a sheep might be,—formerly an inhabitant of Britain with the Elephant and the Hyena, but now found From the more perishable character of vegetable tissues we have far less data for determining the extinction of plant species; but analogy renders it highly probable that these also have died out, and are dying in a corresponding ratio with animals. I am not aware that a single example can be adduced of a plant that has certainly ceased to exist during the historic era. But Humboldt mentions a very remarkable tree in Mexico, of which it is believed only a single specimen remains in a state of nature. It is the Hand-tree (Cheirostemon platanoides), a sterculaceous plant with large plane-like leaves, and with the anthers connected together in such a manner as to resemble a hand or claw rising from the beautiful purplish-red blossoms. "There is in all the Mexican free States only one individual remaining, one single primeval stem of this wonderful genus. It is supposed not to be indigenous, but to have been planted by a king of Toluca about five hundred years ago. I found that the spot where the Arbol de las Manitas stands is 8825 feet above the level of the sea. Why is there only one tree of the kind? Whence did the kings of Toluca obtain the young tree, or the seed? It is equally enigmatical that Montezuma should not have possessed one of these trees in his botanical gardens of Huaxtepec, Chapoltepec, and Iztapalapan, which were used as late as by Philip the Second's There is an example of this interesting plant growing in one of the conservatories at Kew, but I do not know whence it was obtained. It has been asserted that it grows wild in the forests of Guatemala. Leaving plants out of consideration from lack of adequate data, we find that a considerable number of species of animals have certainly ceased to exist since man inhabited the globe. There have been, doubtless, many others that have shared the same fate, which we know nothing about. It is only within the last hundred years that we have had anything approaching to an acquaintance with the living fauna of the earth; yet, during that time some seven or eight creatures we know have been extinguished. Fully half of these,—the Auk, the Didunculus, the Notornis, and the Nestor,—within the last ten years! It would really seem as if the more complete and comprehensive an acquaintance with the animals of the world became, the more frequently this strange phenomenon of expiring species was presented to us. Perhaps it is not extravagant to suppose that—including all the invertebrate animals, the countless hosts of insects, and all the recondite forms that dwell in the recesses of the ocean—a species fades from existence every year. All the examples I know not whether my readers will take the same concern as I do in this subject of the dying-out of species, but to me it possesses a very peculiar interest. Death is a mysterious event, come when and how it will; and surely the departure from existence of a species, of a type of being, that has subsisted in contemporary thousands of individuals, for thousands of years, is not less imposingly mysterious than that of the individual exemplar. We do not know with any precision what are the immediate causes of death in a species. Is there a definite limit to life imposed at first? or is this limit left, so to speak, to be determined by accidental circumstances? Perhaps both: but if the latter, what are those circumstances? Professor Owen says:—"There are characters in land animals rendering them more obnoxious to extirpating influences, which may explain why so many of the larger species of particular groups have become extinct, whilst smaller species of equal antiquity have survived. In proportion to its bulk is the difficulty of the contest which the animal has to maintain against the surrounding agencies that are ever tending to dissolve the vital bond, and "We do not steadily bear in mind," remarks Mr Darwin, "how profoundly ignorant we are of the condition of existence of every animal; nor do we always remember that some check is constantly preventing the too rapid "In the cases where we can trace the extinction of a species through man, either wholly or in one limited dis Geographical distribution is an important element in this question of extinction. A species that is spread over a wide region is far more likely to survive than one which is confined to a limited district; and extraneous influences acting prejudicially will exterminate a species which is confined to an island much sooner than if it had a continent to retire upon. We have seen how the Nestor Parrot became extinct in New Zealand, while it survived in Norfolk Island, because the former was colonised by the Maori race, while the latter remained in its virginity. But how quickly did the poor Parrot succumb as soon as man set his foot on Norfolk and Philip Islands! And how brief was the lease of life accorded to the Didunculus, when once the "Pussies" found their way to the little Samoa isles! Very many islands have a fauna that is to a great extent peculiar to themselves. I know that, in Jamaica, the Humming-birds, some of the Parrots, some of the Cuckoos, most of the Pigeons, many of the smaller birds, and, I think, all of the Reptiles, are found nowhere else. Nay, more, that even the smaller islands of the Antilles have each a fauna of its own, unshared with any other land;—its own Humming-birds, its own Lizards and The common Red Grouse, so abundantly seen during the season hanging at every poulterer's and game-dealer's shop in London, is absolutely unknown out of the British Isles. It could not live except in wide, unenclosed, uncultivated districts; so that when the period arrives that the whole of British land is enclosed and brought under cultivation, the Grouse's lease of life will expire. We owe it to our hard-worked members of Parliament to hope that this condition of things may be distant. |