HOWORTH (1887) continued:
“In Siberia, as we have seen, the death of the Mammoth and its companions was immediately followed by a sudden declension in temperature, which of itself and in the absence of other causes made that area incompatible with the life conditions of the Mammoth, but this was a correlative occurrence, and not the immediate cause of the great destruction. It is unlikely that the cold would have killed the bear and glutton, the musk-sheep, etc., which we know were in many instances overwhelmed by the same cause, whatever it was that destroyed the Mammoth.
The fact of the bones occurring in great caches or deposits, in which various species are mixed pell-mell, is very important. Different species do not come together to do so, nor does the lion come to take his last sleep with the lamb. The fact of finding masses of animal remains of mixed species, all showing the same state of preservation, not only points to a more or less contemporary death, but is quite fatal to the theory that they ended their days peaceably by purely normal causes.
Their state of preservation proves that they were covered over and protected immediately after their deposition, and have remained so covered and protected ever since, and this along many degrees of longitude, and by continuous undisturbed beds of clay and gravel.
Wrangell says, "The best Mammoth bones, as well as the greatest number, are found at a certain depth below the surface, usually in clay-hills, more rarely in black earth. The more solid the clay, the better the bones are preserved. Experience has also shown that more are found in elevations situated near high hills…”
The evidence is equally or even more conclusive from Europe, where, in the great deposits of loess and in the brick clays, &c., in many places, as at Folkestone, Flamborough Head, Bournemouth, &c., we find the caches of bones in positions entirely out of the reach of any possible rivers or river floods, and on the Continent in beds which are quite undisturbed and continuous over large areas, showing that they were spread by some continuous and far-reaching cause.
Schmidt, probably the most skilled geologist who has examined the Siberian Mammoth-beds in situ, says in reference to this very notion, "The northern rivers throw down no great amount of mud. No Mammoth could sink into the brown layers of mud which remain on the low grounds after spring floods.”
Vast hecatombs are found in certain places like New Siberia, 150 miles distant from, or in high grounds far away from any possible river channel…remains are found where no river could possibly flow.
Myriads of fresh skeletons of Mammoths, rhinoceroses, bisons, etc., in Siberia or in Europe...have every sign that they formed parts of a contemporaneous fauna destroyed at the same time.
As Cuvier says, arguing from another point,
"But how have so many ferocious beings that inhabited our forests been extirpated from them? The only answer we can provide is that they must have been destroyed at the same time and by the same cause as the great herbivores that inhabited the forests alongside them, and of whom no more traces are found today."
However ingeniously and with whatever subtlety we may deal with our evidence, the facts constrain us therefore to one inevitable conclusion, namely, that the Mammoth and its companions perished by some wide-spread catastrophe which operated over a wide area and not through the slow processes of the ordinary struggle for existence, and that the greater portion of the remains we find in Siberia and Europe are not the result of gradual accumulation under normal causes for untold ages, but the result of one of Nature's hecatombs on a grand and wide-spread scale, when a vast fauna perished simultaneously.
We must next inquire what the nature of this catastrophe was.
The first piece of evidence I would quote is of a singularly direct kind, and we owe it to the experienced skill of Professor Brandt. Speaking of the famous rhinoceros found on the Wilui by Pallas, he says, "On a careful examination of the head of the Rhinoceros Tichorinus from the Wilui, it was further remarkable that the blood-vessels and even the fine capillaries were seen to be filled with brown coagulated blood, which, in many places still preserved its red colour." This is exactly the kind of evidence we look for when we want to know whether an animal has been drowned or suffocated. Asphyxia is always accompanied by the gorging of the capillaries with blood, and the facts justify at all events a probable inference that this particular rhinoceros was the victim of drowning.
Schrenck submitted the head of the Rhinoceros Merkii, already described, to a similar examination, and one passage in his memoir is singularly interesting when taken in conjunction with the remarks of Brandt just quoted. Speaking of its nostrils, he says, "They were wide open, and in the case of the one on the right side, which was uninjured, a number of horizontal folds were ranged in rows about it. The mouth was also partly open, whence it may be concluded that the animal died from suffocation, which it tried to avoid by keeping the nostrils wide asunder."
To continue. The occurrence of immense caches in which the remains of many species of wild animals are incongruously mixed together pell-mell, often on high ground, seems unaccountable, save on the theory that they were driven to take shelter together on some point of vantage, in view of an advancing flood of water, collecting together on some dry place, and reduced to a common condition of timidity and helplessness by a flood which has overwhelmed the flat country. As Horace says, referring to Deucalion’s deluge,
"Omne cum Proteus pecus egit altos
Visere montes." (When Proteus drove all his flock to visit the high mountains.)
Evidence is forthcoming from the deposits where the Mammoths' remains occur further inland, and where we find marine shells which clearly evidence the former presence of the ocean. This was known to Pallas, and has been confirmed amply by Middendorf and others. Thus the former describes the occurrence near Ust Tatarskoi on the Irtish of numerous shells, mostly fossilized, but others preserving their horny pellicles, and in some cases retaining traces of the mollusk itself. In these same layers were found the bones of elephants and many other animals. "This undoubtedly," he adds, "has come from a great inundation. We have in it an evident proof that the sea once bathed these countries."
At a short distance from Kopanofskoi on the Volga were found several bones of an elephant. Pallas says he "obtained a jaw-bone much petrified, and as-it-were coated with fine gravel and muscles.”
Murchison describes pleistocene marine shells as occurring a long way south of the White Sea. Similar marine shells are found mixed with Mammoths' remains in the valley of the Lower Somme, and in the deposits of the English Channel, while we know that the sea bottom from Lowestoft to Dunkirk is strewn with large numbers of Mammoths' bones; so in Torbay, etc…traces of the results of a catastrophe.
This completes my survey of the evidence furnished by the Mammoth itself, and I believe that not only is it consistent with the conclusion that that animal and its companions were finally extinguished by a sudden catastrophe, involving a great diluvial movement. The evidence is not only ample, but it is evidence which converges from all sides.
I will lastly quote the opinion of Erman, whose critical skill and knowledge were perhaps greater than those of any of the Siberian explorers. He has the following remarks: "The ground at Yakutsk . . . consists, to the depth of at least 100 feet, of strata of loam, pure sand, and magnetic sand. They have been deposited from waters which at one time, and it may be presumed suddenly, overflowed the whole country as far as the Polar Sea. In these deepest strata are found twigs, rocks, and leaves of trees of the birch and willow kinds; Everywhere throughout these immense deposits are now lying the bones of antediluvian quadrupeds along with vegetable remains.
It is only in the lower strata of the New Siberian wood-hills that the trunks have that position which they would assume in swimming or sinking undisturbed. On the summit of the hills they lie flung upon one another in the wildest disorder, forced upright in spite of gravitation, and with their tops broken off or crushed as if they had been thrown with great violence from the south on a bank, and there heaped up. Now a smooth sea covering the tops of these hills on the islands, would, even with the present form of the interjacent ground, extend to Yakutsk, which is but 270 feet above the sea.
The flood may have poured down from the high mountains through the rocky valleys. The animals and trees which it carried off from above could sink but slowly in the muddy and rapid waves, but must have been thrown upon the older parts of Kotelnoi and New Siberia in the greatest number and with the greatest force..”
THE MAMMOTH AND THE FLOOD
HENRY H. HOWORTH (1887)