LITMIR.BIZ

      Published by Good Press, 2019

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      EAN 4057664564771

Table of Contents

       THE ROMANCE OF NATURAL HISTORY.

       I.

       THE EXTINCT.

       II.

       THE MARVELLOUS.

       III.

       MERMAIDS.

       IV.

       THE SELF-IMMURED.

       V.

       HYBERNATION OF SWALLOWS.

       VI.

       THE CRESTED AND WATTLED SNAKE.

       VII.

       THE DOUBTFUL.

       VIII.

       FASCINATION.

       IX.

       SERPENT-CHARMING.

       X.

       BEAUTY.

       XI.

       PARASITES.

       APPENDIX.

       ON THE SEA-SERPENT.

       THE END.

       INDEX.

       BALLANTYNE AND COMPANY, PRINTERS, EDINBURGH.

       By the same Author.

THE ROMANCE OF NATURAL HISTORY.

       Table of Contents

I.

       Table of Contents

THE EXTINCT.

       Table of Contents

      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 species may have assigned to its life, for aught I know, a hundred thousand years as its normal period, and another not more than a thousand. If creation was, with respect to the species, what I have elsewhere proved it was with respect to the individual,[1]—a violent irruption into the cycle of life—then we may well conceive this to have taken place at very varying relative periods in the life-history of the different species;—that is to say, that at a given date, (viz., that of creation) one species might be just completing, ideally, its allotted course, another just commencing, and a third attaining its meridian.

      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 soon see them no more; that the sentence is gone forth against them; that their sands are running to the last grains, and that no effort of ours can materially prolong their existence. The facts from which these conclusions are drawn are highly curious, and I shall endeavour to lay them, with as much brevity as they will allow, before my readers.

      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

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