other Quadrumana had been met with, a short time previously, in different stages of the tertiary series, in India, France, and Brazil.

When we consider the small area of the earth's surface hitherto examined geologically, and our scanty acquaintance with the fossil Vertebrata, even of the environs of great European capitals, it is truly surprising that any naturalist should be rash enough to assume that the Lower Eocene deposits mark the era of the first creation of Quadrumana. It is, however, still more unphilosophical to infer from a single extinct species of this order, obtained in a latitude far from the tropics, that the Eocene Quadrumana had not attained as high a grade of organization as those of our own times, when the naturalist is acquainted with all, or nearly all, the species of monkeys, apes and orangs which are contemporary with man.

To return to the year 1830, Mammalia had not then been traced to rocks of higher antiquity than the Stonesfield Oolite, whereas we have just seen that memorials of this class have at length made their appearance in the Trias of Germany. In 1830 birds had been discovered no lower in the series than the Paris gypsum, or Middle Eocene. Their bones have now been found both in England and the Swiss Alps in the Lower Eocene, and their existence has been established by foot-prints in the triassic epoch in North America (p. 297.). Reptiles in 1830 had not been detected in rocks older than the Magnesian limestone, or Permian formation; whereas the skeletons of four species have since been brought to light (see p. 336.) in the coal-measures, and one in the Old Red sandstone, of Europe, while the footprints of three or four more have been observed in carboniferous rocks of North America, not to mention the chelonian trail above described, from the most ancient of the fossiliferous rocks of Canada, the "Potsdam Sandstone," which lies at the base of the Lower Silurian system. (See above, p. vii.)

Lastly, the remains of fish, which in 1830 were scarcely recognized in deposits older than the coal, have now been found plentifully in the Devonian, and sparingly in the Silurian, strata; though not in any formation of such high antiquity as the Chelonian of Montreal.

Previously to the discovery last mentioned, it was by no means uncommon for paleontologists to speak with confidence of fish as having been created before reptiles. It was deemed reasonable to suppose that the introduction of a particular class or order of beings into the planet coincided, in date, with the age of the oldest rock to which the remains of that class or order happened then to have been traced back. To be consistent with themselves, the same naturalists ought now to take for granted that reptiles were called into existence before fish. This they will not do, because such a conclusion would militate against their favourite hypothesis of an ascending scale, according to which Nature "evolved the organic world," rendering it more and more perfect in the lapse of ages.

In our efforts to arrive at sound theoretical views on such a question, it would seem most natural to turn to the marine invertebrate animals as to a class affording the most complete series of monuments that have come down to us, and where we can find corresponding terms of comparison, in strata of every age. If, in this more complete series of her archives, Nature had really exhibited a more simple grade of organization in fossils of the remotest antiquity, we might have suspected that there was some foundation of facts in the theory of successive development. But what do we find? In the Lower Silurian there is a full representation of the Radiata, Mollusca, and Articulata proper to the sea. The marine Fauna, indeed, in those three classes, is so rich as almost to imply a more perfect development than that which now peoples the ocean. Thus, in the great division of the Radiata, we find asteroid and helianthoid zoophytes, besides crinoid and cystidean echinoderms. In the Mollusca of the same most ancient epoch M. Barrande enumerates, in Bohemia alone, the astonishing number of 253 species of Cephalopoda. In the Articulata we have the crustaceans, represented by more than 200 species of Trilobites, not to mention other genera.

It is only then, in reference to the Vertebrata, that the argument of degeneracy in proportion as we trace fossils back to older formations can be maintained; and the dogma rests mainly for its support on negative evidence, whether deduced from the entire absence of the fossil representatives of certain classes in particular rocks, or the low grade of the first few species of a class which chance has thrown in our way.

The scarcity of all memorials of birds in strata below the Eocene, has been a subject of surprise to some geologists. The bones formerly referred to birds in the Wealden and Chalk, are now admitted to have belonged to flying reptiles, of various sizes, one of them from the Kentish chalk so large as to have measured 16 feet 6 inches from tip to tip of its outstretched wings. Whether some elongated bones of the Stonesfield Oolite should be referred to birds, which they seem greatly to resemble in microscopic structure or to Pterodactyles, is a point now under investigation. If it should be proved that no osseous remains of the class Aves have hitherto been derived from any secondary or primary formation, we must not too hastily conclude that birds were even scarce in these periods. The rarity of such fossils in the Eocene marine strata is very striking. In 1846, Professor Owen, in his "History of the Fossil Mammalia and Birds of Great Britain," was unable to obtain more than four or five fragments of bones and skulls of birds from the London Clay, by the aid of which four species were recognized. Even so recently, therefore, as 1846, as much was known of the Mammalia of the Stonesfield Oolite, as of the ornithic Fauna of our English Eocene deposits.

To reason correctly on the value of negative facts in this branch of Paleontology, we must first have ascertained how far the relics of birds are now becoming preserved in new strata, whether marine, fluviatile, or lacustrine. I have explained, in the "Principles of Geology," that the imbedding of the bones of living birds in deposits now in progress in inland lakes appears to be extremely rare. In the shell-marl of Scotland, which is made up bodily of the shells of the genera Limneus, Planorbis, Succinea, and Valvata, and in which the skeletons of deer and oxen abound, we find no bones of birds. Yet we know that, before the lakes were drained which yield this marl used in agriculture, the surface of the water and the bordering swamps were covered with wild ducks, herons, and other fowl. They left no memorials behind them, because, if they perished on the land, their bodies decomposed or became the prey of carnivorous animals; if on the water, they were buoyant and floated till they were devoured by predaceous fish or birds. The same causes of obliteration have no power to efface the foot-prints which the same creatures may leave, under favourable circumstances, imprinted on an ancient mud-bank or shore, on which new strata may be from time to time thrown down. In the red mud of recent origin spread over wide areas by the high tides of the bay of Fundy, innumerable foot-tracks of recent birds (Tringa minuta) are preserved in successive layers, and hardened by the sun. Yet none of the bones of these birds, though