CHAPTER III.

Lamarck's Theory of Progression illustrated.--Class of Facts which

give Color to it.--The Credulity of Unbelief.--M. Maillet and his

Fish-birds.--Gradation not Progress.--Geological Argument.--The

Present incomplete without the Past.--Intermediate Links of

Creation.--Organisms of the Lower Old lied Sandstone.--The

_Pterichthys_.--Its first Discovery.--Mr. Murchison's Decision

regarding it.--Confirmed by that of Agassiz.--Description.--The

several Varieties of the Fossil yet discovered.--Evidence of Violent

Death in the Attitudes in which they are found.--The _Coccosteus_

of the Lower Old Red.--Description.--Gradations from Crustacea to

Fishes.--Habits of the Coccosteus.--Scarcely any Conception too

extravagant for Nature to realize.

Mr. Lyell's brilliant and popular work, _The Principles of Geology_,

must have introduced to the knowledge of most of my readers the

strange theories of Lamarck. The ingenious foreigner, on the strength

of a few striking facts, which prove that, to a certain extent,

the instincts of species may be improved and heightened, and their

forms changed from a lower to a higher degree of adaptation to

their circumstances, has concluded that there is a natural progress

from the inferior orders of being towards the superior; and that

the offspring of creatures low in the scale in the present time,

may hold a much higher place in it, and belong to different and

nobler species, a few thousand years hence. The descendants of the

_ourang-outang_, for instance, may be employed in some future age in

writing treatises on Geology, in which they shall have to describe

the remains of the _quadrumana_ as belonging to an extinct order.

Lamarck himself, when bearing home in triumph with him the skeleton

of some huge salamander or crocodile of the Lias, might indulge,

consistently with his theory, in the pleasing belief that he had

possessed himself of the bones of his grandfather--a grandfather

removed, of course, to a remote degree of consanguinity, by the

intervention of a few hundred thousand _great-greats_. Never yet

was there a fancy so wild and extravagant but there have been men

bold enough to dignify it with the name of philosophy, and ingenious

enough to find reasons for the propriety of the name.

The setting-dog is _taught_ to set; he squats down and points at the

game; but the habit is an acquired one--a mere trick of education.

What, however, is merely acquired habit in the progenitor, is

found to pass into instinct in the descendant: the puppy of the

setting-dog squats down and sets _untaught_--the educational trick

of the parent is mysteriously transmuted into an original principle

in the offspring. The adaptation which takes place in the forms and

constitution of plants and animals, when placed in circumstances

different from their ordinary ones, is equally striking. The

woody plant of a warmer climate, when transplanted into a colder,

frequently exchanges its ligneous stem for a herbaceous one, as if

in anticipation of the killing frosts of winter; and, dying to the

ground at the close of autumn, shoots up again in spring. The dog,

transported from a temperate into a frigid region, exchanges his

covering of hair for a covering of wool; when brought back again to

his former habitat, the wool is displaced by the original hair. And

hence, and from similar instances, the derivation of an argument,

good so far as it goes, for changes in adaptation to altered

circumstances of the organization of plants and animals, and for the

unprovability of instinct. But it is easy driving a principle too

far. The elasticity of a common bow, and the strength of an ordinary

arm, are fully adequate to the transmission of an arrow from one

point of space to another point a hundred yards removed; but he would

be a philosopher worth looking at, who would assert that they were

equally adequate for the transmission of the same arrow from points

removed, not by a hundred yards, but by a hundred miles. And such,

but still more glaring, has been the error of Lamarck. Fie has argued

on this principle of improvement and adaptation--which, carry it as

far as we rationally may, still leaves the vegetable a vegetable, and

the dog a dog--that, in the vast course of ages, inferior have risen

into superior natures, and lower into higher races; that molluscs and

zoöphytes have passed into fish and reptiles, and fish and reptiles

into birds and quadrupeds; that unformed, gelatinous bodies, with an

organization scarcely traceable, have been metamorphosed into oaks

and cedars; and that monkeys and apes have been transformed into

human creatures, capable of understanding and admiring the theories

of Lamarck. Assuredly there is no lack of faith among infidels;

their "vaulting" credulity o'erleaps revelation, and "falls on the

other side." One of the first geological works I ever read was a

philosophical romance, entitled _Telliamed_, by a M. Maillet, an

ingenious Frenchman of the days of Louis XV. This Maillet was by

much too great a philosopher to credit the scriptural account of

Noah's flood; and yet he could believe, like Lamarck, that the whole

family of birds had existed at one time as fishes, which, on being

thrown ashore by the waves, had got feathers by accident; and that

men themselves are but the descendants of a tribe of sea-monsters,

who, tiring of their proper element, crawled up the beach one sunny

morning, and, taking a fancy to the land, forgot to return.[H]

[Footnote H: Few men could describe better than Maillet. His

extravagances are as amusing as those of a fairy tale, and quite as

extreme. Take the following extract as an instance:--

"Winged or flying fish, stimulated by the desire of prey, or the

fear of death, or pushed near the shore by the billows, have fallen

among reeds or herbage, whence it was not possible for them to resume

their flight to the sea, by means of which they had contracted

their first facility of flying. Then their fins, being no longer

bathed in the sea-water, were split, and became warped by their

dryness. While they found, among the reeds and herbage among which

they fell, any aliments to support them, the vessels of their fins,

being separated, were lengthened and clothed with beards, or, to

speak more justly, the membranes, which before kept them adherent

to each other, were metamorphosed. The beard formed of these warped

membranes was lengthened. The skin of these animals was insensibly

covered with a down of the same color with the skin, and this down

gradually increased. The little wings they had under their belly,

and which, like their wings, helped them to walk in the sea, became

feet, and served them to walk on land. There were also other small

changes in their figure. The beak and neck of some were lengthened,

and those of others shortened. The conformity, however, of the first

figure subsists in the whole, and it will be always easy to know it.

Examine all the species of fowls, large and small, even those of

the Indies, those which are tufted or not, those whose feathers are

reversed, such as we see at Damietta--that is to say, whose plumage

runs from the tail to the head--and you will find species of fish

quite similar, scaly or without scales. All species of parrots, whose

plumages are so different, the rarest and the most singular-marked

birds, are, conformable to fact, painted like them with black, brown,

gray, yellow, green, red, violet color, and those of gold and azure;

and all this precisely in the same parts where the plumages of those

birds are diversified in so curious a manner."--_Telliamed_, p. 224,

ed. 1750.]

"How easy," says this fanciful writer, "is it to conceive the change

of a winged fish, flying at times through the water, at times through

the air, into a bird flying always through the air!" It is a law of

nature, that the chain of being, from the lowest to the highest form

of life, should be, in some degree, a continuous chain; that the

various classes of existence should shade into one another, so that

it often proves a matter of no little difficulty to point out the

exact line of demarcation where one class or family ends, and another

class or family begins. The naturalist passes from the vegetable

to the animal tribes, scarcely aware, amid the perplexing forms of

intermediate existence, at what point he quits the precincts of the

one to enter on those of the other. All the animal families have, in

like manner, their connecting links; and it is chiefly out of these

that writers such as Lamarck and Maillet construct their system.

They confound gradation with progress. Geoffrey Hudson was a very

short man, and Goliath of Gath a very tall one, and the gradations

of the human stature lie between. But gradation is not progress; and

though we find full-grown men of five feet, five feet six inches, six

feet, and six feet and a half, the fact gives us no earnest whatever

that the race is rising in stature, and that at some future period

the average height of the human family will be somewhat between ten

and eleven feet. And equally unsolid is the argument, that from a

principle of gradation in races would deduce a principle of progress

in races. The tall man of six feet need entertain quite as little

hope of rising into eleven feet as the short man of five; nor has the

fish that occasionally flies any better chance of passing into a bird

than the fish that only swims.

Geology abounds with creatures of the intermediate class: there

are none of its links more numerous than its connecting links; and

hence its interest, as a field of speculation, to the assertors of

the transmutation of races. But there is a fatal incompleteness in

the evidence, that destroys its character as such. It supplies in

abundance those links of generic connection, which, as it were,

marry together dissimilar races; but it furnishes no genealogical

link to show that the existences of one race derive their lineage

from the existences of another. The scene shifts, as we pass from

formation to formation; we are introduced in each to a new _dramatis

personæ_; and there exist no such proofs of their being at once

different and yet the same, as those produced in the _Winter's Tale_,

to show that the grown shepherdess of the one scene is identical with

the exposed infant of the scene that went before. Nay, the reverse

is well nigh as strikingly the case, as if the grown shepherdess had

been introduced into the earlier scenes of the drama, and the child

into its concluding scenes.

The argument is a very simple one. Of all the vertebrata, fishes

rank lowest, and in geological history appear first. We find their

remains in the Upper and Lower Silurians, in the Lower, Middle,

and Upper Old Red Sandstone, in the Mountain Limestone, and in

the Coal Measures; and in the latter formation the first reptiles

appear. Fishes seem to have been the master existences of two great

systems, mayhap of three, ere the age of reptiles began. Now fishes

differ very much among themselves: some rank nearly as low as worms,

some nearly as high as reptiles; and if fish could have risen into

reptiles, and reptiles into mammalia, we would necessarily expect to

find lower orders of fish passing into higher, and taking precedence

of the higher in their appearance in point of time, just as in the

_Winter's Tale_ we see the infant preceding the adult. If such be

not the case--if fish made their first appearance, not in their

least perfect, but in their most perfect state--not in their nearest

approximation to the worm, but in their nearest approximation to

the reptile--there is no room for progression, and the argument

falls. Now it is a geological fact, that it is fish of the higher

orders that appear first on the stage, and that they are found to

occupy exactly the same level during the vast period represented by

five succeeding formations. There is no progression. If fish rose

into reptiles, it must have been by sudden transformation--it must

have been as if a man who had stood still for half a lifetime should

bestir himself all at once, and take seven leagues at a stride. There

is no getting rid of miracle in the case--there is no alternative

between creation and metamorphosis. The infidel substitutes

progression for Deity; Geology robs him of his god.

But no man who enters the geological field in quest of the wonderful,

need pass in pursuit of his object from the true to the fictitious.

Does the reader remember how, in Milton's sublime figure, the body

of Truth is represented as hewn in pieces, and her limbs scattered

over distant regions, and how her friends and disciples have to

go wandering all over the world in quest of them? There is surely

something very wonderful in the fact, that, in uniting the links

of the chain of creation into an unbroken whole, we have in like

manner to seek for them all along the scale of the geologist;--some

we discover among the tribes first annihilated--some among the

tribes that perished at a later period--some among the existences

of the passing time. We find the present incomplete without the

past--the recent without the extinct. There are marvellous analogies

which pervade the scheme of Providence, and unite, as it were,

its lower with its higher parts. The perfection of the works of

Deity is a perfection entire in its components; and yet these are

not contemporaneous, but successive: it is a perfection which

includes the dead as well as the living, and bears relation, in its

completeness, not to time, but to eternity.

We find the organisms of the Old Red Sandstone supplying an important

link, or, rather, series of links, in the ichthyological scale,

which are wanting in the present creation, and the absence of which

evidently occasions a wide gap between the two grand divisions

or series of fishes--the bony and the cartilaginous. Of this,

however, more anon. Of all the organisms of the system, one of the

most extraordinary, and the one in which Lamarck would have most

delighted, is the _Pterichthys_, or winged fish, an ichthyolite which

the writer had the pleasure of introducing to the acquaintance of

geologists nearly three years ago, but which he first laid open to

the light about seven years earlier. Had Lamarck been the discoverer,

he would unquestionably have held that he had caught a fish almost

in the act of wishing itself into a bird. There are wings which want

only feathers, a body which seems to have been as well adapted for

passing through the air as the water, and a tail by which to steer.

And yet there are none of the fossils of the Old Red Sandstone which

less resemble any thing that now exists than its _Pterichthys_. I

fain wish I could communicate to the reader the feeling with which I

contemplated my first-found specimen. It opened with a single blow

of the hammer; and there, on a ground of light-colored limestone,

lay the effigy of a creature fashioned apparently out of jet, with a

body covered with plates, two powerful looking arms, articulated at

the shoulders, a head as entirely lost in the trunk as that of the

ray or the sun-fish, and a long, angular tail. My first-formed idea

regarding it was, that I had discovered a connecting link between

the tortoise and the fish--the body much resembles that of a small

turtle; and why, I asked, if one formation gives us sauroid fishes,

may not another give us chelonian ones? or if in the Lias we find

the body of the lizard mounted on the paddles of the whale, why not

find in the Old Red Sandstone the body of the tortoise mounted in

a somewhat similar manner? The idea originated in error; but as it

was an error which not many naturalists could have corrected at the

time, it may be deemed an excusable one, more especially by such of

my readers as may have seen well-preserved specimens of the creature,

or who examine the subjoined prints. (Nos. I. and II.) I submitted

some of my specimens to Mr. Murchison, at a time when that gentleman

was engaged among the fossils of the Silurian System, and employed

on his great work, which has so largely served to extend geological

knowledge regarding those earlier periods in which animal life first

began. He was much interested in the discovery: it furnished the

geologist with additional data by which to regulate and construct

his calculations, and added a new and very singular link to the

chain of existence in its relation to human knowledge. Deferring to

Agassiz, as the highest authority, he yet anticipated the decision

of that naturalist regarding it, in almost every particular. I had

inquired, under the influence of my first impression, whether it

might not be considered as a sort of intermediate existence between

the fish and the chelonian. He stated, in reply, that he could

not deem it referrible to any family of reptiles; that, if not a

fish, it approached more closely to the Crustacea than to any other

class; and that he had little doubt Agassiz would pronounce it to

be an ichthyolite of that ancient order to which the _Cephalaspis_

belongs, and which seems to have formed a connecting link between

crustacea and fishes.[I] The specimens submitted to Mr. Murchison

were forwarded to Agassiz. They were much more imperfect than some

which I have since disinterred; and to restore the entire animal from

them would require powers such as those possessed by Cuvier in the

past age, and by the naturalist of Neufchatel in the present. Broken

as they were, however, Agassiz at once decided from them that the

creature must have been a fish.

[Footnote I: The aborigines of South. America deemed it wonderful

that the Europeans who first visited them should, without previous

concert, agree in reading after the same manner the same scrap of

manuscript, and in deriving the same piece of information from

it. The writer experienced on this occasion a somewhat similar

feeling. His specimens seemed written in a character cramp enough

to suggest those doubts regarding original meaning which lead to

various readings; but the geologist and the naturalist agreed in

perusing them after exactly the same fashion--the one in London, the

other in Neufchatel. Such instances give confidence in the findings

of science. The decision of Mr. Murchison I subjoin in his own

words--his numbers refer to various specimens of _Pterichthys_: "As

to your fossils 1, 2, 3, we know nothing of them here, (London,)

except that they remind me of the occipital fragments of some of

the Caithness fishes. I do not conceive they can be referrible to

any reptile; for, if not fishes, they more closely approach to

crustaceans than to any other class. I conceive, however, that

Agassiz will pronounce them to be fishes, which, together with the

curious genus _Cephalaspis_ of the Old Red Sandstone, form the

connecting links between crustaceans and fishes. Your specimens

remind one in several respects of the _Cephalaspis_."]

[Illustration: _PLATE I._]

I have placed one of the specimens before me. Imagine the figure

of a man rudely drawn in black on a gray ground, the head cut off

at the shoulders, the arms spread at full, as in the attitude of

swimming, the body rather long than otherwise, and narrowing from

the chest downwards, one of the legs cut away at the hip-joint, and

the other, as if to preserve the balance, placed directly under

the centre of the figure, which it seems to support. Such, at a

first glance, is the appearance of the fossil. The body was of very

considerable depth, perhaps little less deep proportionally from back

to breast than the body of the tortoise; the under part was flat;

the upper rose towards the centre into a roof-like ridge; and both

under and upper were covered with a strong armor of bony plates,

which, resembling more the plates of the tortoise than those of the

crustacean, received their accessions of growth at the edges or

sutures. The plates on the under side are divided by two lines of

suture, which run, the one longitudinally through the centre of the

body, the other transversely, also through the centre; and they would

cut one another at right angles, were there not a lozenge-shaped

plate inserted at the point where they would otherwise meet. There

are thus five plates on the lower or belly part of the animal. They

are all thickly tubercled outside with wart-like prominences, (see

Plate I., fig. 4;) the inner present appearances indicative of

a bony structure. The plates on the upper side are more numerous

and more difficult to describe, just as it would be difficult to

describe the forms of the various stones which compose the ribbed

and pointed roof of a Gothic cathedral, the arched ridge or hump of

the back requiring, in a somewhat similar way, a peculiar form and

arrangement of plates. The apex of the ridge is covered by a strong

hexagonal plate, fitted upon it like a cap or helmet, and which

nearly corresponds in place to the flat central plate of the under

side. There runs around it a border of variously formed plates, that

diminish in size and increase in number towards the head, and which

are separated, like the pieces of a dissected map, by deep sutures.

They all present the tubercled surface. The eyes are placed in

front, on a prominence considerably lower than the roof-like ridge

of the back; the mouth seems to have opened, as in many fishes, in

the edge of the creature's snout, where a line running along the

back would bisect a line running along the belly; but this part

is less perfectly shown by my specimens than any other. The two

arms, or paddles, are placed so far forward as to give the body a

disproportionate and decapitated appearance. From the shoulder to

the elbow, if I may employ the terms, there is a swelling, muscular

appearance, as in the human arm; the part below is flattened, so

as to resemble the blade of an oar, and terminates in a strong,

sharp point. The tail--the one leg on which, as exhibited in one

of my specimens, the creature seems to stand--is of considerable

length, more than equal to a third of the entire figure, and of an

angular form, the base representing the part attached to the body,

and the apex its termination. It was covered with small tubercled,

rhomboidal plates, like scales, (see Plate I., fig. 3;) and where the

internal structure is shown, there are appearances of a vertebral

column, with rib-like processes standing out at a sharp angle. The

ichthyolite, in my larger specimens, does not much exceed seven

inches in length; and I despatched one to Agassiz, rather more than

two years ago, whose extreme length did not exceed an inch. Such

is a brief, and, I am afraid, imperfect sketch of a creature whose

very type seems no longer to exist. But for the purposes of the

geologist, the descriptions of the graver far exceed those of the

pen, and the accompanying prints will serve to supply all that may

be found wanting in the text. Fig. 1, in Plate I., and fig. 2, in

Plate II., are both restorations--the first of the upper, and the

second of the under, part of the creature. It may, however, encourage

the confidence of the naturalist, who for the first time looks upon

forms so strange, to be informed that Plate I., with its two figures,

was submitted to Agassiz during his recent brief stay in Edinburgh,

and that he as readily recognized in it the species of the two kinds

which it exhibits, as he had previously recognized the species of the

originals in the limestone.

[Illustration: _PLATE II._]

Agassiz, in the course of his late visit to Scotland, found six

species of the _Pterichthys_[J]--three of these, and the wings of a

fourth, in the collection of the writer. The differences by which

they are distinguished may be marked by even an unpractised eye,

especially in the form of the bodies and wings. Some are of a fuller,

some of a more elongated, form; in some the body resembles a heraldic

shield, of nearly the ordinary shape and proportions; in others the

shield stretches into a form not very unlike that of a Norway skiff,

from the midships forward. In some of the varieties, too, the wings

are long and comparatively slender; in others shorter, and of greater

breadth: in some there is an inflection resembling the bend of an

elbow; in others there is a continuous swelling from the termination

to the shoulder, where a sudden narrowing takes place immediately

over the articulation. I had inferred somewhat too hurriedly, though

perhaps naturally enough, that these wings, or arms, with their

strong sharp points and oar-like blades, had been at once paddles and

spears--instruments of motion and weapons of defence; and hence the

mistake of connecting the creature with the Chelonia. I am informed

by Agassiz, however, that they were weapons of defence only, which,

like the occipital spines of the river bull-head, were erected in

moments of danger or alarm, and at other times lay close by the

creature's side; and that the sole instrument of motion was the tail,

which, when covered by its coat of scales, was proportionally of a

somewhat larger size than the tail shown in the print, which, as in

the specimens from whence it was taken, exhibits but the obscure

and uncertain lineaments of the skeleton. The river bull-head, when

attacked by an enemy, or immediately as it feels the hook in its

jaws, erects its two spines at nearly right angles with the plates

of the head, as if to render itself as difficult of being swallowed

as possible. The attitude is one of danger and alarm; and it is a

curious fact, to which I shall afterwards have occasion to advert,

that in this attitude nine tenths of the _Pterichthys_ of the Lower

Old Red Sandstone are to be found. We read in the stone a singularly

preserved story of the strong instinctive love of life, and of the

mingled fear and anger implanted for its preservation--"The champions

in distorted postures threat." It presents us, too, with a wonderful

record of violent death falling at once, not on a few individuals,

but on whole tribes.

[Footnote J: Agassiz now reckons ten distinct species of

_Pterichthys_--_P. arenatus_, _P. cancriformis_, _P. cornutus_, _P.

major_, _P. Milleri_, P. latus, _P. oblongus_, _P. productus_, _P.

testudinarius_, and _P. hydrophilus_; of these, nine species belong

to the Lower, and one--the _Pterichthys hydrophilus_--to the Upper

Old Red Sandstone.]

[Illustration: _PLATE III._]

Next to the _Pterichthys_ of the Lower Old Red I shall place its

contemporary the _Coccosteus_ of Agassiz, a fish which, in some

respects, must have somewhat resembled it. Both were covered with

an armor of thickly tubercled bony plates, and both furnished

with a vertebrated tail. The plates of the one, when found lying

detached in the rock, can scarcely be distinguished from those of the

other: there are the same marks, as in the plates of the tortoise,

of accessions of growth at the edges--the same cancellated bony

structure within, the same kind of tubercles without. The forms of

the creatures themselves, however, were essentially different. I

have compared the figure of the _Pterichthys_, as shown in some of

my better specimens, to that of a man with the head cut off at the

shoulders, one of the legs also wanting, and the arms spread to the

full. The figure of the _Coccosteus_ I would compare to a boy's kite.

(See Plate III., fig. 1.) There is a rounded head, a triangular body,

a long tail attached to the apex of the triangle, and arms thin and

rounded where they attach to the body, and spreading out towards

their termination like the ancient one-sided shovel which we see

sculptured on old tombstones, or the rudder of an ancient galley.[K]

The manner in which the plates are arranged on the head is peculiarly

beautiful; but I am afraid I cannot adequately describe them. A ring

of plates, like the ring-stones of an arch, runs along what may

be called the hoop of the kite; the form of the keystone-plate is

perfect; the shapes of the others are elegantly varied, as if for

ornament; and what would be otherwise the opening of the arch, is

filled up with one large plate, of an outline singularly elegant. A

single plate, still larger than any of the others, covers the greater

part of the creature's triangular body, to the shape of which it

nearly conforms. It rises saddle-wise towards the centre: on the

ridge there is a longitudinal groove ending in a perforation, a

little over the apex, (Plate III., fig. 2;) two small lateral plates

on either side fill up the base of the angle; and the long tail, with

its numerous vertebral joints, terminates the figure.

[Footnote K: I have since ascertained that these seeming arms or

paddles were simply plates of a peculiar form.]

Does the reader possess a copy of Lyell's lately published elementary

work, edition 1838? If so, let him first turn up the description of

the Upper Silurian rocks, from Murchison, which occurs in page 459,

and mark the form of the trilobite _Asaphus caudatus_, a fossil of

the Wenlock formation. (See _Sil. Sys._, Plate VII.) The upper part,

or head, forms a crescent; the body rises out of the concave with a

sweep somewhat resembling that of a Gothic arch; the outline of the

whole approximates to that of an egg, the smaller end terminating

in a sharp point. Let him remark, further, that this creature was a

_crustaceous_ animal, of the crab or lobster class, and then turn up

the brief description of the Old Red Sandstone in the same volume,

page 454, and mark the form of the _Cephalaspis_, or buckler-head--a

_fish_ of a formation immediately over that in which the remains

of the trilobite most abound. He will find that the fish and the

crustacean are wonderfully alike. The fish is more elongated, but

both possess the crescent-shaped head, and both the angular and

apparently jointed body.[L] They illustrate admirably how two

distinct orders may meet. They exhibit the points, if I may so speak,

at which the plated fish is linked to the shelled crustacean. Now,

the _Coccosteus_ is a stage further on; it is more unequivocally a

fish. It is a _Cephalaspis_ with an articulated tail attached to the

angular body, and the horns of the crescent-shaped head cut off.

[Footnote L: Really jointed in the case of the trilobite; only

apparently so in that of the _Cephalaspis_. The body of the

trilobite, like that of the lobster, was barred by transverse,

oblong, overlapping plates, and between every two plates there was a

joint; the body of the _Cephalaspis_, in like manner, was barred by

transverse, oblong, overlapping scales, between which there existed

no such joints. It is interesting to observe how nature, in thus

bringing two such different classes as fishes and crustacea together,

gives to the higher animal a sort of pictorial resemblance to the

lower, in parts where the construction could not be identical without

interfering with the grand distinctions of the classes.]

Some of the specimens which exhibit this creature are exceedingly

curious. In one, a coprolite still rests in the abdomen; and a common

botanist's microscope shows it thickly speckled over with minute

scales, the indigestible exuviæ of fish on which the animal had

preyed. In the abdomen of another we find a few minute pebbles--just

as pebbles are occasionally found in the stomach of the cod--which

had been swallowed by the creature attached to its food. Is there

nothing wonderful in the fact, that men should be learning at this

time of day how the fishes of the Old Red Sandstone lived, and that

there were some of them rapacious enough not to be over nice in their

eating?

The under part of the creature is still very imperfectly known:

it had its central lozenge-shaped plate, like that on the under

side of the _Pterichthys_, but of greater elegance, (see Plate

III., fig. 3,) round which the other plates were ranged. "What an

appropriate ornament, if set in gold!" said Dr. Buckland, on seeing

a very beautiful specimen of this central lozenge in the interesting

collection of Professor Traill of Edinburgh,--"What an appropriate

ornament for a lady geologist!" There are two marked peculiarities

in the jaws of the _Coccosteus_, as shown in most of the specimens,

illustrative of the lower part of the creature, which I have yet

seen. The teeth, instead of being fixed in sockets, like those of

quadrupeds and reptiles, or merely placed on the bone, like those of

fish of the common varieties, seem to have been cut out of the solid,

like the teeth of a saw or the teeth in the mandibles of the beetle,

or in the nippers of the lobster, (Plate III., fig. 4;) and there

appears to have been something strangely anomalous in the position

of the jaws--something too anomalous, perhaps, to be regarded as

proven by the evidence of the specimens yet found, but which may

be mentioned with the view of directing attention to it. "Do not

be deterred," said Agassiz, in the course of one of the interviews

in which he obligingly indulged the writer of these chapters, who

had mentioned to him that one of his opinions, just confirmed by

the naturalist, had seemed so extraordinary that he had been almost

afraid to communicate it,--"Do not be deterred, if you have examined

minutely, by any dread of being deemed extravagant. The possibilities

of existence run so deeply into the extravagant, that there is

scarcely any conception too extraordinary for nature to realize." In

all the more complete specimens which I have yet seen, _the position

of the jaws is vertical, not horizontal_; and yet the creature, as

shown by the tail, belonged unquestionably to the vertebrata. Now,

though the mouths of the crustaceous animals, such as the crab and

lobster, open vertically, and a similar arrangement obtains among the

insect tribes, it has been remarked by naturalists, as an invariable

condition of that higher order of animals distinguished by vertebral

columns, that their mouths open horizontally. What I would remark as

very extraordinary in the _Coccosteus_--not, however, in the way of

directly asserting the fact, but merely by way of soliciting inquiry

regarding it--is, that it seems to unite to a vertebral column a

vertical mouth, thus forming a connecting link between two orders of

existences, by conjoining what is at once their most characteristic

and most dissimilar traits.[M]

[Footnote M: These statements regarding the character of the teeth

and the position of the jaws of the _Coccosteus_ have been challenged

by very high authorities. I retain them, however, in this edition

in their original form, as first made nearly six years ago. In at

least two of my specimens of Coccosteus the teeth and jaw form

unequivocally but one bone--a result, it is not improbable, of some

after anchylosing process, but which still solicits inquiry as not

yet definitely accounted for. The matter of fact in the case is

certainly one which should be determined, not analogically, but on

its own proper evidence, as furnished by good specimens. As for

the remark regarding the probable position of the creature's jaws,

it was ventured on at first, as the reader may perceive, with much

hesitation, and must now be regarded as more doubtful than ever.

Its repetition here, however, will, I trust, be regarded as simply

indicative of a wish on the part of the writer, that the question

be kept open just a little longer, and that further examination

be made. There is certainly something very peculiar about the

mouth of the Coccosteus not yet understood, and singularly formed

plates, connected with it, which have not been introduced into any

restoration, and the use of which in the economy of the animal

seem wholly unknown. [1850.--I have at length found a very perfect

specimen of the nether jaw of _Coccosteus_, and am prepared to show

that it was of a character altogether unique. It had its two groups

of from six to eight teeth, (exactly where, in the human subject, the

molars are placed,) that seem to have acted on corresponding groups

in the intermaxllaries, and two other groups of from three to five

teeth placed at right angles with these, direct in the symphysis,

and that seem to have acted on each other. But though these unique

teeth of the symphysis formed a vertical line of mouth, it joined

on at right angles to a transverse line of the ordinary type, as

the upright stroke of the letter T joins on to the horizontal line

a-top.] Fourth Edition.]

I am acquainted with four species of _Coccosteus_--_C. decipiens_,

_C. cuspidatas_, _C. oblongus_, and a variety not yet named; and

many more species may yet be discovered.[N] Of all the existences of

the formation, this curious fish seems to have been one of the most

abundant. In a few square yards of rock I have laid open portions of

the remains of a dozen different individuals belonging to two of the

four species, the _C. decipiens_ and _C. cuspidatus_, in the course

of a single evening. None of the other kinds have yet been found at

Cromarty. These two differed from each other in the proportions

which their general bulk bore to their length--slightly, too, in

the arrangement of their occipital plates. The _Coccosteus latus_,

as the name implies, must have been by much a massier fish than the

other; and we find the arch-like form of the plates which covered its

head more complete: the plate representing the keystone rests on the

saddle-shaped plate in the centre, and the plates representing the

spring-stones of the arch exhibit a broader base. The accompanying

print (Plate III.) represents the _Coccosteus cuspidatus_. The

average length of the creature, including the tail, as shown in most

of the Cromarty specimens, somewhat exceeded a foot. A few detached

plates from Orkney, in the collection of Dr. Traill, must have

belonged to an individual of fully twice that length.

[Footnote N: A fifth species has been named _C. maximus._]

The Old Red Sandstone; or, New Walks in an Old Field · 第 3 / 14 章