One of the best marked Placoids of the Upper Ludlow bone-bed is that

_Onchus Murchisoni_ to which the distinguished geologist whose name it

bears refers, in his communication, as so nearly resembling the oldest

Placoid yet known,—that of the Bala Limestone. And the living fishes

with which the _Onchus Murchisoni_ must be compared, says Agassiz,

though “the affinity,” he adds, “may be rather distant,” are those of

the genera “_Cestracion_, _Centrina_, and _Spinax_.” I have placed

before me a specimen of recent _Spinax_, of a species well known to

all my readers on the sea-coast, the _Spinax Acanthias_, or common

dog-fish, so little a favorite with our fishermen. It measures exactly

two feet three inches in length; and of the defensive spines of its two

dorsals,—these spear-like thorns on the creature’s back immediately in

advance of the fins, which so frequently wound the fisher’s hand,—the

anterior and smaller measures, from base to point, an inch and a half,

and the posterior and larger, two inches. I have also placed before me

a specimen of _Cestracion Phillippi_, (the Port Jackson Shark,) a fish

now recognized as the truest existing analogue of the Silurian Placoids.

It measures twenty-two three fourth inches in length, and is furnished,

like _Spinax_, with two dorsal spines, of which the anterior and larger

measures from base to point one one half inch, and the posterior and

smaller, one one fifth inch. But the defensive spine of the _Onchus

Murchisoni_, as exhibited in one of the Ludlow specimens, measures,

though mutilated at both ends, three inches and five eighth parts in

length. Even though existing but as a fragment, it is as such nearly

twice the length of the largest spine of the dog-fish, unmutilated and

entire, and considerably _more_ than twice the length of the largest

spine of the Port Jackson Shark. The spines detected by Professor

Phillips, in an inferior stratum of the same upper deposit, were, as

has been shown, of microscopic minuteness; and when they seemed to

rest on the extreme horizon of ichthyic existence as the most ancient

remains of their kind, the author of the “Vestiges” availed himself of

the fact. He regarded the little creatures to which they had belonged

is the fœtal embryos of their class, or—to employ the language of the

Edinburgh Reviewer—as “the tokens of Nature’s first and half-abortive

efforts to make fish out of the lower animals.” From the latter editions

of his work, the paragraph to which the Reviewer refers has, I find,

been expunged; for the horizon has greatly extended, and what seemed

to be its line of extreme distance has travelled into the middle of

the prospect. But that the passage should have at all existed is a not

uninstructive circumstance, and shows how unsafe it is, in more than

external nature, to regard the line at which, for the time, the landscape

closes, and heaven and earth seem to meet, as in reality the world’s end.

The Wenlock spine, though certainly not microscopic, is, I am informed

by Sir Philip Egerton, of but small size; whereas the contemporary spine

of the Onondago Limestone, though comparatively more a fragment than the

spine of the Upper Ludlow _Onchus_,—for it measures only three inches in

length,—is at least five times as bulky as the largest spine of _Spinax

Acanthias_. Representing one of the massier fishes disporting amid the

some four or five small ones, of which in my illustration, the naturalist

catches a glimpse in fording the unknown lake, it at least serves to

show that all the Silurian ichthyolites must not be described as small,

seeing that not only might many of its undetected fish have been large,

but that some of those which _have_ been detected were actually so.

Another American spine, of nearly the same formation,—for it occurs in

a limestone, varying from twenty to seventy feet in thickness, which

immediately overlies that of the Onondago deposit, though still more

fragmentary than the first, for its length is only two three eighth

inches,—maintains throughout a nearly equal thickness,—a circumstance

in itself indicative of considerable size; and in positive bulk it

almost rivals the Onondago one. Of the Lower Silurian and Bala fishes no

descriptions or figures have yet appeared. And such, up to the present

time, is the testimony derived from this department of Geology, so far

as I have been able to determine it, regarding the size of the ancient

Silurian vertebrata. “No organism,” says Professor Oken, “is, nor ever

has one been, created, which is not microscopic.” The Professor’s pupils

and abettors, the assertors of the development hypothesis, appeal to

the geological evidence as altogether on _their_ side in the case; and

straightway a few witnesses enter court. But, lo! among the expected

dwarfs, there appear individuals of more than the average bulk and

stature.

[Illustration: Fig. 47.

a. _Posterior Spine of Spinax Acanthias._

b. _Fragment of Onondago Spine._

(Natural Size.)]

Still, however, the question of organization remains. Did these ancient

Placoid fishes stand high or low in the scale? According to the poet,

“What can we reason but from what we know?” We are acquainted with the

Placoid fishes of the present time; and from these only, taking analogy

as our guide, can we form any judgment regarding the rank and standing

of their predecessors, the Placoids of the geologic periods. But the

consideration of this question, as it is specially one on which the

later assertors of the development hypothesis concentrate themselves, I

must, to secure the space necessary for its discussion, defer till my

next chapter. Meanwhile, I am conscious I owe an apology to the reader

for what he must deem tedious minuteness of description, and a too

prolix amplitude of statement. It is only by representing things as they

actually are, and in the true order of their occurrence, that the effect

of the partially selected facts and exaggerated descriptions of the

Lamarckian can be adequately met. True, the disadvantages of the more

sober mode are unavoidably great. He who feels himself at liberty to

arrange his collected shells, corals, and fish-bones, into artistically

designed figures, and to select only the pretty ones, will be of course

able to make of them a much finer show than he who is necessitated to

represent them in the order and numerical proportions in which they occur

on some pebbly beach washed by the sea. And such is the advantage, in a

literary point of view, of the ingenious theorist, who, in making figures

of his geological facts, takes no more of them than suits his purpose,

over the man who has to communicate the facts as he finds them. But the

homelier mode is the true one. “Could we obtain,” says a distinguished

metaphysician, “a distinct and full history of all that has passed in

the mind of a child, from the beginning of life and sensation till it

grows up to the use of reason,—how its infant faculties began to work,

and how they brought forth and ripened all the various notions, opinions,

and sentiments which we find in ourselves when we come to be capable

of reflection,—this would be a treasure of natural history which would

probably give more light into the human faculties than all the systems

of philosophers about them since the beginning of the world. But it is

in vain,” he adds, “to wish for what nature has not put within the reach

of our power.” In like manner, could we obtain, it may be remarked, a

full and distinct account of a single class of the animal kingdom, from

its first appearance till the present time, “this would be a treasure

of natural history which would cast more light” on the origin of living

existences, and the true economy of creation, than all the theories of

all the philosophers “since the beginning of the world.” And in order to

approximate to such a history as nearly as possible,—and it does seem

possible to approximate near enough to substantiate the true readings of

the volume, and to correct the false ones,—it is necessary that the real

vestiges of creation should be carefully investigated, and their order of

succession ascertained.

HIGH STANDING OF THE PLACOIDS.—OBJECTIONS CONSIDERED.

We have seen that some of the Silurian Placoids were large of size: the

question still remains, Were they high in intelligence and organization?

The Edinburgh Reviewer, in contending with the author of the “Vestiges,”

replies in the affirmative, by claiming for them the first place among

fishes. “Taking into account,” he says, “the brain and the whole nervous,

circulating, and generative systems, they stand at the highest point of

a natural ascending scale.” They are fishes, he again remarks, that rank

among “the very highest types of their class.”

“The fishes of this early age, and of all other ages previous to

the Chalk,” says his antagonist, in reply, “are, for the most part,

cartilaginous. The cartilaginous fishes—_Chondropterygii_ of Cuvier—are

placed by that naturalist as a second series in his descending scale;

being, however, he says, ‘in some measure _parallel to the first_.’

How far this is different from their being the highest types of the

fish class, need not be largely insisted upon. Linnæus, again, was so

impressed by the low characters of many of this order, that he actually

ranked them with worms. Some of the cartilaginous fishes, nevertheless,

have certain peculiar features of organization, chiefly connected with

reproduction, in which they excel other fish; but such features are

partly partaken of by families in inferior sub-kingdoms, showing that

they cannot truly be regarded as marks of grade in their own class. When

we look to the great fundamental characters particularly to the framework

for the attachment of the muscles, what do we find?—why, that of these

Placoids,—‘the highest types of their class,’—it is barely possible to

establish their being vertebrata at all, the back-bone having generally

been too slight for preservation, although the vertebral columns of later

fossil fishes are as entire as those of any other animals. In many of

them traces can be observed of the muscles having been attached to the

external plates, strikingly indicating their low grade as vertebrate

animals. The Edinburgh Reviewer ‘highest types of their class’ are in

reality a separate series of that class, generally inferior, taking the

leading features of organization of structure as a criterion, but when

details of organization are regarded, stretching farther, both downward

and upward, than the other series; so that, looking at one extremity, we

are as much entitled to call them the lowest, as the Reviewer, looking at

another extremity, is to call them the ‘highest of their class.’ Of the

general inferiority there can be no room for doubt. Their cartilaginous

structure is, in the first place, analogous to the embryonic state of

vertebrated animals in general. The maxillary and intermaxillary bones

are in them rudimental. Their tails are finned on the under side only,—an

admitted feature of the salmon in an embryonic stage; and the mouth is

placed on the under side of the head,—also a mean and embryonic feature

of structure. These characters are essential and important, whatever

the Edinburgh Reviewer may say to the contrary; they are the characters

which, above all, I am chiefly concerned in looking to, for they are

features of embryonic progress, and embryonic progress is the grand key

to the theory of development.”

Such is the ingenious piece of special pleading which this most popular

of the Lamarckians directs against the standing and organization of the

earlier fishes. Let us examine it somewhat in detail, and see whether

the slight admixture of truth which it contains serves to do aught more

than to render current, like the gilding of a counterfeit guinea spread

over the base metal, the amount of error which lies beneath. I know

not a better example than that which it furnishes, of the entanglement

and perplexity which the meshes of an artificial classification, when

converted, in argumentative processes, into symbols and abstractions, are

sure to involve subjects simple enough in themselves.

Fishes, according to the classification of a preponderating majority

of the ichthyologists that have flourished from the earliest times

down to those of Agassiz, have been divided into two great series, the

_Ordinary_ or osseous, and the _Chondropterygii_ or cartilaginous. And

these two divisions of the class, instead of being ranged consecutively

in a continuous line, the one in advance of the other, have been

ranged in two parallel lines, the one directly abreast of the other.

There is this further peculiarity in the arrangement, that the line

of the cartilaginous series, from the circumstance that some of its

families rise higher and some sink lower in the scale than any of the

ordinary fishes, outflanks the array of the osseous series at both

ends. The front which it presents contains fewer genera and species

than that of the osseous division; but, like the front of an army drawn

out in single file, it extends along a greater length of ground. And

to this long-fronted series of the cartilaginous, or, according to

Cuvier, _chondropterygian_ fishes, the Placoid families of Agassiz

belong,—among the rest, the Placoids of the Silurian formations, Upper

and Lower. But though all the Placoids of this latter naturalist be

cartilaginous fishes, all cartilaginous fishes are not Placoids. The

_Sturionidæ_ are cartilaginous, and are, as such, ranked by Cuvier

among the _Chondropterygii_, whereas Agassiz places them in his Ganoid

order. Many of the extinct fishes, too, such as the _Acanthodei_,

_Dipteridæ_, _Cephalaspidæ_, were, as we have seen, cartilaginous in

their internal framework, and yet true Ganoids notwithstanding. The

principle of Agassiz’s classification wholly differs from that of Cuvier

and the older ichthyologists; for it is a classification founded, not

on the character of the internal but on that of the cuticular or dermal

skeleton. And while to the geologist it possesses great and obvious

advantages over every other,—for of the earlier fishes very little more

than the cuticular skeleton survives,—it has this further recommendation

to the naturalist, that, (in so far at least as its author has been true

to his own principles,) instead of anomalously uniting the highest and

lowest specimens of their class,—the fishes that most nearly approximate

to the reptiles on the one hand, and the fishes that sink furthest

towards the worms on the other,—it gathers into one consistent order all

the individuals of the higher type, distinguished above their fellows

by their development of brain, the extensive range of their instincts,

and the perfection of their generative systems. Further, the history of

animal existences, as recorded in the sedimentary rocks of our planet,

reads a recommendation of this scheme of classification which it extends

to no other. We find that in the progress of creation the fishes _began

to be_ by groupes and septs, arranged according to the principle on which

it erects its orders. The Placoids came first, the Ganoids succeeded

them, and the Ctenoids and Cycloids brought up the rear. The march has

been marshalled according to an appointed programme, the order of which

it is peculiarly the merit of Agassiz to have ascertained.

Now, may I request the reader to mark, in the first place that what we

have specially to deal with at the present stage of the argument are the

Placoid fishes of the Silurian formations, Upper and Lower. May I ask him

to take note, in the second, that the long-fronted _chondropterygian_

series of Cuvier, though it includes, as has already been said, the

Placoid order of Agassiz,—just as the red-blooded division of animals

includes the bimana and quadrumana,—is no more to be regarded as

_identical_ with the Placoids, than the red-blooded animals are to be

regarded as identical with the apes or with the human family. It simply

includes them in the character of _one_ of the three great divisions into

which it has been separated,—the division ranged, if I may so express

myself, on the extreme right of the line; its middle portion, or main

body, being composed of the _Sturiones_, a family on the general level of

the osseous fishes; while, ranged on the extreme left, we find the low

division of the _Suctorii_, _i. e._ Cyclostomi, or Lampreys. But with

the middle and lower divisions we have at present nothing to do; for of

neither of them, whether _Sturiones_ or _Suctorii_, does the Silurian

System exhibit a trace. Further be it remarked, that the scheme of

classification which gives an abstract standing to the _Chondropterygii_,

is in itself merely a certain perception of resemblance which existed

in certain minds, having _cartilage_ for its general idea; just as

another certain perception of resemblance in one other certain mind

had _cuticular skeleton_ for its general idea, and as yet another

perception of resemblance in yet other certain minds had _red blood_

for its general idea. As shown by the disparities which obtain among

the section which the scheme serves to separate from the others, it no

more determines rank or standing than that greatly more ancient scheme

of classification into “ring-streaked and spotted,” which served to

distinguish the flocks of the patriarch Jacob from those of Laban his

father-in-law, but which did not distinguish goats from sheep, nor sheep

from cattle.

The effect of introducing, after this manner, generalizations made

altogether irrespective of _rank_, and avowedly without reference to it,

into what are inherently and specifically _questions of rank_, admits of

a simple illustration.

Let us suppose that it was not with the standing of the Silurian Placoids

that we had to deal, but with that of the _mammals_ of the recent

period, including the _quadrumana_, and even the _bimana_, and that we

had ventured to describe them, in the words of the Edinburgh Reviewer,

as “the very highest types of their class.” What would be thought of

the reasoner who, in challenging the justice of the estimate, would

argue that these creatures, men as well as monkeys, belonged simply to

that division of red-blooded animals which includes, with the bimana

and quadrumana, the frog, the gudgeon, and the _earthworm_?—a division,

he might add, “which, when details of organization are regarded,

stretches farther, both downward and upward,” than that division of the

white-blooded animals to which the crab, the spider, the cuttle-fish,

and the dragon fly belong; “so that, looking at one extremity, any one

is as much entitled to call the red-blooded animals the lowest division,

as any other, looking at another extremity, is to call them the highest

division, of animals.” What, it might well be asked in reply, has the

earthworm, with its red-blood to do in a question respecting the place

and standing of the bimana? Or what, in the parallel case, have the

_Suctorii_—the worms of Linnæus—to do in a question respecting the

place and standing of the real Placoids? True it is that, according to

one principle of classification, now grown somewhat obsolete, men and

earthworms are equally red-blooded animals; true it is that, according

to another principle of classification, the Placoids of Agassiz and the

cartilaginous worms of Linnæus are equally _Chondropterygii_. The bimana

and the earthworm have their red blood in common; the glutinous hag and

the true Placoids have as certainly their internal cartilage in common;

and if the fact of the red blood of the worm lowers in no degree the rank

of the bimana, then, on the same principle, the fact of the internal

cartilage of the glutinous hag cannot possibly detract from the standing

of the true Placoid. In both cases they are creatures that entirely

differ,—the earthworms from the bimana, and the cartilaginous _worms_

from the Placoids; and the classification which tags them together,

whether it be that of Aristotle or that of Cuvier, cannot be converted

into a sort of minus quantity, of force enough to detract from the value

and standing of the bimana in the one case, or of the true Placoids

in the other. It is in no degree derogatory to the human family that

earthworms possess red blood; it is in no degree derogatory to the true

Placoids that the _Suctorii_ possess cartilaginous skeletons.

Let the reader now mark the use which has been made, by the author of

the “Vestiges,” of the name and authority of Linnæus. “Linnæus,” he

states, “was so impressed by the low character of many of this order,

(the _Chondropterygii_,) that he actually ranked them with worms.” Now,

what is the fact here? Simply that Linnæus had no such general order as

the _Chondropterygii_ in his eye at all. Though chiefly remarkable as a

naturalist for the artificialness of his classifications, his estimate

of the cartilaginous fishes was remarkable—though carried too far in its

extremes, and in some degree founded in error—for an opposite quality.

It was an estimate formed, in the main, on a natural basis. Instead of

taking their cartilaginous skeleton into account, he looked chiefly at

their standing as animals; and, struck with that extent of front which

they present, and with both their superiority on the extreme right, and

their inferiority on the extreme left, to the ordinary fishes, he erected

them into two separate orders, the one lower and the other higher than

the members of the osseous line. And so far was he from regarding the

true Placoids—those _Chondropterygii_ which to an internal skeleton of

cartilage add external plates, points, or spines of bone—as low in the

scale, that he actually raised them above fishes altogether, by erecting

them into an order of reptiles,—the older _Amphibia Nantes_. Surely, if

the name of Linnæus was to be introduced into this controversy at all, it

ought to have been in connection with _this_ special fact; seeing that

the point to be determined in the question under discussion is simply

the place and standing of that very order which the naturalist rated so

high,—not the place and standing of the order which he degraded. It so

happens that there is one of the _Chondropterygii_ which, so far from

being a true Placoid, does not possess a single osseous plate, point, or

spine: it is a worm like creature, without eyes, without movable jaws,

without vertebral joints, without scales, always enveloped in slime, and

greatly abhorred by our Scotch boatmen of the Moray Frith, who hold that

it burrows, like the grave-worm, in the decaying bodies of the dead.

And this creature, “the glutinous hag,” or, according to north-country

fishermen, the “ramper-eel,” or “poison-ramper,” was regarded by Linnæus

as belonging, not to the class of fishes, but to the Vermes. Now, _this_

is the special fact with which, in the development controversy, the

author of the “Vestiges” connects the name of the Swedish naturalist!

All the fish of the Silurian System belonged to that true Placoid order

which Linnæus, impressed by its high standing, erected into an order,

not of worms, but of reptiles. He elevated A, the true Placoid, while he

degraded B, the glutinous hag. But it was necessary to the argument of

the author of the “Vestiges” that the earliest existing fish should be

represented as fish low in the scale; and so he has cited the name and

authority of Linnæus in its bearing against the glutinous hag B, as if

it had borne against the standing of the true Placoid A. The Patagonians

are the tallest and bulkiest men in the world, whereas their neighbors,

the Fuegians are a slim and diminutive race. And if, in some controversy

raised regarding the real size of the more gigantic tribe, they were to

be described as the “very _tallest_ types of their class,” any statement

in reply, to the effect that some trustworthy voyager had examined

certain races of the extreme south of America, and had found that they

were both short and thin, would be neither relevant in its facts nor

legitimate in its bearing. But if the controversialist who thus strove

to strengthen his case by the voyager’s authority, was at the same time

fully aware that the voyager had seen not only the diminutive Fuegians,

but also the gigantic Patagonians, and that he had described these last

as very gigantic indeed, the introduction of the statement regarding the

smaller race, when he wholly sank the statement regarding the larger,

would be not merely very irrelevant in the circumstances, but also very

unfair. Such, however, is the style of statement to which the author of

the “Vestiges” has (I trust inadvertently) resorted in this controversy.

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