CHAPTER VIII

VERTEBRATE ANATOMY

The Theory of the Vertebrate Skull--Goethe, Oken, Cuvier, and

Owen--Huxley Defends Goethe--His Own Contributions to the

Theory--The Classification of Birds--Huxley Treats them as

"Extinct Animals"--Geographical Distribution--Sclater's

Regions--Huxley's Suggestions.

We have seen that some of the most important of the contributions made

by Huxley to zoölogical knowledge were in the field of the lower

animals, especially of those marine forms for the study of which he

had so great opportunities on the _Rattlesnake_. A great bulk of his

zoölogical work, however, related to the group of back-boned animals.

These, by their natural affinities and anatomical structure, are more

closely related to man, and, as Huxley began his scientific work as a

medical student, the groundwork of all his knowledge was study of the

anatomy and physiology of man. Moreover, throughout the greater part

of his working life, he had more to do with the extinct forms of life.

The vertebrate animals, from the great facility for preservation which

their hard skeleton presents, as well as from the extremely important

anatomical characters of the skeleton, bulk more largely in the study

of palæontology than does any other group. In each of the great

groups of vertebrate animals, in fishes, amphibia, reptiles, birds,

and mammals, Huxley did important work. Much of this is embodied in

his treatise on _Vertebrate Anatomy_, but to some particular parts of

it special attention may now be directed, as much because these serve

as excellent examples of his method of work as because of their

intrinsic importance.

The skull is the most striking feature in the skeleton of vertebrate

animals, and to the theory and structure of the vertebrate skull

Huxley paid special attention, and his views and summary of the views

of others form the basis of our modern knowledge. This work was put

before the public in the course of a series of lectures on Comparative

Anatomy given in 1863, while Huxley was Hunterian Professor at the

Royal College of Surgeons, and the beginnings of it were contained in

a Croonian lecture to the Royal Society in 1858.

The theory of the skull which held the field was known as the

vertebral theory. The great bulk of the nervous system of vertebrate

animals consists of a mass of tissue lying along the dorsal line of

the body and enclosed in a cartilaginous or bony sheath. The nerve

tissue is the brain and spinal cord; the sheath is the skull in front

and the vertebral column along the greater part of the length of the

animal. The brain may be taken simply as an anterior portion of the

nerve mass, corresponding in a general way to an expansion of the

spinal cord in the region of the anterior limbs and an expansion in

the region of the hind limbs, the latter indeed having recently been

shown in some extinct creatures to surpass the brain in size. In a

similar simple fashion the skull may be taken as an expanded anterior

part of the vertebral column, serving as an expanded box for the

brain, just as in the regions of the pectoral and pelvic expansions

of the cord there are similar expansions of the surrounding bony case.

We know now, from greater knowledge of its embryological development,

that the brain contains structures quite peculiar to itself, and

differs from the spinal cord in kind as well as in size; but, at the

same time, when the vertebral theory of the skull was inaugurated,

embryological knowledge and the importance of its relation to

anatomical structure were less considered. What Huxley did was to show

that the skull, in its mode of origin and real nature, was not merely

an expanded portion of the vertebral column, but that it differed from

it in kind.

The hypothesis of the vertebral structure of the skull was due both to

Goethe, the great German poet, and Oken, a most able but somewhat

mystic German anatomist. An attempt had been made by a well-known

English anatomist to cast on Goethe the stigma of having tried to rob

Oken of the credit for this theory. Huxley set that matter finally at

rest, disproving and repelling with indignation the unworthy

suggestion. Oken gave out his theory in 1807, and described how it had

been first suggested to his mind by the accident of picking up a dried

and battered sheep's skull, in which the apparent vertebral structure

was very obvious, as, indeed, anyone may see at a glance. It was in

1820, long after the theory had been made current, that the poet first

publicly narrated that in a similar way he had long before come to the

same conclusion; but Huxley was able to show that, although announcing

it later, Goethe had in reality anticipated the anatomist. A passage

occurs in a letter to a friend, of a date in 1790, which admits of no

doubt. "By the oddest happy chance, my servant picked up a bit of an

animal's skull in the Jews' cemetery at Venice, and, by way of a

joke, held it out to me as if he were offering me a Jew's skull. I

have made a great step in the formation of animals." It is an

interesting trait in Huxley's character, to find him zealous in

defence of the reputation of a great man, even although that man had

been dead more than half a century; but it may be added that his just

zeal was at least stimulated by the fact that the maligner of Goethe

was Owen, the conduct of whom, with regard to Darwin and Huxley,

Huxley had had just reason for resenting.

The theory, then, which had dropped stillborn from Goethe, but which

Oken developed, was simply that the skull consisted of a series of

expanded vertebræ. Each vertebra consists of a basal piece or centrum,

the anterior and posterior faces of which are closely applied to the

face of an adjoining vertebra, and of a bony arch or ring which

encloses and protects the nervous cord. Oken supposed that there were

four such vertebræ in the skull, the centra being firmly fused and the

arches expanded to form the dome of the skull. Quite correctly, he

divided the skull into four regions, corresponding to what he called

an ear vertebra, at the back, through which the auditory nerves

passed; a jaw vertebra, in the sphenoidal region, through which the

nerves to the jaws passed; an eye vertebra in front, pierced by the

optic nerves, and again in front a nose vertebra, the existence of

which he doubted at first. Quite rightly, he discriminated between the

ordinary bones of the skull and the special structures surrounding the

inner ear which he declared to be additions derived from another

source. So far it cannot be doubted that the vertebral theory made a

distinct advance in our knowledge of the skull. It was to a certain

extent, however, thrown into disrepute by various fantastic theories

with which Oken surrounded it. Later on, Cuvier removed from it these

wilder excrescences, and amplified the basis of observation upon which

the underlying theory of the unity of type of the skull throughout the

vertebrates was based. Cuvier, however, came to reject the theory,

except so far as it applied to the posterior or occipital segment of

the skull. Later on, Owen resuscitated the theory, first throwing

doubt on the merit of Goethe, and then suggesting that Oken, instead

of relying on the observed facts, had deduced the whole theory from

his own imagination. Owen, although he made no new contribution to

fact or theory in this matter, practically claimed the whole credit of

it as a scientific hypothesis.

When Huxley took up the subject, the position was that the vertebral

theory was in full possession of the field, under the auspices of

Owen. Huxley began afresh from observed facts. The first object of his

investigation was to settle once for all the question as to whether

the skulls of all vertebrates were essentially modifications of the

same type. He took in succession the skulls of man, sheep, bird,

turtle, and carp, and showed that in all these there were to be

distinguished the same four basi-cranial regions: the basi-occipital,

basi-sphenoid, pre-sphenoid, and ethmoid. These were essentially

identical with the centra of the four vertebræ of Oken. Similarly, he

showed the composition of the lateral and dorsal walls, proving the

essential identity of the structures involved and of their relations

to the nerve exits in the great types he had chosen. In the series of

lectures delivered before the College of Surgeons, he extended his

observations to a much larger series of vertebrates, and substantially

laid down the main lines of our knowledge of the skull. In two

important respects his statements were not merely a codification of

existing knowledge, but an important extension of it. He distinguished

the different modes in which the jaws may be suspended to the skull,

and established for these different kinds of suspensoria the names

which have ever since been employed. He proved clearly what had been

suggested by Oken, that the region of the ear is a lateral addition to

the skull, and he distinguished in it three bones, his names for which

have since become the common property of anatomists. Finally, he made

it plain beyond any possible doubt that the skulls of all vertebrates

were built upon a common plan.

Having established the facts, he proceeded to enquire into the theory.

There was now a new method for investigating such problems, the method

of embryology, which, practically, had not been available to Oken, and

of which neither Cuvier nor Owen had made proper use. By putting

together the investigations of a number of embryologists, by adding to

these himself, and, lastly, by interpreting the facts which his

investigations into comparative anatomy had brought to light, he

shewed that the vertebral theory could not be maintained. He shewed,

by these methods, that, though both skull and vertebral column are

segmented, the one and the other, after an early stage, are fashioned

on lines so different as to exclude the possibility of regarding the

details of each as mere modifications of a common type. "The spinal

column and the skull start from the same primitive condition, whence

they immediately begin to diverge." "It may be true to say that there

is a primitive identity of structure between the spinal or vertebral

column and the skull; but it is no more true that the adult skull is

a modified vertebral column than it would be to affirm that the

vertebral column is a modified skull." Taking the embryological facts,

he shewed that the skull arose out of elements quite different from

those of the vertebral column. The notochord alone is common to both.

The skull is built up of longitudinal cartilaginous pieces, now known

as the "parachordals" and "trabeculæ," of sense capsules enclosing the

nose and ear, and of various roofing bones. In the historical

development of the skull three grades become apparent; a primitive

stage, as seen in Amphioxus, where there is nothing but a fibrous

investment of the nervous structures; a cartilaginous grade, as seen

in the skate or shark, where the skull is formed of cartilage, very

imperfectly hardened by earthy deposits; a bony stage, seen in most of

the higher animals. He shewed that in actual development of the higher

animals these historical grades are repeated, the skull being at first

a mere membranous or fibrous investment of the developing nervous

masses, then becoming cartilaginous, and, lastly, bony. He made some

important prophetic remarks as to the probable importance that future

embryological work would give to the distinction between cartilage and

membrane bones--a prophecy that has been more than fully realised by

the investigations of Hertwig and of others. Our present knowledge of

the skull differs from Huxley's conception practically only in a

fuller knowledge of details. We know now that throughout the series

there is a primitive set of structures common to all animals higher in

the scale than Amphioxus, and forming the base and lateral walls of

the skull. This is termed the Chondrocraninm, because it is laid down

in cartilage; it is composed of the separate elements which Huxley

indicated, and, in different animals, as Huxley suggested, the exact

limits of the ossification of the primitive cartilages differ in

extent, but occur in homologous situations. This primitive skull is

roofed over by a series of membrane bones which have no connection in

origin with the other portions of the skull, and which have no

representative in the vertebral column, but which are the direct

descendants of the bony scales clothing the external skin in

cartilaginous fishes. In one respect only was Huxley erroneous. Partly

by inadvertence, and partly because the minute details of vertebrate

embryology became really familiar to zoölogists only after the

elaborate work of Balfour of Cambridge, Huxley, in his account of the

formation of the first beginnings of the skeleton in the embryo, made

confusion between the walls of the primitive groove, which, in

reality, give rise to the nervous structures, and those embryonic

tissues which form the skeletal system.

The next great piece of work which we may take as typical of Huxley's

contributions to vertebrate anatomy, is his classical study on the

classification of birds. The great group of birds contains a larger

number of species than is known in any other group of vertebrates,

and, in this vast assemblage of forms there is strikingly little

anatomical difference. The ostrich and the humming-bird might perhaps

be taken as types of the extremest differences to be found, and yet,

although these differ in size, plumage, adaptations, habits, mode of

life, and almost everything that can separate living things, the two

conform so closely to the common type of bird structure that knowledge

of the anatomy of one would be a sufficient guide, down to minute

details, for dissection of the other. None the less, there are

hundreds of thousands of species of birds between these two types. It

is not surprising that to reduce this vast assemblage of similar

creatures to an ordered system of classification has proved one of the

most difficult tasks attempted by zoölogists. Before Huxley, it had

been attempted by a number of distinguished zoölogists; but, for the

most part, these had relied too much on merely external characters and

on superficial modifications in obvious relation to habits. When

Huxley, in the course of a set of lectures on Comparative Anatomy, was

about to approach the subject of birds he was asked by a zoölogist how

he proposed to treat them. "I intend," he replied, "to treat them as

extinct animals." By that he meant that it was his purpose to make a

prolonged study of their skeletal structures the basis of his

grouping, following the lines which Cuvier, Owen, and he himself had

pursued so successfully in the case of the fossil remains of

vertebrates. The result was that this first systematic study of even

one set of the anatomical characters of the group completely reformed

the method by which all subsequent workers have tried to grapple with

the problem; ornithology was raised from a process akin to

stamp-collecting to a reasoned scientific study. The immediate

practical results were equally important. He was able to shew that

among the innumerable known forms there were three grades of

structure. The lowest had already been recognised and named by

Haeckel; it consisted of the Saururæ, or reptile-like, birds, and

contained a single fossil form, Archæopteryx, distinguished from all

living birds by the presence of a hand-like wing in which the

metacarpal bones were well developed and freely movable, and by the

possession of a long lizard-like tail actually exceeding in length

the remainder of the spinal column. The next group of Ratites,

although it contained only the Ostrich, Rhea, Emu, Cassowary, and

Apteryx, he shewed to be equivalent in anatomical coherence to the

third great group of Carinates, which includes the vast majority of

living birds. In his arrangement of the latter group, he laid most

stress on the characters of the bony structures which form the palate,

and by this simple means was able to lay down clearly at least the

main lines of a natural classification of the group.

Huxley's work upon birds, like his work in many other branches of

anatomy, has been so overlaid by the investigations of subsequent

zoölogists that it is easy to overlook its importance. His employment

of the skeleton as the basis of classification was succeeded by the

work of others who made a similar use of the muscular anatomy, of the

intestinal canal, of the windpipe, of the tendons of the feet, and

many other structures which display anatomical modifications in

different birds. The modern student finds that all these new sets of

facts are much greater in bulk than the work of Huxley, and it is easy

for him to remain in ignorance that they were all suggested and

inspired by the method which Huxley employed. He finds that further

research has supplanted some of Huxley's conclusions, and it is easy

for him to remain in ignorance that the conclusions themselves

suggested the investigations which have modified them. Huxley's

anatomical work was essentially living and stimulating, and too often

it has become lost to sight simply because of the vast superstructures

of new facts to which it gave rise.

Closely associated with vertebrate anatomy is the subject of

geographical distribution. In 1857 the study of this important

department of zoölogy was placed on a scientific basis, practically

for the first time, by a memoir on the geographical distribution of

birds published in the _Journal_ of the Linnæan Society of London. It

was known in a general way that different kinds of creatures were

found in different parts of the world, but little attempt had been

made to map out the world into regions characterised by their animal

and vegetable inhabitants, as the political divisions of the world are

characterised by their different governments and policies. Mr.

Sclater, who two years later became secretary of the Zoölogical

Society of London, in his memoir introduced the subject in the

following words:

"It is a well-known and universally acknowledged fact that we can

choose two portions of the globe of which the respective fauna

and flora shall be so different that we should not be far wrong

in supposing them to have been the result of distinct creations.

Assuming, then, that there are, or may be, more areas of creation

than one, the question naturally arises how many of them are

there, and what are their respective extents and boundaries; or,

in other words, what are the most natural primary ontological

divisions of the earth's surface?"

Mr. Sclater's answer was that there are six great regions;

Neotropical, Nearctic, Palæarctic, Ethiopian, Indian, and Australian,

and his answer, with minor alterations and the addition of a great

wealth of detail, has been accepted by zoölogy.

Two years later, however, Darwin gave a new meaning and a new

importance to Sclater's work, by the new interpretation he caused to

be placed on the words "centres of creation." Sclater's facts and

areas remained the same; Darwin rejected the idea of separate

creations in the older sense of the words, and laid stress on the

impossibility of accounting for the resemblances within a region and

for the differences between regions by climatic differences and so

forth. He raised the questions of modes of dispersal and of barriers

to dispersal, of similarities due to common descent, and of the

modifying results produced by isolation. He gave, in fact, a theory of

the "creations" which Mr. Sclater had shewn to be a probable

assumption. It was in the nature of things that Huxley should make a

contribution to a set of problems so novel and of so much importance

to zoölogy. In 1868, in the course of a memoir on the anatomy of the

gallinaceous birds and their allies, he made a useful attempt, nearly

the first of its kind, to correlate anatomical facts with geographical

distribution. Having shewn the diverging lines of anatomical structure

that existed in the group of creatures he had been considering, he

went on to shew that there was a definite relation between the

varieties of structure and the different positions on the surface of

the globe occupied at the present time by the creatures in question.

He made, in fact, the geographical position a necessary part of the

whole idea of a species or of a group, and so introduced a conception

which has become a permanent part of zoölogical science.

With regard to the number and limits of the zoölogical regions into

which the world may be divided, Huxley raised a number of problems

which have not yet reached a full solution. Mr. Sclater had divided

the world into six great regions: the Nearctic, including the

continent of North America, with an overlap into what is called South

America by geographers; the Palæarctic, comprising Europe and the

greater part of Asia; the Oriental, containing certain southern

portions of Asia, such as India south of the Himalayas and many of the

adjacent islands; the Ethiopian, including Africa, except north of

the Sahara, and Madagascar; the Australian, containing Australia and

New Zealand and some of the more southeastern of the islands of Malay;

the Neotropical, including South America. Huxley first called

attention to certain noteworthy resemblances between the Neotropical

and the Australian regions of Sclater, and held that a primary

division of the world was into _Arctogæa_, comprising the great land

masses of the Northern Hemisphere with a part of their extension

across the equator, and _Notogæa_, which contained Australia but not

New Zealand and South America. Although this acute suggestion has not

been generally accepted as a modification of Mr. Sclater's scheme, it

called attention in a striking fashion to some very remarkable

features in the distribution of animals. Subsequent writers have

considerably extended Huxley's conception of the similarities to be

found among the more southern land areas. They have pointed out that

the most striking idea of the distribution of land and water on the

surface of the globe is to be got by considering the globe alternately

from one pole and from the other. In the south, a clump of ice-bound

land, well within the Antarctic Circle, surrounds the pole. All else

is a wide domain of ocean broken only where tapering and isolated

tongues of land, South America, the Cape, Australia, lean down from

the great land masses of the north. On the other hand, all the great

land masses expand in the Northern Hemisphere, and shoulder one

another round the North Pole. America is separated from Asia only by

the shallowest and narrowest of straits; an elevation of a few fathoms

would unite Greenland with Europe. Science points definitely to some

part of the great northern land area as the centre of life for at

least the larger terrestrial forms of life. We know that these arose

successively, primitive birds like the ostriches being older than

higher forms like the parrots and singing birds; the pouched

marsupials preceding the antelopes and the lion; the lemurs coming

before the man-like apes. Each wave of life spread over the whole area

producing after its kind; then, pressing round the northern land area,

it met a thousand different conditions of environment, different

foods, enemies, and climates, and broke up into different genera and

species. But there was never a wave of life that was not followed by

another wave. In the struggle for existence between the newer and the

older forms, the older forms were gradually driven southwards towards

the diverging fringes of the land masses. The vanquished left behind

them on the field of battle only their bones, to become fossils.

Sometimes succeeding waves swept along to the extreme limits of the

land, and many early types were utterly destroyed. But others found

sanctuary in the ends of the South, and such survivors of older and

earlier types of life cause a similarity between the southern lands

that Huxley called Notogæa, although the extent of his region must be

increased.

Recently, however, there has been a recurrence to Huxley's suggested

union of South America and Australia, based on new evidence of a

direct kind, quite different from that which had just been given.

Various groups of naturalists have stated that there are similarities

between the invertebrate inhabitants of Australia and of South America

of a kind which makes the existence of a direct land connection in the

Southern Hemisphere extremely probable. Moreover, Ameghino has

recently described some marsupial fossils from South America which, he

states, belong to the Australian group of Dasyuridæ, and Oldfield

Thomas has described a new mammal from South America which is unlike

the opossums of America and like the diprotodonts of Australia. So

that, while the general opinion has been against Huxley's division,

Notogæa, in the strict meaning which he gave to it, there has recently

been an opinion growing in its favour.

Huxley also made minor alterations in Mr. Sclater's scheme by forming

an additional circumpolar region for the Northern Hemisphere, and by

elevating New Zealand into a separate region, distinct from Australia.

On these points there is a balance of opinion against his views.

Before leaving the subject of Huxley's contributions to vertebrate

anatomy, the actual details of which would occupy far too much space,

it is necessary to mention the great importance to zoölogy of the new

terms and new ideas he introduced into classification. His mind was,

above all things, orderly and comprehensive, and while, in innumerable

minute points, from the structure of the palate of birds to the

structure of the roots of human hair (actually the subject of Huxley's

first published contribution to scientific knowledge), he added to the

number of known facts, he did even more important work in

co-ordinating and grouping together the known body of facts. To him

are due not only the names, but the idea, that the mammalian animals

fall into three grades of ascending complexity of organisation: the

reptile-like Prototheria, which lay large eggs, and which have many

other reptilian characters; the Metatheria, or marsupial animals; the

Eutheria, or higher animals, which include all the common animals from

the mole or rabbit up to man. In a similar fashion, he grouped the

vertebrates into three divisions, and named them: Ichthyopsida, which

include the fish and Amphibia, creatures in which the aquatic habit

dominates the life history and the anatomical structure; Sauropsida,

including birds and reptiles, on the close connection between which he

threw so much light; Mammalia.

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