I have, above, made a passing reference to the fact that Mr. Darwin did

not fail to take account of some among these effects directly produced

on organisms by surrounding inorganic agencies. Here are extracts from

the sixth edition of the _Origin of Species_ showing this.

“It is very difficult to decide how far changed conditions, such as

of climate, food, &c., have acted in a definite manner. There is

reason to believe that in the course of time the effects have been

greater than can be proved by clear evidence.... Mr. Gould believes

that birds of the same species are more brightly coloured under a

clear atmosphere, than when living near the coast or on islands; and

Wollaston is convinced that residence near the sea affects the

colours of insects. Moquin-Tandon gives a list of plants which, when

growing near the sea-shore, have their leaves in some degree fleshy,

though not elsewhere fleshy” (pp. 106-7). “Some observers are

convinced that a damp climate affects the growth of the hair, and

that with the hair the horns are correlated” (p. 159).

In his subsequent work, _Animals and Plants under Domestication_, Mr.

Darwin still more clearly recognizes these causes of change in

organization. A chapter is devoted to the subject. After premising that

“the direct action of the conditions of life, whether leading to

definite or indefinite results, is a totally distinct consideration from

the effects of natural selection;” he goes on to say that changed

conditions of life “have acted so definitely and powerfully on the

organisation of our domesticated productions, that they have sufficed to

form new sub-varieties or races, without the aid of selection by man or

of natural selection.” Of his examples here are two.

“I have given in detail in the ninth chapter the most remarkable

case known to me, namely, that in Germany several varieties of maize

brought from the hotter parts of America were transformed in the

course of only two or three generations.” (Vol. ii, p. 277.) [And in

this ninth chapter concerning these and other such instances he says

“some of the foregoing differences would certainly be considered of

specific value with plants in a state of nature.” (Vol. i, p. 321.)]

“Mr. Meehan, in a remarkable paper, compares twenty-nine kinds of

American trees, belonging to various orders, with their nearest

European allies, all grown in close proximity in the same garden and

under as nearly as possible the same conditions.” And then

enumerating six traits in which the American forms all of them

differ in like ways from their allied European forms, Mr. Darwin

thinks there is no choice but to conclude that these “have been

definitely caused by the long-continued action of the different

climate of the two continents on the trees.” (Vol. ii, pp. 281-2.)

But the fact we have to note is that while Mr. Darwin thus took account

of special effects due to special amounts and combinations of agencies

in the environment, he did not take account of the far more important

effects due to the general and constant operation of these agencies.[3]

If a difference between the quantities of a force which acts on two

organisms, otherwise alike and otherwise similarly conditioned, produces

some difference between them; then, by implication, this force produces

in both of them effects which they show in common. The inequality

between two things cannot have a value unless the things themselves have

values. Similarly if, in two cases, some unlikeness of proportion among

the surrounding inorganic agencies to which two plants or two animals

are exposed, is followed by some unlikeness in the changes wrought on

them; then it follows that these several agencies taken separately, work

changes in both of them. Hence we must infer that organisms have certain

structural characters in common, which are consequent on the action of

the medium in which they exist: using the word medium in a comprehensive

sense, as including all physical forces falling upon them as well as

matters bathing them. And we may conclude that from the primary

characters thus produced there must result secondary characters.

Before going on to observe those general traits of organisms due to the

general action of the inorganic environment upon them, I feel tempted to

enlarge on the effects produced by each of the several matters and

forces constituting the environment. I should like to do this not only

to give a clear preliminary conception of the ways in which all

organisms are affected by these universally-present agents, but also to

show that, in the first place, these agents modify inorganic bodies as

well as organic bodies, and that, in the second place, the organic are

far more modifiable by them than the inorganic. But to avoid undue

suspension of the argument, I content myself with saying that when the

respective effects of gravitation, heat, light, &c, are studied, as well

as the respective effects, physical and chemical, of the matters forming

the media, water and air, it will be found that while more or less

operative on all bodies, each modifies organic bodies to an extent

immensely greater than the extent to which it modifies inorganic bodies.

* * * * *

Here, not discriminating among the special effects which these various

forces and matters in the environment produce on both classes of bodies,

let us consider their combined effects, and ask—What is the most general

trait of such effects?

Obviously the most general trait is the greater amount of change wrought

on the outer surface than on the inner mass. In so far as the matters of

which the medium is composed come into play, the unavoidable implication

is that they act more on the parts directly exposed to them than on the

parts sheltered from them. And in so far as the forces pervading the

medium come into play, it is manifest that, excluding gravity, which

affects outer and inner parts indiscriminately, the outer parts have to

bear larger shares of their actions. If it is a question of heat, then

the exterior must lose it or gain it faster than the interior; and in a

medium which is now warmer and now colder, the two must habitually

differ in temperature to some extent—at least where the size is

considerable. If it is a question of light, then in all but absolutely

transparent masses, the outer parts must undergo more of any change

producible by it than the inner parts—supposing other things equal; by

which I mean, supposing the case is not complicated by any such

convexities of the outer surface as produce internal concentrations of

rays. Hence then, speaking generally, the necessity is that the primary

and almost universal effect of the converse between the body and its

medium, is to differentiate its outside from its inside. I say almost

universal, because where the body is both mechanically and chemically

stable, like, for instance, a quartz crystal, the medium may fail to

work either inner or outer change.

Of illustrations among inorganic bodies, a convenient one is supplied by

an old cannon-ball that has been long lying exposed. A coating of rust,

formed of flakes within flakes, incloses it; and this thickens year by

year, until, perhaps, it reaches a stage at which its exterior loses as

much by rain and wind as its interior gains by further oxidation of the

iron. Most mineral masses—pebbles, boulders, rocks—if they show any

effect of the environment at all, show it only by that disintegration of

surface which follows the freezing of absorbed water: an effect which,

though mechanical rather than chemical, equally illustrates the general

truth. Occasionally a “rocking-stone” is thus produced. There are formed

successive layers relatively friable in texture, each of which, thickest

at the most exposed parts, and being presently lost by weathering,

leaves the contained mass in a shape more rounded than before; until,

resting on its convex under-surface, it is easily moved. But of all

instances perhaps the most remarkable is one to be seen on the west bank

of the Nile at Philæ, where a ridge of granite 100 feet high, has had

its outer parts reduced in course of time to a collection of

boulder-shaped masses, varying from say a yard in diameter to six or

eight feet, each one of which shows in progress an exfoliation of

successively-formed shells of decomposed granite: most of the masses

having portions of such shells partially detached.

If, now, inorganic masses, relatively so stable in composition, thus

have their outer parts differentiated from their inner parts, what must

we say of organic masses, characterized by such extreme chemical

instability?—instability so great that their essential material is named

protein, to indicate the readiness with which it passes from one

isomeric form to another. Clearly the necessary inference is that this

effect of the medium must be wrought inevitably and promptly, wherever

the relation of outer and inner has become settled: a qualification for

which the need will be seen hereafter.

* * * * *

Beginning with the earliest and most minute kinds of living things, we

necessarily encounter difficulties in getting direct evidence; since, of

the countless species now existing, all have been subject during

millions upon millions of years to the evolutionary process, and have

had their primary traits complicated and obscured by those endless

secondary traits which the natural selection of favourable variations

has produced. Among protophytes it needs but to think of the

multitudinous varieties of diatoms and desmids, with their

elaborately-constructed coverings; or of the definite methods of growth

and multiplication among such simple _Algæ_ as the _Conjugatæ_; to see

that most of their distinctive characters are due to inherited

constitutions, which have been slowly moulded by survival of the fittest

to this or that mode of life. To disentangle such parts of their

developmental changes as are due to the action of the medium, is

therefore hardly possible. We can hope only to get a general conception

of it by contemplating the totality of the facts.

The first cardinal fact is that all protophytes are cellular—all show us

this contrast between outside and inside. Supposing the multitudinous

specialities of the envelope in different orders and genera of

protophytes to be set against one another, and mutually cancelled, there

remains as a trait common to them—an envelope unlike that which it

envelopes. The second cardinal fact is that this simple trait is the

earliest trait displayed in germs, or spores, or other parts from which

new individuals are to arise; and that, consequently, this trait must be

regarded as having been primordial. For it is an established truth of

organic evolution that embryos show us, in general ways, the forms of

remote ancestors; and that the first changes undergone, indicate, more

or less clearly, the first changes which took place in the series of

forms through which the existing form has been reached. Describing, in

successive groups of plants, the early transformations of these

primitive units, Sachs[4] says of the lowest Algæ that “the conjugated

protoplasmic body clothes itself with a cell-wall” (p. 10); that in “the

spores of Mosses and Vascular Cryptogams” and in “the pollen of

Phanerogams” ... “the protoplasmic body of the mother-cell breaks up

into four lumps, which quickly round themselves off and contract, and

become enveloped by a cell-membrane only after complete separation” (p.

13); that in the _Equisetaceæ_ “the young spores, when first separated,

are still naked, but they soon become surrounded by a cell-membrane” (p.

14); and that in higher plants, as in the pollen of many Dicotyledons,

“the contracting daughter-cells secrete cellulose even during their

separation” (p. 14). Here, then, in whatever way we interpret it, the

fact is that there quickly arises an outer layer different from the

contained matter. But the most significant evidence is furnished by “the

masses of protoplasm that escape into water from the injured sacs of

_Vaucheria_, which often instantly become rounded into globular bodies,”

and of which the “hyaline protoplasm envelopes the whole as a skin” (p.

41) which “is denser than the inner and more watery substance” (p. 42).

As in this case the protoplasm is but a fragment, and as it is removed

from the influence of the parent-cell, this differentiating process can

scarcely be regarded as anything more than the effect of

physico-chemical actions: a conclusion which is supported by the

statement of Sachs that “not only every vacuole in a solid protoplasmic

body, but also every thread of protoplasm which penetrates the

sap-cavity, and finally the inner side of the protoplasm-sac which

encloses the sap-cavity, is also bounded by a skin” (p. 42). If then

“every portion of a protoplasmic body immediately surrounds itself, when

it becomes isolated, with such a skin,” which is shown in all cases to

arise at the surface of contact with sap or water, this primary

differentiation of outer from inner must be ascribed to the direct

action of the medium. Whether the coating thus initiated is secreted by

the protoplasm, or whether, as seems more likely, it results from

transformation of it, matters not to the argument. Either way the action

of the medium causes its formation; and either way the many varied and

complex differentiations which developed cell-walls display, must be

considered as originating from those variations of this

physically-generated covering which natural selection has taken

advantage of.

The contained protoplasm of a vegetal cell, which has self-mobility and

when liberated sometimes performs amœba-like motions for a time, may be

regarded as an imprisoned amœba; and when we pass from it to a free

amœba, which is one of the simplest types of first animals, or

_Protozoa_, we naturally meet with kindred phenomena. The general trait

which here concerns us, is that while its plastic or semi-fluid sarcode

goes on protruding, in irregular ways, now this and now that part of its

periphery, and again withdrawing into its interior first one and then

another of these temporary processes, perhaps with some small portion of

food attached, there is but an indistinct differentiation of outer from

inner (a fact shown by the frequent coalescence of the pseudopodia in

Rhizopods); but that when it eventually becomes quiescent, the surface

becomes differentiated from the contents: the passing into an encysted

state, doubtless in large measure due to inherited proclivity, being

furthered, and having probably been once initiated, by the action of the

medium. The connexion between constancy of relative position among the

parts of the sarcode, and the rise of a contrast between superficial and

central parts, is perhaps best shown in the minutest and simplest

_Infusoria_, the _Monadinæ_. The genus _Monas_ is described by Kent as

“plastic and unstable in form, possessing no distinct cuticular

investment; ... the food-substances incepted at all parts of the

periphery”;[5] and the genus _Scytomonas_ he says “differs from _Monas_

only in its persistent shape and accompanying greater rigidity of the

peripheral or ectoplasmic layer.”[6] Describing generally such low

forms, some of which are said to have neither nucleus nor vacuole, he

remarks that in types somewhat higher “the outer or peripheral border of

the protoplasmic mass, while not assuming the character of a distinct

cell-wall or so-called cuticle, presents, as compared with the inner

substance of that mass, a slightly more solid type of composition.”[7]

And it is added that these forms having so slightly differentiated an

exterior, “while usually exhibiting a more or less characteristic normal

outline, can revert at will to a pseud-amœboid and repent state.”[8]

Here, then, we have several indications of the truth that the permanent

externality of a certain part of the substance, is followed by

transformation of it into a coating unlike the substance it contains.

Indefinite and structureless in the simplest of these forms, as instance

again the _Gregarina_,[9] the limiting membrane becomes, in higher

_Infusoria_, definite and often complex: showing that the selection of

favourable variations has had largely to do with its formation. In such

types as the _Foraminifera_, which, almost structureless internally

though they are, secrete calcareous shells, it is clear that the nature

of this outer layer is determined by inherited constitution. But

recognition of this consists with the belief that the action of the

medium initiated the outer layer, specialized though it now is; and that

even still, contact with the medium excites secretion of it.

A remarkable analogy remains to be named. When we study the action of

the medium in an inorganic mass, we are led to see that between the

outer changed layer and the inner unchanged mass, comes a surface where

active change is going on. Here we have to note that, alike in the

plant-cell and in the animal-cell, there is a similar relation of parts.

Immediately inside the envelope comes the primordial utricle in the one

case, and in the other case the layer of active sarcode. In either case

the living protoplasm, placed in the position of a lining to the cuticle

of the cell, is shielded from the direct action of the medium, and yet

is not beyond the reach of its influences.

* * * * *

Limited, as thus far drawn, to a certain common trait of those minute

organisms which are mostly below the reach of unaided vision, the

foregoing conclusion appears trivial enough. But it ceases to appear

trivial on passing into a wider field, and observing the implications,

direct and indirect, as they concern plants and animals of sensible

sizes.

Popular expositions of science have so far familiarized many readers

with a certain fundamental trait of living things around, that they have

ceased to perceive how marvellous a trait it is, and, until interpreted

by the Theory of Evolution, how utterly mysterious. In past times, the

conception of an ordinary plant or animal which prevailed, not

throughout the world at large only but among the most instructed, was

that it is a single continuous entity. One of these living things was

unhesitatingly regarded as being in all respects a unit. Parts it might

have, various in their sizes, forms, and compositions; but these were

components of a whole which had been from the beginning in its original

nature a whole. Even to naturalists fifty years ago, the assertion that

a cabbage or a cow, though in one sense a whole, is in another sense a

vast society of minute individuals, severally living in greater or less

degrees, and some of them maintaining their independent lives

unrestrained, would have seemed an absurdity. But this truth which, like

so many of the truths established by science, is contrary to that common

sense in which most people have so much confidence, has been gradually

growing clear since the days when Leeuwenhoek and his contemporaries

began to examine through lenses the minute structures of common plants

and animals. Each improvement in the microscope, while it has widened

our knowledge of those minute forms of life described above, has

revealed further evidence of the fact that all the larger forms of life

consist of units severally allied in their fundamental traits to these

minute forms of life. Though, as formulated by Schwann and Schleiden,

the cell-doctrine has undergone qualifications of statement; yet the

qualifications have not been such as to militate against the general

proposition that organisms visible to the naked eye, are severally

compounded of invisible organisms—using that word in its most

comprehensive sense. And then, when the development of any animal is

traced, it is found that having been primarily a nucleated cell, and

having afterwards become by spontaneous fission a cluster of nucleated

cells, it goes on through successive stages to form out of such cells,

ever multiplying and modifying in various ways, the several tissues and

organs composing the adult.

On the hypothesis of evolution this universal trait has to be accepted

not as a fact that is strange but unmeaning. It has to be accepted as

evidence that all the visible forms of life have arisen by union of the

invisible forms; which, instead of flying apart when they divided,

remained together. Various intermediate stages are known. Among plants,

those of the _Volvox_ type show us the component protophytes so feebly

combined that they severally carry on their lives with no appreciable

subordination to the life of the group. And among animals, a parallel

relation between the lives of the units and the life of the group is

shown us in _Uroglena_ and _Syncrypta_. From these first stages upwards,

may be traced through successively higher types, an increasing

subordination of the units to the aggregate; though still a

subordination leaving to them conspicuous amounts of individual

activity. Joining which facts with the phenomena presented by the

cell-multiplication and aggregation of every unfolding germ, naturalists

are now accepting the conclusion that by this process of composition

from _Protozoa_, were formed all classes of the _Metazoa_[10]—(as

animals formed by this compounding are now called); and that in a

similar way from _Protophyta_, were formed all classes of what I suppose

will be called _Metaphyta_, though the word does not yet seem to have

become current.

And now what is the general meaning of these truths, taken in connexion

with the conclusion reached in the last section. It is that this

universal trait of the _Metazoa_ and _Metaphyta_, must be ascribed to

the primitive action and re-action between the organism and its medium.

The operation of those forces which produced the primary differentiation

of outer from inner in early minute masses of protoplasm, pre-determined

this universal cell-structure of all embryos, plant and animal, and the

consequent cell-composition of adult forms arising from them. How

unavoidable is this implication, will be seen on carrying further an

illustration already used—that of the shingle-covered shore, the pebbles

on which, while being in some cases selected, have been in all cases

rounded and smoothed. Suppose a bed of such shingle to be, as we often

see it, solidified, along with interfused material, into a conglomerate.

What in such case must be considered as the chief trait of such

conglomerate; or rather—what must we regard as the chief cause of its

distinctive characters? Evidently the action of the sea. Without the

breakers, no pebbles; without the pebbles, no conglomerate. Similarly

then, in the absence of that action of the medium by which was effected

the differentiation of outer from inner in those microscopic portions of

protoplasm constituting the earliest and simplest animals and plants,

there could not have existed this cardinal trait of composition which

all the higher animals and plants show us.

So that, active as has been the part played by natural selection,

alike in modifying and moulding the original units—largely as

survival of the fittest has been instrumental in furthering and

controlling the combination of these units into visible organisms,

and eventually into large ones; yet we must ascribe to the direct

effect of the medium on the first forms of life, that character of

which this everywhere-operative factor has taken advantage.

* * * * *

Let us turn now to another and more obvious attribute of higher

organisms, for which also there is this same general cause. Let us

observe how, on a higher platform, there recurs this differentiation of

outer from inner—how this primary trait in the living units with which

life commences, re-appears as a primary trait in those aggregates of

such units which constitute visible organisms.

The Factors of Organic Evolution · 第 4 / 6 段