A history without dates must seem very unsatisfactory to a historian,

and the question will naturally arise whether we can assign any

definite time to the various critical events recorded in the

evolution of the earth. At present we can only make more or less

plausible estimates. Thus, from a consideration of the thickness of

the sedimentary crust, and the rate at which sediments are now being

deposited, it has been asserted that the interval which separates

us from the close of the Archæan era may amount to about twenty-six

millions of years. Professor Joly, basing his argument on the undoubted

fact that the ocean derives the greater part of its salt from the

dissolved material contributed to it by rivers, comes to the conclusion

that the ocean first came into existence about one hundred millions

of years ago. As regards the birth of the moon, Sir George Darwin has

given a minimum limit of fifty-four millions of years, but he adds that

it may have taken place many hundreds of millions of years before this.

Lord Kelvin has attempted to determine the time which has elapsed since

the earth first acquired a solid crust. If we only knew the rate at

which the earth is cooling we might calculate back to this time with

some assurance of certainty, always, however, on the assumption that

the earth is simply a hot body cooling like any other hot body--such,

say, as a red-hot cannonball. But a few years ago it began to be

seriously suspected that this assumption was a very doubtful one, for

a new element--radium--was discovered in 1898, which possesses the

remarkable property of spontaneously liberating heat, and this not in

small quantities, but at an astonishing rate. One gramme of radium, for

example, gives out enough heat in one hour to raise the temperature of

one gramme of water to boiling point; hour after hour, year in, year

out, this wonderful substance is setting free the energy it contains,

and will continue to do so until, some thousands of years hence,

it has exhausted its store. If this element should happen to exist

in sufficient quantity within the earth, then the earth could not be

said to be cooling just like a piece of hot iron, and the increase of

temperature we experience as we descend towards the interior of the

earth might possibly be due to the heat set free from radium. Indeed,

the argument is not confined to the earth; it may apply also to the

sun, and much of the heat we derive from that luminary may be provided

by bursting atoms of radium. This was pointed out by Sir George Darwin

and Professor Joly in 1903.

It became obviously a question of the first importance to discover

what proportion of the earth’s crust consists of radium, and an

investigation was undertaken for this purpose by the Hon. R. J.

Strutt, who finds that the rocks composing the earth’s crust contain

a superabundance of radium--sufficient, if this element is uniformly

distributed through the whole earth in the same proportion as it occurs

at the surface, not only to make good the heat which is radiated away

into space, but actually to raise the temperature of our planet, which,

on this evidence, should, therefore, be growing not colder, but hotter.

This is a result as disconcerting at first sight as it is astonishing,

and its effects are very wide-reaching. Of course, it completely

destroys the validity of Lord Kelvin’s argument, but it also deprives

the nebular hypothesis of one of its cherished lines of evidence--a

loss which the force of the general argument enables us to bear with

equanimity.

[Sidenote: On the Eve of great Events]

In any case, the vast body of facts bearing on the history of the earth

suffices to show that its temperature cannot be rising. Mr. Strutt

has, therefore, imagined that the radium is not uniformly distributed

throughout the mass of the planet, and supposes that it is restricted

to an external zone forty-five miles in thickness; this would suffice

to maintain the earth at its existing temperature. If, however, we

admit a restriction of this kind, we are in no way bound to fix the

limit at forty-five miles. All we can say is that we do not know how

far downwards the radium reaches--for aught we know five miles, or even

less, is as likely a limit as forty-five miles. Professor Joly, indeed,

maintains that the radium we meet with is not proper to the earth at

all, but comes from the sun.

Radium is a short-lived element, its existence being limited to a

few thousand years; but as fast as it decays it is reproduced at the

expense of another element--uranium--the lifetime of which is measured

by hundreds of millions of years.

The last quarter of a century has proved fertile in great

discoveries--more so than any corresponding period in the past. As a

result, the whole world of scientific thought has been thrown into

commotion; old-established theories, and even the most fundamental

notions, seem to be in a state of flux. Under the stimulus of new ideas

great questions, such as the constitution of matter, the origin of

species, and the birth of worlds are being re-investigated with renewed

energy, and we seem to be on the eve of great events.

WILLIAM JOHNSON SOLLAS

FOUR PERIODS OF THE EARTH’S DEVELOPMENT

A Postscript to Professor Sollas’s Chapter on the Wonderful Story

of the World’s Birth, beginning on page 79

The earth was once “a fluid haze of light.” The whole solar system

once formed a vast nebula, consisting of glowing gas, or a swarm of

meteoroids. Our planet was slowly shaped into a globe out of this

primitive nebula.

This globe was at first intensely hot, and probably liquid. A solid

crust formed on the surface as heat was lost by radiation, and this

crust consisted of the oldest rocks of igneous formation like the

granites and gneisses. During this Archæan or Eozoic Period, the earth

acquired its atmosphere and its oceans, and it is probable that the

mysterious origin of life took place.

The later history of the earth since the stratified rocks began to

appear, and life existed, is divided into four main periods, of which

the first is known as Primary, or Palæozoic.

The First Period of the Earth

CAMBRIAN SYSTEM. The rocks formed in the Cambrian Age are

mainly grits, quartzites, and conglomerates, with shales, schists, and

limestones. The earth was then mostly covered by seas, and the first

well-defined forms of life were of marine origin.

SILURIAN SYSTEM. The Silurian rocks are mostly sandstones,

shales, and slates deposited in the seas. The first vertebrates made

their appearance as fishes, whilst insects began to flutter in the air,

and occasionally to alight on the emerging land.

DEVONIAN SYSTEM. This was the age of the old red sandstone.

Fishes reached a high state of development, whilst the first traces

appeared of land vegetation, ferns and lycopods.

CARBONIFEROUS SYSTEM. This system is exceptionally important,

because its chief rock is coal, the fossilised remains of the luxuriant

vegetation which grew in tropical swamps. The first terrestrial

animals, true air breathers, now appeared.

PERMIAN SYSTEM. The last of the primary systems gave us the

new red sandstone, distinguished from the old by lying above the coal

measures. The Permian Age was apparently unfavourable to life, and is

only notable for the first appearance of the land reptiles into which

the amphibians developed.

The Second Period of the Earth

The Secondary Period marks the emergence of the dry land into

importance greater than that of the sea.

TRIASSIC SYSTEM. The Triassic rocks chiefly consist of

sandstones and hardened clays laid down in shallow sea basins. Land

vegetation now first began to assume a modern type, with conifers and

cycads. The seas were still richly peopled, and the land first gave a

home to huge reptiles, or dinosaurs.

JURASSIC SYSTEM. This system is marked by a great variety

of limestones, the product of dead sea creatures. It is essentially

the age of reptiles. The ichthyosaurus disputed the seas with the

plesiosaurus; the pterodactyl ruled the air; whilst on land, huge

monsters like the brontosaur and diplodocus browsed on tropical

vegetation. From these reptiles the birds were developing, whilst small

marsupials, the oldest of the great mammalian race, skipped under the

branches.

CRETACEOUS SYSTEM. This was the age of the great chalk

deposits. The birds, now emerging from their reptilian ancestry,

dominated its life, and the first modern plants appeared on the land.

The Third Period of the Earth

The Tertiary Period marks the true beginning of modern geological

history, when the great outlines of geography were laid down, and

the first representatives of modern plants and animals made their

appearance.

EOCENE SYSTEM. The Eocene rocks are mainly limestones, with

sandstone and hardened clays. We owe them to the sea and its organisms.

Modern evergreen trees now first appeared. The mammals come to the

front, with the tapir-like palæotherium and the first recognisable

ancestor of the horse.

MIOCENE SYSTEM. The Miocene Age was a mountain-building

period, when the great chain which runs from the Alps into Central

Asia received its final uplift. Deciduous trees, like the beech and

elm, now made their appearance. The giant mastodon and the formidable

sabre-toothed tiger roamed the Miocene forest, and true apes--man’s

first forerunners--mopped and mowed in the boughs.

PLIOCENE SYSTEM. The last of the Tertiary ages set the final

stamp on the geological moulding of the earth’s crust. Its plants were

transitional to the flora of modern Europe. Great herds of herbivora

now appeared.

The Fourth Period of the Earth

The Quaternary Period is that in which we are still living. Its

outstanding feature is the appearance of man.

PLEISTOCENE OR GLACIAL SYSTEM. Its essential feature was the

appearance of glacial conditions over most of the northern hemisphere,

when great ice sheets rubbed our land into shape. The vegetation was

Arctic, and only animals like the reindeer and the hairy mammoth could

endure the cold.

HUMAN OR RECENT SYSTEM. The precise antiquity of man is still

uncertain, but it was only after the close of the Glacial Period that

he made his home in Europe, where he shared a precarious existence

with mammoth, cave-bear, and rhinoceros. Man developed through the

_Palæolithic_ and _Neolithic_ ages of stone implements to the _Bronze_

and _Iron_ ages, when metal was first worked. In the last of these we

live.

GEOLOGICAL CLOCK OF THE WORLD’S LIFE

This page is an effort, based on Professor Lester Ward’s calculations

in “Pure Sociology,” to show the comparative length of each geological

period, and the thin white line between Tertiary and Archæan indicates

the period of human history. Thin as this line is--and we could not

show it thinner--it is too thick, and out of proportion to the rest

of the clock. If we assume that from the beginning of the world--from

its first forming into a solid sphere--to the present, time may be

represented by a day of twenty-four hours, the time occupied by human

history does not exceed twelve seconds. This is reckoning human history

as ten thousand years. There is, of course, no possibility of obtaining

more than relative figures for such a scheme as this, which should be

regarded in connection with the previous page and the chart of the

Beginnings of Life, facing page 96

[Illustration: The thin white line between the Tertiary and the Archæan

periods represents the duration of human history]

TABLE SHOWING PROPORTIONS OF YEARS AND HOURS

Geological Periods | Years | Hours

------------------------+-------------+---------

Archæan | 18,000,000 | 6

Laurentian | 18,000,000 | 6

Cambrian | 6,000,000 | 2

Silurian | 6,000,000 | 2

Devonian | 6,000,000 | 2

Carboniferous | 6,000,000 | 2

Triassic | 3,000,000 | 1

Jurassic | 3,000,000 | 1

Cretaceous | 3,000,000 | 1

Tertiary and Quaternary | 3,000,000 | 1

------------------------+-------------+---------

The Quaternary Period | 72,000,000 = 24

is that in which we live|

TERTIARY AND QUATERNARY PERIODS

At a rough guess, three million years may be allowed for the Tertiary

and Quaternary periods

--------------------+-----------+------+------+------

Geological Periods | Years | Hrs. | Min. | Sec.

--------------------+-----------+------+------+------

Tertiary | 2,600,000 | -- | 52 | --

Pleistocene | 300,000 | -- | 6 | --

Human | 100,000 | -- | 2 | --

+-----------+------+------+------

Total | 3,000,000 | 1 | -- | --

--------------------+-----------+------+------+------

Human History | 10,000 == == 12

HOW LIFE BECAME POSSIBLE ON THE EARTH

BY DR. ALFRED RUSSEL WALLACE

Early writers on the relation of man and animated nature to the

material universe not only assumed that the latter existed for the

former, but that both alike were the results of special acts of

creation.

Furthermore, they usually took it for granted that all things were

created very much in the condition in which we now see them, and that

any changes that have since taken place are but slight superficial

modifications of a permanent and unchanging whole. Not only were the

sun and moon and stars created as appanages of the earth, but the earth

itself in all its details of sea and land, hills and valleys, mountains

and precipices, swamps and deserts, was made and fashioned just as we

now see it, and every feature of its surface was supposed to have some

purpose in connection with man.

[Sidenote: The Old Ideas of Creation]

These purposes we could, in some cases, understand, while in others

they seemed wholly unintelligible, and much ingenuity was bestowed

by the natural theologian and others to explain more and more of the

observed facts from this point of view. The same opinions prevailed in

regard to the infinite variety of animals and plants, each individual

species being supposed to have been an independent creation, and all to

have some definite and preordained purpose in relation to mankind.

These views, however absurd they seem to most people now, were almost

universally held so recently as during the seventeenth and eighteenth

centuries, and were thus coincident with one of the most brilliant

epochs of our literature and our dawning science. It was only towards

the beginning of the nineteenth century, when geology became widely

studied and its results were fully appreciated, that the more rational

conception of a very slow development of the earth’s surface during

countless ages began to be generally accepted.

[Sidenote: Changing Conditions of the Earth]

The grand nebular hypothesis of Laplace came to reinforce the views of

the geologists, by showing how the earth itself may have originated

as a gaseous or molten globe; and its slow process of cooling, with

the reaction of the interior and exterior on each other, served to

elucidate the facts of the heated interior, as shown by hot springs and

volcanoes, as well as many of the phenomena presented by the distorted

and metamorphosed strata which formed its crust. Hence it gradually

came to be perceived that the condition of the earth, with all its

endless variations of surface, of continents and oceans, of seas and

islands, of vast plateaux and lofty mountain ranges and extensive low

plains, with their ravines and cataracts, their great lakes and stately

rivers, was subject to perpetual change from that remote epoch when it

seems to have been actually the case that “the earth was without form

and void,” and that owing to the greater density of the vapour-laden

atmosphere, “darkness was upon the face of the deep.”

[Sidenote: Changing Forms of Life]

Another field of geological research forced us to the conclusion that

the same continued process of change had affected the forms of life

upon the earth. When carefully investigated, the crust was found

to abound in the fossilised remains of animals and plants. Careful

study of these showed that the oldest of all were of comparatively

simple structure, and that the higher forms only appeared in more

recent epochs; while the highest of all were probably very little

older than man himself. It is only during the last half century that

the theory of Evolution has been elaborated and has become generally

accepted as applicable to the whole of the vast cosmic process--from

the development of the nebulæ into stars and suns and systems, with a

corresponding development of planets from an early condition of intense

heat, through a more or less lengthy period of cooling and contraction,

to an ultimate state of refrigeration, the earlier and later stages

being alike unsuited to the existence of life.

[Sidenote: Theory of Natural Selection]

More important still, the discovery of the theory of Natural Selection

by Darwin--and at a later period by myself--has led to a satisfactory

explanation of the successive appearance of higher and more complex

forms of life, and also of that wonderfully minute and complex

_adaptation_ of every species to its conditions of existence and to

its organic as well as its inorganic environment, which all other

theories--even the most recent--have failed to grapple with.

[Sidenote: Wonderful Complexity of the Universe]

The logical completeness as well as the extreme simplicity of this

explanation of organic evolution has led great numbers of thoughtful

but ill-informed persons to reject it, because it seems to render

unnecessary the existence of a primary intelligent cause; while

another equally large but, as I think, equally ill-informed class--the

so-called monists--use it to demonstrate the non-existence, or, at all

events, the needlessness, of any such cause. Both alike err, because

they fail to take cognisance of the fact that every form of evolution,

and pre-eminently that of the organic world, is an explanation of a

process of change, a law of development, not in any sense or by any

possibility an explanation of fundamental laws, causes, or origins.

It presupposes the existence not only of matter--itself a thing whose

nature is becoming more and more mysterious and unthinkable with the

advance of physical science--but of all the vast complex of laws

and forces which act upon it--mechanical, physical, chemical, and

electrical laws and forces--all more or less dependent on the still

more mysterious, all-pervading ether. Thus, the universe in its purely

physical and inorganic aspect is now seen to be such an overwhelmingly

complex organism as to suggest to most minds some vast intelligent

power pervading and sustaining it.

Persons to whom this seems a logical necessity will not be much

disturbed by the dilemma of the agnostics--that, however wonderful the

material universe may be, a being who could bring it into existence

must be more wonderful, and that they prefer to hold the lesser

marvel to be self-existent rather than the greater. When, however,

we pass from the inorganic to the organic world, governed by a new

set of laws, and apparently by some regulating and controlling forces

altogether distinct from those at work in inorganic nature; and when,

further, we see that these organisms originated at some definite epoch

when the earth had become adapted to sustain them, and thereafter

developed into two great branches of non-sentient and sentient

life, the latter gradually acquiring higher and higher senses and

faculties till it culminated in man--a being whose higher intellectual

and moral nature seems adapted for, even to call for, indefinite

development--this logical necessity for some higher intelligence to

which he himself owes his existence, and which alone rendered the

origin of sentient life possible, will seem still more irresistible.

[Sidenote: Mind Behind the World]

The preceding remarks are intended to suggest that the theory of

evolution, combined with the quite recent and very startling advances

in physical science, so far from making the universe around us more

intelligible as a self-sustaining and self-existent whole, has really

rendered it less so, by showing that it is infinitely more complex

than we had formerly supposed; and further, that matter itself,

instead of being, as was once believed, a comparatively simple thing,

eternal and indestructible, is in all its various forms subject to

decay and disintegration. We now see that the only thing known to us

that we can conceive as having unending existence is mind itself; and,

just as Darwin’s theory of Natural Selection has opened up to us an

infinite field of study and admiration in the forms and colours and

mutual relations of the various species of animals and plants, so does

modern science open up to us new and unfathomable depths in the inner

structure of matter and of the cosmos, and thus compels us more and

more to recognise a mental rather than a mere physical substratum to

account for its existence.

There is, however, another set of relations which have been hitherto

very little studied--those between the organic and the inorganic

worlds in their broader aspects. These are now found to be very much

more complex and more remarkable than is usually supposed, and they

also have an important bearing upon the great problem of the origin

and destiny of man. This is a subject which opens up a variety of

considerations of extreme interest, showing that the exact adaptations

of our earth--and presumably of any other planets--to enable it to

sustain organic life, from its first appearance and through its long

course of development, is as varied and complex and as much beyond

the possibilities of chance coincidences as are any of the individual

adaptations of animals and plants to their immediate environment. Most

of these latter adaptations have been made known to us by Darwin and

his followers, and they have excited the admiration and astonishment

of all lovers of Nature. When the antecedent and grander relations of

planet to life are studied with equal care, these also will, I believe,

excite deeper admiration, still more profound astonishment, because

any secondary laws that could have brought them about are less easy to

discover, or even to imagine.

[Sidenote: Essential Conditions of Life]

Before we can form any adequate idea of the nature of a world which

shall be able to support and develop organic life, we must consider

what are the special conditions that alone render such life possible.

We, of course, refer to the whole of the organic world, from the lowest

to the highest, not to the few exceptional cases in which life may be

possible under conditions that would be fatal to the higher as well as

to most of the lower forms.

[Sidenote: The Miracle of Human Life]

The one striking speciality of the higher animals--and to a less

degree of the higher plants--is that of continuous, all-pervading

motion, every portion of their substance being in a state of flux:

each particle itself moving, growing, living and dying, and being

replaced by other particles of the same nature and fulfilling the

same functions. To keep up this growth, and to enable every part of

the structure to be continually renewed, food is required. This is

taken into the stomach of animals in the solid or liquid form, is

then decomposed and recomposed, that which is useless or superfluous

being thrown off by the intestines, while what is needed for growth

is transformed into blood and by a wonderfully intricate system of

branching tubes is carried to every part of the body, furnishing

nourishment and repair alike to bone and muscle, to all the internal

organs and all the outward integuments, and to that marvellously

complex nervous system which also permeates every part of the body and

is essential to the higher manifestations of life--to the exertion of

force, voluntary motion, and, apparently, to thought itself. Add to

this the constant influx of air, which at once purifies the blood and

supplies animal heat, and is so important that its cessation for a

few minutes is usually fatal, and we have a machine so complex in its

structure and mode of action that the most elaborate of human machines

is but as a grain of sand to a world in comparison.

[Sidenote: Basis of Physical Life]

Now the very possibility of such a material organism as this depends

upon a highly complex form of matter termed protoplasm, which is at

once extremely plastic and of extreme instability, and is yet capable

of secreting or building up its atoms into such solid and apparently

durable forms as bone, horn, and hair, besides the various liquids and

semi-solids which build up the organism. This fundamental organic

substance consists of only four chemical elements--nitrogen, hydrogen,

oxygen and carbon, and almost all animal and vegetable structures and

products have the same elemental constitution, though with such widely

different characteristics. Four other elements--sulphur, lime, silicon,

and phosphorus--also occur in small quantities in organic tissues,

to supply special needs; but these are not essential to all forms of

life, and are only taken up and utilised by the living protoplasm when

required. Protoplasm is undoubtedly the basis of physical life, yet

it only exists in, and is produced by, living organisms. The moment

such an organism dies, disorganisation and decay set in, and the whole

mass becomes gradually changed into more stable compounds, or into its

constituent elements. It appears, therefore, that some agency--usually

termed “vital force”--must be at work, first to produce this wonderful

compound, then to form it into “cells”--the physiological units of

all organisms--and afterwards to direct the energies supplied by heat

and light so as to build up the excessively complex structures, with

all their wonderful powers and potentialities, which we term animals

and plants. All this seems to imply not “a force” only, but very many

forces, all of which must have some kind of mind in or behind them,

to direct these forces to such infinitely varied yet perfectly defined

ends.

[Sidenote: A Marvel of Every Day]

The Book of History (Vol. 1 of 18) A History of All Nations from the Earliest Times to the Present · 第 13 / 58 段