All who have occupied themselves with the structure of _Anchitherium_,

from Cuvier onwards, have acknowledged its many points of likeness to a

well-known genus of extinct Eocene mammals, _Palaeotherium_. Indeed, as

we have seen, Cuvier regarded his remains of _Anchitherium_ as those of

a species of _Palaeotherium_. Hence, in attempting to trace the pedigree

of the horse beyond the Miocene epoch and the Anchitheroid form, I

naturally sought among the various species of Palaeotheroid animals for

its nearest ally, and I was led to the conclusion that the _Palaeotherium

minus_ (_Plagiolophus_) represented the next step more nearly than any

form then known.

I think that this opinion was fully justifiable; but the progress of

investigation has thrown an unexpected light on the question, and has

brought us much nearer than could have been anticipated to a knowledge

of the true series of the progenitors of the horse.

You are all aware that, when your country was first discovered by

Europeans, there were no traces of the existence of the horse on any

part of the American Continent. The accounts of the conquest of Mexico

dwell upon the astonishment of the natives of that country when they

first became acquainted with that astounding phenomenon--a man seated

upon a horse. Nevertheless, the investigations of American geologists

have proved that the remains of horses occur in the most superficial

deposits of both North and South America, just as they do in Europe.

Therefore, for some reason or other--no feasible suggestion on that

subject, so far as I know, has been made--the horse must have died out

on this continent at some period preceding the discovery of America. Of

late years there has been discovered in your Western Territories that

marvellous accumulation of deposits, admirably adapted for the

preservation of organic remains, to which I referred the other evening,

and which furnishes us with a consecutive series of records of the fauna

of the older half of the Tertiary epoch, for which we have no parallel

in Europe. They have yielded fossils in an excellent state of

conservation and in unexampled numbers and variety. The researches of

Leidy and others have shown that forms allied to the _Hipparion_ and the

_Anchitherium_ are to be found among these remains. But it is only

recently that the admirably conceived and most thoroughly and patiently

worked-out investigations of Professor Marsh have given us a just idea

of the vast fossil wealth, and of the scientific importance, of these

deposits. I have had the advantage of glancing over the collections in

Yale Museum; and I can truly say, that so far as my knowledge extends,

there is no collection from any one region and series of strata

comparable, for extent, or for the care with which the remains have been

got together, or for their scientific importance, to the series of

fossils which he has deposited there. This vast collection has yielded

evidence bearing upon the question of the pedigree of the horse of the

most striking character. It tends to show that we must look to America,

rather than to Europe, for the original seat of the equine series; and

that the archaic forms and successive modifications of the horse's

ancestry are far better preserved here than in Europe.

Professor Marsh's kindness has enabled me to put before you a diagram,

every figure of which is an actual representation of some specimen which

is to be seen at Yale at this present time (Fig. 9).

The succession of forms which he has brought together carries us from

the top to the bottom of the Tertiaries. Firstly, there is the true

horse. Next we have the American Pliocene form of the horse

(_Pliohippus_); in the conformation of its limbs it presents some very

slight deviations from the ordinary horse, and the crowns of the

grinding teeth are shorter. Then comes the _Protohippus_, which

represents the European _Hipparion_, having one large digit and two

small ones on each foot, and the general characters of the fore-arm and

leg to which I have referred. But it is more valuable than the European

_Hipparion_ for the reason that it is devoid of some of the

peculiarities of that form--peculiarities which tend to show that the

European _Hipparion_ is rather a member of a collateral branch, than a

form in the direct line of succession. Next, in the backward order in

time, is the _Miohippus_, which corresponds pretty nearly with the

_Anchitherium_ of Europe. It presents three complete toes--one large

median and two smaller lateral ones; and there is a rudiment of that

digit, which answers to the little finger of the human hand.

The European record of the pedigree of the horse stops here; in the

American Tertiaries, on the contrary, the series of ancestral equine

forms is continued into the Eocene formations. An older Miocene form,

termed _Mesohippus_, has three toes in front, with a large splint-like

rudiment representing the little finger; and three toes behind. The

radius and ulna, the tibia and the fibula, are distinct, and the short

crowned molar teeth are anchitheroid in pattern.

But the most important discovery of all is the _Orohippus_, which comes

from the Eocene formation, and which is the oldest member of the equine

series, as yet known. Here we find four complete toes on the front-limb,

three toes on the hind-limb, a well-developed ulna, a well-developed

fibula, and short-crowned grinders of simple pattern.

Thus, thanks to these important researches, it has become evident that,

so far as our present knowledge extends, the history of the horse-type

is exactly and precisely that which could have been predicted from a

knowledge of the principles of evolution. And the knowledge we now

possess justifies us completely in the anticipation, that when the still

lower Eocene deposits, and those which belong to the Cretaceous epoch,

have yielded up their remains of ancestral equine animals, we shall

find, first, a form with four complete toes and a rudiment of the

innermost or first digit in front, with probably, a rudiment of the

fifth digit in the hind foot;[6] while, in still older forms, the series

of the digits will be more and more complete, until we come to the

five-toed animals, in which, if the doctrine of evolution is well

founded, the whole series must have taken its origin.

That is what I mean by demonstrative evidence of evolution. An inductive

hypothesis is said to be demonstrated when the facts are shown to be in

entire accordance with it. If that is not scientific proof, there are no

merely inductive conclusions which can be said to be proved. And the

doctrine of evolution, at the present time, rests upon exactly as secure

a foundation as the Copernican theory of the motions of the heavenly

bodies did at the time of its promulgation. Its logical basis is

precisely of the same character--the coincidence of the observed facts

with theoretical requirements.

The only way of escape, if it be a way of escape, from the conclusions

which I have just indicated, is the supposition that all these different

equine forms have been created separately at separate epochs of time;

and, I repeat, that of such an hypothesis as this there neither is, nor

can be, any scientific evidence; and, assuredly, so far as I know, there

is none which is supported, or pretends to be supported, by evidence or

authority of any other kind. I can but think that the time will come

when such suggestions as these, such obvious attempts to escape the

force of demonstration, will be put upon the same footing as the

supposition made by some writers, who are, I believe, not completely

extinct at present, that fossils are mere simulacra [images], are no

indications of the former existence of the animals to which they seem to

belong; but that they are either sports of Nature, or special creations,

intended--as I heard suggested the other day--to test our faith.

In fact, the whole evidence is in favour of evolution, and there is none

against it. And I say this, although perfectly well aware of the seeming

difficulties which have been built up upon what appears to the

uninformed to be a solid foundation. I meet constantly with the argument

that the doctrine of evolution cannot be well founded because it

requires the lapse of a very vast period of time; while the duration of

life upon the earth, thus implied, is inconsistent with the conclusions

arrived at by the astronomer and the physicist. I may venture to say

that I am familiar with those conclusions, inasmuch as some years ago,

when president of the Geological Society of London, I took the liberty

of criticising them, and of showing in what respects, as it appeared to

me, they lacked complete and thorough demonstration. But, putting that

point aside, suppose that, as the astronomers, or some of them, and some

physical philosophers tell us, it is impossible that life could have

endured upon the earth for so long a period as is required by the

doctrine of evolution--supposing that to be proved--I desire to be

informed, what is the foundation for the statement that evolution does

require so great a time? The biologist knows nothing whatever of the

amount of time which may be required for the process of evolution. It is

a matter of fact that the equine forms, which I have described to you,

occur, in the order stated, in the Tertiary formations. But I have not

the slightest means of guessing whether it took a million of years, or

ten millions, or a hundred millions, or a thousand millions of years, to

give rise to that series of changes. A biologist has no means of

arriving at any conclusions as to the amount of time which may be needed

for a certain quantity of organic change. He takes his time from the

geologist. The geologist, considering the rate at which deposits are

formed and the rate at which denudation goes on upon the surface of the

earth, arrives at more or less justifiable conclusions as to the time

which is required for the deposit of a certain thickness of rocks; and

if he tells me that the Tertiary formations required 500,000,000 years

for their deposit, I suppose he has good ground for what he says, and I

take that as a measure of the duration of the evolution of the horse

from the _Orohippus_ up to its present condition. And, if he is right,

undoubtedly evolution is a very slow process, and requires a great deal

of time. But suppose now, that an astronomer or a physicist--for

instance, my friend Sir William Thomson--tells me that my geological

authority is quite wrong; and that he has weighty evidence to show that

life could not possibly have existed upon the surface of the earth

500,000,000 years ago, because the earth would have then been too hot to

allow of life, my reply is: "That is not my affair; settle that with the

geologist, and when you have come to an agreement among yourselves I

will adopt your conclusions." We take our time from the geologists and

physicists, and it is monstrous that, having taken our time from the

physical philosopher's clock, the physical philosopher should turn round

upon us, and say we are too fast or too slow. What we desire to know is,

is it a fact that evolution took place? As to the amount of time which

evolution may have occupied, we are in the hands of the physicist and

the astronomer, whose business it is to deal with those questions.

[Illustration: Fig. 9]

Fore Foot. Hind Foot. Fore-arm. Leg. Upper Molar. Lower Molar.

RECENT.

EQUUS.

PLIOCENE.

PLIOHIPPUS.

PROTOHIPPUS

(_Hipparion_).

MIOCENE.

MIOHIPPUS

(_Anchitherium_).

MESOHIPPUS.

EOCENE.

OROHIPPUS.

FOOTNOTES:

[5] I use the word "type" because it is highly probable that many of the

forms of _Anchitherium_-like and _Hipparion_-like animals existed in the

Miocene and Pliocene epochs, just as many species of the horse tribe

exist now; and it is highly improbable that the particular species of

_Anchitherium_ or _Hipparion_, which happen to have been discovered,

should be precisely those which have formed part of the direct line of

the horse's pedigree.

[6] Since this lecture was delivered, Professor Marsh has discovered a

new genus of equine mammals (_Eohippus_) from the lowest Eocene

deposits of the West, which corresponds very nearly to this

description.--_American Journal of Science_, November, 1876.

FIGHTING PESTS WITH INSECT ALLIES

LELAND O. HOWARD

[Dr. Howard is Chief of the Division of Entomology in the

United States Department of Agriculture at Washington. He is

a lecturer at Swarthmore College and at Georgetown

University. He has written "The Insect Book," published by

Doubleday, Page & Co., New York; and a work on Mosquitoes,

issued by McClure, Phillips & Co., New York. Both are books

of interest from the hand of a master: they are fully

illustrated. The narrative which follows appeared in

_Everybody's Magazine_, June, 1901.]

Some twenty-five years ago there appeared suddenly upon certain acacia

trees at Menlo Park, California, a very destructive scale bug. It

rapidly increased and spread from tree to tree, attacking apples, figs,

pomegranates, quinces, and roses, and many other trees and plants, but

seeming to prefer to all other food the beautiful orange and lemon trees

which grow so luxuriantly on the Pacific Coast, and from which a large

share of the income of so many fruit-growers is gained. This insect,

which came to be known as the _white scale_ or _fluted scale_ or the

_Icerya_ (from its scientific name), was an insignificant creature in

itself, resembling a small bit of fluted wax a little more than a

quarter of an inch long. But when the scales had once taken possession

of a tree, they swarmed over it until the bark was hidden; they sucked

its sap through their minute beaks until the plant became so feeble that

the leaves and young fruit dropped off, a hideous black smut-fungus

crept over the young twigs, and the weakened tree gradually died.

In this way orchard after orchard of oranges, worth a thousand dollars

or more an acre, was utterly destroyed; the best fruit-growing sections

of the State were invaded, and ruin stared many a fruit-grower in the

face. This spread of the pest was gradual, extending through a series of

years, and not until 1886 did it become so serious a matter as to

attract national attention.

In this year an investigation was begun by the late Professor C. V.

Riley, the Government entomologist then connected with the Department of

Agriculture at Washington. He sent two agents to California, both of

whom immediately began to study the problem of remedies. In 1887 he

visited California himself, and during that year published an elaborate

report giving the results of the work up to that point. The complete

life-history of the insect had been worked out, and a number of washes

had been discovered which could be applied to the trees in the form of a

spray, and which would kill a large proportion of the pests at a

comparatively small expense. But it was soon found that the average

fruit-grower would not take the trouble to spray his trees, largely from

the fact that he had experimented for some years with inferior washes

and quack nostrums, and from lack of success had become disgusted with

the whole idea of using liquid compounds. Something easier, something

more radical was necessary in his disheartened condition.

Meantime, after much sifting of evidence and much correspondence with

naturalists in many parts of the world, Professor Riley had decided that

the white scale was a native of Australia, and had been first brought

over to California accidentally upon Australian plants. In the same way

it was found to have reached South Africa and New Zealand, in both of

which colonies it had greatly increased, and had become just such a pest

as it is in California. In Australia, however, its native home, it did

not seem to be abundant, and was not known as a pest--a somewhat

surprising state of affairs, which put the entomologist on the track of

the results which proved of such great value to California. He reasoned

that, in his native home, with the same food plants upon which it

flourished abroad in such great abundance, it would undoubtedly do the

same damage that it does in South Africa, New Zealand, and California,

if there were not in Australia some natural enemy, probable some insect

parasite or predatory beetle, which killed it off. It became therefore

important to send a trained man to Australia to investigate this

promising line.

After many difficulties in arranging preliminaries relating to the

payment of expenses (in which finally the Department of State kindly

assisted), one of Professor Riley's assistants, a young German named

Albert Koebele, who had been with him for a number of years, sailed for

Australia in August, 1888. Koebele was a skilled collector and an

admirable man for the purpose. He at once found that Professor Riley's

supposition was correct: there existed in Australia small flies which

laid their eggs in the white scales, and these eggs hatched into grubs

which devoured the pests. He also found a remarkable little ladybird, a

small, reddish-brown convex beetle, which breeds with marvellous

rapidity and which, with voracious appetite, and at the same time with

discriminating taste, devours scale after scale, but eats fluted scales

only--does not attack other insects. This beneficial creature, now known

as the Australian ladybird, or the Vedalia, Mr. Koebele at once began to

collect in large numbers, together with several other insects found

doing the same work. He packed many hundreds of living specimens of the

ladybird, with plenty of food, in tin boxes, and had them placed on ice

in the ice-box of the steamer at Sydney; they were carried carefully to

California, where they were liberated upon orange trees at Los Angeles.

[Illustration: Vedalia, or Australian Ladybird]

These sendings were repeated for several months, and Mr. Koebele, on his

return in April, 1889, brought with him many more living specimens which

he had collected on his way home in New Zealand, where the same Vedalia

had been accidentally introduced a year or so before.

[Illustration: Larvae of Vedalia eating White Scale]

The result more than justified the most sanguine expectations. The

ladybirds reached Los Angeles alive, and, with appetites sharpened by

their long ocean voyage, immediately fell upon the devoted scales and

devoured them one after another almost without rest. Their hunger

temporarily satisfied, they began to lay eggs. These eggs hatched in a

few days into active grub-like creatures--the larvae of the beetles--and

these grubs proved as voracious as their parents. They devoured the

scales right and left, and in less than a month transformed once more to

beetles.

And so the work of extermination went on. Each female beetle laid on an

average 300 eggs, and each of these eggs hatched into a hungry larva.

Supposing that one-half of these larvae produced female beetles, a simple

calculation will show that in six months a single ladybird became the

ancestor of 75,000,000,000 of other ladybirds, each capable of

destroying very many scale insects.

[Illustration: Twig of olive infected with Black Scale]

Is it any wonder, then, that the fluted scales soon began to disappear?

Is it any wonder that orchard after orchard was entirely freed from the

pest, until now over a large section of the State hardly an Icerya is to

be found? And could a more striking illustration of the value of the

study of insects possibly be instanced? In less than a year from the

time when the first of these hungry Australians was liberated from his

box in Los Angeles the orange trees were once more in bloom and were

resuming their old-time verdure--the Icerya had become practically a

thing of the past.

[Illustration: Rhizobius, the imported enemy of the Black Scale of the

Olive.]

This wonderful success encouraged other efforts in the same direction.

The State of California some years later sent the same entomologist,

Koebele, to Australia to search for some insect enemy of the black

scale, an insect which threatened the destruction of the extensive olive

orchards of California. He found and successfully introduced another

ladybird beetle, known as _Rhizobius ventralis_, a little dark-coloured

creature which has thrived in the California climate, especially near

the seacoast, and in the damp air of those regions has successfully held

the black scale in check. It was found, however, that back from the

seacoast this insect did not seem to thrive with the same vigor, and the

black scale held its own. Then a spirited controversy sprung up among

the olive-growers, those near the seacoast contending that the

_Rhizobius_ was a perfect remedy for the scale, while those inland

insisted that it was worthless. A few years later it was discovered that

this olive enemy in South Europe is killed by a little caterpillar,

which burrows through scale after scale eating out their contents, and

an effort was made to introduce the caterpillar into California, but

these efforts failed. Within the past two years it has been found that a

small parasitic fly exists in South Africa which lays its eggs in the

same black scale, and its grub-like larvae eat out the bodies of the

scales and destroy them. The climate of the region in which this

parasite exists is dry through a large part of the year, and therefore

this little parasitic fly, known as _Scutellista_, was thought to be

the needed insect for the dry California regions. With the help of Mr.

C. P. Lounsbury, the Government entomologist of Cape Colony, living

specimens of this fly were brought to this country, and were colonized

in the Santa Clara Valley, near San Jose, California, where they have

perpetuated themselves and destroyed many of the black scales, and

promise to be most successful in their warfare against the injurious

insect.

This same _Scutellista_ parasite had, curiously enough, been previously

introduced in an accidental manner into Italy, probably from India, and

probably in scale-insects living on ornamental plants brought from

India. But in Italy it lives commonly in another scale insect, and with

the assistance of the learned Italian, Professor Antonio Berlese, the

writer made an unsuccessful attempt to introduce and establish it a year

earlier in some of our Southern States, where it was hoped it would

destroy certain injurious insects known as "wax scales."

In the meantime the United States, not content with keeping all the good

things to herself, has spread the first ladybird imported--the

_Vedalia_--to other countries. Four years ago the white scale was

present in enormous numbers in orange groves on the left bank of the

river Tagus, in Portugal, and threatened to wipe out the orange-growing

industry in that country. The California people, in pursuance of a

far-sighted policy, had with great difficulty, owing to lack of food,

kept alive some colonies of the beneficial beetle, and specimens were

sent to Portugal which reached there alive and flourishing. They were

tended for a short time, and then liberated in the orange groves, with

precisely the same result as in California. In a few months the scale

insects were almost entirely destroyed, and the Portuguese

orange-growers saved from enormous loss.

This good result in Portugal was not accomplished without opposition. It

was tried experimentally at the advice of the writer, and in the face of

great incredulity on the part of certain Portuguese newspapers and of

some officials. By many prominent persons the account published of the

work of the insect in the United States was considered as untrustworthy,

and simply another instance of American boasting. But the opposition was

overruled, and the triumphant result silenced all opposition. It is safe

to say that the general opinion among Portuguese orange-growers to-day

is very favourable to American enterprise and practical scientific

acumen.

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