This volume of the evolution series of the
pocket library is, like its predecessors, an expansion
of a lecture which the author has frequently
given before popular audiences. It differs
from its immediate predecessor in that it is
more loosely planned, and less obviously designed
to instruct. Geologic tables and explanations
have been omitted entirely; these the
reader can secure from the volume in this
Series (No. 47) entitled “Animals of Ancient
Seas,” while something about fossils and their
origin is given in the first chapter of “The
Building of the Earth.” (No. 275.)
The lecturer is more fortunate than the writer
in that his illustrations are more numerous; indeed,
a good stereopticon lecture need be little
more than a collection of beautiful and accurate
slides interestingly described. However, the
publishers have been generous in the number
of illustrations used in these booklets, so that
the difficulty is in a measure overcome.
It remains for me to acknowledge my indebtedness
to the various authors and articles mentioned
in the text and in notes. Dr. Lucas’ excellent
and interesting book, “Animals of the
Past,” has afforded in a concise form much information
that otherwise could have come only
from scattered technical papers. The article
by Dr. Case has furnished the base for the entire
first chapter, much of the material being
reproduced with but the slightest changes in
wording and arrangement, with the omission
of some technical data. Professor Case’s position
as our principal authority on Permian
vertebrates gives this chapter a reliability that
could not be achieved by a second-hand re-writing
of material from his larger and more
detailed monographs.
C. L. F.
CHAPTER I. THE FIRST LAND DWELLERS. — FOOTNOTES:
In the first book of this series, “Animals of
Ancient Seas,” (No. 47) we followed the evolution
of animal life from the most primitive
one-celled creatures to the fishes, and from the
most primitive fishes to those which possessed
lung-like organs that enabled them to breathe
from air as well as water. The next stage in
evolution was the development of feet and legs
from the fish fin, and this was accomplished
before the end of that geologic period known
as the Devonian, or more commonly, as the
“Age of Fishes.” True, no actual remains have
been found, but one fortunate collector succeeded
in getting out a fossil footprint, which
is all that is needed to prove the case. This
footprint was made by an animal that looked
much like the mud puppy, or salamander, of
modern streams and lakes, and was related
also to the frogs and toads. Like these creatures,
he spent the early part of his life in
water, breathing with gills, and possessing a
more or less fish-like form, while in his maturity
he lived at least partly on land, and
breathed by means of lungs. This type of development,
almost universal among his class,
has gained for them the name of Amphibians,
or “double livers.”
During those periods which are correctly
known as the Mississippian and Pennsylvanian,
but which are more commonly grouped under
the one name Carboniferous, the amphibians
increased in variety, and gave rise to a new
and immensely important group of animals, the
Reptiles. Since everyone knows the general
characters of this group, we shall not take the
trouble to define them. The important thing
about them, so far as evolution is concerned
is that they are capable of living on land
throughout their whole lives, not even the eggs
having to be deposited in water. This, as can
readily be seen, is a very fundamental character,
for as long as animals were confined to
water during their earliest stages, great progress
was quite impossible. Imagine what a
state humanity would be in if every child had
to begin life in some brook, lake, or pond, and
could not emerge from the water until it was
fifteen to twenty years old!
Unfortunately for our knowledge of life in
the past, fossils of both amphibians and reptiles
are by no means common in the Carboniferous
systems. It was not until the times of
coal deposition were almost past, and great
mountains and broad plains were taking the
place of shallow seas and sombre swamps, that
land dwelling animals became really abundant.
This appearance of dry land was not only the
cause of the development of the wonderful array
of animals that inhabited the Permian
world, but also the reason why so few of them
are preserved as fossils, for it is only when the
bones of animals become buried in water-soaked
layers of sediment, or covered by water, that
they are readily petrified. An animal that dies
and remains exposed to the open air stands
very little chance of becoming a fossil; its
bones are gnawed by carrion feeders, worn by
the wind, and broken up by decay. Thus of
the hundreds of thousands, even millions, of
buffalo, cattle, antelope, and elk whose carcasses
have dotted the plains of this continent in the
past half century there remain but a few rotten
and frost-split horns and bones. Without question
there are, in the muddy banks and bars
of rivers, skeletons and parts of skeletons that
are undergoing the slow process of petrification,
and that will be dug up and treasured in
the museums of some future civilization. And
just as the record of animal life of today will
be but a fragment of that which actually exists,
so the record of the great land fauna of the
Permian period is but the merest trace of the
myriad creatures of that time. It is only in
the most exceptional places that great quantities
of bones were brought together under
conditions favorable to fossilization, and such
a district is found in northern Texas.
“When the Appalachian Mountains were raised,
an extension of their southern end reached
across what are now Arkansas and Oklahoma,
terminating in the Wichita Mountains....
North of this range rose a broad upland, reaching
from the Rockies to the Appalachians and
to the Canadian line on the north; south of
the mountains a shallow sea reached nearly
to their base, and some great rivers from the
mountains and uplands poured their flood
waters into the sea and built up a great delta.
The remains of animals which haunted the
banks of the rivers were swept into them in
time of flood and carried out to be deposited in
the delta, which covered most of what is now
Wichita, Archer, Wilbarger counties in the
State of Texas. Naturally, most of the remains
which found their way into the streams were
already fragmentary, as they had rotted on the
banks, and had been torn by predatory animals,
but in their course to the sea they were
still further disintegrated so that, rolled by the
waters and beaten by the waves, they sank to
their burial as little more than water-worn
fragments; ends of limb bones, isolated vertebrae,
and broken skulls, which do little more
than tantalize the student with the hints of
new forms and new relationships that can not
be verified. In some places these water-worn
fragments are so thick upon the ground that
they literally can be shoveled up by the wagon
load. In some instances the bodies of animals
found their way unharmed into the water and,
distended by the gases of decomposition, floated
far and uninjured until they came to rest
on some mud flat beyond the reach of sharks
or other predatory animals. Such skeletons
are preserved entire with most remarkable perfection,
but they are exceedingly rare, and it
is a fortunate collector who turns up even one
in the course of a whole season of search.”[1]
FIG. 1
Cacops, a remarkable Permian amphibian.
Among the most remarkable of the animals
found in the stratified rocks of this ancient
delta are the amphibians. During the preceding
ages, as we have seen, they were the masters
of the continental world—the largest and
most progressive of land dwellers. But by the
time of the Permian they were on the downward
road which was to lead them, not to extinction,
but to the obscure positions of toads,
frogs and salamanders. But this decline did
not come at once, and with overwhelming completeness;
the early amphibians did not yield
tamely to the fate of old age. During the
Permian, and the succeeding age, the Triassic,
there lived some of the largest and strangest
amphibians that the world has known. Some
of them returned to the water and developed
eel-like bodies with enormous, arrow-like
heads; some lived in trees, where their remains
have been found by geologists studying
coal deposits; others protected themselves by
armor and crawled about more or less unmolested,
while not a few even went so far as to
take refuge in the ground.
The giant among all amphibians was Eryops,
of the Permian, with a length of about eight
feet. He looked somewhat like an immensely
overgrown salamander with flabby sprawling
legs that were incapable of lifting his body
from the ground except by the greatest effort.
His skull was from two to two and a half feet
in length, and looked like that of a gigantic
frog, the jaws were equipped with sharp, cone-shaped
teeth and sharp, powerful tusks. Evidently
Eryops held about the same position in
Permian swamps of Texas as the alligator does
in the Georgia bayous of today, lying near the
surface of the water with only its eyes and
nostrils exposed until the approach of a victim
stirred it to movement.
Sharply contrasted with the giant Eryops,
and doubtless often its victim, was the unique
Diplocaulus. The head of this amphibian was
the form of a rather angular crescent, with
strong spines directed to the rear, and protected
by heavy armor. The eyes and nostrils
were directed straight upward, and situated at
the forward end of the skull. The body, remarkably
enough, was long, thin, and eel-like,
with only rudimentary limb bones, and delicate
ribs. Probably the animal spent its entire life
in the water, wriggling along and pushing its
enormous head before it along the slimy bottom.
Perhaps, when attacked from above, Diplocaulus
was thrown into a frenzy of energy
that lifted his heavy, armored head above the
bottom, and thrashed it about in the water,
but anything like swimming must have been
quite beyond his power.
FIG. 2
Diplocaulus, the most bizarre
amphibian known.
But, bizarre though the amphibians of this
Permian deposit are, they are exceeded by the
reptiles. These creatures, as we have seen,
made their appearance
in the Pennsylvanian,
or late “Carboniferous,”
and already, in the very
beginning of their history,
they showed an
astonishing diversity of
form and habit. There
were reptiles that lived
in the water, and reptiles
that lived on dry
land; reptiles that ate
flesh, reptiles that ate
plants, and reptiles that
ate both. Some of them
were extremely primitive,
closely resembling
their amphibian ancestors,
while others were
like nothing that has
lived either before or
since.
The simplest of the
flesh-eating reptiles
were aquatic, living in
the waters of swamps
and rivers, and perhaps
even in the sea. Their
bodies and tails were
long and slender; their
teeth were simple, cone-shaped
affairs of almost
equal size throughout the entire length of
the jaw. Such a dentition indicates that the
reptiles possessing it preyed upon small animals
which they did not have to tear to pieces;
they merely seized their food and swallowed it,
leaving the entire process of digestion to the
internal organs, just as do the snakes of today.
The upper portions—called dorsal spines—of
the backbones in these forms were short, as
they are in most lizards, and did not project
through the skin.
In other, and somewhat higher reptiles, the
teeth appear to be differentiated, those at the
forward ends of both jaws being enlarged to
form tusks, while the posterior ones are flattened,
so that cutting edges are developed that
would cut the prey and assist materially in its
capture. In some of these same forms the
dorsal spines of the backbones are very high,
and project above the back as does the fin of
a fish.
In Dimetrodon, the last of the series of
spiny backed, carnivorous reptiles, these characters
reached their culmination. The incisor
and canine tusks attained an enormous length
and strength, projecting from the jaws as much
as three inches. The notch back of the incisors
is large and deep, and the posterior teeth
of both jaws are recurved and have sharp,
serrated edges so that they must have had all
of the cutting power of a Malay knife or kris.
A more effective set of weapons for the cruel
business of capturing prey and holding it despite
its desperate, agonized struggles hardly
could be conceived. At the same time, the
spines on the back developed to an enormous
length, and in some species tapered with the
delicacy of a whip lash. The tail was short
and strong, and the feet armed with well-developed
claws, all of which go to show that
the animal was purely land dwelling in habit.
Dimetrodon reached lengths of more than eight
feet, and was by all odds the largest and most
powerful creature of his day. We can imagine
him crouching in the bushes or tall grasses by
the side of some stream, watching for other
reptiles that come to quench their thirst, and
making a fierce, scuttling rush upon his prey.
Most often, perhaps, this was another reptile,
but the ponderous, slow-moving amphibians
also must have suffered from the attack of the
powerful Dimetrodon. There is ample evidence
that these animals often waged fierce
battles among themselves, for it is common to
find bones which have been broken during life
and healed again, telling of furious reptilian
contests for mates or territory, or perhaps with
the single brute idea of a cannibalistic meal.
PLATE I.
Restoration of Dimetrodon, the largest animal of
the Permian lands.
PLATE II.
Naosaurus (Edaphosaurus), the profusely spined
mud-grubber. (After Case.)
But a more wonderful animal still has left
its remains among the rocks of this delta.
Like Dimetrodon, it possessed high spines on
the back, but instead of being simple and tapering,
they were furnished with projecting processes
on either side, much like the yard arms
of old fashioned sailing ships. This resemblance
led Cope, a pioneer American paleontologist,
to call the animal Naosaurus, or “Ship
Lizard.” But in spite of his fierce appearance,
Naosaurus was totally unlike Dimetrodon in
habit, being a peaceful, sluggish eater of shellfish,
and perhaps of plants. This animal probably
has the most remarkable dentition of any
creature known. The incisor teeth are chisel-like,
as though useful in cutting strong, coarse
vegetation; behind them are five triangular
teeth not unlike those of such flesh-eaters as
the lion and tiger; behind these are simple
cones, like those of the primitive lizards. But,
most wonderful of all, on both the palate and
the corresponding portion of the lower jaw are
heavy plates of bone covered by short, stumpy
teeth, such as occur in the jaws of those fish
which live upon shellfish. Seemingly, therefore,
the animal ate all sorts of food, but instead
of having a generalized pattern of teeth
like the pig or man, it possessed a separate
set for each type of diet.
The discovery that Naosaurus was an eater
of plants and molluscs, and not a predatory
form, makes more perplexing than ever the
question as to the use of the spines on the
back. On such a thick-bodied, sluggish mud-grubber
the cross-barred spines must have had
about the same value as an ornamental frieze
on a canal boat. What conditions of environment
could have produced similar structures on
creatures of such dissimilar habits as Dimetrodon
and Naosaurus?
The structure of the animal shows that these
spines were not covered by flesh, but by a thin
membrane of skin, through which the spines
showed as plainly as the rays in the fin of a
fish. It is hard to conceive of this great dorsal
frill as being anything but a hindrance to both
pursuer and pursued. Cope suggested, in a
spirit of fun, that these animals were the natural
precursors of the modern fin-keeled yacht,
and that when they wished to navigate the
Permian waters they swam upon their backs.
Other authors have made other suggestions of
about the same note, but few have been able
to make any serious contribution on the subject.
The obvious suggestion is that the spines
served as some form of protective mimicry,
helping the animal to remain concealed among
the reeds which bordered the lakes or streams.
But this seems hardly necessary in an animal
that was the dominant form of its time and
needed no concealment unless as an aid to lying
in wait or making an unseen approach until
sufficiently near for its final rush upon its unsuspecting
prey. This last, is perhaps, a fair suggestion,
but it seems that the burden of maintaining
such a weak structure must have far
outweighed any advantage of concealment. The
spines were slender and were constantly being
broken in battle and by accident, and the animal
must have expended no inconsiderable amount
of energy in repairing the damaged structure.
There remains the suggestion that the spines
were remnants of a formerly useful structure,
and that their mature condition was purely due
to overgrowth. It seems certain that when a
structure has developed so far as to give
an animal a distinct advantage it may
continue to grow until it is a burden rather
than a help. Thus the spines, originating as
a protective feature, may have given their
possessors such a decided advantage that they
were almost free from attack. In this stage
they may have become over-nourished, and have
continued growing by a sort of inertia or momentum
until they reached their greatly exaggerated
development.[2] Furthermore, there is
a tendency, both in plants and in animals, for
a species nearing its extinction to develop a
spiny or horny habit. This we saw in the invertebrates,
among the aging Cephalopods, and
it is quite conceivable that a similar state of
affair prevails among these reptiles. For Dimetrodon
and Naosaurus,[3] dominant though
they were, were nearing the end of their life
cycle. In their senile aberrations they carried
the development of spines to greater and
greater lengths, until, in their declining strength
they were unable to maintain their species,
and so disappeared from the earth.
PLATE III.
Permian vertebrates, restored by Williston and
others. 1-3 are reptiles, while 4 is an amphibian.
[1] Case, E. C., “A Great Permian Delta and its Vertebrate
Life,” Pop. Sci. Monthly, Dec. 1908.
This quotation is somewhat paraphrased, while
the remainder of this chapter is based very
largely on the article.
[3] A relatively recent discovery, made by Dr. Case,
shows that the name Naosaurus must be
dropped, being replaced by the earlier name
Edaphosaurus. The former name, however, is
the commoner, as well as the more descriptive.
CHAPTER II. THE DINOSAURS. — FOOTNOTES:
The continent of North America during that
portion of the earth’s history which we may
call the Age of Reptiles would have seemed to
our eyes like another world. The present
coastal outlines, mountain chains, valleys,
rivers, lakes, and plains have, with few exceptions,
come into being long since that time.
During the early part[4] of the age there were
high mountains in the eastern part of the continent,
which sent strong, muddy streams flowing
to the Atlantic. California, on the other
hand, was under the Pacific; the Sierra Nevada
region was a great trough, while throughout
that region which is now eastern Colorado,
Utah, western Texas, and Arizona there lay a
belt of broad, shallow lakes.
The plant life of those times differed as
much from that of previous ages as from those
that were to follow. The great Pennsylvanian
coal forests of lepidodendrons, sigillarias, and
their allies, had almost completely vanished
from the earth. The higher lands were clothed
with cone-bearers, such as the Aurucarian pines
of present day Australia. Thick, gloomy forests
of tree ferns covered the moist regions,
while great “canebrakes” of horsetail reeds
whose stems reached four or five inches in
thickness bordered the bayous and marshes.
Cycads, trees which, though related to the
pines and spruces, look like palms, were abundant
in the forests of this time.
During the middle portion of the Age of
Reptiles conditions, both in geography and in
plant life, underwent no striking change. But
in the late Mesozoic, the Cretaceous period,
there were many changes. The Atlantic Ocean
encroached on the eastern part of the continent,
while the Gulf of Mexico extended as far
north as Illinois, and reached westward over
Texas. A broad mediterranean sea stretched
from the Gulf to the Arctic Ocean, and from
Iowa to Utah, with the Colorado Mountains
rising from it as a chain of islands. West of
the sea was a broad belt of swamp land which
extended from northern Alberta almost to
Mexico.
The plants of the Cretaceous changed with
the geography. The Cycads, so abundant in
the early Mesozoic, became rare in most regions.
The highest types of flowering plants
gained an almost complete ascendancy, and
forests of a decidedly modern appearance covered
the continent from the Gulf of Mexico to
the Arctic Ocean. “Among the kinds of forest
trees whose remains are found in the continental
deposits of the Cretaceous are the
magnolia, the myrtle, the laurel, the fig, the tulip
tree, the chestnut, the oak, beech, elm,
poplar, willow, birch and maple. Forests of
Eucalyptus grew along the coast of New England,[5]
and palms on the Pacific shores of
British Columbia. Sequoias of many varieties
ranged far into northern Canada. In northern
Greenland there were luxuriant forests of
magnolias, figs, and cycads; and a similar flora
has been disinterred from the Cretaceous rocks
of Alaska and Spitsbergen. Evidently the
lands within the Arctic Circle enjoyed a warm
and genial climate, as they had done during
the Paleozoic. Greenland had the temperature
of Cuba and southern Florida, and the time
was yet far distant when it was to be wrapped
in glacier ice.”[6]
Such were the conditions under which flourished
the mightiest race of animals that has
ever lived upon land. The Dinosaurs not only
were the dominant animals of their time, but
they reached sizes so great that they have been
rivalled by but one group of mammals—the
whales. They maintained their supremacy
throughout a long period of time estimated at
from nine to one hundred millions of years;
they survived important changes in geography
and climate, and became extinct through a
combination of causes which are yet only half
known. Perhaps the great changes in life
conditions at the end of the Cretaceous had
much to do with their disappearance, as may
also have been true of other reptiles living at
the same time. Not improbably, too, the rise
of egg-eating mammals, more intelligent and
active than the dinosaurs, was a factor; and last
of all, there remains the ever ready and ever
probable hypothesis of racial old age.
The Dinosaurs were descended, in the opinion
of those who have studied them, from
primitive, lizard-like reptiles with fairly long
limbs, long tails, five toes on each foot, and a
complete series of sharp pointed teeth. In
all probability, according to Dr. W. D. Matthew,[7]
this ancestor was fully capable of living
on dry land, and was more or less in the habit
of walking on its hind legs alone.
One of the most striking things about the
Dinosaurs is their notable lack of brain power.
In man, a creature weighing anywhere from
one hundred twenty to two hundred pounds,
on the average, the weight of a normal brain
is about three pounds. The smallest brain that
can exist and possess reasoning powers is about
two pounds, while the smallest human brain
known to be fitted for life alone weighs just
a little more than ten ounces.
We can readily see that if conditions were
proportionate among the Dinosaurs the size of
the brain would be almost unbelievable. Instead,
the reptile Claosaurus, which once inhabited
the valleys of Maryland, and was
twenty-five feet long and more than twelve feet
high, had a brain so small that it must have
weighed less than one pound. Brachiosaurus,
probably the biggest beast that ever walked,
was not much better equipped, while Triceratops,
a Dinosaur having more than twice the
bulk of the average elephant, possessed a brain
weighing about two pounds. Truly they who
are prone to refer to the “brainlessness” of human
beings should consider the Dinosaurs before
they speak! These great beasts must have
known just about enough to rest when they
were tired and eat when they were hungry;
“coming in out of the rain” doubtless was an
idea altogether too complicated for them to
grasp.
But, as Lucas and others have emphasized,
intelligence is one thing and living another and
a very different one. The poor, weak brains
of the Dinosaurs doubtless had but little to
do with the primary functions of life; the
spinal cord took care of them. In some of the
beasts, notably in the armored giant Stegosaurus,
the spinal cord possessed a sacral enlargement
that was twenty times as large as
the brain. This remarkable fact, when announced
by Professor Marsh, attracted great
attention, and was made the subject of much
newspaper writing. Thousands of people who
would never recognize the name Stegosaur are
familiar with the marvelous character of that
beast as he is described in this catchy though
fanciful poem:
PLATE IV.
The armored giant Stegosaurus.
THE DINOSAUR.
Behold the mighty dinosaur,
Famous in prehistoric lore,
Not only for his weight and strength
But for his intellectual length.
You will observe by these remains
The creature had two sets of brains—
One in his head (the usual place),
The other at his spinal base.
Thus he could reason a priori
As well as a posteriori.
No problem bothered him a bit:
He made both head and tail of it.
So wise he was, so wise and solemn,
Each thought just filled a spinal column.
If one brain found the pressure strong
It passed a few ideas along;
If something slipt his forward mind
’Twas rescued by the one behind;
And if in error he was caught
He had a saving afterthought.
As he thought twice before he spoke
He had no judgments to revoke;
For he could think without congestion,
Upon both sides of every question.
O’ gaze upon this model beast,
Defunct ten million years at least!
The Dinosaurs, like all other groups of animals,
may be divided into sub-groups, depending
on habits, structure, etc. The commonest
classification separates them into three divisions:
the carnivorous, the amphibious, and
the beaked. One of the most remarkable of the
flesh-eating species, though not the largest, is
Allosaurus, a powerful reptile that once roamed
over the western part of North America. He
walked by means of his hind legs only, using
his long tail as a balance for his body. The
huge head, armed with long, sharp teeth, was
set on a heavy, short neck; casts of the brain
indicate that it was of much the same type as
that of the modern alligator, but considerably
less effective.
PLATE V.
One of the greater carnivorous dinosaurs, showing
the large head, long teeth, tiny fore limbs
and ponderous walking legs typical of the
group. (Modified after Lull.)
Allosaurus lived upon dry land, seldom venturing
into the great Mesozoic swamps. He
was predaceous, attacking his prey in swift,
mighty rushes, tearing it with the jaws and
occasionally striking it with the powerful tail.
Anything like the elaborate stalking of game
such as we see in the tiger and lion of today
was impossible to the Dinosaur; he simply lay
in wait until the close approach of prey stimulated
him to his tremendous but half instinctive
rush. The kill was torn to pieces and
swallowed without chewing, as is the case with
the alligator of today.
The amphibious Dinosaurs, which must have
provided much of the food for Allosaurus and
his kin, were characterized by blunt teeth and
claws, strong, elephant-like legs and feet, long
neck, and small head. They attained very
great size, some of them, as we have said, being
the largest of land animals. They may
well be typified by Brontosaurus, the Thunder
Lizard, which though not the longest, was
one of the largest of his kind. The skeleton
which is mounted in the American Museum
is sixty-six feet long, the animal when alive
having weighed about thirty-eight tons. The
body was large and rather short; the neck long,
and the head small. The tail was long and
thick, and the legs massive and post-like. The
bones of the legs were very long and heavy, the
thigh bones being from five to six feet long—the
largest single bones so far discovered. The
vertebrae, or “backbones,” were as much as
four and one-half feet high, being larger than
those of the whale.
The teeth and general structure of Brontosaurus
give fairly reliable evidence as to the
habits of the animal. It spent its life in the
shallow water of lagoons, feeding upon the
succulent water plants. There is no evidence
that it swam very much; probably its principal
mode of progression was wading, with
the immense body partly supported by the
water. Perhaps the beast occasionally left the
water for the purpose of laying eggs, as is
shown in Knight’s oft-printed restoration. It
appears, however, that Brontosaurus was not
built for land travel; that his joints were so
imperfectly formed that he could not have
moved on land without tearing those of the
leg to pieces. Dr. Matthew thinks that the
species of this genus bore their young alive,
as do certain modern reptiles, and therefore
had no need to leave the swamps and bayous
at any time during their lives.
Within the last few years there have come
sketchy preliminary accounts of a mammoth
find near Tendaguru, Africa, by an expedition
sent out from Germany. They announce the
discovery of a Dinosaur whose neck and fore
limbs far exceeded those of Brontosaurus, although
the hinder parts of the skeleton were
relatively small. It appears that this giant,
which the German savants appropriately
named Gigantosaurus, is identical with the
American form Brachiosaurus, whose fragmentary
remains are on exhibit at the Field
Museum of Chicago. It is, without question
the largest known Dinosaur, so far as weight
goes—a long-necked wading creature that
lived much as did Brontosaurus but was capable
of going into considerably deeper waters,
quite beyond reach of the fierce carnivorous
giants of the land.
PLATE VI.
Fig. 1—Diplodocus, the longest Dinosaur known.
Fig. 2—Brontosaurus, the giant that could not walk except in water,
because of his great weight and feeble joints.
The distinctive character of the third group
of Dinosaurs is the possession of a horny
beak or bill, much like that of modern birds.
Indeed, there are many features in the anatomy
of these reptiles that indicate their relationship
to the birds, and it is probable that the remote
ancestors of the two groups were very
closely connected—perhaps identical. But the
ancestral birds developed feathers and took
to flying, while the ancestral beaked Dinosaurs
(Predentates) specialized in the direction of
land life, and in their later development became
even more widely diversified in form
than did their feathered relatives.
The beaked Dinosaurs lived entirely upon
vegetable food. The best known of them,
Triceratops or “He-of-the-three-horned-head,”
looked more like a gigantic, long-tailed rhinoceros
than a reptile. Above each eye was a
long, sharp horn which extended forward; the
bony cores which remain in the fossils are as
much as thirty-three inches long, and during
life the horny covering must have lengthened
them by six inches to a foot. The horn above
the nose was considerably shorter, yet would
have compared favorably with that of many
rhinoceroses.
“Standing before the skull of Triceratops,”
says Dr. Lucas, “... one notices in front of
each eye a thick guard of projecting bone, and
while this must have interfered with vision directly
ahead it must have also furnished protection
for the eye. So long as Triceratops
faced an adversary he must have been practically
invulnerable, but as he was the largest
animal of his time, upward of twenty-five feet
in length, it is probable that his combats were
mainly with those of his own kind and the
subject of dispute some fair female upon whom
two rival suitors had cast covetous eyes. What
a sight it would have been to have seen two of
these big brutes in mortal combat as they
charged upon each other with all the impetus
to be derived from ten tons of infuriate flesh!
We may picture to ourselves horn clashing
upon horn, or glancing from each bony shield
until some skilful stroke or unlucky slip placed
one combatant at the mercy of the other, and
he went down before the blows of his adversary
‘as falls on Mount Alvernus a thunder-smitten
oak?’”
Two Triceratops horns in the possession of
the United States National Museum bear the
marks of such an encounter as that described
by Dr. Lucas, for one of them is broken about
half way between the tip and the base, and
the stump is healed and rounded over. Evidently
their owner was not seriously injured
in the fight, but lived to a ripe old age in spite
of his infirmity.
Triceratops had a number of relatives, at
least one of which is even more famous than
himself. This is Stegosaurus, the great Armored
Dinosaur that possessed the remarkable enlargement
of the spinal cord. Like his three-horned
relative, Stegosaurus was a land dweller
that walked upon four legs. His head was
very small, as were his fore limbs; his body
was very large, and his tail long and powerful.
Along his back ran two rows of bony plates,
some of which were four inches thick at the
base, and two and one-half feet high. The tail
bore, near the tip, two pairs of spines which
were almost as long as the back plates, and
half again as thick. The hind limbs were long
and straight, in marked contrast with the front
ones, so that the creature when walking must
have appeared to be in constant danger of
turning a somersault.
PLATE VII. Triceratops, the Three Horned Reptile.
Stegosaurus was a contemporary of Brontosaurus
and the carnivorous Allosaurus. Like
the former, he was a peaceful plant feeder,
but unlike him, did not flee to the shallows in
order to avoid his flesh-eating relatives. For
this great armor, although undoubtedly developed
in the interests of peace, was hardly
designed with any consideration for the Hebrew
creed of turning one cheek when the
other is smitten. Stegosaurus was too brainless
and to clumsy to go about seeking trouble,
but to those creatures foolhardy enough to attack
him he could offer stiff resistance. A
few blows of the huge spiked tail, more powerful
than the club of the mightiest ogre of mythology,
would be quite enough for even such
giants as Allosaurus. Stegosaurus, like the
rhinoceros of modern Africa, probably went
his way unharming and unharmed.
The Dinosaurs first appeared during the
Triassic period when they roamed through the
valleys of eastern North America in great numbers,
leaving their footprints on the soft, fine
mud of the valley flats. The succeeding period,
the Jurassic, was their Golden Age—the age of
Brontosaurus, Allosaurus, Stegosaurus, Diplodocus
and other monsters. During the Comanchean
and Cretaceous periods the larger
Dinosaurs became extinct, and were supplanted
by the smaller beaked forms, such as Triceratops.
At the end of the Cretaceous period,
which was also the end of the Age of Reptiles,
the Dinosaurs became almost totally extinct.
Perhaps a few of them survived in specially
favored localities, for Dinosaur bones are found
in rocks which a number of geologists refer
to the beginning of the Age of Mammals. But
such survivals were of small importance, and
had little effect on the general annihilation.
The Dinosaurs were unable to meet the demands
of a dry-land environment, and joined
the great hosts of creatures that at various
times have held the earth in their sway and
then, defeated by causes at which we can only
guess, have passed into extinction.
[4] The Mesozoic Era, or Age of Reptiles, is divided
into four periods—Triassic, Jurassic, Comanchean,
and Cretaceous. The first two are here
referred to as the “early” part of the age; the
third as the “middle,” and the fourth as the
“late.”
[5] The Eucalyptus is now common in Australia,
while the Sequoia is the “Big Tree” of California.
[7] Dr. Matthew, curator of vertebrate paleontology
at the American Museum of Natural History, is
one of the authorities on Dinosaurs. His book,
“Dinosaurs,” published by the Museum, has afforded
much of the material to be found in
this chapter.
CHAPTER III. REPTILES RE-CONQUER THE SEA. — FOOTNOTES:
The sea, as we have seen, was the metropolis
of primitive life. Then came the amphibia, and
the scene of animal activities was partially
transferred to land, while with the coming of
reptiles the abandoning of the sea by the
higher forms of life seemed to be insured.
Yet the change did not come so rapidly as one
might think, for the reptiles after having
begun their conquest of the land sent not less
than three great branches back to the water,
and one of these, at least, extended its domain
around the world, from the islands of the
South Seas to what are now the plains of
North America.
During the latter part of the Age of Reptiles
a great island sea spread over a large part of
this continent, while other portions of the
world were similarly inundated. Almost everywhere
on the expanse of the shallow Cretaceous
waters might have been seen the forms of
huge, snake-like reptiles, the Elasmosaurs,
whose arrow-shaped heads, poised on long
necks rose from ten to twenty feet above the
surface as they swam about searching for food
or avoiding enemies. When the prey was located,
the reptiles dived to capture it; when an
enemy approached they swam away with almost
incredible swiftness. Their long necks
were attached to large, thick bodies which ended
in long, tapering tails. The legs were modified
to form broad paddles, of great value in
swimming; the front pair, perhaps, were used
in seizing prey. Being carnivorous, the Elasmosaur
ate whatever it could catch, and
Elasmosaur bones are commonly found along
with those of creatures on which they fed. Not
uncommonly large quantities of rounded pebbles
are found with the remains of these reptiles,
sometimes a peck of them in a single
deposit. These stones filled the same purpose
as do the “gizzard stones” found in the
stomachs of modern birds. Evidently the Elasmosaurs
and their allies did not tear or bite
their food into small bits, but relied on the
action of their stomachs, assisted by these
stones, to do the work.
PLATE VIII. An Elasmosaur swimming, as drawn by Williston.
But, remarkable though these reptiles may
seem, they were by no means the rulers of the
Mesozoic oceans and seas. The great Mosasaurs
were not only the giants of those waters,
but were far more numerous and wide-spread
than their less hardy and prolific contemporaries.
We may quite properly call these animals
great, for so they were. But it is well to remember
that among the lower animals as
among men there are degrees of greatness;
moreover there is a general desire on the part
of men to magnify the animals of the past,
and consider them as being far larger than
any that live today. Few people, when thinking
of ancient creatures, stop to recollect that
the whales of today are by far the largest animals
that ever lived on the earth, just as modern
shellfish compare very favorably with
those of past ages. True, there are no reptiles
today that compare with the largest of the
Dinosaurs, but by no means all of the Dinosaurs
were giants. A few Mosasaurs attained
a length of forty feet—some even forty-five—but
most of them were less than twenty.
Among modern reptiles, the Mugger, or Man-eating
Crocodile of Africa grows, if allowed
to live long enough, to a length of twenty-five
or thirty feet, and therefore exceeds in measurements
as well as weight the average Mosasaur.
The Mosasaurs were elongated and gracefully
fish-like in form. Their heads were large, flattened,
and conical; the eyes were placed on
the sides rather than the top of the skull.
Their tails were long, with flattened, fin-like
extensions that assisted the four broad, powerful
flippers when the creatures were swimming.
Like their distant relatives, the snakes,
they possessed four rows of teeth on the roof
of the mouth. These teeth were valueless for
chewing, but were of utmost service in holding
the prey, which was swallowed entire. The
probability is that the tongue was long and
forked, while the structure of the throat and
windpipe indicates that the mighty Mosasaur’s
only call was a serpent-like hiss.
The first Mosasaur was discovered in the
quarries beneath St. Peter’s Mount, near Maestritch,
Germany, some ninety feet below the
surface. Immediately on finding the specimen
the workmen informed Dr. Hoffman, the surgeon
of the local forces, and an ardent collector
of fossils. He labored with the quarrymen
for two weeks, and was rewarded by an
almost perfect specimen which he took to his
home and cleaned with great care and success.
The fossil was so unusual, and was made the
basis of so many papers, illustrations, and discussions,
that the canon of the cathedral which
stands on St. Peter’s decided that he should
own the specimen. Dr. Hoffman refused to
give it up, and Canon Goddin instituted a long,
expensive, and harassing law-suit, making certain
feudal rights the basis of his claim. The
whole chapter, of course, stood with their reverend
brother, and the decree went against
the surgeon, who was forced to give up his
specimen and pay the costs of the trial. For
several years the skull remained in the possession
of the clergyman, and Hoffman died
without regaining it. Finally, during the
French revolution, Maestritch was bombarded
and captured. During the attack, the artillerymen
had not been allowed to shoot into that
part of the city where the fossil was known
to be. The canon, guessing the reason for
this particular favor, hid the skull in a vault,
but was forced to give it up when the city was
plundered. The French, who did not hesitate
to appropriate anything of value in either science
or art, bore the famous Mosasaur off to
Paris, and put it in the museum at the Jardin
des Planes, where it still remains.
PLATE IX.
A Mosasaur swimming.
The first American Mosasaur discovery took
place in 1820, at Great Bend, Mo. Major O’Fallon,
an Indian agent, found a fine specimen
which he took to his home in the town of St.
Louis. A few years later the relic was taken
to Germany by Prince Maximilian of Wied,
after his famous trip through the United States
in search of natural history specimens and information.
Since that time hundreds, even
thousands, of specimens have been collected
and described from the Cretaceous rocks of
this country. The shallow seas that covered
Kansas were the headquarters of the Mosasaurs,
and their skeletons are abundant in the
chalk cliffs of the district.
Among the fishes which were the prey of
the Mosasaurs was the great Portheus, or Bulldog
fish, whose long, sharp teeth and powerful
body indicate that it often evened matters by
capturing smaller mosasaurs. The head of this
monster was twice as large as that of a grizzly
bear, while the muzzle was stouter and deeper
than that of a bulldog. Some of the teeth projected
as much as three inches above the gums,
sinking a full inch into the pits—as long as
the fangs of a tiger, but more slender. Two
pairs of these deadly teeth crossed each other
on either side of the snout, and were re-enforced
by numerous other long, conical teeth
farther back on the jaw.
Above the water soared or flew—it is not yet
decided which—the great Pterosaurs, or winged
reptiles. According to the current conception,
these great beasts flew above the water,
swooping down to snatch fishes and smaller
mosasaurs, on which they fed. Some of the
Pterosaurs had wing spreads of eighteen to
twenty feet, and if they actually did fly, were
without doubt the largest of all denizens of the
air. At night and while resting they clung to
cliffs and rocks by means of the long claws
with which their wings were equipped.
While we do not know whether or not the
Mosasaurs fed upon turtles, there were plenty
from which they might have made their
choice. One of them, at least, was of gigantic
size, having a flipper spread of at least fifteen
feet. The skin was smooth and leathery, that
over the back being strengthened by several
ridges of stiffer integument. The back flippers
were relatively small, while the front ones were
very broad and without an armor of claws.
Gradually, after countless centuries of relative
quiet, the earth began to re-shape its
surface. Mountains, plains, and plateaus arose,
leaving those sea-dwellers that could not swim
or crawl to perish in the hot suns of a new
time. The once broad seas grew smaller and
smaller, were divided into lakes and basins,
continued shrinking. The sea-dwellers were
imprisoned in these basins, where they preyed
upon each other with greater ease than had
been possible in the open waters of earlier times,
while the fishes died from the constant freshening
of the water. The stronger gorged upon
the weaker until they were left stranded on
the ever rising bars, with no food but their
kindred, and little strength to either attack
or escape. At the last they may have made
desperate attempts to escape by land, or else
lay starving in the shallow, muddy pools. Perhaps
as the waters shrank a few of the great
saurians fed with them, eventually making their
way into the new sea and ocean areas. But
in all probability any such refugees were so
beaten and starved that they had but little
chance for success in life under their new environment.
By the time of the great uplift
which proved their undoing, the Mosasaurs and
their allies were an old race,[8] and had little
vitality left with which to cope with new situations.
They died, leaving no descendants,[9]
and only the scattered remains in Cretaceous
rocks remain to tell of the once mighty hordes.
[8] For a discussion of the age of groups, life cycle
of species, etc., see the author’s booklet, “Animals
of Ancient Seas,” No. 47 of this Series.
[9] Rumors of Paleozoic monsters living in remote
portions of the earth appear constantly, but
without foundation in fact. Just this year
(1922) newspapers and some magazines have
made a great to-do about a Plesiosaur that
was supposed to be living in a South American
lake. The Plesiosaurs, aside from being as
ancient as the Mosasaurs, were exclusively
marine; therefore, a report of one of them in
a lake is utterly absurd.
CHAPTER IV. THE MOST ANCIENT BIRDS. — FOOTNOTES:
When and how the first bird came into being
is one of the undiscovered secrets of paleontology.
The probability is that at some time during
the late Triassic—the first division of the
Mesozoic, or “Middle Life” era—a little reptile
somewhat like the smallest of the bird-like
dinosaurs developed feathers and began to make
short flights through the air. Whether this
reptile, which actually may have been a dinosaur,
developed wings on his forelegs and rose
from the ground, or whether he developed
feathers on both front and hind legs and began
by gliding, is a matter of theory. Just now the
latter view seems to be the more elaborately
worked out, and therefore the more widely accepted.
But there is fashion in theories just
as there is in dress, and some new discovery
may easily render the supposed four-winged
ancestor passe.
But, uncertain though the origin of birds
may be, there is little doubt regarding the most
ancient known member of the class. It is the
famous Archeopteryx, found in the equally
noted lithographic quarries at Solenhofen,
Bavaria. This ancient bird, for all practical
purposes the starting point in the history of
the feathered animals,[10] was considerably smaller
than a crow, and possessed a short, strong
beak which was armed with sharp, reptile-like
teeth. The wings were short and broad, while
the tail was considerably longer than the rest
of the body, and was of very remarkable construction.
As everyone who has ever shot
sparrows or plucked a chicken knows, the tail
of a modern bird is made up very much like
a feather fan, and closes up like one, with the
bony part very short and broad. In the Archeopteryx,
however, the tail was long and lizard-like,
with the feathers placed in pairs, one pair to
each tail joint. Thus the creature when flying
must have looked much like an undersized crow
dragging after him a palm leaf instead of a
tail.
As may be inferred from the foregoing description,
the feathers of Archeopteryx are well
preserved in the two fossils which have been
found. However, they are shown only on certain
parts of the body, and from this some
scientists have concluded that the bird possessed
feathers on only the wings, tail, and
thighs. There seems, however, to be little
ground for this conclusion, and restorations of
the creature showing it as a bird-like lizard
with a few tufts of feathers are hardly to be
relied upon. It is very improbable that such
highly developed feathers as those which are
preserved should have been present without
the more primitive ones being found on the
back, breast, and neck. Also, since the feathers
of the latter type are smaller and more easily
destroyed than those of the wings and tail, it is
quite natural that they should fail to be preserved
in the old Jurassic sediments.
PLATE X.
The fossil remains of Archeopteryx.
The Archeopteryx lived during the period
when the Dinosaurs were in the height of their
glory. Whether or not he was descended from
any of the birds who, without much question,
left tracks in the Connecticut valley during
the preceding age cannot be determined. Doubtless
those ancient forms would hardly have
been recognizable as birds, yet inasmuch as they
wore feathers they may properly be placed in
that group. For we may both concisely and
accurately define birds as animals with feathers,
for feathers are possessed by every bird that
lives, and are possessed by no creatures other
than birds. Flight, as we shall see in the next
chapter, is a characteristic that is by no means
universal in the bird world, but even the flightless
birds, such as the ostrich and the Apteryx,
are covered with feathers. True, in the penguins,
birds that spend most of their time on
and under the water, the feathers have been
changed so that they are hardly recognizable,
yet a closer examination shows the essential
structure to be there, and our definition is
upheld.
PLATE XI.
Hesperornis swimming beneath the water.
(After Lucas.)
The next birds of which we have relics were
inhabitants of the western part of our own
country, and although separated by tens or hundreds
of thousands of years from the Jurassic
Archeopteryx, they still possessed teeth—a
characteristic that separates them sharply from
all modern birds. They were first collected
during the years 1870-71 by Professor O. C.
Marsh, who was at that time exploring the
chalk beds of western Kansas. It was not until
1873, however, that Marsh was able to give his
specimens a thorough laboratory examination
and discovered that the jaws were set with
teeth, thus establishing a new and most important
fact in evolution.[11] Previous to this men
had been quite willing to believe that birds
were descended from toothed animals, for all
the creatures from which they might have come
were toothed, but not a few hesitated to acknowledge
that birds themselves possessed similar
equipment. But with Marsh’s discovery the
case was proved, and “scarce as hen’s teeth”
ceased to be a joke, at least so far as fossils
are concerned.
The larger of the two species of birds found
in Kansas was a truly remarkable creature, in
some ways the most astonishing bird that has
ever lived. Hesperornis (western bird) looked
much like an overgrown, wingless loon, or “hell
diver,” and was quite as much at home in the
water as is that bird. Instead of swimming with
the wings, as does the penguin of Antarctic
regions, Hesperornis swam with its legs and
feet, and did it so successfully that the wings
disappeared, with the exception of a single
bone. At the same time, the muscles of the
breast, which are used in moving the wings,
dwindled away, so that Hesperornis, although
some five feet in length, was remarkably slender
and torpedo-shaped.
Concerning its habits and probable appearance
during life Dr. Lucas says: “As a swimming
bird, one that swims with its legs and
not with its wings, Hesperornis has probably
never been equalled, for the size and appearance
of the bones indicate great power, while
the bones of the foot were so joined to those of
the leg as to turn edgewise as the foot was
brought forward and thus offer the least possible
resistance to the water. It is a remarkable
fact that the leg bones of Hesperornis are hollow,
remarkable because as a rule the bones of
aquatic animals are more or less solid, their
weight being supported by the water; but those
of the great diver were almost as light as if it
had dwelt upon the dry land. That it did not
dwell there is conclusively shown by its build,
and above all its feet, for the foot of a running
bird is modified in quite another way.
“The bird was probably covered with smooth,
soft feathers, something like those of an Apteryx;
this we know because Professor Williston
found a specimen showing the impression
of the skin of the lower part of the leg as well
as of the feathers that covered the ‘thigh’ and
head. While such a covering seems rather
inadequate for a bird of such exclusively aquatic
habits as Hesperornis must have been, there
is no getting away from the facts in the case
in the shape of Professor Williston’s specimen,
and we have in the Snake Bird, one of the most
aquatic of recent birds, an instance of similarly
poor covering....
“The restoration which Mr. Gleeson has
drawn[12] differs radically from any yet made, and
is the result of careful study of the specimen
belonging to the United States National
Museum. No one can appreciate the peculiarities
of Hesperornis and its remarkable departures
from other swimming birds who has not
seen the skeleton mounted in a swimming attitude.
The great length of the legs, their position
at the middle of the body, the narrowness
of the body back of the hip joint, and the disproportionate
length of the outer toe are all
brought out in a manner which a picture of the
bird squatting upon its haunches fails utterly
to show. As for the tail, it is evident from the
size and breadth of the bones that something
of the kind was present; it is also evident that
it was not like that of an ordinary bird, and
so it has been drawn with just a suggestion of
Archaeopteryx about it.
“The most extraordinary thing about Hesperornis,
however, is the position of the legs relative
to the body, and this is something that was
not even suspected until the skeleton was mounted
in a swimming attitude. As anyone knows
who has watched a duck swim, the usual place
for the feet and legs is beneath and in a line
with the body. But in our great extinct diver
the articulations of the leg bones are such that
this is impossible, and the feet and lower joint
of the legs (called the tarsus) must have stood
out nearly at right angles to the body, like a
pair of oars. This is so peculiar and anomalous
an attitude for a bird’s legs that, although apparently
indicated by the shape of the bones, it
was at first thought to be due to the crushing
and consequent distortion to which the bones
had been subjected, and an endeavor was made
to place the legs in the ordinary position, even
though this was done at the expense of some
little dislocation of the joints. But when the
mounting of the skeleton had advanced further
it became more evident that Hesperornis was
not an ordinary bird, and that he could not have
swum in the usual manner, since this would
have brought his great knee-caps up into his
body, which would have been uncomfortable.
And so, at the cost of some little time and
trouble, the mountings were so changed that
the legs stood out at the sides of the body, as
shown in the picture.”[13]
The birds progressed while their kindred and
ancestors, the reptiles, were declining. By the
dawn of the Eocene, the first period of the Age
of Mammals, the birds were very much like
those of modern times, and in the last three
million years or more very little change has
taken place. However, there were a number of
bizarre and gigantic forms which arose during
the later ages of bird ascendancy, and those we
shall consider in the following chapter.
One who has observed the great abundance
of birds today might well conclude that bird
remains should be among the commonest of
the vertebrate fossils. Exactly the opposite,
however, is true, for bird bones are among the
rarest finds of the paleontological collector.
Bones of the wings and legs, and occasional
skulls, go to make up the bulk of the finds, with
smaller bones, and impressions of the feathers
turning up just often enough to keep the collector
in a constant state of anticipation. A few
eggs, also, have been found in the strata of western
United States, but as yet the birds that laid
them are unknown.
The scarcity of bird fossils is a problem to
which no satisfactory answer has yet been
given. The commonest theory is that dead
birds, because of their very light weight, float
for long periods of time, and are thus exposed
to the attacks of weather, bacteria, and carrion
feeding birds and animals. The bones, too, are
light and easily broken, so that they will not
stand the wear as will the heavier remains of
mammals and sea-dwelling shellfish. Yet, in
certain formations of France and Oregon, where
conditions are not notably different from those
of other and barren strata, remains of birds
are fairly common. This proves that under
proper conditions, whatever they may have
been, bird bones did fossilize—a fact which
holds out the hope that some day a fortunate
collector will unearth a large and varied deposit,
and will then be able to fill out some of
the greater gaps in the history of feathered
creatures.
[10] That is, until a more ancient specimen is discovered.
One must always be prepared for new
discoveries in paleontology, just as in other
sciences.
[11] Although the first specimen of Archeopteryx
had been found several years before, it was too
poorly preserved to show the teeth. It was
not until 1877 that the famous Berlin specimen,
which shows the teeth and feathers so
admirably, was discovered.
[12] This restoration served as the copy for the accompanying
plate.
CHAPTER V. GIANTS OF THE FEATHERED WORLD. — FOOTNOTES:
As we have seen in the preceding chapter,
the earliest birds were both stranger and, in
some cases at least, larger than most of the
species found on earth today. But as we go
upward in the geologic scale, we find that the
primitive birds were far outstripped by their
relatively modern descendants. Some of these
feathered Goliaths, such as the Ostrich of Africa,
are alive today; some have but recently become
extinct, and their relics are found by thousands
in the districts where they once roamed. Still
others, though probably not the largest of their
class, died out thousands, or even millions of
years before man appeared upon the earth.
They, like the mighty dinosaurs that preceded
them, succumbed to the many enemies which
constantly attack every animal that lives and
left the earth to their more successful rivals
and descendants.
Among the best known of the more recent
avian giants, so recently extant that it still
lives in the traditions of the peoples whose
ancestors feasted upon its flesh, is the great
Moa of New Zealand. The first announcement
of the existence of this remarkable bird was
made by the Rev. W. Colenso, a missionary who
later became Bishop of New Zealand. Early
in the year of 1838, while on a missionary trip
in the North Island, Bishop Colenso secured
from the natives of Waiapu legends regarding
a mammoth bird, called the Moa, which possessed
a human head, and which inhabited a
mountain some eighty miles inland. This creature,
according to the legends, was the last of
his kind, and was carefully guarded by two
gigantic lizards who stood watch while the
bird slept. When an enemy, especially a man,
approached, these lizards roused the Moa, who
immediately rushed upon the intruders and
trampled them to death. It appeared that none
of the savages had ever seen this bird—due,
perhaps, to its watchful guardians and fierce
prowess—but they were very sure of its existence.
In fact, they used bones of his dead
relatives in making their fishing implements,
and these bones, they assured the bishop, were
quite as large as those of the European ox.
But a short time later, another missionary,
the Rev. Richard Taylor, discovered a bone
which was said to belong to the Moa, and received
considerable free information about its
possessor from the natives with whom he was
associated. But, as Dr. Lucas remarks in telling
of the incident, just “as the foot of the
rainbow moves away as we move toward it, in
his case the bird was said to dwell in a quite
different locality from that given by the natives
of East Cape” where Rev. Colenso had
secured his information. Taylor’s informants,
like the other natives, had not seen the Moa,
nor did they even know anyone who had, but
they had no doubt of its existence. When after
many years of search, however, there was not
a single explorer who had seen, heard, or tracked
the giant bird, scientists refused to believe
the tales of the natives, and some went so far
as to deny that the Moa had lived at any time
within the era of man.
These latter, however, went somewhat too
far in their questioning. For even though no
man has seen the living Moa, its remains are
scattered abundantly over the hills, valleys and
swamps of New Zealand, and from them scientists
have been able to gain a very reliable idea
of the size, structure, and general appearance
of the feathered giant. Probably the most remarkable
find of Moa remains was made in
one of the large, dry caves of South Island,
where collectors secured not only a number
of bones with the original flesh adhering, but
also several patches of skin to which clung
numerous feathers of a chestnut color tipped
with white. True, these small, rusty-brown
feathers were not very spectacular, but when
we stop to consider that they have been kept
for hundreds, perhaps even thousands, of years
without any preservative whatever, and that
they belonged to a race of creatures now totally
extinct, our respect for them increases greatly.
Since the original possessor of those feathers
died in his New Zealand cavern many wars
have been won and lost, powerful nations have
arisen, new languages and systems of thought
have been established, and the surface of the
earth has been carved, planed, and pitted by
the restless inventive animal called man. And
now that same man is spending a considerable
amount of his most prized possession—money—to
gather and preserve the broken, dried remains
of that old New Zealand bird, his relatives
and ancestors.
It is now well known, that instead of but
one species of Moa, as the New Zealand savages
told the missionaries, there were twenty
or more. Some of these were quite small—but
little larger than the turkey—while others,
such as Dinornis (terrible bird) must have
reached a height of at least ten feet, and were,
in all probability, the largest birds that have
ever been seen on earth. Remarkably enough,
some writers have not been satisfied with even
these great dimensions, and have stated the
height of some of the Moas to be from twelve
to fourteen feet. These measurements, however,
can be attained only by placing the skeleton
in a most unnatural position, which the
bird could not possibly have maintained while
alive. There is a natural desire on the part
of man to magnify his discoveries, and the
remains of extinct creatures are favorite subjects
for such romancing. Unfortunately for
the writers, these same bones offer incontestable
evidence as to the actual sizes of the creatures
to which they belonged, and sooner or
later all errors must be corrected and “the
high made low.” As Dr. F. A. Lucas has insisted
over and over again, the greatest monster
always shrinks before the application of
a two-foot rule.
The Moas, like the modern Ostriches, were
quite incapable of flight. Indeed, many of them
were totally wingless, lacking even the tiny,
almost invisible vestigial wings that are to be
found in such modern species as the Cassowary
and Apteryx. But what they lacked in wings
the Moas more than made up for in legs. Those
of one species, dubbed elephantopus (elephant-footed)
were so ponderous that one cannot but
wonder what purpose they served. The theory
most generally accepted is that they were of
value in digging out the roots of ferns, upon
which the Moas appear to have fed. Furthermore,
when we remember that one blow from
the foot of an angry ostrich is quite enough to
kill a man, we cannot doubt that the Moa was
quite able to either trample underfoot, or smash
to a shapeless pulp almost any enemy that
might have assailed it. The lizard watchmen
of the Maori legend are, of course, inventions,
but the ferocious habits of the enraged Moa
are without question matters of pure fact.
So far as known, the Moas were confined to
New Zealand, some species inhabiting North
Island, some South, but with very few common
to both. From this fact Lucas, and others who
have studied the birds, conclude that the two
islands were originally one, and that long
after the Moas came into existence there was
a submergence which divided the island into
two. After that submergence sufficient time
elapsed to allow for the development of several
species of Moas, each restricted to one
island. Inasmuch as the birds could not fly,
and probably were poor swimmers, there was
but little intermingling of the faunas. “Although
Moas were still numerous when man
made his appearance in this part of the world,
the large deposits of their bones indicate that
they were on the wane, and that natural causes
had already reduced the feathered population
of these islands. A glacial period is believed
to have wrought their destruction, and in one
great morass, abounding in springs, their bones
occur in such enormous numbers, layer upon
layer, that it is thought the birds sought the
place where the flowing springs might afford
their feet at least some respite from the biting
cold, and there perished miserably by thousands.”[14]
The glacial cold, however, did not completely
destroy the Moas. We have already seen
that legends of the birds were told to the pioneering
white missionaries, and other tales of
Moa hunts and Moa feasts were not uncommon.
It is uncertain whether the last of these giants
was eaten by the ancient Maoris, or by a race
that preceded them. Some authors have suggested,
apparently on fairly good ground, that
Moas formed the sole important flesh food of
these prehistoric peoples, and that with the
dying out of the avian food supply, the hereditary
liking for flesh naturally led to cannibalism.
Thus the savages who destroyed the Moas
turned to destroying themselves, were supplanted
by another race which handed on the knowledge
of the Moas to the white man who in turn
set about killing off the savages.
From the New Zealand Moa to Sinbad the
Sailor, and his huge and unintentionally beneficent
Roc, is, at first thought, a very far
cry, yet the separation is not so great as it
seems. The Arabian tales give the habitation
of the Roc as either Madagascar or one of the
adjoining islands, and it seems very probable
that the original of the huge bird that carried
the adventurous Sinbad out of the crater of
diamonds was the Aepyornis, a distant relative
of the Moas, and an inhabitant of Madagascar.
It is quite true that the Roc was a gigantic
bird quite capable of carrying off an elephant
to make a meal for its young, while the
Aepyornis was little larger than an ostrich,
was incapable of flight, and fed upon plants.
These facts, however, would in no way interfere
with the fancy of an Arabian story teller,
whose original materials probably were a collection
of Aeypornis legend substantiated by
fragments of the bird’s enormous eggs. Hardly
greater exaggerations are perpetrated weekly
by the “feature writers” of American Sunday
newspapers, and these men have all the
resources of modern science at their disposal.
The actual scientific “discovery” of Aepyornis
did not take place until 1834, when Jules
Verreaux, a French ornithologist received a
sketch of a huge egg, found in the island of
Madagascar. The informant, a traveler, said
that he had seen two of these eggs, one of
which had been used in cracking rice, while
the other had been sawed in two to be used
as bowls. Later on, some fragments of a shell
were secured by another traveler, and finally,
in 1851, two entire eggs and a number of bones
were secured and sent to France. They were
studied by Geoffroy St-Hilaire, a noted naturalist
and pioneer evolutionist, who christened
them Aepyornis maximus, or “greatest lofty
bird.” The last part of the name was appropriate
so far as the eggs are concerned, for they
stand as the largest of all eggs. Some idea of
their size may be gained by comparisons; the
measurements alone do not mean a great deal.
The egg of the ostrich, which is usually considered
to be quite immense, measures four and
one-half by six inches; that of the Aepyornis is
not less than nine by thirteen inches, and
would hold the whites and yolks of six ostrich
eggs! The size seems even greater when we
say that it would hold the contents of more
than twelve dozen hens’ eggs or thirty thousands
of the tiny, bean-like eggs of the hummingbird.
Had there been giants in the old
days, as fairy tales and occasional newspaper
articles seek to convince us, they would have
had no trouble in satisfying their breakfast
appetites with a couple of Aepyornis eggs,
poached. Fortunately for Aepyornis, in his day
there were neither giants nor newspapers; had
either existed he doubtless would have been
exterminated by hunters long before his time.
Despite the excellence of their preservation,
relics of the giant birds of New Zealand and
Madagascar are not easily seen by the student.
There are fine collections at Harvard University,
and the American Museum in New York,
and in museums in Europe and New Zealand,
but there are few, if any Moa eggs in the
United States. Specimens of this sort are very
expensive; Aepyornis eggs have sold in London
for as high as two hundred pounds (about nine
hundred seventy-two dollars) and most American
museums are desperately poor, being
forced to rely on the generosity of private individuals
for money with which to buy specimens.[15]
Leaving the giant eastern birds, and the
scarcity of collections of their remains, we may
transfer our attention to a group of American
birds, the huge Phororhacidae of
Patagonia. Although far older, geologically
these birds were not discovered until long
after the Moas and Aepyornis were well
known. Even then, it was not believed that
so massive a bone as the jaw of Phororhacos
could possibly belong to a bird, and it was
necessary to find much more complete relics
before the case could be proved.
It is one of the ludicrous facts of paleontology
that most of the large-sounding names
were used up on the Moas, some of which were
small, and that Dinornis (terrible bird) was
wasted on root-eating creatures that probably
were of meekest temperament when not annoyed.
In the Patagonian birds, on the other
hand, we have species that were really terrible,
with their powerful legs, huge heads, sharp,
crooked beaks, and strong talons. One of them,
Brontornis, or thunder bird, possessed leg
bones larger than those of an ox, the drumstick
being thirty inches long and two and
one-half inches thick. The corresponding bone
in the turkey, largest of the domestic birds,
the length is but five and one-half inches. The
most imposing of the Patagonian birds, however,
is the Phorohacos, a creature unique
among the bird world. This creature stood
seven or eight feet in height, possessed a head
larger than that of a horse and a neck as
thick, and was armed with huge, sharply
hooked beak and long, sharp claws. One of
Dr. Lucas’ illustrations shows the skull of the
race-horse Lexington placed beneath that of
Phororhacos. That of the bird is one inch
longer and one and one-half deeper.
The structure of Phororhacos, like that of
all other animals, affords an excellent key to its
food habits. Probably they did not feed upon
roots, as did the Moas, for had they done so
their strong, hooked beaks would have been
useless, or nearly so. Neither is it probable
that they caught fish; the beaks of most fish-eating
birds, and particularly of the herons,
which are related to Phororhacos, are long,
adapted to spearing. Beaks and claws like
those of the Patagonian giant are found, in
most cases, in birds that feed on either carrion
or living animals, or both. In the accompanying
illustration the bird is shown as
just having killed a small grass-eating animal,
and preparing to devour it. Were it to be
proved—as it can hardly be—that Phororhacos
fed upon carrion alone, the restoration would
have to be modified greatly, in appearance
though not in proportion. Carrion eaters seldom
have feathers on the upper part of the
neck and the head, as may be seen by examining
such notorious eaters of dead flesh as
the vultures or “buzzards.” But the designer
of the original restoration, as life-drawings of
extinct animals are called, was satisfied to consider
his subject as a swift-running bird of
prey that preferred fresh killed meat, and did
the killing itself.
PLATE XII.
Phororhacos preparing to devour its prey.
(After Lucas.)
[14] Lucas, Animals of the Past, 1st Ed., p. 143. Note
that, since the Moas were on the decline when
man appeared in their environment, and they
had no other powerful enemies, the huge legs
could hardly have had defence as their chief
function.
[15] This is true of the United States National Museum,
at Washington, where the customary appropriation
for securing specimens is $10,000
per year. At this national institution it is not
rare for employees to draw upon their own
small resources in order to secure particularly
desirable collections. The same condition is to
be found in other museums of the country, excepting
the American Museum of Natural History
in New York. It, though privately endowed,
is housed by the city of New York, and
is the largest and best supported museum in
the western hemisphere.
Transcriber’s Note
Footnotes were moved to the ends of the chapters in which they appeared.
Illustrations were moved to the ends of the paragraphs in which they appeared.
The list of illustrations was not in the original text. Plate V was originally
untitled.
Inconsistencies in hyphenation have been standardized.
Minor punctuation errors have been changed without notice.
Spelling was retained as in the original except for the following changes: