The Pony at Work.It has already been explained that the Shetland pony is now little used for work in his native Islands, having been displaced by larger ponies and horses as the development of roads has substituted driving for riding, and carts for the creels and pack-saddles which are now found only in the remoter districts. A TEAM OF MARES. The progressive disuse, however, of the pony, as a work animal in Shetland, has been accompanied by a much greater increase in its use elsewhere. This has specially been the case in the employment of ponies in coal-pits, which grew to its height It was in the middle of last century that ponies were first used in coal-pits in the north of England, A considerable sentimental repugnance exists to the employment of ponies below ground; and to the unaccustomed such a life appears sufficiently unattractive either to man or horse; but the fact remains that the life is not on the whole unhealthy: if it lacks the summer sun it is spared the winter nights. The fable that the ponies become blind has no better foundation than is given by the fact that a short time is required to accustom their eyes to the light when they return to the surface. They are no doubt exposed to accidents; and they are less protected against overwork and other unfair treatment than they should be; though this is partly rectified by the provisions of the “Mines Act” of 1911. It is only right to say plainly that the By permission of the Proprietors of ‘Punch.’ A CHIP OF THE OLD BLOCK. It must be admitted, nevertheless, that the pit-ponies are the less fortunate class of Shetlanders, and that the pleasanter career belongs to those which are selected for what appears to be the natural office of the pony—that of the child’s first mount. This is no new occupation for him. A letter, dated 1737, from “Mellerstains” to the writer’s brother in Bressay, runs: Trustworthy as the Shetland pony is, it must still be added that not only must he be educated, mouthed, and mannered as carefully as a larger horse, but also he should not be subjected to the temptations of power. Until a child can really manage and control him, the leading rein must be kept in regular use, so as to avoid those premature conflicts and accidents that are as fatal to future horsemanship as they are to equine manners. ON DUTY. The Shetland pony now goes far afield. In the United States he has enthusiastic supporters, who allow more laxity in height than British breeders approve—admitting 44 inches as a legitimate stature. He goes to The Sheltie has the great advantage of a singular longevity. Every one who really associates with them knows how disastrously short a time dogs and horses live: on no reasonable calculation can they grow old with their owners. Even the Shetland pony fails of this, but he makes the bravest of attempts. The pony is the most easily kept of all animals. For two or three pounds a-year he can be maintained; for a little more he can be kept in hard-working condition—a useful member of a small establishment, and no unprofitable part of the equine staff of a farm, going over much more ground, with light loads, and a boy to drive him, than a cart-horse that will cost nearly ten times as much to keep. Yet in the end it is idle to deny that it is not his indisputable economic validity that binds the Sheltie’s lovers to him: rather it is himself—his wisdom and his courage, his companionable ways, his gay and willing service. The Making of the Shetland Ponyby J. COSSAR EWART, M.D., F.R.S. PROFESSOR OF NATURAL HISTORY IN THE UNIVERSITY OF EDINBURGH The Making of the Shetland Pony. “The horses that are ancient we honour because we know not whence they came, but the new ones we slight because we know their beginning.” The Shetland pony belongs to an ancient breed famed for its intelligence and docility, strength and hardiness, but especially remarkable because of its small size. In a recent article on the Shetland pony it is said that “the highest authorities rather incline to the view that he is an instance of arrested development, and that all the equine race originally sprang from ancestors far more diminutive than the smallest Shetland.” It is doubtless true that the remote ancestors of the EquidÆ were small, but it does not necessarily follow that Shetland, Java, and It will be well at the outset to ascertain whether the small size is due to reversion or to dwarfing, induced, partly by unfavourable surroundings, partly by inbreeding and artificial selection. The Size of the Shetland Pony.—Nature unaided has made a pigmy hippopotamus, pigmy elephants, and pigmy races of man, but there is no evidence that nature unaided in Europe or Asia in pre-glacial or post-glacial times produced a wild pigmy race of true horses—i.e., of horses with only one complete toe for each foot. The smallest wild horses in Britain at the end of the PalÆolithic period (i.e., according to a recent estimate some six thousand years ago) were apparently never under 12 hands at the withers. During the Bronze age, alike in wild and tame varieties, a size of at least 48 inches seems to have been maintained all over Europe. Further, remains from Roman military stations indicate that the smallest horses in Britain during the first century were probably never under 46 inches at the withers. It may hence be assumed that Shetland and other small breeds are not directly descended from pigmy wild races, but are the dwarfed descendants of one or more small varieties or A consideration of pigmy races makes it evident that dwarfing may be either equal or unequal, that it may result in the formation of a miniature having all the leading traits of the large race to which it belongs, or give rise to a pigmy variety in which certain parts are more dwarfed than others. In some small strains of dogs the relative proportion of all the parts are practically the same as in large strains, but sometimes in a small strain not only are the limbs more dwarfed than the trunk but certain parts of the limbs are more reduced than others. An example of unequal or disproportional dwarfing we have in the dachshund. In this breed the dwarfing has been carried further in the legs than in the body, and in the forearm than in the foot. In a normally constructed small hound in which the length of the body is 390 mm., the length from the elbow to the ground is 215 mm., from the elbow to the wrist 145 mm., In the case of pigmy horses are the proportions of their normal ancestors invariably retained, or are the legs in some cases more dwarfed than the trunk, and as in the dachshund is the dwarfing greater in one part of the limb than in another? In Java ponies I have had under observation for some years the head and limbs bear practically the same relation to the body as in well-proportioned Arabs. For example, in a 41-inch Java mare (fig. 1) the height at the withers, as in typical desert Arabs, is 2·7 times the length of the head, But while in tropical islands the relative proportion of the various parts of pigmy horses may be maintained, in islands near the Arctic Circle dwarfing may imply undue shortening of the limbs, and that certain parts of the limb are more reduced than others. A striking instance of unequal reduction we have in the Udganger or Nordlands ponies, once common in Bodo, a small island within the Arctic Circle off the coast of Norway. Fig. 2 shows that the limbs of the Bodo ponies were relatively nearly as much dwarfed as in a dachshund, while fig. 3 shows that Iceland ponies of the Nordlands type may closely agree in conformation with Exmoor and other well-built ponies of the Celtic race. Very little is known about the make and size of the horses which first reached Shetland. The evidence as far as it goes indicates that they belonged to small varieties measuring Dwarfing in Shetland Ponies of the Celtic or Riding Type.—That well-proportioned Shetland ponies of the riding or Celtic type still exist is suggested by the measurements of Pamela and certain other fine-limbed pedigree ponies. Pamela (40 inches at the withers, 25 inches from elbow to ground, and 5·25 inches below the knee), in the form and length of the head, length of the limbs and their relation to the height at the withers, very closely agrees with the 41-inch Java pony. The skeletons of Shetland ponies of the riding type available for study (viz., of Highland Chieftain, Egil, and Eric) also indicate that in a considerable number of cases the dwarfing is uniform. Though in many Shetland ponies the distance between the knees and the fetlocks looks very short, the front cannon-bones may be relatively as long as in thoroughbred race-horses. In Highland Chieftain The only striking difference between Highland Chieftain and a typical 12-hands Celtic pony is in the face. In modern horses, while the form of the cranium or brain-box is nearly constant, the face varies both in size and in its relation to the cranium. In the wild steppe horse (Equus przewalskii) of Mongolia, which during part of the year subsists on hard dry food, the jaws are so long that the length of the face (fig. 8) is twice the width across the orbits, thus giving a frontal index of 50; whereas in a broad-browed Iceland or Highland pony the face may be only 1·6 times the width, which implies a frontal index of 60. In the Celtic race (to which Highland Chieftain mainly belongs) the normal frontal index is 54—i.e., the length of the face is 1·8 times the width—but, as in Highland Chieftain, the length of the face is In the case of Egil As Egil probably belonged to an unimproved stock, it may be asked, Does his skeleton lend support to the view that modern pigmy horses reproduce, apart from their size, the characteristics of their remote ancestors? In Miocene, as in prehistoric times, there were light as well as heavy horses, but in the light as well as in the heavy each limb had three hoofs (fig. 18). In Neohipparion, a late Miocene three-toed horse, about 40 inches at the withers, the skull is longer by 12 mm., and the molar teeth are more specialised than in Egil, the 40-inch modern island pony. In the EquidÆ the cannon-bones are especially interesting; strange as it may appear, the middle cannon-bones are relatively longer and Having seen that, apart from the face, the only essential difference between the skeleton of an unimproved Shetland and the skeleton of an Exmoor pony is a difference in size, let us next direct attention to the skeleton of Eric, a 36·5-inch improved pedigree pony of the riding type, for some time in the possession of Mr Charles M. Douglas of Auchlochan. In Eric, who died when six years old, the fore limb from the elbow to the ground was 22 inches, the length from the point of the hock to the ground 15·4 inches, the circumference below In Eric the face (fig. 6) is so short that the frontal index is 67, the length being only 1·4 times the width instead of 1·8 as in 12-hands ponies of the riding type. The length of Eric’s head when alive was 410 mm. (16¼ inches). A typical Celtic pony with a 410 mm. head measures 40 inches at the withers. Eric, though having the head of at least a 40-inch pony, only measured 36·5 inches. It may hence be assumed that, through dwarfing, his total height was reduced by 3·5 inches. Further, as Eric’s metacarpal (fig. 9a), instead of measuring 166 mm. (the normal length in a 40-inch pony), had only a length of 143 mm., it follows that practically one inch of the dwarfing was due to a reduction in the length of the cannon-bones. Moreover, as Eric actually measured 36·5 inches, his metacarpals should have measured 152 mm. instead of 143 mm.—143 mm. being the length in a normal pony measuring 34 inches at the withers. Though Eric had the head and trunk of a 40-inch pony and the metacarpals of a 34-inch pony, the metacarpals bear the same relation to the radius and the humerus as in Persimmon—i.e., in Eric the relative lengths of the different parts of the limb were maintained (not lost, as in the dachshund) during the dwarfing process. Although the cannon-bones in Eric had been considerably reduced in length, they had not been reduced in width—i.e., they are as wide as the metacarpals of the 40-inch Shetland pony Egil, in which the limbs It was at one time the ambition of some breeders to have Shetland ponies as small as their remote three-toed Miocene ancestors. As a matter of fact, ponies smaller than some of the Miocene species have long existed in Shetland. Eric, though an average-sized pony, was at least a hand smaller than the late Miocene horse, Protohippus sejunctus, in which the front cannon-bones (fig. 9b) were 177 mm. long and 21 mm. wide—i.e., 34 mm. (1·37 inches) longer but 5 mm. narrower than in Eric; while Seedpearl (31·75 inches at the withers) and other still smaller living ponies have shorter limbs than the very ancient three-toed Mesohippus from the Badlands of South Dakota. But while some Shetland ponies are actually smaller and have relatively decidedly shorter legs Shetland Ponies of the Cart-horse or “Forest” Type.—For want of material nothing very definite can be said about the nature of the dwarfing of ponies of the heavy or cart-horse type. In a typical 12-hands Celtic pony the metacarpals are 200 mm. long, 27·5 mm. wide, but in a typical 12-hands “forest” horse the metacarpals are, on an average, 193 mm. long and 35·1 mm. wide. An undwarfed, thick-set, 36-inch Sheltie built on the same lines as a 12-hands “forest” horse should have metacarpals about 145 mm. in length and 26·4 mm. in width, and should measure 5·5 inches below the knee. The measurements available indicate that in a pedigree 36-inch Sheltie of the This conclusion is supported by the measurements of Odin, a 38-inch pony, 6 inches below the knee; of Vulcan, a 32-inch pony, 5 inches below the knee; and of other ponies of the Londonderry type belonging to the Ladies Hope, and also by those of Everlasting, Frederick, and other thick-set Auchlochan ponies. For example, in Everlasting, a 38-inch pony, the distance from the elbow to the ground is 22·75 inches, In heavy horses, but especially in Shire colts, one (or more) of the limbs has occasionally an extra digit ending in a well-formed hoof. In a three-weeks’ horse embryo there are no rudiments of limbs; at four weeks the limbs are represented by paddle-like structures; at five weeks the paddles contain rudiments of three toes—miniatures of the three toes of Hypohippus (fig. 20). In ordinary circumstances the development of the outer and inner toes (ii. and iv.) is soon arrested, but occasionally one of these rudiments develops into a toe as large and complete as in three-toed Miocene horses of the “forest” type. When this happens, when in addition to the third toe there is a toe corresponding to the human forefinger, we have a marvellous instance of reversion. If in the Shetland breed there is a tendency Dwarfing of the face and the reduction of the nasal chambers has apparently been carried further in some of the miniature cart-horses than in Eric and other flat-boned Shelties. In Jupiter, The Causes of the Dwarfing of Shetland Ponies.—Given sufficient food and shelter, horses up to 15 hands—the size of the tallest prehistoric Old World wild horse—can easily be bred and reared in both the Western and Northern Islands of Scotland. On the other hand, large breeds are soon dwarfed when, in addition to a limited supply of food, the conditions during a considerable part of the year are extremely unfavourable. If Shetland ponies have not sprung from a small wild pigmy race, it may be safely asserted that their small size is mainly due to isolation in small areas where they were forced to shift for themselves under, as a rule, extremely unfavourable conditions. Evidence in support of the view that the descendants of the Spanish and south-country horses, introduced about 1710 and after 1745, were soon either eliminated or dwarfed, we have from Dr Johnson and others. Dr Johnson tells us that the pony he rode in Coll was very low, and that a bulky man on one of the native horses made “a very disproportionate appearance,” and, after referring to the small horses of Rum, mentions that he had heard of a yet smaller race in Barra, “of which the highest is not above 36 inches.” Barra was one of the islands which benefited by the introduction of Spanish horses by Clanranald. That dwarfing may be the direct result of an inadequate supply of nourishment during development is suggested by the condition of foetuses I found some years ago in a wild But while dwarfing may be, or appear to be, directly caused by the environment, there are other possible causes. Sometimes the small size of one or more members of a family or litter is due to reversion to small ancestors. For example, in a litter of five puppies bred some months ago (from parents in which West Highland and Mexican (Spanish?) blood prevails) there is marked variation in size. When these pups of mixed origin were weighed three days after birth, two males weighed 7·5 oz. each, two females 5·5 oz. each, and one male 4·5 oz. When again weighed at the end of the twelfth week, the But dwarfs often enough turn up in old-established “pure” breeds, and now and again a dwarf is found in an otherwise normal human family. There is no reason for supposing that such dwarfs are the result of reversion. Just as one of a litter of pups may prove a dwarf, one of five or six foals, full brothers and sisters, may prove a dwarf. It may, I think, be assumed that in the case of horses living under natural conditions, “spontaneous variation,” without the aid of reversion, will, as a rule, provide sufficient material to admit of a variety being evolved well adapted in size and other respects for the conditions which at the moment prevail. It need hardly be pointed out that little will be gained by speculating as to whether Many breeders, more especially breeders of dogs, seem to think that dwarfing is invariably the result of inbreeding. It is doubtless true that the members of many recently formed pigmy breeds are closely inbred, but it is well to bear in mind that there are closely inbred large as well as closely inbred small breeds—that size is largely a matter of selection—that in the case of natural races size depends more on the surroundings and the extent of the range than on the consanguinity. The view that dwarfing is caused by inbreeding is insisted on by Sir Everett Millais in a book on Rational Breeding. Sir Everett states that, though in the case of the Shetland pony the “climate, bad food, &c., had been a factor in reducing the size, the primary cause was inbreeding due to isolation.” It seems to me, however, highly probable If Shetland ponies are the pigmy descendants of one or more ancient races at least as tall as Exmoor and Welsh ponies, one would expect them to increase in size when bred and reared under favourable conditions. It has been again and again asserted that “the climate and comparative privation of the Shetland Isles were necessary to maintain the small stature of the ponies, and that the breed would inevitably lose this and all other characteristics if bred away from Shetland and under more generous conditions.” Some of the ponies recently brought south from Shetland have increased so much in size that, if otherwise eligible, they could not be registered in the ‘Shetland Pony Stud-Book’—i.e., they are now over 42 inches at the withers. Some 500 years ago a female rabbit and her young were turned out on the small island of Porto Santo near Madeira. In course of time this island was so overrun with rabbits The Ancestors of the Shetland Pony.—From pigmy horses it seems but a step to the little “fossil” horses of bygone days. It is hence not surprising that many are led to inquire to which particular branch of the equine family tree the Shetland pony belongs. Not many years ago it was said the horse tribe was at the start represented by a primitive race about the size of a fox but with as many hoofs as a tapir—four in front and three Now, however, we know that in Eocene times there were several kinds or species of four-toed “horses” from which were derived, in the Oligocene and Miocene periods, numerous three-toed species, some of them doomed to early extinction, others to bring forth one-toed races which in due time produced the ancestors of the modern horses, asses, and zebras. Hence it is now admitted that, in the past as in the present, the horse tribe was always represented by several species, not a few of which at times occupied the same area. It is also now admitted that the modern domestic breeds include several wild prehistoric species among their ancestors. Is it possible to say which of the wild horses of prehistoric times contributed to the making of the Shetland pony? To be in a position to Hyracotherium lived in the south-eastern part of England—his remains occur in the London Clay near Herne Bay and in the Red Crag of Suffolk—i.e., in deposits formed two or three or it may be six million years ago. This ancient fossil horse—though not unlike a long-faced fox terrier—Owen regarded as a relation of the Hyrax or Coney of Palestine, hence the name Hyracotherium. Evolved in Western Europe—perhaps in England—this primitive small-brained terrier-on-hoofs not only wandered across Europe and Asia, but actually crossed into America—then freely connected with north-eastern Asia—and ranged at least as far south as New Mexico. So conservative was this small forerunner of the great horse family that the American rep Though at the beginning of the Eocene period the milk-givers were backward and small (Eohippus was probably only 12 inches at the withers), the struggle for existence was probably keen enough. At any rate, the European varieties of Hyracotherium either died off without leaving descendants or gave rise to odd-toed ungulates which took no part in forming the modern EquidÆ. But for the American branch of the Hyracotherium family there would have been no horses. In course of time Eohippus was supplanted by Protorohippus (a 14-inch horse longer in the limbs and with more complex teeth), which towards the close of the Eocene period gave place to the still more specialised Orohippus. It may be mentioned that Epihippus, a slightly modified The limbs of Orohippus North America during Eocene times “was clad with forests in which grew both evergreen and deciduous trees distinctly modern in character. The moist climate gave rise to many streams and lakes, along the shores of which grew sedgy meadows that in turn gave rise to grassy plains.” It is impossible to say how many thousands of years are represented by the Eocene and Oligocene deposits, but an idea of the time that has elapsed since the beginning of the Tertiary period will be gained if it is mentioned that “when the fox-like Hyracotherium was wandering on the marshes of Kent not only was the Himalaya non-existent, but that along the line of its very heart—where the kiang now lives at an elevation of from thirteen thousand to sixteen thousand feet—extended an arm of the sea of no inconsiderable depth.” During the Miocene period the horse passed through the most interesting phases of his evolution, his elaborate dental battery was almost brought to perfection, and the second and fourth toes were gradually dwarfed and hidden out of sight, not even a trace of the hoofs being left, as in sheep, to suggest polydactylous ancestors. As already hinted, though Europe was the birthplace of the The Oligocene species which proved sufficiently plastic to respond to the new conditions varied in different directions, and gave rise to, amongst other types, one well adapted for a forest life, and one highly specialised for ranging far and wide over boundless prairies. In Hypohippus we have an example of a “forest” horse, in the American Hipparion (Neohipparion) we have a horse more specialised for a desert life than the fleetest Arab, while in Merychippus we have a link with In Merychippus the orbit is complete, and the crowns of the permanent molars are cemented as in recent horses, but the hoof bone has a cleft at the apex (fig. 19), and in some cases there is a minute vestige of the “splint” bone of the fifth or outer digit of the fore-foot. In fig. 11a, the fore-foot of Neohipparion, the Miocene race-horse, is represented. Fig. 19 gives the fore-foot, and fig. 16 is a restoration of Merychippus. Hitherto Merychippus, through Protohippus and Pliohippus, has been by many regarded as the progenitor of all the modern horses, as well as of the extinct Hipparions. That Hypohippus, like Eohippus, but unlike all the known Oligocene horses, had in the fore limb, in addition to three complete and functional toes, a distinct vestige of the first metacarpal—i.e., of the bone which in man carries the thumb. No vestige of a first metacarpal has ever been found in slender-limbed breeds, but once and again a vestige of the first metacarpal occurs in coarse-limbed breeds. The vestigial first metacarpal, taken along with other facts, suggests, as already said, that coarse-limbed breeds include a browsing race with limbs of the Hypohippus type amongst their ancestors. A few years ago it was assumed that Hypohippus, the The fore-foot of Hypohippus is represented in fig. 20. When a toe corresponding to the second digit of Hypohippus (II. fig. 20) appears in a modern horse it has sometimes, as in Hypohippus and Eohippus (I. fig. 10), a vestige of the first metacarpal at its upper. Fig. 15 is a restoration of Hypohippus. Ponies in Prehistoric Times.—During the Pleistocene period some eight or more species of true horses and ponies inhabited North America. Apparently before PalÆolithic man reached the New World all these American species had become extinct. About the American true horses which, like Hipparion, reached and found a home in Eastern Asia, very little is known. Some of their descendants found their way during Pliocene times into India; others reached south-eastern Europe. One of the Indian Pleistocene species (E. namadicus) from the Narbada valley had large long-pillared molars like E. complicatus of North America and E. fossilis of England (fig. 22); another (E. sivalensis), well represented in Pliocene deposits of the Indian Siwaliks, is the oldest true horse about which we have definite information. Like Pliohippus, Some of the Kirghiz breeds, in which the face is strongly bent downwards on the cranium, probably include this ancient Siwalik race amongst their ancestors. Some of the Eastern races which reached Europe Partly from fossil teeth and limb-bones, and partly from the engravings on the walls of caves and on pieces of horn, the conclusion was arrived at that E. fossilis, the assumed common ancestor of modern breeds, was characterised by a large coarse head, coarse limbs, and long-pillared molars (fig. 22). Prjevalsky’s horse when first discovered was said to be characterised by coarse limbs as well as by a large heavy head. As it was further assumed a generation ago that all domestic horses had long-pillared molars, and that the cannon- But though in Prjevalsky’s horse the head is coarse, the limbs are nearly as fine as in thoroughbred race-horses, and though in horses of the Prjevalsky or steppe type the pillars of the molars are long, they are not long in all modern horses. Moreover, though there is evidence of the existence in Europe in prehistoric times of a species with a coarse head and relatively fine cannon-bones, there is no evidence of the existence of a species which combined a coarse head with short broad cannon-bones. On the other hand, it has been ascertained that since Miocene times there have been living side by side in Europe big-boned and fine-boned species, and that, except by dwarfing, long narrow cannon-bones The skulls from the Roman military station at Newstead proved conclusively that there lived in Scotland during the first century large and small horses with short-pillared molars (fig. 23). This led to the discovery that in Shetland and other ponies of the Celtic type, and in Arabs and thoroughbreds of the Libyan or Siwalik type, some of the molars have as short pillars as in E. stenonis (fig. 21) of the Val d’Arno Pliocene deposits. The investigations of the last decade having indicated that during the Ice Age in Europe, as in America, there were always several species of horses living contemporaneously, an attempt must be made to ascertain from which of the wild prehistoric species Shetland ponies are mainly descended. In addition to steppe horses of the Prjevalsky make and horses allied in skull, teeth, and limbs to E. sivalensis of India, there were in prehistoric times large and small varieties of browsing or forest The “Elephant-Bed” and Kent’s Cavern small “forest” horses are best represented to-day by the long, low, broad-browed Iceland ponies, while the 13-hands small fine-boned race of Kent’s Cavern is best represented by Exmoor and other ponies of the “Celtic” Through the courtesy of Sir William Turner I recently had the opportunity of examining some horse, sheep, and dog bones found near Grangemouth 30 feet below the surface, at the point where the Carron joins the Forth. Two imperfect horse skulls belonged to ponies of the “forest” type, which probably measured 12 hands at the withers, a broken sheep skull belonged to a member of the peat or turbary race, and a dog skull differed but little from that of a modern greyhound. Taking into consideration the position and nature of the deposit, one may provisionally assume that the bones belong to animals which lived in the Forth valley about the end of the Neolithic Age,—the dog and sheep undoubtedly lived under domestication, but whether the horses were tame or wild is uncertain. The next horse bones from Scotch deposits available for study consisted of the skulls and limb-bones from Newstead, already referred to. Several of the horses in the possession The bones of the Celtic shorthorn and of turbary sheep, the presence of hammer-stones, pieces of pottery and scrapers, of limpet and other shells, together with the bones and implements collected during the excavations by the late Mr John Bruce of Sumburgh, support Mr Douglas’s view that horses reached Shetland some centuries before the turbulent Norse jarls, harassed by Harold Fairhair, began to settle in the Northern and Western Islands of Scotland. It may hence be assumed that Shetland ponies are mainly descended from the “small and fleet” race yoked to the chariots of the Caledonians at the battle of Mons Graupius. This ancient race (which was probably brought to Britain during the late Celtic period) was probably originally a blend of the slender-limbed, Arab-like ponies of the Swiss Lake-dwellers and of a thick-set race of the Elephant-Bed type. That the Shetland Fig. 1.—A 41-inch Java pony. Many East Indian ponies are said to be saturated with Arab blood. In the Java mare figured the head and limbs bear nearly the same relation to the trunk as in small desert Arabs. Fig. 2.—A Norwegian Udganger pony in which the legs are relatively nearly as short as in the dachshund. From a specimen in the Bergen Museum. Fig. 3.—A 42-inch pony of the Udganger type from Iceland, in which the head and legs bear nearly the same relation to the trunk as in Exmoor ponies. This pony is characterised by a fine head, large eyes, and small ears; by fine limbs, sloping shoulders, and a short back; and by the absence of the hind chestnuts and all four ergots. Plate I. Fig. 1. A 41-inch JAVA PONY. Fig. 2. A DWARFED UDGANGER PONY, NORWAY. Fig. 3. A 42-inch ICELAND PONY, UDGANGER TYPE. Fig. 4.—Skeleton of a 33-inch Shetland pony (Highland Chieftain) in the American Museum of Natural History, New York. Though the front cannon-bone is 1·5 inches shorter than in the three-toed Miocene horse Protohippus, it has only been dwarfed about one-quarter of an inch. From a photograph lent by Prof. H. Fairfield Osborn. Fig. 5.—Skeleton of Persimmon, a 66-inch race-horse belonging to the late King Edward VII. The bones of the limbs of Persimmon bear practically the same relation to each other and to the trunk as in Highland Chieftain, but in Persimmon the skull is relatively shorter and the withers are relatively higher. Plate II. Fig. 4.—Skeleton of Highland Chieftain, a 33-inch Shetland Pony. Fig. 5.—Skeleton of Persimmon, a 66-inch Thoroughbred. Fig. 6.—Side view of skull of Eric, a 36·5-inch Shetland pony of the riding type. Fig. 7.—Skull of a new-born foal of the Celtic or riding type. Fig. 8.—Skull of a four-year-old Prjevalsky horse from Mongolia. In the foal the cranium is relatively large and the face decidedly dished; in the Sheltie the face is longer than in the foal, but less bent downwards on the cranium and less dished; in the Prjevalsky stallion the cranium is less globular, while the face is very long and, owing to the bulging outwards of the nasals, “Roman-nosed.” Though in some Shetland ponies the face is long, the wild horse now found in Mongolia seems to have contributed little to the making of the modern Sheltie. Dimensions of Skulls.
Plate III. Fig. 6.—Skull of Eric, a 36·5-inch Shetland Pony. Fig. 7.—Skull of a new-born foal, Celtic type. Fig. 8.—Skull of a wild Prjevalsky horse, from Mongolia. Fig. 9a. Middle metacarpal (front cannon-bone) of Eric, a 36·5-inch Shetland pony; length, 143 mm. (5·6 inches), width at middle of shaft, 26 mm. In Eric the reduction or dwarfing of the front cannon-bones is estimated at 1 inch. Half nat. size. Fig. 9b. Middle metacarpal of the Miocene 3-toed (36-inch?) horse Protohippus sejunctus; length, 177 mm. (6·9 inches), width, 21 mm.—i.e., 1·3 inches longer than in Eric. Half nat. size. Fig. 9c. Middle metacarpal of Hypohippus, the (40-inch?) Miocene 3-toed “forest” horse of Montana and South Dakota; length, 215 mm. (8·4 inches), width, 22 mm.—i.e., 2·8 inches longer than in Eric. Half nat. size. Fig. 10. Bones of fore and hind foot (half nat. size) of Eohippus (fig. 12). After Marsh. Fig. 11. Bones of fore and hind foot (half nat. size) of Orohippus (fig. 13). After Marsh. Fig. 11a. Bones of the three front toes (II., III., and IV.) of Neohipparion, the 10-hands American Miocene desert horse with deer-like limbs. In this ancient race-horse the II. and IV. toes are very much shorter than in Hypohippus (fig. 20), a late Miocene “forest” horse. Fig. 11b. Engraving of a small-headed horse made during the Early Stone Age in the Combarelles Cave, France. The short face, small ear, and flowing mane suggest a race to which Shelties may be related. One-fourth nat. size. Plate IV. Cannon-bones, half nat. size. Fig. 9a. Eric. Fig. 9b. Protohippus. Fig. 9c. Hypohippus. Fig. 10.—Fore and hind foot, Eohippus, ½ nat. size. Fig. 11.—Fore and hind foot, Orohippus, ½ nat. size. Fig. 11a. Forefoot, Neohipparion, ¼ nat. size. Fig. 11b.—Engraving of a small-headed horse. Fig. 12.—Restoration of Eohippus, the American Hyracotherium, size about 12 inches. See fig. 10. Fig. 13.—Orohippus, a late Eocene four-toed horse, size about 16 inches. See fig. 11. Fig. 14.—Mesohippus, an Oligocene horse about 24 inches. In some of the three-toed Oligocene horses the cannon-bones were as long as in a 32-inch Shetland pony. See fig 18. Fig. 15.—Hypohippus, a three-toed Miocene “forest” horse, with the II. and IV. toes long and functional. In 40-inch specimens of Hypohippus the cannon-bones were 2·5 inches longer than in some 40-inch Shetland ponies. See figs. 9 and 20. Fig. 16.—Merychippus, a 9-hands three-toed Miocene horse. Protohippus (a possible ancestor of modern fine-limbed breeds) and the extinct Hipparions seem to have been derived from Merychippus. Fig. 17.—A 33-inch Shetland pony. In modern Shelties the legs are relatively shorter than in the three-toed horses of the later Miocene deposits. Shetland ponies have probably partly sprung from ancestors allied to Merychippus and partly from ancestors with limbs of the Hypohippus type. Figs. 12 to 16 after Osborn and Lull. Plate V. Fig. 16.—Merychippus, 36 inches. Fig. 12.—Eohippus, 12 inches. Fig. 15.—Hypohippus, 40 inches. Fig. 14.—Mesohippus, 24 inches. Fig. 13.—Orohippus, 16 inches. Fig. 17.—Shetland, 33 inches. All the figures one-thirtieth nat. size. Fig. 18.—Skeleton of fore-foot of Mesohippus. The II., III., and IV. digits are complete, the V. is represented by the upper end of the metacarpal. Oligocene of America. After Marsh. Fig. 19.—Forefoot of Merychippus (or Protohippus). Digits II. and IV. shorter than in fig. 18, and the vestige of digit V. very small or absent. American Miocene. After specimen in American Museum of Natural History. Fig. 20.—Forefoot of Hypohippus, the Miocene “forest” horse. Digits II. and IV. long as in Mesohippus, digits I. and IV. represented by small “splints” not seen in figure. After specimen in American Museum of Natural History. Fig. 21.—Upper molar, E. stenonis, natural size. The internal pillar (p) is only one-third the length of the grinding surface of the crown. Pliocene. After Boule. Fig. 22.—Upper molar, E. fossilis, natural size. The internal pillar (p) is more than half the length of the grinding surface of crown. Pleistocene. Kent’s Cavern, Devonshire. After Owen. Fig. 23.—Premolar and molars (natural size) of a small mediÆval? horse from Aberdour, Aberdeenshire. The internal pillars are short. Small horses with short-pillared teeth have lived in Europe since the end of the Pliocene. In the 36·5-inch Shetland pony Eric the molars very closely agree with those figured. From specimens received from Prof. Arthur Thomson, Aberdeen. Fig. 24.—Premolar and molars of a small horse from the Roman Fort, Newstead. The pillars are long, as in E. robustus of SolutrÈ and other small Pleistocene horses of Europe; as in the 11-hands E. tau of the Mexican Pleistocene; and as in Shetland ponies of the “forest” or Londonderry type. Plate VI. Fig. 21. Fig. 22. Fig. 23. Fig. 24. Fig. 18. Mesohippus. Fig. 19. Merychippus. Fig. 20. Hypohippus. PRINTED BY WILLIAM BLACKWOOD AND SONS. |