Ancient Man in Britain. Donald Alexander Mackenzie
had written in this vein after seeing the collection of stone weapons and implements in the Northern Institution at Inverness. "The most practised eye", he commented, "can hardly distinguish between the weapons of the Old Scot and the New Zealander." Eyes have become more practised in dealing with flints since Miller's time. Andrew Lang remembered his Miller when he wrote:
"Now just as the flint arrowheads are scattered everywhere, in all the continents and isles—and everywhere are much alike, and bear no very definite marks of the special influence of race—so it is with the habits and legends investigated by the student of folk-lore".8
The recent discovery that the early flints found in Western Europe and in England were shaped by the Neanderthals and the pre-Neanderthals compels a revision of this complacent view of an extraordinarily difficult and complex problem. It is obvious that the needs and constructive powers of the Neanderthals, whose big clumsy hands lacked "the delicate play between the thumb and fingers characteristic of modern races", could not have been the same as those of the Crô-Magnons, and that the finely shaped implements of the Crô-Magnons could not have been evolved from the rough implements of the Neanderthals. The craftsmen of one race may, however, have imitated, or attempted to imitate, the technique of those of another.
There was a distinct break in the continuity of culture during the Palæolithic Age, caused by the arrival in Western Europe of the ancestors of Modern Man. The advent of the Crô-Magnons in Europe "represents on the cultural side", as Professor Elliot Smith says in Primitive Man, "the most momentous event in its history".
Photo. Mansell
EXAMPLES OF LOWER PALÆOLITHIC INDUSTRIES FOUND IN ENGLAND
(British Museum)
Some urge that the term "Palæolithic" should now be discarded altogether, but its use has become so firmly established that archæologists are loth to dispense with it. The first period of human culture has, however, had to be divided into "Lower" and "Upper Palæolithic"—Lower closing with the disappearance of the Neanderthals, and Upper beginning with the arrival of the Crô-Magnons. These periods embrace the sub-divisions detected during the latter half of last century by the French archæologists, and are now classified as follows:
Lower Palæolithic—
1. Pre-Chellean.
2. Chellean (named after the town of Chelles, east of Paris).
3. Acheulian (named after St. Acheul in Somme valley).
4. Mousterian (named after the caves of Le Moustier in the valley of the River Vézère).
Upper Palæolithic—
1. Aurignacian (named after Aurignac, Haute Garonne).
2. Solutrean (named after Solutré, Saône-et-Loire).
3. Magdalenian (named after La Madeleine in the valley of the River Vézère).
Then follows, in France, the Azilian stage (named after Mas d'Azil, a town at the foot of the Pyrenees) which is regarded as the link between Upper Palæolithic and Neolithic. But in Western Europe, including Britain, there were really three distinct cultures during the so-called "Transition Period". These are the Azilian, the Tardenoisian, and the Maglemosian. These cultures were associated with the movements of new peoples in Europe.
The pre-Chellean flints (also called Eoliths) were wrought by the pre-Neanderthals. Chellean probably represents the earliest work in Europe of a pre-Neanderthal type like Piltdown man. The most characteristic implement of this phase is the coup de poing or pear-shaped "hand axe", which was at first roughly shaped and unsymmetrical. It was greatly improved during the Acheulian stage, and after being finely wrought in Mousterian times, when it was not much used, was supplanted by smaller and better chipped implements. The Neanderthals practised the Mousterian industry.
Chellean Coup de Poing or "Hand Axe"
Right-hand view shows sinuous cutting edge.
A profound change occurred when the Aurignacian stage of culture was inaugurated by the intruding Crô-Magnons. Skilled workers chipped flint in a new way, and, like the contemporary inhabitants of North Africa, shaped artifacts from bone; they also used reindeer horn, and the ivory tusks of mammoths. The birth of pictorial art took place in Europe after the Crô-Magnons arrived.
It would appear that the remnants of the Neanderthals in the late Mousterian stage of culture were stimulated by the arrival of the Crô-Magnons to imitate new flint forms and adopt the new methods of workmanship. There is no other evidence to indicate that the Crô-Magnons came into contact with communities of the Neanderthals. In these far-off days Europe was thinly peopled by hunters who dwelt in caves. The climate was cold, and the hairy mammoth and the reindeer browsed in the lowlands of France and Germany. Italy was linked with Africa; the grass-lands of North Africa stretched southward across the area now known as the Sahara desert, and dense forests fringed the banks of the River Nile and extended eastward to the Red Sea.
Neanderthal man had originally entered Europe when the climate was much milder than it is in our own time. He crossed over from Africa by the Italian land-bridge, and he found African fauna, including species of the elephant, rhinoceros, hippopotamus, lion, and the hyæna, jackal, and sabre-tooth tiger in Spain, France, Germany. Thousands of years elapsed and the summers became shorter, and the winters longer and more severe, until the northern fauna began to migrate southward, and the African fauna deserted the plains and decaying forests of Europe. Then followed the Fourth Glacial phase, and when it was passing away the Neanderthals, who had long been in the Mousterian phase of culture, saw bands of Crô-Magnons prospecting and hunting in southern Europe. The new-comers had migrated from some centre of culture in North Africa, and appear to have crossed over the Italian land-bridge. It is unlikely that many, if any, entered Europe from the east. At the time the Black Sea was more than twice its present size, and glaciers still blocked the passes of Asia Minor.
A great contrast was presented by the two types of mankind. The short, powerfully built, but slouching and slow-footed Neanderthals were, in a conflict, no match for the tall, active, and swift-footed Crô-Magnons, before whom they retreated, yielding up their flint-working stations, and their caves and grottoes. It may be, as some suggest, that fierce battles were fought, but there is no evidence of warfare; it may be that the Neanderthals succumbed to imported diseases, as did so many thousands of the inhabitants of the Amazon Valley, when measles and other diseases were introduced by the Spaniards. The fact remains that the Neanderthals died out as completely as did the Tasmanians before the advance of British settlers. We do not know whether or not they resisted, for a time, the intrusion of strangers on their hunting-grounds. It may be that the ravages of disease completed the tragic history of such relations as they may have had with the ancestors of Modern Man.
At this point, before we deal with the arrival in Britain of the representatives of the early races, it should be noted that differences of opinion exist among scientists regarding the geological horizons of the Palæolithic culture stages. In the Pleistocene Age there appear to have been four great glacial epochs and two minor ones. Geological opinion is, however, divided in this connection.
WESTERN EUROPE DURING THE THIRD INTER-GLACIAL EPOCH
(According to the Abbé Breuil the Strait of Gibraltar was open and the Balearic group a great island.)
During the First Glacial epoch the musk-ox, now found in the Arctic regions, migrated as far south as Sussex. The Pliocene9 mammals were not, however, completely exterminated; many of them survived until the First Interglacial epoch, which lasted for about 75,000 years—that is three times longer than the First Glacial epoch. The Second Glacial epoch is believed to have extended over 25,000 years. It brought to the southern shores of the Baltic Sea the reindeer and the hairy mammoth. Then came the prolonged Second Interglacial stage which prevailed for about 200,000 years. The climate of Europe underwent a change until it grew warmer than it is at the present
The last division of the Tertiary period.