Britain BC: Life in Britain and Ireland Before the Romans. Francis Pryor
etc. By the same token, in the past it was possible to have relationships at long distance between people who were illiterate, by way of gifts and other material gestures of affection, aided sometimes by a helpful third party. Modern human beings (and in ‘modern’ I include the Crô-Magnons) can go even further. They can have loving relationships with objects (Clive Gamble mentions sports cars), pets, or something as bizarre as archaeological theory.
Gamble characterises social life in his third period as being truly complicated, rather than simply complex. I will let him sum up what life at the closing stages of the Ice Ages was about. He is writing about the ability of people to create social, personal and symbolic networks, which for the first time included both human beings and objects. I have no problem in identifying with the lives they led, even if I couldn’t have survived in their world for very long: ‘The surrounding environment in the Upper Palaeolithic was now richly layered with meaning and symbolically linked. Social occasions with rituals and resources now structured the seemingly unfettered life of the Palaeolithic person.’16
One of the aspects of earlier prehistory that I find the hardest to come to terms with is the extent to which the immediate surroundings of what was shortly to become the British Isles changed. Perhaps my inability to feel at home with the colossal transformations of the entire North European Plain simply reflects the short-lived, ephemeral world in which I spend my professional life: a matter of perhaps five millennia. In terms of what had gone before, the Iron Age (700 BC-AD 43) is a mere blink of an eye. In later prehistory we deal with events on a human scale, events we can relate to, such as those years when rivers flooded and farmers were forced to abandon their lowest meadow pastures. These may have been catastrophic events at the time, but in terms of the Upper Palaeolithic they are storms in thimbles, let alone teacups.
During the height of the last glacial maximum, around eighteen thousand years ago, when the climate was at its coldest and vast amounts of fresh and seawater were locked up in ice caps and glaciers, the North European Plain (whose remnants survive in parts of north-western Germany, the Low Countries and eastern England) extended right across the southern North Sea. A narrow channel was all that separated Scandinavia from Scotland. The Hebrides were part of mainland Britain. The climate then warmed a great deal, reaching a peak about thirteen thousand years ago when, as has been mentioned earlier, the climate of Britain was if anything warmer than today. This is the warm spell that preceded the final or Loch Lomond cold sub-phase. Shortly after the warmest period at twelve thousand years ago, the North Sea extended very much further southwards, and Orkney and Shetland were beginning to look more like islands-to-be. Despite this shrinkage of the North European Plain, there is still a huge width of ‘land bridge’ available to those settlers who recolonised Britain to set up the Creswellian tradition around 12,600 years ago.
We have reached a turning point in our story. The ice has melted, the climate is suddenly growing warmer. It’s ten thousand years ago – and it’s that time of year to change the clocks. In this instance we’ll pretend it’s spring, and we’ll turn the clocks forward two thousand years. So, ‘ten thousand years ago’ will become ‘8000 BC’. There’s no good reason for this, other than the fact that many archaeologists, myself included, are happier working in years BC after the Ice Age. It’s also symbolic, and after what has gone before – and the momentous changes that are just around the corner – we ought to do something symbolic of the new era we are about to enter.
I’VE LONG BEEN OF THE OPINION that archaeological terminology can get in the way of sense and meaning, which is why so far I’ve tried to keep matters as straightforward as possible. The trouble is that the Palaeolithic was so long-lived, and the complexities of human physical evolution were such, that any attempt at greater simplification would actually have become misleading. But from now on, the people we are dealing with will be physically identical to us in every respect, and the dates, which will be expressed in years BC, are plain enough. This is just as well, because from here on the pace of our story really does begin to speed up. We will also have a larger canvas available to us, as Scotland emerges from the cold, and Ireland is populated by people who have made the journey west across the channel that was later to become the Irish Sea.
The period we are concerned with in this chapter is known as the Mesolithic or Middle Stone Age, and it begins with the onset of the postglacial some ten thousand years ago, when the Loch Lomond cold snap finished. The climate grew rapidly warmer (the most intense warming lasted a mere fifty years), so that within two or three lifetimes, average temperatures were as high as they are today.1 This is the background to the final five thousand years of Britain as a realm exclusively inhabited by groups of hunters.
In every way, the Mesolithic was transitional: between the Ice Ages and the postglacial, and between hunting/gathering and farming. It would be a great mistake to view these changes of culture and environment as abrupt steps, because they weren’t. The more closely we examine the material record of that period, the more we realise that, the initial postglacial warming aside, change was essentially gradual or evolutionary. There were no sudden and dramatic swerves of direction, just as there was no abrupt break between the Final Upper Palaeolithic and the Mesolithic. They were the same people, doing more or less the same things, in an environment that had grown dramatically warmer. And as it grew warmer, so it grew wetter underfoot, as sea levels began to rise – mainly as a result of melting ice.
When I was a student at Cambridge, my first Professor of Archaeology was a specialist in the Mesolithic, Grahame (later Sir Grahame) Clark.2 He excavated what is now the most famous Mesolithic site in Britain, at Star Carr, in the flat, open Vale of Pickering, in north-eastern Yorkshire. It’s a drowned landscape, buried beneath layers of peat, that closely resembles the East Anglian fens, where I’ve spent most of my professional life. Strangely, I have no recollection of Professor Clark lecturing about Star Carr, but that could well be down to my youthful inability to get up in the morning. Alternatively, it could reflect the fact that the Professor’s lectures were very dry indeed. They did not linger fondly in the memory, perhaps because they were so very flinty – almost obsessively flinty.3
In fairness to Clark, he did view the study of flints as a means of reaching the people who made and used them, but at the time I found his enormous interest in their typology daunting. Typology, incidentally, is an archaeological term that describes how one thing gradually develops into another. An example often used to teach the concept to students is the development of the first railway coaches, which initially resembled horse-drawn carriages on flanged wheels, then were joined together on the same chassis, before finally taking the form of something which resembled the railway coach of today. It was a process that took several decades. The history of archaeology is full of typological studies, of which perhaps the most famous is the development of bronze from stone axes. The succession of Upper Palaeolithic and then Mesolithic flint typologies is, however, truly frightening.
In a vastly simplified nutshell, it is essentially a story of miniaturisation. Many of the tiny flints were used to provide barbs or points for composite bone or antler spears which were used for hunting or fishing. Others were used for other purposes – to do, for example, with working bone, or shaping leather. These so-called microliths were made in a highly developed technique that was ultimately based on the core and blade tradition of the Earlier Upper Palaeolithic. Mesolithic microliths occur in a bewildering variety of geometric shapes that are tailor-made for the detailed typological analyses that have kept many scholars gainfully employed for decades. I shan’t attempt to summarise their work here. As I have said previously, life is too short.
Although his lectures were as dry as a charcoal biscuit, and I found him impossible to relate to as a student, Clark was