Britain BC: Life in Britain and Ireland Before the Romans. Francis Pryor
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Название: Britain BC: Life in Britain and Ireland Before the Romans
Автор: Francis Pryor
Издательство: HarperCollins
Жанр: Историческая литература
isbn: 9780007378685
isbn:
The site has been dated by radiocarbon to about 6500 BC, so it’s significantly later than Thatcham or Star Carr, but in many respects it’s quite similar.26 It’s positioned near water in woods of birch and hazel, but unlike either English site, Peter Woodman’s excavations produced huge quantities of fishbones, of which salmon and sea trout were by far the commonest. This gives us an important clue as to the time of year the site would have been occupied. Both fish are migratory, and enter rivers from the sea to spawn in summer and autumn. It seems most probable that this was when the site was occupied. We don’t know where the occupants went for the rest of the year, although the seaside is a possibility. Other evidence shows that their food was not confined to these very delicious fish; they also ate eel, wild pig, various birds including game birds, and hazelnuts. I can think of worse diets.
Mount Sandel is principally famous for its lightweight houses, which are still, I believe, the oldest proven domestic structures in the British Isles. There were two types. Six examples of the first type were found. It consists of a roughly circular or oval arrangement of angled stake- or post-holes, plus a doorway; sometimes there’s also evidence for a central hearth. The house was probably built from curved or hooped poles covered with hides, and the average size was just over five metres across, giving a floor area of about thirty square metres, which is broadly comparable with the ‘void’ area at Thatcham.
The second type of house was more tent-like, and about half the size of the hooped pole structures. It consists of four banana-shaped, shallow ditches or gullies arranged in a rough circle. Presumably these were dug to take the run-off of water from a tent-like structure. There’s no evidence for post-holes, so we must assume the framework didn’t need to be securely anchored, being structurally stable and able to shed all but the severest of gales. In this instance the hearth was positioned outside, but opposite, the entranceway.
Both styles of structure are lightweight and appropriate to people whose pattern of life requires movement through the landscape. Can we call them houses? I don’t see why not. A house is where people choose to live. As soon as we start to talk about ‘huts’ – or worse, ‘shacks’ – we do these buildings a disservice. The small structure within the four gullies at Mount Sandel is undoubtedly a tent-house, the other is a house, albeit a lightweight one. I strongly dislike the term ‘hut’, which I see in the archaeological literature far too often. Huts are for wheelbarrows and garden tools, not for people.
We’ve looked at Mesolithic settlements in England and Ireland, but what was happening further north, in Scotland – was it too cold for settlement in postglacial times? The answer is that it wasn’t; Scotland has produced plentiful evidence of life in the period. One of the most revealing sites was excavated by John Coles, who lectured to me on the Palaeolithic at Cambridge and co-authored the standard textbook of the day.27 He also lectured on the European Bronze Age, and a few years later co-authored another standard work.28 At the time he was busily engaged in experimental archaeology, and was dipping his toes into the waters of wetland archaeology, which posterity will probably judge to have been his major contribution. So he’s a man of many parts, which is perhaps why he was invited to take over an existing Mesolithic excavation at Morton, in the Kingdom of Fife, in 1967. The main dig took place in 1969 and 1970.29
I should perhaps note here that we still know of no evidence for postglacial occupation in Scotland before about 9000 BC. To the best of my knowledge the earliest site on the mainland is currently Cramond, near Edinburgh, which has produced radiocarbon dates from hazelnut shells to around 8500 BC.30 This is remarkably early, given the fact that it is generally agreed that most of Scotland would still have been uninhabitable before around 9600 BC.
Like most other Mesolithic sites, Morton shows clear evidence for more than one episode of occupation, and there are at least two centres of interest, which are known as Sites A and B. Today these are located a short distance inland, but in the fifth millennium BC they would have been very close to the shoreline. Radiocarbon dates indicate the sites were occupied three or four centuries before 4000 BC. So we are now approaching the end of the Mesolithic in this particular part of Scotland. Elsewhere in Britain some formerly Mesolithic communities will already have started to adopt the techniques of farming – to become in effect Neolithic.
Morton isn’t far from St Andrews, the home of golf, and the countryside round about reflects this, being gentle and undulating. In the fifth millennium BC the area was cloaked in open oak woodland (with elm) and an under-storey of hazel. These woods probably didn’t extend right down to the shoreline, which is where we find our two areas of occupation.
I hesitate to call both Sites A and B settlements, because Site B was very specialised, being in effect a huge dump or midden – a mound no less – of seashells. Mesolithic shell midden mounds are found in many places around the coasts of Britain and Ireland, but the shores of Scotland and the Western Isles boast some of the largest. Some are massive: substantial hillocks you could build a small bungalow on. They demonstrate, among other things, that shellfish were a highly important part of the seasonal round. The shells of shellfish such as the common cockle grow at varying rates at different times of year, in response to a variety of factors including air/water temperature and the salinity of the seawater. Using the information encoded within the shells at Morton, Margaret Deith of Cambridge University was able to demonstrate that a high proportion of them had been harvested high on the beach, and that no particular season seems to have been favoured.31 If anything, wintertime, when the meat of cockles is less nutritious than in summer, was the most popular period for visiting Morton beach.
The impression gained is of opportunistic visits, the way one ‘grabs a bite’ whilst busily engaged in something else – at Morton this may have been the collection of suitable beach pebbles from which to fashion implements. The midden did however show clear signs that small temporary squats or camps had been scooped into it, perhaps as refuges from the worst of the wind. The surviving mound of shells was large, gently curving, and about thirty by 3.5 metres; its maximum thickness was 0.78 metres. At one point John Coles was able to identify a succession of five scoops or hollows which were floored with an occupation deposit – essentially crushed shells and an organic ‘dark earth’ – and showed clear signs of human use, including ‘bashed lumps’, stones that had been roughly hit to provide usable cutting edges and sharp points. But the signs of settlement on the midden were far less intensive than at Site A, about 150 metres to the south. The midden produced just 372 stone artefacts – compared with over thirteen thousand on Site A – and large quantities of fish and mammal bones, including red and roe deer, wild cattle and pig. By way of numerical compensation, it was composed of some ten million shells.
Why did these vast mounds of shells accumulate? The beach is a very hostile environment, lashed by winds, waves and storms. Heaps of shells wouldn’t last for long unless (a) they were carefully positioned to be out of the reach of storms and tides, and (b) people wanted СКАЧАТЬ