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The Archaeology of Britain: An introduction from ... - waughfamily.ca

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Hunter-gatherers <strong>of</strong> the Mesolithic<br />

• 53 •<br />

<strong>of</strong> foliage for wild game (Simmons and Innes 1996). <strong>An</strong>other form <strong>of</strong> animal management may<br />

have been the transport <strong>of</strong> some species to <strong>of</strong>fshore islands.<br />

Shell middens and coastal exploitation<br />

<strong>The</strong> coastal zone is likely to have been the most productive part <strong>of</strong> <strong>Britain</strong> during the Mesolithic.<br />

It is not surprising that the largest sites, including Culverwell, are lo<strong>ca</strong>ted there. Access to woodland<br />

with its large game, as well as marine mammals and fish and the rich resources <strong>of</strong> the seashore,<br />

including crustaceans, seaweeds and shellfish, would have been simple.<br />

<strong>The</strong> clearest picture <strong>of</strong> coastal exploitation comes <strong>from</strong> western Scotland, notably the middens<br />

on Oronsay. Others are known <strong>from</strong> <strong>ca</strong>ves and open sites around Oban bay (Argyll), and on<br />

other islands (e.g. Ulva Cave <strong>of</strong>f Mull). Such middens typi<strong>ca</strong>lly reveal an immense diversity <strong>of</strong><br />

species. Red deer and otter, over 30 types <strong>of</strong> birds, crabs, seals, shellfish and fish are attested on<br />

Oronsay. Over 90 per cent <strong>of</strong> the fish bones come <strong>from</strong> saithe and testify to marine fishing,<br />

although hooks and nets are absent. Limpets dominate the mollus<strong>ca</strong>n remains, but periwinkle<br />

and dogwhelk are well represented.<br />

Otoliths (ear bones) <strong>of</strong> fish indi<strong>ca</strong>te the season <strong>of</strong> occupation. As there is a strong correlation<br />

between the size <strong>of</strong> a fish and these bones, and as young saithe grow rapidly, the size distributions<br />

<strong>of</strong> otoliths are indi<strong>ca</strong>tive <strong>of</strong> the season(s) <strong>of</strong> the <strong>ca</strong>tches—assuming that spawning occurred at<br />

the same time as today. On Oronsay, different middens had distinctive otolith size distributions,<br />

implying that they accumulated in different seasons, with summer occupation at Cnoc Sligeach,<br />

for instance, while the Priory midden was used <strong>from</strong> the start <strong>of</strong> winter until early spring. In fact,<br />

all seasons are represented in this set <strong>of</strong> middens, leading some to suggest that people lived on<br />

Oronsay all year round. This seems unlikely in light <strong>of</strong> its size; a more realistic interpretation is<br />

that whenever foragers visited, they chose the optimum site with regard to prevailing winds, tides<br />

and the specific resources then available.<br />

Mollus<strong>ca</strong>n remains <strong>ca</strong>n provide detailed information about foraging patterns. <strong>The</strong> shape <strong>of</strong><br />

limpet shells is related to the position on the shore where this mollusc is found: those <strong>from</strong> its<br />

lowest part have relatively flat shells, while those higher up are progressively more coni<strong>ca</strong>l. Limpets<br />

in the Ulva Cave midden are quite flat, indi<strong>ca</strong>ting that Mesolithic foragers had searched the<br />

lowest, and probably most productive, part <strong>of</strong> the shore (Russell et al. in Fischer 1995). Although<br />

the shellfish at Ulva were dominated by the three species noted on Oronsay, 19 other species,<br />

including tiny ones, were represented. One, the blue-rayed limpet (Helicon pellucidum), less than 10<br />

mm in size, is an unlikely foodstuff. This species lives on Laminaria spp. (the seaweed kelp, regularly<br />

harvested in modern times). It is likely that the Mesolithic foragers were also collecting kelp,<br />

perhaps as food.<br />

<strong>The</strong> use <strong>of</strong> plants<br />

A contentious aspect <strong>of</strong> Mesolithic subsistence concerns the importance <strong>of</strong> plant foods. Clarke<br />

(1976) argued that early Postglacial environments would have been rich in plant foods, which are<br />

likely to have made a major contribution to diet. Evidence to support this assertion has slowly<br />

been accumulating for the whole <strong>of</strong> Europe (Zvelebil 1994).<br />

Plant remains survive only if normal processes <strong>of</strong> de<strong>ca</strong>y are halted, which in <strong>Britain</strong> would<br />

mean a totally waterlogged site, the like <strong>of</strong> which remains absent. Charring also preserves plant<br />

foods, although the resulting assemblage is biased: charring depends on the proximity <strong>of</strong> fire, and<br />

many plant foods were probably eaten raw. Even when plant remains are preserved, their recovery<br />

<strong>from</strong> sediments requires sieving through very fine-grained mesh or flotation methods that many<br />

early, and some recent, ex<strong>ca</strong>vations have neglected to employ. In consequence, the limited amounts<br />

<strong>of</strong> plant foods known <strong>from</strong> Mesolithic sites do not reflect their signifi<strong>ca</strong>nce in the diet. Raspberry

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