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Neolithic and Bronze Age Landscapes of North Mayo: Report 2011

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When the charcoal is examined through different time periods, it is clear that hazel<br />

dominates the <strong>Neolithic</strong> samples, while the picture <strong>of</strong> woodl<strong>and</strong>s during the Early <strong>Bronze</strong><br />

<strong>Age</strong> is quite different, being dominated by willow <strong>and</strong> elm (Figure 21).<br />

Annual ring counts range from 1 to 20 in the Rathlackan material. Growth is medium, with<br />

instances also <strong>of</strong> fast <strong>and</strong> slow growth. The fragments are mainly strongly curved, with some<br />

weakly curved annual rings indicating the use <strong>of</strong> larger branches or trunks.<br />

Discussion<br />

It is generally assumed that fuel <strong>and</strong> wood will be gathered from as close to the site as<br />

possible (Shackleton <strong>and</strong> Prins 1992) <strong>and</strong> therefore archaeological charcoal can reflect the<br />

surrounding environment. There are <strong>of</strong> course problems with this principle, such as<br />

particular species may have been selected over others <strong>and</strong> there are issues with charcoal<br />

fragmentation. Yet, for the purposes <strong>of</strong> environmental reconstruction, charcoal can be used<br />

to provide a floristic background to archaeological sites, particularly when integrated with<br />

other environmental data. It is impossible to know, however, how close to or far away from<br />

a site wood was gathered.<br />

fragment count<br />

100%<br />

90%<br />

80%<br />

70%<br />

60%<br />

50%<br />

40%<br />

30%<br />

20%<br />

10%<br />

0%<br />

E24 921E40 E494 E109 E580<br />

Ulmus<br />

Taxus<br />

Salix<br />

Quercus<br />

Pinus<br />

Maloideae<br />

Ilex<br />

Hedera<br />

Fraxinus<br />

Corylus/Alnus<br />

Corylus<br />

Betula<br />

Alnus<br />

Figure 22 Comparison <strong>of</strong> charcoal data from all sites: N= 4195<br />

The Middle <strong>Neolithic</strong> Glenulra scatter (92E140) <strong>and</strong> <strong>Neolithic</strong>/Early <strong>Bronze</strong> <strong>Age</strong> Rathlackan<br />

(E580) sites are similar in the high levels <strong>of</strong> hazel (Figure 22). More oak is evident in<br />

Rathlackan than Glenulra, however. In contrast, both the Middle <strong>Neolithic</strong> Glenulra scatter<br />

(E24) <strong>and</strong> the Late <strong>Neolithic</strong>/Early <strong>Bronze</strong> <strong>Age</strong> Céide visitor centre (E494) are dominated by<br />

birch. The levels <strong>of</strong> oak are low within the Céide visitor centre while they are important in<br />

the Glenulra enclosure. The highest number <strong>of</strong> fragments was identified from Belderg Beg<br />

41

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