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The Oxford Handbook of Neolithic Europe

Page 34

by Chris Fowler


  The emergence of new mortuary practices in the early Neolithic (see Fowler and Scarre, this volume) is also hard to relate to the Mesolithic evidence in an unequivocal way. Cave burial was dominant in the early Mesolithic (Conneller 2006), but a gap in radiocarbon dated cave burials between c. 5000 and c. 4000 BC has been visible for some time. The only certain later Mesolithic human remains in Britain come from shell middens on Oronsay off the west coast of Scotland (Meiklejohn et al. 2005). In general there is a clear lack of evidence for the kind of social complexity agreed to exist within southern Scandinavia. The general assumption has tended to be that monumental burial, in the form of long barrows and stone chambered tombs, was introduced at the very beginning of the Neolithic. Early radiocarbon dates for such sites therefore implied an earlier beginning to the Neolithic as a whole (e.g. Schulting 2000). However, a recent programme of mass sampling from both long barrows and chambered tombs in southern England gives a start date during the fourth millennium BC, c. 3750 BC, rather than at its beginning (Whittle et al. 2007). Whilst it is possible that some smaller chambered tombs in western Britain, such as portal dolmens, may begin earlier (Sheridan 2004), there is no substantial evidence supporting this. The dates for causewayed enclosures are rather similar, probably beginning around 3700 BC (Whittle et al. 2011). These monuments therefore play no role in the Mesolithic–Neolithic transition in Britain—as in Scandinavia they may mark a significant social change during the Neolithic.

  There may be an earlier beginning to causewayed enclosures in Ireland, perhaps around 4000 BC at Magheraboy in County Sligo (Danaher 2007). Indeed, it is clear that there are some significant differences between Ireland and Britain. These have traditionally been seen in terms of Irish deficiencies, such as the ‘loss’ of microliths, but there are significant features of the Irish Mesolithic which do not occur in Britain, such as the production of ground stone axes. The most striking difference is that there are radiocarbon dates before 4000 BC for cattle (and possibly also sheep) in Ireland from Ferriter’s Cove, County Kerry (two dates with an average of c. 4300 BC: Woodman and McCarthy 2003; cf. Rowley-Conwy and Legge, this volume; Tresset, this volume). There is no evidence for aurochsen in Ireland, thus the cattle must be domestic. Taken together, this evidence may suggest an earlier inception to the Neolithic in Ireland than in Britain (Cooney 2007).

  This reminds us of the crucial importance of regional variation, and the need to consider multiple trajectories of change. Concerning houses, domesticated animals, and crops, there is a persuasive case for a greater degree of early Neolithic sedentism than recognized in the models currently dominant. However, in itself this does not mean that we need to return to the hypothesis of massive immigration. Instead a combination of limited population movement and indigenous change seems most plausible at present (e.g. Whittle 2007).

  ATLANTIC IBERIA

  In western Iberia (Spain and Portugal) the transition to the Neolithic occurred c. 5500 BC. The background to the transition is quite different to areas further north due to the impact of the Cardial culture, originating possibly in Italy or southern France, in eastern Spain from c. 5500 BC (Guilaine and Manen 2007). The lack of Mesolithic evidence locally, particularly for long-distance contacts and social complexity, has recently been combined with ancient DNA from Catalonia to support an interpretation of migrating farmers (Gamba et al. 2011). Cardial ware reached parts of north-west Spain and northern Portugal only shortly later (Arias 2007), implying a rapid shift to the Neolithic.

  The late Mesolithic of the Atlantic coast is known almost entirely from the large shell midden sites of the Tagus estuary, especially those of Muge (van der Schriek et al. 2007). These persisted until c. 5000 BC, and thus overlap with the inland early Neolithic by some five centuries (Carvalho 2010). As with shell middens elsewhere along the Atlantic these were major sites, perhaps monumental in scale, with a strong burial record. Central Portugal saw a movement of the Neolithic frontier around 5200 BC, but in Cantabria and northern Portugal, neolithization occurred only after 5000 BC. The abandonment of coastal sites has been related either to resource depletion or to environmental changes (Dean et al. 2011).

  In Iberia, megalithic tombs are constructed from c. 5400 BC. There is a possibility that, just as in Brittany, megalithic constructions began with menhirs, some carved with a shepherd’s crook (Calado 2002), but this speculation needs to be supported by dating evidence.

  The patchy and piecemeal nature of the early Neolithic and the lengthy transition in those areas lacking a Neolithic presence leads to the current interpretation of a mixture of colonization and local adoption (e.g. Arias 2007; Ruiz 2005).

  CONCLUSION

  The overall picture is that recent archaeological research and opinion broadly favours a strongly indigenous Mesolithic–Neolithic transition, but in many areas along the Atlantic population movement was also involved in neolithization. In addition, it is clear that there is much variation in the nature and speed of the transition even within regions, and thus the consensus is that a mixture of local, regional, and western European processes was at work in creating the observed patchwork.

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