By the later part of the third millennium BCE, Britain had become connected to mainland Europe by the so-called ‘Beaker network’. This appears to have involved the circulation of people, materials, and cultural innovations over trans-continental distances. Most tellingly, it included direct evidence for cross-Channel contact and the movement of individual people into Britain who had lived much or most of their lives in continental Europe. However, the evidence for such contact during the previous few centuries is very much sparser. If, as it seems reasonable to infer, developed passage tombs were ultimately an Atlantic European phenomenon that was adopted in idiosyncratic ways in Ireland, Scotland, and finally Scandinavia during the course of the fourth millennium, routine interactions with the Continent are less easy to identify thereafter. In marked contrast with this, the period after 3000 BCE saw the emergence of a range of new interregional connections within Britain and Ireland. These have been less consistently recognized, as they conflict with the traditional narrative in which populations in central and south-west Asia engaged in periodic wholesale migration northward and westward. Such a narrative of external stimulus to change is less secure in this period because we now realize that the social and cultural changes that overtook Britain in the earlier third millennium originated predominantly in the northern and western parts of these islands. Some of the most significant innovations of the third millennium throughout Britain were ultimately generated in the Orkney archipelago and its immediate sphere of contact. While aspects of the unique developments that took place in the Orkneys can be attributed to connections with Ireland and the Western Isles, these contributed to the emergence of a distinctive social formation that was at once highly competitive and spectacularly creative. By the start of the third millennium, Orkney had become a crucible of social and cultural change, but developments in the islands arguably began to diverge from those on the mainland soon after the Neolithic began, perhaps during the thirty-seventh century BCE.
Tell Sabi Abyad, Syria: Radiocarbon Chronology, Cultural Change, and the 8.2 ka Event
