“…Thus, blanket-bog growth may have been initiated early in the Neolithic, but it did not overwhelm the woodland at Srahwee until the end of the Neolithic or the early Bronze Age. This is comparable to the case of Céide fields in north County Mayo where peat encroached diachronously over the Neolithic landscape of farmland, ritual monuments, and settlement sites, following their abandonment (Molloy and O'Connell, 1995;Caulfield et al, 1998). The fact that peat growth followed, rather than caused, abandonment of agricultural activity at both Céide fields to the north and in the Connemara National Park to the south (Molloy and O'Connell, 1993;O'Connell, 1994), supports the hypothesis that climate change promoted peat growth more strongly than anthropogenic factors in the Murrisk Peninsula.…”