Short communicationFirst evidence of a Late Upper Palaeolithic human presence in Ireland
Introduction
The colonisation of North West Europe by humans and biota following the amelioration of severe conditions after the Last Glacial Maximum (circa 28,200–20,400 cal BP; Clark et al. 2012) has been the subject of considerable discussion for many decades and within different disciplines (Corbet, 1961, Woodman, 1998, Yalden, 1999, Jacobi and Higham, 2011, Woodman, 2011, Woodman, 2015, Montgomery et al., 2014). Evidence for the recolonisation of Britain by humans dates from circa 15,000 cal BP, represented by lithic assemblages, human remains and worked animal bones from at least 16 caves (Yalden, 1999, Pettitt and White, 2012). Until now, the earliest detected human presence on the island of Ireland has been the Early Mesolithic hunter-gatherer camp at Mount Sandel, Co. Derry–occupied from 10,290–9790 cal BP (UBA-2357, 8990 ± 80 BP) (Bayliss and Woodman, 2009) (Fig. 1). Even though an island since approximately 20,600–18,100 cal BP (Clark et al., 2012, Peters et al., 2015), that human colonisation of Ireland should take place so late has been considered improbable because of the potentially suitable environmental conditions and ecosystem present for several millennia prior to the Mount Sandel settlement (Woodman, 1986, Woodman et al., 1997, Wickham-Jones and Woodman, 1998, Woodman, 1998, Woodman, 2011, Woodman, 2015, 171–9). Furthermore, Palaeolithic settlements are known from along the Welsh coast (Pettitt and White, 2012), western Scotland (Mithen et al., 2015), Scandinavia (Aaris-Sørensen et al., 2007), and Iberia (Birks et al., 2015)–all locations that would have been navigable by boat.
This study involved dating three brown bear (Ursus arctos) bones, two of which have been humanly modified in the form of exhibiting butchery or cutmarks. The bones were recovered from two caves located just 380 m apart - Alice and Gwendoline Cave and the Catacombs - in County Clare in the west of Ireland, during excavations conducted by the Committee Appointed to Explore Irish Caves in 1902 and 1903 (Scharff et al. 1906) (Fig. 1). To date, at least 25 brown bear bones and 30 brown bear bones have been identified from Alice and Gwendoline Cave and the Catacombs respectively; many of these were previously unidentified or misidentified in the original antiquarian report (Carden, unpub. data). The bear patella, which forms the focus of this paper, was found in one of the deeper strata in Alice and Gwendoline Cave. The antiquarian report noted the find as, ‘a knee-cap of a large bear (E.A. 131) [which] shows clearly the incisions of a knife, which was probably used to divide the tendons’ (ibid., 44). The patella, along with the entire faunal assemblage from the site, was packed in cardboard boxes and deposited in the National Museum of Ireland (NMI) (Natural History Division) in the early 1920s. In 2011, one of the authors (RFC) rediscovered the patella during a project involving the reassessment of the antiquarian faunal cave assemblages from Ireland stored in the NMI collections. Modified or butchered bear bones are quite rare in Ireland which led one of the authors (MD) to propose a project to radiocarbon date these samples. At the inception of the project there was no idea of what dates to expect. Alice and Gwendoline Cave and the Catacombs had produced remains of Late Pleistocene fauna (Carden, unpub. data) as well as archaeological material suggesting Neolithic and Bronze Age activities (Dowd, 2015); thus the bear bones could conceivably have related to any such period as bear survived in Ireland until the Middle Bronze Age (Edwards et al. 2011).
In this study, we subjected the brown bear patella with human-induced cutmarks to two independent radiocarbon laboratory dating processes. The results are interpreted and discussed in light of current archaeological knowledge of a post-LGM human presence and faunal colonisation history of Ireland.
Section snippets
Site and context
The humanly modified (butchered) adult brown bear right patella (NMING: F23919) was one of several thousand bones recovered during antiquarian investigations at Alice and Gwendoline Cave in 1903 (circa 3.5 km southwest of Ennis town, County Clare in the west of Ireland). The standard of excavation and recording was exceptionally good for the early twentieth century. Each cave was divided into grids measuring 0.6 m in length and as wide as the cave passage. Grids were excavated stratigraphically
Patella cutmarks
The patella is in fresh condition and shows no signs of weathering (Fig. 3). There are no signs of antiquarian conservation efforts, and the National Museum of Ireland records indicate the bone was not treated in any way since its acquisition in the 1920s. Five linear cutmarks (24–30 mm) on the anterior surface display asymmetrical cross-sections with sloping lower edges and vertical upper sides. Superficial bone diagenesis within the cutmarks is consistent with that on the adjacent bone
Discussion and conclusions
The humanly modified patella from Alice and Gwendoline Cave has significant ramifications in terms of establishing the first human footfall or colonisation of Ireland. The calibrated dates fall within the Younger Dryas stadial (circa 12,900–12,550 cal BP) and would be considered Final Palaeolithic if, for instance, the find was from a site in England or Wales (P. Pettitt, pers. comm.). The possibility that Ireland was inhabited during the Upper Palaeolithic has been mooted since the 1860s and
Acknowledgements
We thank the Royal Irish Academy and the Institute of Technology Sligo for funding the radiocarbon dates which were processed by the Chrono Centre, Queen's University Belfast and the ORAU, University of Oxford. Jill Cook, Alice Choyke and Terry O'Connor provided valued advice on the cutmarks. At the National Museum of Ireland we are grateful to Nigel Monaghan, Matthew Parkes, Pat Wallace, Raghnall Ó Floinn, Ned Kelly and Paul Mullarkey. Thanks to Thorsten Kahlert, Elaine Lynch, Eve
References (35)
- et al.
The Scandinavian reindeer (Rangifer tarandus L.) after the last glacial maximum: time, seasonality and human exploitation
J. Arch. Sci.
(2007) - et al.
A new Bayesian chronology for Mesolithic occupation at Mount Sandel, Northern Ireland
Proc.. Prehist. Soc.
(2009) - et al.
Phylogeographical analysis of two cold-tolerant plants with disjunct Lusitanian distributions does not support in situ survival during the last glaciation
J. Biogeogr.
(2014) - et al.
Impacts of palaeoclimate change 60 000–8000 years ago on humans and their environments in Europe: integrating palaeoenvironmental and archaeological data
Quat. Int.
(2015) - et al.
Recent and planned developments of the program OxCal
Radiocarbon
(2013) - et al.
Phylogeographic, ancient DNA, fossil and morphometric analyses reveal ancient and modern introductions of a large mammal: the complex case of red deer (Cervus elaphus) in Ireland
Quat. Sci. Rev.
(2012) The exploitation of carnivores and other fur-bearing mammals during the North-Western European late upper Palaeolithic and Mesolithic
Oxf. J. Arch.
(1997)- et al.
Pattern and timing of retreat of the last British-Irish ice sheet
Quat. Sci. Rev.
(2012) Origin of the British insular races of small mammals and of the ‘Lusitanian’ fauna
Nature
(1961)- et al.
Evidence for high-frequency late Glacial to mid-Holocene (16,800 to 5,500 cal yr B.P.) climate variability from oxygen isotope values of Lough Inchiquin, Ireland
Quat. Res.
(2006)