Elsevier

Quaternary Science Reviews

Volume 139, 1 May 2016, Pages 158-163
Quaternary Science Reviews

Short communication
First evidence of a Late Upper Palaeolithic human presence in Ireland

https://doi.org/10.1016/j.quascirev.2016.02.029Get rights and content

Highlights

  • First archaeological evidence of humans in Palaeolithic Ireland.

  • Results rewrite the antiquity of human occupation of Ireland.

  • Butchered brown bear bone dated to circa 12,800–12,600 cal BP (Late Glacial).

  • Results raise questions concerning the faunal colonisation history since the LGM.

Abstract

The colonisation of North West Europe by humans and fauna following the Last Glacial Maximum (LGM) has been the subject of considerable discussion in recent decades and within multiple disciplines. Here we present new evidence that pushes back the date of human footfall in Ireland by up to 2500 cal BP to the Upper Palaeolithic. An assemblage of animal bones recovered from a cave in the west of Ireland during antiquarian excavations in 1903 included a butchered brown bear bone (patella) which was recently subjected to two independent radiocarbon dating processes; the resultant dates were in agreement: 12,810–12,590 cal BP and 12,810–12,685 cal BP. This find rewrites the antiquity of human occupation of Ireland and challenges the traditional paradigm that certain biota may have naturally colonised the island prior to human arrival.

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)

  • K. Aaris-Sørensen et al.

    The Scandinavian reindeer (Rangifer tarandus L.) after the last glacial maximum: time, seasonality and human exploitation

    J. Arch. Sci.

    (2007)
  • A. Bayliss et al.

    A new Bayesian chronology for Mesolithic occupation at Mount Sandel, Northern Ireland

    Proc.. Prehist. Soc.

    (2009)
  • G.E. Beatty 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)
  • H.H. Birks 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)
  • C. Bronk Ramsey et al.

    Recent and planned developments of the program OxCal

    Radiocarbon

    (2013)
  • R.F. Carden 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)
  • R. Charles

    The exploitation of carnivores and other fur-bearing mammals during the North-Western European late upper Palaeolithic and Mesolithic

    Oxf. J. Arch.

    (1997)
  • C.D. Clark et al.

    Pattern and timing of retreat of the last British-Irish ice sheet

    Quat. Sci. Rev.

    (2012)
  • G.B. Corbet

    Origin of the British insular races of small mammals and of the ‘Lusitanian’ fauna

    Nature

    (1961)
  • A.F. Deifendorf 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)
  • M. Dowd

    The Archaeology of Caves in Ireland

    (2015)
  • C.J. Edwards et al.

    Ancient hybridization and an Irish origin for the modern polar bear matriline

    Cur. Bio

    (2011)
  • M. Germonpré et al.

    Fossil bear bones in the Belgian upper Palaeolithic: the possibility of a proto bear-ceremonialism

    Arct. Anthro

    (2007)
  • A.J. Grindon et al.

    Irish Cepaea nemoralis land snails have a cryptic Franco-Iberian origin that is most easily explained by the movements of Mesolithic humans

    PLoS One

    (2013)
  • R. Jacobi et al.

    Radiocarbon dating and understanding the human record during the EUP

  • A.M. Lister

    The evolution of the giant deer, Megaloceros giganteus (Blumenbach)

    Zool. J. Linn. Soc.

    (1994)
  • F. McCormick

    A note on tool-worked giant irish deer antler (04E1014:4:1) from Ballyoran Bog

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