Critical reassessment of putative Acheulean Porosphaera globularis beads |
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Authors: | Solange Rigaud Francesco d'Errico Marian Vanhaeren Christian Neumann |
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Affiliation: | 1. UMR 5199 PACEA, Institut de Préhistoire et de Géologie du Quaternaire, Université Bordeaux I, Avenue des Facultés, F-33405 Talence, France;2. Institute for Human Evolution, University of the Witwatersrand, Johannesburg, South Africa;3. CNRS UMR 7041 ArScAn, Ethnologie préhistorique, 21 allée de l''université, F-92023 Nanterre Cedex, France;4. Museum für Naturkunde, Humboldt University, Invalidenstrasse 43, D-10115 Berlin, Germany |
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Abstract: | Excavations at Acheulean sites in northern Europe at the end of the 19th century have yielded fossil sponges belonging to the Late Cretaceous species Porosphaera globularis. The spherical morphology of these fossils, their small size, and the presence of a natural complete perforation in their center have led some archaeologists to interpret them as the oldest known beads. Others argue that the presence of these fossils at archaeological sites is due to natural processes. Re-examination of material collected during the 19th century has recently revived the bead interpretation. We tested the bead hypothesis by analyzing 13 samples of Porosphaera from nine sites in Britain and France. We conducted morphometric and microscopic analyses on specimens recovered from archaeological sites (n = 349), a natural geological sample, which was collected directly from Cretaceous strata (n = 352), and a sample from a Bronze Age burial (n = 43). Reappraisal of contextual data shows that the association of these finds with Acheulean artifacts is uncertain. Our results show that archaeological specimens are significantly different in size and perforation pattern from those of the natural geological sample. This may be due to size-sorting caused by sedimentary processes, size-selection by Palaeolithic people or by 19th century collectors. Modifications of the fossils' natural shape were detected on a few specimens in the form of localized abrasions and microchipping along the hole margins. A single specimen displays a facet close to the hole produced by grinding. The surfaces of these features exhibit a hue lighter than that observed on the remainder of the specimens indicating that they may be recent in origin and due to post-excavation and preservation treatment. However, this seems contradicted, for some specimens from Bedford, by the fact that according to Smith, W.G. [1884. On a Palaeolithic floor at North-East London. Journal of the Anthropological Institute of Great Britain and Ireland 13, 357–384] the specimens bearing microchipping and abrasions were found by him and “not touched or manipulated by the workmen”. We conclude that new excavations of these sites, involving systematic screening of sediments, are needed in order to attempt to solve the Porosphaera “mystery”. |
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Keywords: | Behavioural modernity Lower Palaeolithic Ornaments Symbolism Taphonomy Fossil sponges |
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