Heritage and participatory governance: An analysis of political strategies and social fractures in Spain

In the heritage field, institutions tend to see social participation as a synonym for good governance practice. This extends to other areas such as the environment, humanitarian aid, and sustainable development. In this article, the authors analyze the use of participatory models in the management of heritage through the study of three heritage sites in Spain: the prehistoric paintings in Altamira, the Mosque‐Cathedral in Córdoba, and the Cabo de Gata‐Nijar Natural Park. Their study suggests that, despite the promises of more democratic heritage governance, participatory methods are commonly bounded by social fractures that are concomitant to certain ‘heritage regimes’. They conclude that the critical study of participation in heritage should go beyond the dichotomy between ‘good and bad’ participation. Rather, it should focus on understanding what participation does to the entire heritagization process.     

Radiocarbon age determinations of fossil Margaritifera auricularia (Spengler) from the River Thames in West London

In the early 1900s shells of a large freshwater mussel, Margaritifera auricularia (Spengler), were discovered in calcreted gravel dredged from the channel of the Thames at several sites between Mortlake and Battersea in west London. These specimens were said to have been associated with Neolithic polished stone axes, supposedly as food remains. M. auricularia is now extinct in Britain, but it has been reported living in several large rivers in southern Europe although apparently not in recent years. Three radiocarbon dates of 4140±50, 4340±45 and 4860±40 bp have been obtained from Thames specimens, supporting a Neolithic age for these shells. The theory that the shells represent debris from imported human food is discounted and it is considered more likely that M. auricularia was actually living in the Thames in Neolithic times. Its extinction in Britain should be seen as part of a general recession during the Post-glacial, as revealed by fossil occurrences to the north and east of its present-day range.