Capitalist Expansion and the Decline of Common Property Ecosystems in China,Vietnam and India

This article identifies some of the multiple processes of capitalist development through which access to common property resources and their utility for communities are undermined. Three sites in upland Asia demonstrate how patterns of exclusion are mediated by the unique and selective trajectories through which capital expands, resulting in a decline of common property ecosystems. The process is mediated by economic stress, ecological degradation and political processes such as state‐sanctioned enclosure. The first case study from Shaoguan, South China, indicates how rapid capitalist industrialization has depleted the aquatic resource base, undermining the livelihoods of fishing households yet to be absorbed into the urban working class. At the second site, in Phu Yen, Vietnam, capitalist development is limited. However, indirect articulations between capitalism on the lowlands and the peasant economy of the uplands is driving the commercialization of agriculture and fishing and undermining the utility of communal river and lake ecosystems. In the third site, Buxa in West Bengal, India, there is only selective capitalist development, but patterns of resource extraction established during the colonial period and contemporary neoliberal ‘conservation’ agendas have directly excluded communities from forest resources. Restrictions on access oblige them to contribute subsidized labour to local enterprises. The article thus shows how communities which are differentially integrated into the global economy are excluded from natural resources through complex means.     

Energy dispersive X-ray fluorescence analysis of 1st millennium ad glass from Britain

A series of energy dispersive X-ray fluorescence analyses has been undertaken in response to archaeological problems relating to 1st millennium AD glass excavated in Britain. The aim of the work was to furnish a set of comparable analytical results to be used in assessing hypotheses concerning the general state and development of glass technology through this period. Within this framework, however, it has also been possible to attempt answers to specific archaeological questions relating to material from particular sites. The paper discusses the background to, and the interpretation of such results, particulars of the analytical technique used, a general overview of approximately 200 analyses and three examples of the use of this data in relation to specific archaeological problems.     

St Columba and the convention at Druimm Cete: peace and politics at seventh‐century Iona

Attendance at the ‘convention of kings’ at Druimm Cete in north‐east Ireland is one of the most famous episodes in the career of St Columba or Colum Cille, who died in 597. Discussion of the significance of this shadowy summit, largely informed by unreliable late evidence, has hitherto focused upon what (may have) transpired there between kings based in Ireland and Scotland. The result has been the neglect of the hagiographical dimension of the presentation of Druimm Cete in our principal source, Adomnán's Vita Sancti Columbae, composed c.700. Analysis of this material shows that Adomnán's information about the convention came from his principal source, composed some sixty years earlier. It reveals moreover that Druimm Cete assumed prominence within the Columban dossier in the 640s for what it represented, rather than because of what actually happened there. Once the hagiographical agenda of Vita Sancti Columbae and its principal source is restored to its rightful place in evaluating the text, it emerges that several of its best‐known stories – including the story of Columba's ordination of a Scottish king – are much more problematic as witnesses to sixth‐century history than is conventionally supposed. As scholars begin to lose their grip upon the historical Columba, however, they grow better able to grasp seventh‐century political history in north‐east Ireland and Gaelic Scotland.     

Pliocene corals from the Togopi Formation of the Dent Peninsula,Sabah, northeastern Borneo,Malaysia

Saw, J.V.M., Hunter, A.W., Johnson, K.G. & Abdul Rahman, A.H.B., November 2018. Pliocene corals from the Togopi Formation of the Dent Peninsula, Sabah, northeastern Borneo, Malaysia. Alcheringa 43, 291–319. ISSN 0311-5518

The palaeobiology of the Malay Archipelago region remains poorly documented, despite its present-day significance as a modern global marine biodiversity hotspot. The Togopi Formation of the Dent Peninsula, situated in Borneo on the western Sulu Sea and eastern coast of Sabah, Malaysia, preserves Plio-Pleistocene sedimentary sequences interpreted to represent localized transgressive episodes, and which have a relatively high coral diversity. Fossil corals were sampled from three available quarries on the Dent Peninsula, the sediments of which have been previously dated as 4.5–3.4?Ma in age based on foraminiferal data and radiometric analyses. These Pliocene corals are identified here based on their macromorphology, micromorphology and microstructural characteristics. In total, this study describes 28 fossil coral taxa, with 16 genera recognized and 22 taxa identified to species level, 21 of which can be confidently assigned to extant species. These new data have resulted in revised stratigraphic ranges for eight of these species. As the most comprehensive systematic survey of corals from the Pliocene of the Indo-Pacific to date, this study indicates a high diversity of corals on the margin of the Sabah Sea, Borneo, at this time, including taxa found today, thus casting doubt on the local impact of the Plio-Pleistocene extinction previously reported from faunal analyses of the central Indo-Pacific.

Jasmin V.M. Saw [varnmay@yahoo.com] Department of Petroleum Geosciences, Universiti Teknologi PETRONAS, 32610 Seri Iskandar, Perak, Malaysia; Aaron W. Hunter* [awh31@cam.ac.uk] Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK; Kenneth G. Johnson [k.johnson@nhm.ac.uk] Department of Earth Sciences, The Natural History Museum, Cromwell Road, London SW7 5BD, UK; Abdul Hadi B Abdul Rahman [hadi_rahman@utp.edu.my] Department of Petroleum Geosciences, Universiti Teknologi PETRONAS, 32610 Seri Iskandar, Perak, Malaysia. *Also affiliated with: School of Earth Sciences, The University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia.