Howden Church

Shrewsbury's late sixteenth-century Old Market Hall—recently restored and returned to public use—is among the most prominent buildings in the town centre and, or so it would seem, a reminder of the town's pre-eminence as a marketing centre in the central Marches in the early modern period. Combining documentary evidence, archaeology, and the evidence of the building itself, this inter-disciplinary study sets out to examine the real reasons for the Hall's construction, how it was built, and the way in which it functioned. The paper also looks backwards to the growth of marketing in this part of Shrewsbury in the thirteenth century, and its promotion by considerable civic investment in the 1260s when a new market square was created from what was previously a wet wasteland. Looking forward, it tells the story of the Hall's use in the post- medieval period, and of past attempts to deal with inherent structural defects in the original design.     

“.. . And Jill came tumbling after”

Milan Stuchlik. Life on a Half Share: Mechanisms of Social Recruitment among the Mapuche of Southern Chile. New York: St. Martin's Press, 1976. 222 pp. Maps, illustrations, tables, figures, and bibliography. $25.00.     

Studying healing practices by geographical region

Parsons, Claire D., ed. Healing Practices in the South Pacific. The Institute for Polynesian Studies. Distributed by University of Hawaii Press, Honolulu, Hawaii, 1985. xiv + 250 pp. including references, index and maps. $22.50 cloth.

du Toit, Brian M., and Ismail H. Abdalla, eds. African Healing Strategies. New York: Trado‐Medic Books, 1985. x + 279 pp. including chapter references, and illustrations. $39.95 cloth, $20.00 paperback.     

Holocene land-use evolution and associated soil erosion in the French Prealps inferred from Lake Paladru sediments and archaeological evidences

A source-to-sink multi-proxy approach has been performed within Lake Paladru (492 m a.s.l., French Prealps) catchment and a 6-m long sediment sequence retrieved from the central lacustrine basin. The combination of minerogenic signal, specific organic markers of autochthonous and allochthonous supply and archaeological data allows the reconstruction of a continuous record of past human disturbances. Over the last 10,000 years, the lacustrine sedimentation was dominated by autochthonous carbonates and the watershed was mostly forest-covered. However, seven phases of higher accumulation rate, soil erosion, algal productivity and landscape disturbances have been identified and dated from 8400 to 7900, 6000 to 4800, 4500 to 3200, 2700 to 2050 cal BP as well as AD 350–850, AD 1250–1850 and after AD 1970. Before 5200 cal BP, soil erosion is interpreted as resulting from climatic deterioration phases towards cooler and wetter conditions. During the Mid-Late Holocene period, erosion fluxes and landscape disturbances are always associated with prehistorical and historical human activities and amplified by climatic oscillations. Such changes in human land-used led to increasing minerogenic supply and nutrients loading that affected lacustrine trophic levels, especially during the last 1600 years. In addition, organic and molecular markers document previously unknown human settlements around Lake Paladru during the Bronze and the Iron Ages.     

Spreading of Innovative Technical Traits and Cumulative Technical Evolution: Continuity or Discontinuity?

This paper questions the spreading of techniques considered as advantageous when measured in terms of energetic efficiency. A present-day case study, in which techniques do not spread, is used to highlight a transmission model that can be used to understand the spread of technical systems in terms of demic or cultural processes. The model is then applied to the spread of the potter’s wheel in the second and third millennium bc in the southern and northern Levant. Results show that both demic and cultural processes explain how the potter’s wheel became prevalent in the Levant. The selective forces are discussed by comparing the ceramic production contexts. We conclude that technical evolution is regulated by social mutations, i.e., major discontinuities.