Comment nommer les éléments? les catégories anthropologiques en afrique du sud

South African anthropology has been historically divided into two schools. One, associated with the Afrikaans-language universities, was favourable toapartheid. The other, associated with the English-language universities, was opposed to segregation and racial discrimination. Afrikaner anthropology focused on culture, tradition, and ethnicity, while the other school was committed to the study of South Africa as a single, rapidly changing society. This opposition has sometimes been exaggerated, and it was most significant during the period of highapartheid in the sixties and seventies but there has always been considerable debate over the very objects of anthropological research, and in particular about the nature of the «racial» and «tribal» groups in South Africa. These issues were politically of the greatest significance, forcing anthropologists to confront great questions about government policy. This paper traces the history of these debates on the classification of the peoples of Southern Africa.     

‘The Best-Laid Schemes o’ Mice an’ Men’? Proposals,Planning, Defeat,and Legacy,of Devolution in the 1970s*

The question of whether devolved assemblies should be established for Scotland and Wales dominated considerable parliamentary time in the 1970s and became a key pillar of the Labour government's legislative agenda after the two 1974 general elections. The main building blocks of the government's devolution proposals for Scotland and Wales were in place from 1975 with the publication of the white paper, Our Changing Democracy, which outlined proposals for a primary lawmaking assembly for Scotland and a Scottish executive, operating under a ‘conferred powers model of devolution’. For Wales, the assembly was to be a body corporate (with no split between executive and assembly) exercising only executive functions and able only to pass secondary legislation. With some important modifications (including crucially the requirement for a referendum, which was then further amended to require a Yes tally equating to 40% of the electorates in both nations), these proposals were eventually incorporated into law as the Scotland and Wales Acts 1978. While the political debates surrounding devolution in this period are well known, less attention has been paid to the practical plans undertaken by the civil service for devolution to become a reality. Considerable time was spent drawing up, from an early stage, detailed preparations for devolution, particularly in Scotland. In Wales, planning was more tentative, yet, none the less, was taken seriously by the Welsh Office. These plans never materialised in the way envisaged, with neither Welsh nor Scottish devolution able to pass the referendum thresholds put in place. However, as this article also demonstrates, both the Scotland and Wales Acts had a constitutional legacy when devolution became reality under New Labour in the late 1990s.     

Record of the meso- and neoholocene palaeoenvironmental changes in the Jesionowa landslide peat bog (Beskid Sądecki MTS. Polish Outer Carpathians)

The paper presents an analysis of depositional sequences of landslide peat bog situated in the depressions developed within the landslide landforms Jesionowa in the Beskid Sądecki Mts. (Outer Carpathians). The peat bog, with depositional sequence 2.80 m long, started to form at the beginning of the Atlantic Phase ca. 6390–5910 cal BC. Palynological and lithological analyses as well as several (14) radiocarbon age determinations of different horizons in the sediments enabled the reconstruction of palaeoenvironmental changes during the Meso-and Neoholocene. The increase in climate humidity at the beginning of the Subboreal and Subatlantic Phases was observed as delivery of minerogenic material to the peat bog basin and formation of a mineral horizon and an illuvial level within the peat. The particularly intensive delivery of allochthonous material to the peat bog took place at the beginning of the Subboreal Phase and was the result of both significant humid climate and increased human impact (colonization of the Funnel Beaker Culture) in the landslide area. Similar influence of younger colonisations of landslide area (Przeworsk Culture and, later, Valachian colonisation) was also recorded within the deposits of peat bog (illuvial and mineral horizons) in the early Subatlantic Phase. Rejuvenation of the landslide zone and formation of the younger landslide were connected with the increase in climate humidity at the beginning of the Subboreal Phase. The peat bog deposits situated within this younger landslide, which are ca. 1.8 m thick, are significantly contaminated with mineral material.