Illusions of revolution: François Furet's critique of Marx

In this article it will be argued that François Furet's attempt in Interpreting the French Revolution to provide a conceptual history of the French Revolution through a synthesis of Tocqueville and Cochin's historical and sociological accounts fails methodologically. It does so in two ways: Firstly, in its aim to distinguish between conceptual, explanatory history and empirical, narrative history, and secondly, in its distinction between revolution as process and revolution as act. Drawing on Claude Lefort and Paul Ricoeur's interventions in the historiographical debate, I demonstrate that these seemingly methodological concerns, conceal a deeper historical and political question concerning the nature of the ‘event’ of revolution. In response to Furet's oblique turn to Hegel in his later work, this article traces the nature of the ‘conceptual inversion’ Furet claims to find in Hegel and Marx's accounts of the French Revolution. In relation to Marx, it is argued that Furet's critique fails to capture the allegorical nature of the political in Marx's thought, and underplays the significance of revolution as the basis for both the separation of the social and the political and their attempted unity. The article ends with some remarks on the importance of language and culture in rethinking the relationship between Hegel and Marx.     

Variabilité et fréquence des cycles de gel‐dégel dans la région de Québec, 1977–2006

Freeze‐thaw cycles are most common at the beginning or near the end of the winter season. These cycles have various effects on the ecosystems of Eastern Canada, affecting both biotic and abiotic components of temperate cold environments. Using air temperature minima and maxima from four meteorological stations close to Québec City, we determined the frequency of daily freeze‐thaw cycles for the last 30 years. The results show no significant increase in the number of freeze‐thaw cycles despite a small increase in air temperature. Polynomial curves describing the relationship between mean air temperatures and the number of freeze‐thaw cycles were calculated. Based on these equations and anticipating a climate change scenario, we projected future freeze‐thaw cycles. Assuming a 5 °C increase in mean air temperatures by 2100, we estimated that the number of days with a freeze‐thaw cycle could increase by approximately 20 days per winter. The increase in the number of such cycles will be concentrated during the coldest months of the winter (January and February).