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  • l'argument d'autochtonie apporte aux dynamiques de négociation entre acteurs. Ils en relatent la chronologie dans un pays où elle n'a pas cessé d'être manipulée et modelée au gré des discours dominants sur la société et la nation.
  • 2012
  • [b1] UMR 151 IRD - LPED Centre Saint Charles Case 10, MARSEILLE, France
  • The interactions between all neighbouring organisms : The roles of Charles Darwin, Ernst Haeckel and Eugenius Warming in the evolution of ideas on plant dynamics
  • 2012
  • John Shary, Charles Pease, and contested irrigation landscapes in early-twentieth-century South Texas
  • 2012
  • 2012
  • [b4] Charles Darwin Univ., Northern Territory, Darwin, Australie
  • Asie ; Changement social ; Crise économique ; Domination ; Géographie politique ; Géopolitique ; Monde ; Monde arabe ; Pouvoir ; Relations internationales ; Rôle de l'Etat
  • Arab World ; Asia ; Domination ; Economic crisis ; Geopolitics ; International relations ; Political geography ; Power ; Role of the State ; Social change ; World
  • ‘shatter belt’ known by contemporary crises and similar processes in the near past. The western economic and military forces are perhaps loosing the role of key-factor in the area. In the near future, Asiatic powers might play a dominant role. - (IKR)
  • 2012
  • Différence entre sexes ; Domination ; Espace ; Genre ; Géographie sociale ; Relations sociales ; Société
  • Domination ; Gender ; Gender difference ; Social geography ; Societal relations ; Society ; Space
  • 2012
  • 2012
  • [b3] School of Humanities and Social Sciences, Charles Sturt Univ., Wagga Wagga, Australie
  • 2012
  • [b1] Department of Social Geography and Regional Development, Faculty of Science, Charles Univ., Praha, Tcheque, Republique
  • 2012
  • [b1] Inst. de sociologie, Fac. des Sciences sociales, Univ. Charles, Prague, Tcheque, Republique
  • 2012
  • [b1] Dept. of Social Geography and Regional Development, Charles Univ., Praha, Tcheque, Republique
  • L’A. propose une approche géohistorique de la province de Guipúzcoa et analyse le rôle des rois Ferdinand le Catholique et de Charles Premier d’Angleterre dans la guerre de Navarre entre 1512-1524. Il étudie la présence espagnole dans les Conciles
  • 2012
  • ) is the dominant clay mineral and was mainly inherited from the parent sediments and by neoformation. The pedons located in the highest points of the alluvial plain were classified as Chromic Haploxererts and those in the lowest landscape were classified as Typic
  • Haploxererts. The properties of these Vertisols reflect the impact of climate (alternating wet–dry periods), landscape position (alluvial plain; seasonally water saturated), and parent material (clayey, smectite-dominated fluvio-lacustrine, highly calcareous
  • 2012
  • structures, and degree of segregation between siliciclastic and bioclastic particles, facies analysis revealed 10 facies grouped into 5 associations. They suggest the occurrence of either wave or current dominated environments, showing different degrees
  • of heterolithic segregation between siliciclastic and bioclastic particles. The depositional system was characterised by a gentle sloping profile irregularly undulated by syndepositional gentle folds. Waves dominated the shallowest areas of the mixed system
  • and the terrigenous fraction derived mainly from wave erosion of substrate (arenaceous) rocks. In the deepest sector of the system (offshore), pervasive bioturbation dominated causing unsegregation of the siliciclastic and bioclastic fractions. - (NF)
  • 2012
  • content, and plant macronutrients were compared between sites where casuarinas dominated versus sites where casuarinas were absent. A multivariate ordination showed that casuarina-dominated soils were more similar to one another than to non-casuarina soils
  • . Thus, soil characteristics from casuarina-dominated areas appear to differ from comparable habitats devoid of casuarinas. There are at least 2 possible explanations : certain soil properties may have been more conducive to casuarina invasions
  • 2012
  • river sediment load data showed that the dissolved load dominated sediment transport prior to August 2005 with a switch to the dominance of bedload transport, post-dambreak. The higher post-dambreak bedload rates were particularly evident during
  • the first years after the dam failure due to significant coarse material coupling between active sediment sources (undercut banks/talus cones) and the Partnach River. In the last years of the observation period (2009 and 2010) the dominance of dissolved load
  • 2012