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1.
20 p, 1.1 MB Climate change and inter-connected risks to sustainable development in the Mediterranean / Cramer, Wolfgang (Institut Méditerranéen de Biodiversité et d'Ecologie marine et continentale) ; Guiot, Joël (Aix-Marseille Université) ; Fader, Marianella (Unesco. International Centre for Water Resources and Global Change) ; Garrabou, Joaquim (Institut de Ciències del Mar) ; Gattuso, Jean-Pierre (Laboratoire d'Océanographie de Villefranche-sur-Mer) ; Iglesias, Ana (Universidad Politécnica de Madrid. Departamento de Economía Agraria) ; Lange, Manfred A. (Cyprus Institute. Energy, Environment and Water Research Center) ; Lionello, Piero (Università del Salento. Dipartimento di Scienze e Tecnologie Biologie ed Ambientali) ; Llasat, Maria Carmen (Universitat de Barcelona. Departament de Física Aplicada) ; Paz, Shlomit (University of Haifa. Department of Geography and Environmental Studies) ; Peñuelas, Josep (Centre de Recerca Ecològica i d'Aplicacions Forestals) ; Snoussi, Maria (Université Mohammed V. Faculté des Sciences) ; Toreti, Andrea (Comissió Europea) ; Tsimplis, Michael N. (Hong Kong City University. School of Law) ; Xoplaki, Elena (Justus-Liebig Universität Gießen. Department of Geography)
Recent accelerated climate change has exacerbated existing environmental problems in the Mediterranean Basin that are caused by the combination of changes in land use, increasing pollution and declining biodiversity. [...]
2018 - 10.1038/s41558-018-0299-2
Nature climate change, Vol. 8, issue 11 (Nov. 2018) , p. 972-980  
Detailed record -
2.
11 p, 1.4 MB Constraints on alluvial clay mineral assemblages in semiarid regions. The Souss Wadi Basin (Morocco, Northwestern Africa) / Elmouden, A. (Université Ibn Zohr. Faculté des Sciences Laboratoire de Géologie Appliquée et Géo-Environnement (LAGA GE)) ; Bouchaou, L. (Université Ibn Zohr. Faculté des Sciences Laboratoire de Géologie Appliquée et Géo-Environnement) ; Snoussi, M. (Université Mohamed V. Département de Géologie)
Illite, chlorite and kaolinite, resulting directly from substratum weathering, dominate the clay assemblages recorded in altered rocks and soils of the Souss Wadi watershed. Nevertheless, the transformation and neoformation of diverse clay minerals, which is mainly controlled by changing climatic, lithological and topographic conditions, enables one to establish three distinctive source areas. [...]
2005 - 10.1344/105.000001410
Geologica acta, Vol. 3, Núm. 1 (2005) , p. 3-13  
Detailed record - Creative Commons

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1 Snoussi, Maria
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