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  Légère, Anne, Ph.D. - A...  
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Légère, A. (2009). « La malherbologie au coeur des enjeux du XXIe siècle1. », Phytoprotection, 90, p. 5-11.
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Légère, A. (2009). "Weed science at the core of 21st century issues.", Phytoprotection, 90, pp. 5-11.
  La malherbologie au coe...  
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La malherbologie au coeur des enjeux du XXIe siècle1.
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Weed science at the core of 21st century issues.
  Un siècle de science - ...  
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Que peut-on lui demander de mieux? Bien d'autres choses, répondent les coprésidents d'un organisme scientifique canadien qui a étudié pendant trois ans le potentiel de la pomme de terre au XXIe siècle.
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"The introduction of the Shepody potato is one of the contributing factors in the success of McCain Foods," says Dr. Yves Leclerc, the company's head of agronomy. "The variety's adaptability to various environments has allowed our company to expand our global activity and provide customers around the world with quality product." Leclerc says the short-season Shepody allowed farmers and processors north of the border to compete with their American counterparts for the lucrative fast-food market.
  Société ITOCHU - Agricu...  
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Attendu que ITOCHU est une société commerciale japonaise de premier plan, intégrée mondialement, qui exerce ses activités dans des secteurs très variés tels le textile, la machinerie, l'aérospatiale, les technologies de l'information, les métaux, l'énergie, les produits chimiques, les produits forestiers, la vente au détail, les services financiers et autres, et qui, dernièrement, a fait des aliments et de l'agrobiotechnologie ses principales priorités du XXIe siècle.
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Whereas, ITOCHU is Japan's leading general trading company and globally integrated corporation, highly diversified with interests in textiles, machinery, aerospace, information technology, metals, energy, chemicals, forest products, retail, financial services and others, that has recently positioned food as well as agriculture biotechnology as its key priorities in the 21st century. The Innovative Technology Business Development Office, Corporate Planning Group focuses on Agri-Food Bio business, including Functional foods, Biomedical information, Regenerative medicine and Nanotechnology;
  Evaluating the quantity...  
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D’ici la fin du XXIe siècle, le réchauffement prévu qui pourrait atteindre 8 °C dans la zone du pergélisol circumpolaire fera augmenter l’épaisseur de la couche active et libérera le C que le gel protégeait auparavant contre la dégradation microbienne.
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Turbic Cryosols contain almost 80% of the soil organic carbon (C) in the Canadian Arctic. Predicted warming of up to 8 °C in the circumpolar permafrost zone by the end of the 21st century will increase the thickness of the active layer and release C that was previously protected from microbial degradation by freezing. Little is known about the disposition, biochemical composition, and potential biodegradability of this soil organic matter (SOM). In this study we characterized SOM in the active layer and near-surface permafrost in three Turbic Cryosols in the Northwest Territories, Canada. We used physical (size fractionation), chemical (sequential cold- and hot-water extraction), and biological (100-d bioassay for mineralizable C) methods to estimate the quantities of labile SOM. Soil C and N storage in the profiles (measured to 70–110 cm) ranged from 15 to 46 kg C m-2 and 1.3 to 3.1 kg N m-2, with 16 to 78% contained in horizons with cryoturbation features and 4 to 66% in perennially frozen horizons. The concentrations of C and N in the whole soil and all fractions typically declined with depth. The proportion of total C and N in particulate organic matter in horizons with cryoturbation features was large (usually > 30%) compared to other ecosystems, whereas that in the water extracts was < 5%, and the fraction of potentially mineralizable C was < 2%. The contribution of C and N to the total storage in each SOM fraction in the perennially frozen horizons with cryoturbated features was generally larger than that observed in mineral horizons of the active layer with cryoturbated features. Our results suggest that the amount of labile SOM in horizons with cryoturbation features is small and that the relative bioavailability of SOM in near surface permafrost horizons with cryoturbated features is similar or greater than the SOM in the active layer horizons with cryoturbated features.