In: Plant and Cell Physiology, 2008, vol. 49, no. 4, p. 557-569
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In: Monthly Notices of the Royal Astronomical Society, 2010, vol. 409, no. 1, p. 48-65
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In: Human Molecular Genetics, 1999, vol. 8, no. 7, p. 1169-1176
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In: Medical Mycology, 2011, vol. 49, no. 2, p. 132-142
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In: Bulletin of the Geological Society of America, 2013, vol. 125, no. 1-2, p. 89-108
Prior to their Alpine overprinting, most of the pre-Mesozoic basement areas in Alpine orogenic structures shared a complex evolution, starting with Neoproterozoic sediments that are thought to have received detrital input from both West and East Gondwanan cratonic sources. A subsequent Neoproterozoic–Cambrian active margin setting at the Gondwana margin was followed by a Cambrian–Ordovician...
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In: Swiss Journal of Geosciences, 2011, vol. 104, no. 1, p. 67-79
The pre-Mesozoic, mainly Variscan metamorphic basement of the Col de Bérard area (Aiguilles Rouges Massif, External domain) consists of paragneisses and micaschists together with various orthogneisses and metabasites. Monazite in metapelites was analysed by the electron microprobe (EMPA-CHIME) age dating method. The monazites in garnet micaschists are dominantly of Variscan age (330–300 Ma)....
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In: Plant and Cell Physiology, 2008, vol. 49, no. 4, p. 557-569
The enormous metabolic plasticity of plants allows detoxification of many harmful compounds that are generated during biosynthetic processes or are present as biotic or abiotic toxins in their environment. Derivatives of toxic compounds such as glutathione conjugates are moved into the central vacuole via ATP-binding cassette (ABC)-type transporters of the multidrug resistance-associated protein...
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