ISRR 2018

Silicon Deposition in Roots and its Possible Functions

Alexander Lux 1,2 Boris Bokor 1,2 Marek Vaculik 1 Milan Soukup 1,4 Miroslav Svec 5 Philip J. White 3,6 Jana Kohanova 1 Marieluise Weidinger 7
1Department of Plant Physiology, Faculty of Natural Sciences, Comenius University in Bratislava, Ilkovičova 6, 84215 Bratislava, Slovakia
2Comenius University Science Park, Ilkovičova 8, 841 04 Bratislava, Comenius University in Bratislava, Slovakia
3The James Hutton Institute, Ecological Sciences, Invergowrie, Dundee DD2 5DA, UK
4Institute of Chemistry, Slovak Academy of Sciences, Dubravska cesta 9, 845 38 Bratislava
5Department of Genetics, Faculty of Natural Sciences, Comenius University in Bratislava, Ilkovičova 6, 84215 Bratislava, Slovakia
6Distinguished Scientist Fellowship Programme, King Saud University, Riyadh 11451, Saudi Arabia
7Core Facility of Cell Imaging and Ultrastructure Research, University of Vienna, Althanstrasse 14, 1090 Wien / Vienna, Austria

Silicon (Si) is a mysterious element in plants. It is not considered to be an essential element, but its tissue concentration can exceed that of many essential elements in some plant species and many studies show that it alleviates abiotic and biotic stresses. This occurs even in evolutionary distant species, from the most primitive to the most advanced. In the majority of these species the root takes up Si and transports it to aboveground organs. In addition, in some plant species root tissues are also sites of high Si accumulation. Three different modes of Si deposition in roots have been identified: (1) impregnation of tertiary endodermal cell walls (e.g. in cereals, such as Triticum [wheat] and Oryza [rice], and bamboos); (2) formation of Si-aggregates associated with endodermal cell walls (e.g. in the Andropogoneae family, which includes Sorghum and Saccharum [sugarcane]); (3) formation of Si aggregates in “stegmata” cells, which form a sheath around sclerenchyma fibres in some palm species (e.g. Phoenix [date palm]). In addition to differences in its location, the ratio of mineral to organic Si in roots also varies between plant species. However, despite differences in the magnitude and location of Si accumulation among plant species, phylogenetic analysis indicates high sequence homology of Si transporters. In this presentation, the various forms of Si deposition in roots will be illustrated together with relative transcript quantification of Si transporters; their functions and possible roles in stress resistance will be discussed.

Acknowledgement

The work was supported by Slovak Research and Development Agency under the Contract APVV-15-0156 and APVV SK-AT 2015-0009.









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