@article{FrickSchuesslerSommeretal.2018,
  author    = {Frick, Daniel Alexander and Sch{\"u}ßler, Jan Arne and Sommer, Michael and von Blanckenburg, Friedhelm},
  title     = {Laser Ablation In Situ Silicon Stable Isotope Analysis of Phytoliths},
  series = {Geostandards and geoanalytical research},
  volume    = {43},
  journal   = {Geostandards and geoanalytical research},
  number    = {1},
  publisher = {Wiley},
  address   = {Hoboken},
  issn      = {1639-4488},
  doi       = {10.1111/ggr.12243},
  pages     = {77 -- 91},
  year      = {2018},
  abstract  = {Silicon is a beneficial element for many plants and is deposited in plant tissue as amorphous bio-opal called phytoliths. The biochemical processes of silicon uptake and precipitation induce isotope fractionation: the mass-dependent shift in the relative abundances of the stable isotopes of silicon. At the bulk scale, delta Si-30 ratios span from -2 to +6 parts per thousand. To further constrain these variations in situ, at the scale of individual phytolith fragments, we used femtosecond laser ablation multi-collector inductively coupled plasma-mass spectrometry (fsLA-MC-ICP-MS). A variety of phytoliths from grasses, trees and ferns were prepared from plant tissue or extracted from soil. Good agreement between phytolith delta Si-30 ratios obtained by bulk solution MC-ICP-MS analysis and in situ isotope ratios from fsLA-MC-ICP-MS validates the method. Bulk solution analyses result in at least twofold better precision for delta Si-30 (2s on reference materials <= 0.11 parts per thousand) over that found for the means of in situ analyses (2s typically <= 0.24 parts per thousand). We find that bushgrass, common reed and horsetail show large internal variations up to 2 parts per thousand in delta Si-30, reflecting the various pathways of silicon from soil to deposition. Femtosecond laser ablation provides a means to identify the underlying processes involved in the formation of phytoliths using silicon isotope ratios.},
  language  = {en}
}