Silicon, oxygen and carbon isotope composition of wheat (Triticum aestivum L.) phytoliths: implications for palaeoecology and archaeology

By Martin John Hodson, A. Parker, M. Leng, H. Sloane. 2008

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A review of diatom δ18O in palaeoceanography (2009, background): “This problem may be exacerbated in the marine environment by the presence of other siliceous organisms such as radiolarians, sponges or phytoliths, the δO of which remains poorly understood (Mopper and Garlick, 1971; Matheney and Knauth, 1989; Webb and Longstaffe, 2003; Hodson et al., 2008).”
A Review of the Stable Isotope Bio-geochemistry of the Global Silicon Cycle and Its Associated Trace Elements (2018, background): “Rayleigh fractionation during the transportation of Si within plants also causes heavier isotopes to be concentrated within the xylem whilst lighter isotopes are preferentially deposited in phytoliths lower down the plant (Ding et al., 2005, 2008a,b; Opfergelt et al., 2006a,b; Hodson et al., 2008).”