Information
about plant photosynthetic carbon assimilation, physiology,
and biochemistry is locked in the 18O/16O ratios
of the individual positions of higher plants carbohydrates but is
under-utilized, because of the difficulty of making these determinations.
We report the extension of the wet chemistry approach we used to access
the 18O/16O ratio of O-3 of glucose with a novel
GC/Pyrolysis/IRMS-based method, to determine the 18O/16O ratios of O-4, O-5, and O-6. The O atoms (OH groups) at
positions 1, 2, 5, and 6 of glucose were protected by acetonation
(converting to 1,2;5,6-di-O-isopropylidene-glucofuranose,
DAGF). The DAGF was then converted to 6-bromo-6-deoxy-1,2;3,5-di-O-isopropylidene-glucofuranose (6-bromoDAGF) with the simultaneous
removal of O-6 with N-bromosuccinimide and triphenylphosphine.
The DAGF was also methylated at O-3 with CH3I under the
catalysis of NaH to 3-methylDAGF, which was then deacetonated to 1,2-O-isopropylidene-3-O-methyl-glucofuranose
(3-methylMAGF). O-5 and O-6 were then removed as a whole from 3-methylMAGF
by I2 oxidization under the catalysis of Ph3P and imidazole. Isotope mass balance was then applied to calculate
the 18O/16O of O-5 and O-6 as a whole and O-6,
respectively. Sampling at different stages of substrate conversion
to product and applying a Rayleigh-type fractionation model were employed,
when quantitative conversion of substrate was unachievable to calculate
the δ18O of the converted substrate. Quantitative
conversion of glucose with phenylhydrazine to phenylglucosazone also
allowed for the calculation of δ18O2 by
applying isotope mass balance between the two. A C4 starch-derived
glucose intramolecular δ18O profile is now determined:
O-3 is relatively enriched (by 12.16 mUr), O-4 is relatively depleted
(by 20.40–31.11 mUr), and O-2 is marginally enriched (by 2.40
mUr) against the molecular average.