For analysis of carbon isotope discrimination in wood, cellulose or holocellulose is often preferred to whole tissue because of the variability in isotopic composition of different wood components and the relative immobility of cellulose. Most currently used methods for the preparation of wood components for stable isotope analysis (e.g., the Jayme-Wise method) produce a residue of holocellulose. The Jayme-Wise method was initially developed to extract holocellulose from small (~1 g) samples of wood, and despite subsequent modifications, the method requires specialized glassware, considerable time, and entails the risk of sample loss. For carbon isotope analysis, we adapted an acid-catalyzed solvolytic method for preparing crude cellulose by treating wood meal with acidified di-glycol methyl ether (diglyme). The one-step process requires no special glassware, is complete within 24 hours, and enables over 100 samples to be processed in a day. This method gives similar δ13C values to the Jayme-Wise method for wood of Eucalyptus globulus Labill., Pinus radiata D. Don, and Pinus pinaster Ait. The relationship between δ13C of wood and crude cellulose is as strong as that observed between wood and α-cellulose and stronger than that observed between wood and holocellulose in other species. These relationships suggest that variation in δ13C of wood may result from hemicellulose and that analysis of stable carbon isotopes in crude cellulose is preferable. If the consistent -0.3‰ bias in the value of δ13C of cellulose resulting from residual lignin is corrected for, then the relationship between δ13C of wood and crude cellulose may be used to predict δ13C of cellulose from a small subsample. The method is well suited to species with low concentrations of extractives, but further testing is needed to assess its general applicability.
CITATION STYLE
Macfarlane, C., Warren, C. R., White, D. A., & Adams, M. A. (1999). A rapid and simple method for processing wood to crude cellulose for analysis of stable carbon isotopes in tree rings. Tree Physiology, 19(12), 831–835. https://doi.org/10.1093/treephys/19.12.831
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