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Carbon, Nitrogen and Oxygen Stable Isotope Ratios in Chitin

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Chitin

Part of the book series: Topics in Geobiology ((TGBI,volume 34))

Abstract

Stable isotope ratios in chitin are firmly imprinted during biopolymer biosynthesis and reflect dietary, metabolic, and environmental influences. Chitin is a chemically complex amino sugar biopolymer that also includes non-amino-sugar moieties with contrasting isotopic compositions. Reproducible N, C, O-stable isotope determinations should rely on a chemically purified chitin substrate with limited non-amino-sugar contributions. Insecta, Crustacea and Merostomata are not distinguished by systematic isotopic differences. δ13C, δ15N and δ18O values of arthropod chitins show a few ‰ variance within a single individual (lobster), among individuals within a population, along ecdysis (i.e., molting), and age, as long as growth is not accompanied by strong dietary or behavioral changes. Marine arthropod chitin averages 9.1‰ more 13C-enriched than terrestrial chitin. δ15N values of chitin become more positive with increasing trophic level. Although δ18Ochitin from a large array of aquatic crustacean species across many ecosystems expresses only weak overall correlation with δ18Owater and no clear dependence on temperature, a more careful selection of specific modern insect fauna or preserved insect chitin from sediments yields δ18Ochitin values that are useful for reconstructing the isotopic composition of paleoenvironmental water, and for constraining paleohumidity and paleotemperatures. Experimental oxic and anoxic heating and partial biodegradation of chitin in marine anoxic mud and in terrestrial oxic soils did not result in any significant C, N, O-isotopic shifts in the preserved amino sugar. Chemically preserved archeological chitin was found to be isotopically compatible with modern chitin from comparable environments. New analytical stable isotope techniques with reduced sample size requirements open opportunities to utilize geologically preserved chitin in paleoenvironmental studies.

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Acknowledgements

Expert advice and contributions were provided by Drs. Hideyuki Doi, Randy F. Miller, John E. Motz, Teresa M. Tibbets, and Matthew Wooller. I gratefully acknowledge support from the U.S. Department of Energy, Basic Energy Sciences Research Grant number DEFG02-00ER15032, and from National Science Foundation grant OCE-0550295. Several figures were adapted and re-drawn, and accompanying text was reproduced from earlier publications, with permission from (1) American Chemical Society Symposium Series 1998, 707, 226–242 (© 1998 American Chemical Society), (2) Contributions in Marine Science 1986, 29, 113–130 (© 1986 Marine Science Institute of the University of Texas at Austin), and from (3) the dissertation of John E. Motz 2000 (© 2000 John E. Motz).

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Schimmelmann, A. (2011). Carbon, Nitrogen and Oxygen Stable Isotope Ratios in Chitin. In: Gupta, N. (eds) Chitin. Topics in Geobiology, vol 34. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-9684-5_4

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