Abstract
Several techniques are available to examine the isotopic composition of historic lake waters, providing data that can subsequently be used to examine environmental changes. A recently-developed technique is the stable oxygen isotope analysis of subfossil chironomid (Diptera: Chironomidae) head capsules (mostly chitin) preserved in lake sediments. This technique involves a high Temperature Conversion Elemental Analyzer (TC/EA), which has been a relatively recent addition to the suite of online peripherals for analyzing the stable isotopic composition of organic samples. The highly precise and accurate 18O/16O and D/H measurements obtainable using the TC/EA with samples in the microgram range make this instrumentation suitable for studying geochemical and biological processes. Preparation of organic samples for isotopic analysis typically requires first weighing each sample into silver/tin capsules. These capsules can introduce oxygen and hydrogen contamination (a “blank effect”), which is especially problematic for analysis of small organic samples (e.g. less than 100 μg). Here we tested tin and silver capsules from two manufacturers and a range of sizes to assess contamination to small organic samples on the TC/EA. We also assessed how a method for cleaning silver capsules affected our analysis of commercial chitin. In general, capsules made of silver have less detectible oxygen than those made of tin, and capsules from the two manufacturers varied in their detectible oxygen. There was no detectable H contamination from silver capsules. In addition to our empirical findings, we present a model demonstrating the influence that contaminant oxygen can have on the δ18O of small organic samples. Sample mass becomes an important issue for such analyses. In light of our findings, we recommend a minimum sample mass ≥50 μg (approximately 120 whole chironomid head capsules) on a TC/EA-IRMS (Deltaplus XP system). Finally, we present a detailed protocol for preparing and transferring chironomid head capsules into silver capsules that minimizes the influence of contaminant oxygen. This protocol provides the paleo-community with another potential method for reconstructing paleoenvironments.
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Acknowledgements
This research was supported by the National Science Foundation (NSF ESH-0317766 to Wooller) and the Alaska Stable Isotope Facility (ASIF) at the University of Alaska Fairbanks. The authors thank ASIF colleagues Tim Howe and Norma Haubenstock for their diligent work and valuable comments for experimental design and suggestions. We are grateful to participants and organizers, especially Dr. Ian Walker and Dr. Pete Landgon, at the international “Dead midges 2005 workshop” for stimulating encouragement for stable isotope applications on chironomid fossil heads. Thanks also to Dr. Yarrow Axford and Dr. Gifford Miller from the Institute for Arctic and Alpine Research (INSTAAR), Boulder, Colorado for valuable comments and support for method development in the early stages. We also thank Lena Krutikov and two anonymous reviewers for their constructive reviews of our paper.
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Wang, Y., Francis, D.R., O’Brien, D.M. et al. A protocol for preparing subfossil chironomid head capsules (Diptera: Chironomidae) for stable isotope analysis in paleoclimate reconstruction and considerations of contamination sources. J Paleolimnol 40, 771–781 (2008). https://doi.org/10.1007/s10933-008-9197-3
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DOI: https://doi.org/10.1007/s10933-008-9197-3