C Signatures Differently Even in Closely Related Soil Fauna

1. Studies of stable isotope signatures can reveal and quantify trophic carbon transfer between organisms. However, preservation of the samples before analysis cannot always be avoided. Some preservation agents are known to alter tissue δ 13 C values considerably, but we do not yet understand how variation in such preservation artifacts may be determined by variation in body traits of different invertebrate species and life stage. 2. Here we tested the effect of four different preservation methods on 13 C signatures of two morphologically and ecologically distinct springtails, Folsomia candida and Orchesella cincta. These springtails were fed on the fungus Cladosporium cladosporioides grown on either a C3 or C4 carbon source, resulting in springtails with two contrasting initial δ 13 C values. Subsequently these springtails were preserved for 46 days. In addition a juvenile-adult comparison was made for F. candida. 3. Freeze-drying and subsequent dry storage did not affect 13 C signatures of either species; neither did killing springtails with liquid nitrogen and storing them at-80°C. Preservation in 70% ethanol slightly depleted δ 13 C values of adult F. candida but not of O. cincta. In contrast, storage in saturated salt solution depleted both species considerably. Life stage affected preservation success significantly; storage in 70% ethanol depleted adult F. candida but not its juveniles. Initial δ 13 C values of the springtails did not interact with preservation artifacts, suggesting that the shifts in δ 13 C values are caused by effects of the preservative on the animal tissue rather than by its remainders. 4. We recommend freezing-drying as a preservation method. However, our results suggest that inter-specific differences (e.g. in body size, cuticle thickness) as well as intra-specific difference (e.g. life stage dependent changes in the proportion of fat reserves) are important determinants of preservation effects on 13 C signatures. This makes interpreting stable isotope data obtained from preserved springtails relatively difficult, especially when natural 13 C abundances are used to study trophic interactions or interspecific functional differences. We predict that such complications also apply to other invertebrate taxa and types.