Carbon and nitrogen stable isotope ratios (δ13C and δ15N) have been used for more than two decades in analyses of food web structure. The utility of isotope ratio measurements is based on the observation that consumer δ13C values are similar (<1‰ difference) to those of their diet, while consumer δ15N values are about 3‰ higher than those of their diet. The technique has been applied most often to aquatic and aboveground terrestrial food webs. However, few isotope studies have examined terrestrial food web structure that includes both above- and belowground (detrital) components. Here, we review factors that may influence isotopic signatures of terrestrial consumers in above- and belowground systems. In particular, we emphasize variations in δ13C and δ15N in belowground systems, e. g., enrichment of 13C and 15N in soil organic matter (likely related to soil microbial metabolism). These enrichments should be associated with the high 13C (~3‰) enrichment in belowground consumers relative to litter and soil organic matter and with the large variation in δ15N (~6‰) of the consumers. Because such enrichment and variation are much greater than the trophic enrichment generally used to estimate consumer trophic positions, and because many general predators are considered dependent on energy and material flows from belowground, the isotopic variation in belowground systems should be taken into account in δ13C and δ15N analyses of terrestrial food webs. Meanwhile, by measuring the δ13C of key predators, the linkage between above- and belowground systems could be estimated based on observed differences in δ13C of primary producers, detritivores and predators. Furthermore, radiocarbon (14C) measurements will allow the direct estimation of the dependence of predators on the belowground systems.
- Above- and belowground
- Carbon and nitrogen stable isotopes
- Food webs
- Terrestrial ecosystem
ASJC Scopus subject areas
- Ecology, Evolution, Behavior and Systematics