Journal
LIMNOLOGY AND OCEANOGRAPHY
Volume 65, Issue 11, Pages 2688-2696Publisher
WILEY
DOI: 10.1002/lno.11541
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Funding
- River Fund [25-1215-023, 25-1263-017]
- KAKENHI Grant [18H02513]
- Eel River Critical Zone Observatory NSF [CZP EAR-1331940]
- National Center for Earth surface Dynamics, NSF Cooperative Agreement [EAR-0120914]
- Grants-in-Aid for Scientific Research [18H02513] Funding Source: KAKEN
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Radiocarbon natural abundance (Delta C-14) has emerged as a useful dietary tracer in freshwater ecology for the past decade, yet its applicability for separating aquatic and terrestrial resources has not been examined quantitatively. Here, we report Delta C-14 values of stream invertebrates in different functional feeding groups collected from the upper South Fork Eel River watershed, northern California. We found that algae-grazing insect larvae show low Delta C-14 values (-43.1 +/- 21.8 parts per thousand, mean +/- standard deviation,N = 6), reflecting the signal of dissolved inorganic carbon weathered from ancient inorganic carbon or respiration of old organic carbon. In contrast, the Delta C-14 values of leaf-shredding insect larvae (21.7 +/- 31.9 parts per thousand,N = 5) were close to those of contemporary atmospheric CO(2)except at the SF Eel River where algal production was highest. The Delta C-14 values of predators (-6.1 +/- 35.7 parts per thousand,N = 14) were intermediate between those of grazers and shredders. In a Bayesian mixing model, Delta C-14 provided a more ecologically realistic estimate for terrestrial vs. aquatic source contributions to invertebrates with lower uncertainty (i.e., narrower credible interval) than did the stable carbon isotopes (delta C-13). These results demonstrate that Delta C-14 can be used, in combination with delta C-13, to more precisely estimate organic matter sources to stream animals.
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