Controls of longitudinal variation in δ13C-DIC in rivers: A global meta-analysis
Controls of longitudinal variation in δ13C-DIC in rivers: A global meta-analysis
Previously Published Material: These findings are in review in the journal Ecosystems.
Abstract ID#: 36699
English Abstract:
Gas exchange between the water and the atmosphere strongly influences the δ13C signature of the inorganic carbon pool in large rivers. Because the δ13C signature of DIC at isotopic equilibrium with the atmosphere (δ13C-DICequilibrium) is dependent on pH and temperature, we were interested in determining if these physicochemical variables could be used to generate an isoscape, or a map of the stable isotope variation in DIC, in rivers. We conducted a literature survey to examine the relationship between δ13C-DIC and δ13C-DICequilibrium in rivers throughout the world. We then used generalized additive mixed models to investigate if deviations from δ13C-DICequilibrium (δ13C-DICdisequilibrium) and δ13C-DIC in lotic ecosystems were related to ecological variables including the partial pressure of dissolved CO2, elevation, and Strahler order. To evaluate if carbonate weathering or groundwater inflow was responsible for longitudinal variation in δ13C-DIC, we compared within-river trends in weathering products and groundwater inflow with within-river trends in δ13C-DIC in the main stem of 18 of the rivers. For more than 99% of the samples, DIC was more depleted in 13C than δ13C-DICequilibrium. The GAMMs revealed that, whereas morphometric variables (elevation, Strahler order) explained a large fraction of the variation in δ13C-DICdisequilibrium, morphometric and geochemical variables (DIC, pH, pCO2) explained a large fraction of the variation in δ13C-DIC. In all rivers with limited groundwater inputs, headwaters were isotopically heavier than downstream reaches, suggesting greater inputs of DIC from groundwater than from terrestrial ecosystems. Rivers with groundwater inflow in both upper and lower reaches had higher rates of change in δ13C-DIC than rivers where groundwater inflow was limited to lower reaches, indicating that rivers with groundwater inputs in headwaters will be more suitable for use of δ13C in analyses of the spatial ecology of consumers.
