Dissolved Carbon Export by Large River Systems Is Influenced by Source Area Heterogeneity

Rivers and streams export inorganic and organic carbon derived from contributing landscapes and so downstream carbon fluxes are important quantitative indicators of change in ecosystem function and for the full accounting of terrestrial carbon budgets. Carbon concentration-discharge (C-Q) relationships in rivers provide important information about carbon source and behavior in watersheds and are useful for estimating carbon export. However, C-Q relationships are complex in large river systems because of spatial and temporal heterogeneity in carbon dynamics across the watershed and river networks. We quantified dissolved organic carbon (DOC) and dissolved inorganic carbon (DIC) fluxes in the Upper Mississippi River basin and investigated their relationships with land cover and hydrology. The magnitude of dissolved carbon yields ranged widely among stations, 0.6-5.7 g DOC m(-2) yr(-1) and 2.9-11.8 g DIC m(-2) yr(-1). Spatial patterns in carbon fluxes were strongly related to land cover, with agricultural sites having high DIC/low DOC exports and forested and wetland areas having the opposite. DIC was always negatively related to discharge (Q), while the DOC-Q relationship varied with land cover. Differential behavior of carbon across the basin resulted in Q having a weak relationship with DOC and DIC at the basin outlet. Hence, there is a need to improve understanding of headwater terrestrial-to-aquatic carbon connections in order to improve basin-to-continental-scale carbon export estimates. Our results demonstrate that quantitative understanding of carbon export by large rivers can be improved by incorporating stream network information, such as the timing, location, and source of constituent flux, rather than relying solely upon relationships between constituent behavior and seasonality or discharge at the basin outlet.

Automated summary

Rivers and streams play an important role in carbon export from contributing landscapes, and carbon fluxes downstream serve as important quantitative indicators for ecosystem function and carbon budgets. The relationships between carbon concentration-discharge (C-Q) in rivers provide valuable information about carbon source and behavior in watersheds, but are complex in large river systems due to spatial and temporal heterogeneity. This study examined dissolved organic carbon (DOC) and dissolved inorganic carbon (DIC) fluxes in the Upper Mississippi River basin and found significant relationships with land cover and hydrology. Carbon export was influenced by land cover, with agricultural sites exporting more DIC and forested/wetland areas exporting more DOC. Understanding the carbon connections from headwaters to aquatic systems is crucial for accurate carbon export estimates.