Bioavailability of dissolved organic matter varies with anthropogenic landcover in the Upper Mississippi River Basin

Derrick R. Vaughn*, Anne M. Kellerman, Kimberly P. Wickland, Robert G. Striegl, David C. Podgorski, Jon R. Hawkings, Jaap H. Nienhuis, Mark M. Dornblaser, Edward G. Stets, Robert G.M. Spencer

*Corresponding author for this work

Research output: Contribution to journalArticleAcademicpeer-review

Abstract

Anthropogenic conversion of forests and wetlands to agricultural and urban landcovers impacts dissolved organic matter (DOM) within streams draining these catchments. Research on how landcover conversion impacts DOM molecular level composition and bioavailability, however, is lacking. In the Upper Mississippi River Basin (UMRB), water from low-order streams and rivers draining one of three dominant landcovers (forest, agriculture, urban) was incubated for 28 days to determine bioavailable DOC (BDOC) concentrations and changes in DOM composition. The BDOC concentration averaged 0.49 ± 0.30 mg L−1 across all samples and was significantly higher in streams draining urban catchments (0.72 ± 0.34 mg L−1) compared to streams draining agricultural (0.28 ± 0.15 mg L−1) and forested (0.47 ± 0.17 mg L−1) catchments. Percent BDOC was significantly greater in urban (10% ± 4.4%) streams compared to forested streams (5.6% ± 3.2%), corresponding with greater relative abundances of aliphatic and N-containing aliphatic compounds in urban streams. Aliphatic compound relative abundance decreased across all landcovers during the bioincubation (average -4.1% ± 10%), whereas polyphenolics and condensed aromatics increased in relative abundance across all landcovers (average of +1.4% ± 5.9% and +1.8% ± 10%, respectively). Overall, the conversion of forested to urban landcover had a larger impact on stream DOM bioavailability in the UMRB compared to conversion to agricultural landcover. Future research examining the impacts of anthropogenic landcover conversion on stream DOM composition and bioavailability needs to be expanded to a range of spatial scales and to different ecotones, especially with continued landcover alterations.

Original languageEnglish
Article number119357
Number of pages11
JournalWater Research
Volume229
DOIs
Publication statusPublished - 1 Feb 2023

Bibliographical note

Publisher Copyright:
© 2022 Elsevier Ltd

Funding

This work was supported by the U.S. Geological Survey (USGS) Biological Carbon Sequestration Program, the USGS National Research Program, the National Science Foundation NSF-EAR-GLD-1810855, and the American Chemical Society through PRF #59916-DNI8. The National High Magnetic Field Laboratory ICR User Facility is supported by the National Science Foundation Division of Chemistry through DMR-1644779 and the State of Florida.

FundersFunder number
National Science Foundation Division of ChemistryDMR-1644779
State of Florida
National Science FoundationNSF-EAR-GLD-1810855
U.S. Geological Survey
American Chemical Society59916-DNI8
National High Magnetic Field Laboratory

    Keywords

    • Bioavailability
    • Dissolved organic carbon
    • Dissolved organic matter
    • FT-ICR MS
    • Landcover

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