4.6 Article

How humans alter dissolved organic matter composition in freshwater: relevance for the Earth's biogeochemistry

Journal

BIOGEOCHEMISTRY
Volume 154, Issue 2, Pages 323-348

Publisher

SPRINGER
DOI: 10.1007/s10533-021-00753-3

Keywords

Dissolved organic matter composition; Climate change; Land use change; Biogeochemical processes; Ecosystem function

Funding

  1. Canada's Natural Sciences and Engineering Council (NSERC) Discovery Grant
  2. NSERC Undergraduate Student Research Award
  3. U.S. National Science Foundation [1754363]
  4. Division Of Environmental Biology
  5. Direct For Biological Sciences [1754363] Funding Source: National Science Foundation

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Dissolved organic matter (DOM) is crucial in freshwater ecosystems, but its composition can be altered by human activities, impacting processes like carbon outgassing, nutrient cycles, ecosystem metabolism, and drinking water quality in contrasting ways. Understanding the links between DOM properties and biogeochemical dynamics is essential for addressing future environmental challenges.
Dissolved organic matter (DOM) is recognized for its importance in freshwater ecosystems, but historical reliance on DOM quantity rather than indicators of DOM composition has led to an incomplete understanding of DOM and an underestimation of its role and importance in biogeochemical processes. A single sample of DOM can be composed of tens of thousands of distinct molecules. Each of these unique DOM molecules has their own chemical properties and reactivity or role in the environment. Human activities can modify DOM composition and recent research has uncovered distinct DOM pools laced with human markers and footprints. Here we review how land use change, climate change, nutrient pollution, browning, wildfires, and dams can change DOM composition which in turn will affect internal processing of freshwater DOM. We then describe how human-modified DOM can affect biogeochemical processes. Drought, wildfires, cultivated land use, eutrophication, climate change driven permafrost thaw, and other human stressors can shift the composition of DOM in freshwater ecosystems increasing the relative contribution of microbial-like and aliphatic components. In contrast, increases in precipitation may shift DOM towards more relatively humic-rich, allochthonous forms of DOM. These shifts in DOM pools will likely have highly contrasting effects on carbon outgassing and burial, nutrient cycles, ecosystem metabolism, metal toxicity, and the treatments needed to produce clean drinking water. A deeper understanding of the links between the chemical properties of DOM and biogeochemical dynamics can help to address important future environmental issues, such as the transfer of organic contaminants through food webs, alterations to nitrogen cycling, impacts on drinking water quality, and biogeochemical effects of global climate change.

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