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Updated: Feb 15, 2026

Understanding Dissolved Organic Matter Biogeochemistry Through In Situ Nutrient Manipulations in Stream Ecosystems
Published on: October 29, 2016
Unifying Concepts Linking Dissolved Organic Matter Composition to Persistence in Aquatic Ecosystems
Anne M Kellerman1, François Guillemette1, David C Podgorski1
1National High Magnetic Field Laboratory Geochemistry Group and Department of Earth, Ocean, and Atmospheric Science , Florida State University , Tallahassee , Florida 32306 , United States.
Dissolved organic matter (DOM) composition influences aquatic carbon cycling. Molecular structure, isotopes, and optical properties reveal DOM
Area of Science:
- Environmental Chemistry
- Biogeochemistry
- Organic Geochemistry
Background:
- The composition and reactivity of dissolved organic matter (DOM) are critical for understanding aquatic systems' role in the global carbon cycle.
- However, unifying concepts that explain the molecular composition of DOM remain elusive.
- Aquatic DOM originates from both external (allochthonous) and internal (autochthonous) sources, each with distinct characteristics.
Purpose of the Study:
- To establish unifying concepts for the molecular composition of DOM.
- To link DOM composition to its reactivity and role in the carbon cycle.
- To investigate how DOM composition varies across diverse aquatic ecosystems and source types.
Main Methods:
- Characterization of 37 DOM isolates from diverse aquatic environments (US, Pacific Ocean, Antarctic lakes).
- Analysis of stable and radiocarbon isotopes (δ13C-DOC and Δ14C-DOC).
- Measurement of optical properties (absorbance and fluorescence, including SUVA254).
- Determination of molecular composition using ultrahigh-resolution mass spectrometry.
Main Results:
- Modern Δ14C-DOC and optical properties (e.g., SUVA254) correlated with polyphenolic and polycyclic aromatic compounds, indicative of allochthonous DOM.
- Enriched δ13C-DOC and optical properties correlated with aliphatic compounds, characteristic of autochthonous DOM.
- Autochthonous DOM from different locations (Pacific Ocean vs. Antarctic lakes) showed distinct molecular signatures due to varying degradation levels.
- A consistent compositional shift with aging was observed across all sites, with certain biomolecules persisting over time.
Conclusions:
- Molecular composition, isotopic signatures, and optical properties provide a framework for understanding DOM.
- DOM composition is strongly linked to its source (allochthonous vs. autochthonous) and degradation state.
- Aging processes lead to predictable shifts in DOM molecular makeup, impacting its environmental fate and reactivity.
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