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Updated: Oct 29, 2025

Understanding Dissolved Organic Matter Biogeochemistry Through In Situ Nutrient Manipulations in Stream Ecosystems
Published on: October 29, 2016
Active dissolved organic nitrogen cycling hidden in large river and environmental implications
Zhenwei Yan1, Na Yang2, Zhou Liang3
1Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Institute for Advanced Ocean Study, Ocean University of China, Qingdao, Shandong, China.
Dissolved organic nitrogen (DON) cycling in the Yellow River is complex. Researchers found that smaller DON molecules mineralize into nitrate, influenced by geography and microbes, impacting nitrogen cycling in marginal seas.
Area of Science:
- Environmental Chemistry
- Riverine Biogeochemistry
- Microbial Ecology
Background:
- Large rivers are critical sources of terrestrial dissolved organic matter (DOM) to marginal seas.
- Dissolved organic nitrogen (DON) is crucial for DOM cycling, but its dynamics in high dissolved inorganic nitrogen (DIN) rivers like the Yellow River remain poorly understood.
- The Yellow River's high DIN and low DON concentrations present measurement challenges and obscure DON cycling.
Purpose of the Study:
- To investigate the dissolved organic nitrogen (DON) cycling in the Yellow River, a major global river with high dissolved inorganic nitrogen (DIN).
- To elucidate the role of DON in the river's biogeochemical processes and its contribution to marginal seas.
- To develop a method for quantifying mineralized DON flux in large rivers.
Main Methods:
- Analysis of 17 water samples from the Yellow River's middle to downstream sections.
- Utilized spectroscopy, tangential flow filtration, nitrogen isotope analysis (δ15N), and DNA sequencing.
- Employed redundancy analysis to assess relationships between geographical features, microbial communities, and DON cycling.
Main Results:
- Dissolved organic nitrogen smaller than 1 kDa (DON<1kDa) dominated the DON pool and inversely correlated with DIN, suggesting mineralization into nitrate.
- Nitrogen isotope data (δ15NDON<1kDa) and ammonia-oxidizing bacteria/archaea abundance supported the mineralization hypothesis.
- Geographical features and microbial communities were identified as key drivers of DON cycling.
Conclusions:
- Active DON cycling, particularly DON mineralization, occurs in large rivers with high DIN concentrations.
- DON mineralization plays a significant role in the nitrogen and carbon cycling within these rivers and subsequently in marginal seas.
- A novel method for quantifying mineralized DON flux in large rivers was proposed.
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