Related Experiment Video
Updated: Jul 12, 2026

08:05
Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O
Published on: October 7, 2020
Nitrogen uptake, dissolved organic nitrogen release, and new production
Summary
Phytoplankton release significant dissolved organic nitrogen (DON) during nitrogen uptake. Traditional methods underestimate nitrogen uptake and production by failing to measure DON release, impacting ecological assessments.
Area of Science:
- Marine biology
- Biogeochemistry
- Oceanography
Background:
- Phytoplankton are crucial primary producers in marine ecosystems.
- Nitrogen is a key limiting nutrient for phytoplankton growth.
- Dissolved inorganic nitrogen (DIN) uptake by phytoplankton can lead to the release of dissolved organic nitrogen (DON).
Purpose of the Study:
- To quantify the release rates of DON by phytoplankton in oceanic, coastal, and estuarine environments.
- To assess the impact of DON release on the accuracy of nitrogen uptake measurements using traditional methods.
- To determine DON turnover times in different marine environments.
Main Methods:
- Nitrogen-15 (N-15) uptake experiments were conducted.
- Measurements included the release of dissolved inorganic nitrogen (NH(4)(+) and NO(3)(-)) and dissolved organic nitrogen (DON).
- DON release rates and turnover times were calculated for oceanic, coastal, and estuarine sites.
Main Results:
- Phytoplankton released 25–41% of absorbed inorganic nitrogen as DON.
- DON release rates in oceanic systems varied from 4 to 26 ng-N L⁻¹ h⁻¹.
- Traditional N-15 techniques underestimated new and regenerated production by up to 74% and 50%, respectively, due to unmeasured DON release.
Conclusions:
- DON production is a significant process in marine nitrogen cycling.
- Accurate assessment of phytoplankton production requires accounting for DON release.
- Established nitrogen uptake methodologies may require revision to incorporate DON measurements for precise ecological modeling.
Related Concept Videos
Overview of Nitrogen Metabolism
Nitrogen is a very important element for life because it is a major constituent of proteins and nucleic acids. It is a macronutrient, and in nature, it is recycled from organic compounds and stored in the form of ammonia, ammonium ions, nitrate, nitrite, or nitrogen gas by many metabolic processes. Many of these metabolic processes are carried out only by prokaryotes.
The largest pool of nitrogen available in the terrestrial ecosystem is gaseous nitrogen (N2) from the air, but this nitrogen...
The largest pool of nitrogen available in the terrestrial ecosystem is gaseous nitrogen (N2) from the air, but this nitrogen...
The Nitrogen Cycle
Nitrogen atoms, present in all proteins and DNA, are recycled between abiotic and biotic components of the ecosystem. However, the primary form of nitrogen on Earth is nitrogen gas, which cannot be used by most animals and plants. Thus, nitrogen gas must first be converted into a usable form by nitrogen-fixing bacteria before it can be cycled through other living organisms. The use of nitrogen-containing fertilizers and animal waste products in human agriculture has greatly influenced the...
Inorganic Nitrogen Assimilation
Nitrogen is an essential element in biological systems, forming a crucial component of proteins, nucleic acids, and other cellular constituents. Many bacteria and archaea acquire nitrogen in the form of nitrate (NO₃⁻) or ammonia (NH₃), which are then assimilated into biomolecules through specific enzymatic pathways.Assimilatory Nitrate ReductionWhen nitrate enters the cell, it undergoes a two-step reduction process known as assimilatory nitrate reduction. Initially, the enzyme nitrate reductase...
Microbes and the Nitrogen Cycle
The nitrogen cycle is a complex biogeochemical process critical to maintaining the balance of nitrogenous compounds in ecosystems. This cycle involves multiple microbial-mediated transformations through which nitrogen changes oxidation states, supporting essential ecological functions and contributing to plant and microbial growth.Nitrogen Fixation and AmmonificationNitrogen fixation initiates the cycle by converting inert atmospheric nitrogen (N₂) into bioavailable ammonia (NH₃), a process...
Primary Production
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
Metabolism of Chemolithotrophs
Chemolithotrophs are microorganisms that obtain energy by oxidizing inorganic molecules such as hydrogen gas (H₂), ammonia (NH₃), reduced sulfur compounds (H₂S, S²⁻), and ferrous iron (Fe²⁺). Unlike heterotrophic organisms that rely on organic carbon, chemolithotrophs transfer electrons from these inorganic donors to the electron transport chain (ETC), generating a proton motive force (PMF) that drives ATP synthesis through oxidative phosphorylation. However, because inorganic electron donors...

