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Related Concept Videos

Overview of Nitrogen Metabolism01:20

Overview of Nitrogen Metabolism

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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.
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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...
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Preparation of Amines: Alkylation of Ammonia and Amines01:30

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Alkylation is one of the methods used to prepare amines. Direct alkylation of ammonia or a primary amine with an alkyl halide gives polyalkylated amines along with a quaternary ammonium salt through successive SN2 reactions. This process of making the quaternary salt through the direct alkylation method is called exhaustive alkylation.
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The Roles of Bacteria and Fungi in Plant Nutrition02:11

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Primary Production01:06

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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.
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Bioremediation00:46

Bioremediation

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Bioremediation is the use of prokaryotes, fungi, or plants to remove pollutants from the environment. This process has been used to remove harmful toxins in groundwater as a byproduct of agricultural run-off and also to clean up oil spills.
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Related Experiment Video

Updated: Jun 29, 2025

Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O
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Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O

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Ammonification by kelp associated microbes increases ammonium availability.

Alex Hochroth1, Catherine A Pfister2,3

  • 1The College, The University of Chicago, Chicago, IL, United States of America.

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|March 29, 2024
PubMed
Summary
This summary is machine-generated.

Marine microbes on bull kelp convert organic nitrogen into ammonium, a vital nutrient. This process supports kelp growth, especially under stress, highlighting the importance of microbial nitrogen cycling in coastal ecosystems.

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Measurement of the Potential Rates of Dissimilatory Nitrate Reduction to Ammonium Based on 14NH4+/15NH4+ Analyses via Sequential Conversion to N2O
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Area of Science:

  • Marine microbiology
  • Ocean biogeochemistry
  • Macrophyte-microbe interactions

Background:

  • Microbes provide essential nitrogen to oceans via nitrogen fixation and organic matter mineralization.
  • Coastal marine environments host abundant microbial communities on plants and algae.
  • The specific role of these microbiomes in host nitrogen cycling is not well understood.

Purpose of the Study:

  • To investigate if microbes living on bull kelp (Nereocystis luetkeana) contribute to host nitrogen acquisition.
  • To determine if epiphytic microbial ammonification increases ammonium availability in the surrounding seawater.
  • To assess the impact of host stress on microbial nitrogen cycling rates.

Main Methods:

  • Incubation of bull kelp with 15N-labeled amino acid tracers.
  • Measurement of 15N accumulation in kelp tissues and seawater ammonium.
  • Metagenomic analysis of microbial communities on kelp surfaces.

Main Results:

  • Evidence of dissolved organic nitrogen conversion to ammonium by kelp-associated microbes.
  • 15N tracer confirmed uptake of microbially produced ammonium by kelp.
  • Stressed kelp populations exhibited higher ammonification rates despite sparser microbial communities.

Conclusions:

  • Epiphytic microbes on bull kelp actively contribute to nitrogen cycling by producing ammonium.
  • This microbial ammonification can enhance nitrogen availability for host kelp assimilation.
  • Microbial nitrogen cycling is crucial for supporting coastal macrophyte health, particularly under environmental stress.