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Biology · Ecosystems, Energy Flow & Biogeochemical Cycles

Nitrogen, phosphorus and microbial transformations

An organism can need nitrogen while being unable to use atmospheric nitrogen gas directly. Another can use a form produced by microbial transformations. A nutrient cycle connects chemical forms and organisms, but the existence of a route does not reveal its rate or make every organism perform it.

Begin with Organisms, Environments & Ecological Niches for ecological boundaries and scales, and Energy, Enzymes & Metabolism for chemical energy and respiration. Communities, Species Interactions & Food Webs explains why feeding relations form a web. That chapter is a reading preparation path once available, rather than a claim of an already published lesson. The budgets here introduce every symbol and require ordinary addition, subtraction and ratios. Advanced carbon-cycle measurement methods and chemical reaction mechanisms are not required.

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By the end, you can

Distinguish nitrogen chemical transformations, phosphorus transfers and specified nutrient requirements without imposing a universal limiting nutrient.

01

Nitrogen transformations form a network

Nitrogen fixation converts molecular nitrogen into biologically available reduced forms through organisms with the relevant capacity. It differs from assimilation, which incorporates available nitrogen into organic material. A plant taking up nitrate is assimilating a form of nitrogen; that uptake is not itself nitrogen fixation.

The selected conceptual network connects molecular nitrogen, ammonium, nitrite, nitrate and organic nitrogen. It includes fixation, mineralisation from organic forms, nitrification through selected reduced-to-oxidised forms, assimilation from ammonium or nitrate, and denitrification returning nitrogen to molecular gas. Microorganisms with suitable metabolism mediate important transformations; no single organism is assigned every arrow.

These are selected pathways, not an exhaustive sequence every nitrogen atom must follow. Other routes, ecological conditions and coupled transformations matter. The symbols N2, NH4+, NO2- and NO3- represent chemical forms rather than equal numbers of nitrogen atoms in one molecule. If a numerical account were added, molecular nitrogen has two nitrogen atoms per molecule, so molecule counts could not silently become element counts.

A pathway network is not a mandatory sequence

A pathway network is not a mandatory sequenceSelected nitrogen-form nodes connect fixation, mineralisation, assimilation, nitrification and denitrification with distinct typed arrows.Molecular nitrogen (N2)Ammonium (NH4+)Nitrite (NO2-)Nitrate (NO3-)Organic nitrogenMolecular nitrogen (N2) → Ammonium (NH4+): Selectednitrogen fixationOrganic nitrogen → Ammonium (NH4+):Organic-to-inorganic mineralisationAmmonium (NH4+) → Nitrite (NO2-): Selectednitrification pathwayNitrite (NO2-) → Nitrate (NO3-): Selectednitrification pathwayAmmonium (NH4+) → Organic nitrogen: Incorporationinto organic materialNitrate (NO3-) → Organic nitrogen: Incorporation intoorganic materialNitrate (NO3-) → Molecular nitrogen (N2): Selectedreturn to molecular nitrogenSelected forms and links; additional routes omittedNo arrow assigns a transfer rateGas molecules and single-nitrogen ions have differentnitrogen-atom counts
Each typed arrow identifies a selected nitrogen transformation. The symbols identify chemical forms; the arrows are not complete reaction equations.
Read the diagram in words

Molecular nitrogen connects to ammonium through fixation. Organic nitrogen can return to ammonium through mineralisation. Selected nitrification links ammonium, nitrite and nitrate. Ammonium and nitrate connect to organic nitrogen through assimilation; nitrate connects to molecular nitrogen through denitrification.

A pathway network is not a mandatory sequence
Molecular nitrogen (N2) / Ammonium (NH4+) / Nitrite (NO2-) / Nitrate (NO3-) / Organic nitrogen
Molecular nitrogen (N2)
Ammonium (NH4+)
Nitrite (NO2-)
Nitrate (NO3-)
Organic nitrogen
A pathway network is not a mandatory sequence
Molecular nitrogen (N2) / Ammonium (NH4+) / Nitrite (NO2-) / Nitrate (NO3-) / Organic nitrogenSelected nitrogen fixation / Organic-to-inorganic mineralisation / Selected nitrification pathway / Incorporation into organic material / Selected return to molecular nitrogen
Molecular nitrogen (N2) → Ammonium (NH4+)Selected nitrogen fixation
Organic nitrogen → Ammonium (NH4+)Organic-to-inorganic mineralisation
Ammonium (NH4+) → Nitrite (NO2-)Selected nitrification pathway
Nitrite (NO2-) → Nitrate (NO3-)Selected nitrification pathway
Ammonium (NH4+) → Organic nitrogenIncorporation into organic material
Nitrate (NO3-) → Organic nitrogenIncorporation into organic material
Nitrate (NO3-) → Molecular nitrogen (N2)Selected return to molecular nitrogen

Selected forms and links; additional routes omitted

No arrow assigns a transfer rate

Gas molecules and single-nitrogen ions have different nitrogen-atom counts

Qualitative selected nitrogen transformations only. No rates, enzymes, culture or treatment procedure, universal taxon assignment or exhaustive pathway claim. Node symbols identify forms; arrows do not assert balanced chemical reactions.

02

A mineral-derived element can enter living material

Phosphorus moves between mineral, dissolved and organic forms through physical, chemical and biological processes. Weathering can supply available forms; uptake incorporates phosphorus into organisms; transformations of organic material can return it to available pools. Transport and sediment movement connect a local ecosystem to surrounding reservoirs.

The original phosphorus account starts with available phosphorus five and organic phosphorus ten. It assigns external weathering input three, uptake four, organic-to-available mineralisation two and external export one. Available phosphorus ends with five and organic phosphorus with twelve. The combined total rises from fifteen to seventeen.

The unchanged available pool does not mean uptake is absent: input three and mineralisation two balance uptake four and export one. This account uses element-phosphorus units and selected forms only. It neither claims phosphorus exists only as phosphate nor rules out all atmospheric transport or every other chemical pathway.

A stable available pool can feed a growing organic pool

A stable available pool can feed a growing organic poolTwo phosphorus stocks connect uptake and mineralisation while external weathering input and export change the combined total.Element-phosphorus units during one intervalCombined phosphorus stockAvailable phosphorus poolBeginning stock: 5Ending stock: 5Organic phosphorus poolBeginning stock: 10Ending stock: 12Outside the selected ecosystemOutside the selected ecosystem → Availablephosphorus pool: External weathering input; 3Available phosphorus pool → Organic phosphorus pool:Uptake and incorporation; 4Organic phosphorus pool → Available phosphorus pool:Organic-to-available return; 2Available phosphorus pool → Outside the selectedecosystem: Boundary export; 1Beginning stockAvailable phosphoruspool5Organic phosphorus pool10012Ending stockAvailable phosphoruspool5Organic phosphorus pool12012Combined phosphorus stock: Beginning stock 15; Ending stock 17
The stable available stock conceals nonzero opposing transfers. Internal uptake and return cancel only in the combined account.
Read the diagram in words

Available phosphorus begins and ends five: five plus three minus four plus two minus one. Organic phosphorus rises from ten to twelve: ten plus four minus two. Combined stock grows by external three minus one, from fifteen to seventeen.

Combined phosphorus stock
Available phosphorus pool / Organic phosphorus poolBeginning stockEnding stock
Available phosphorus pool55
Organic phosphorus pool1012
A stable available pool can feed a growing organic pool
Available phosphorus pool / Organic phosphorus pool / Outside the selected ecosystemExternal weathering input / Uptake and incorporation / Organic-to-available return / Boundary exportElement-phosphorus units during one interval
Outside the selected ecosystem → Available phosphorus poolExternal weathering input3
Available phosphorus pool → Organic phosphorus poolUptake and incorporation4
Organic phosphorus pool → Available phosphorus poolOrganic-to-available return2
Available phosphorus pool → Outside the selected ecosystemBoundary export1
Combined phosphorus stock
Beginning stockEnding stock
1517

Complete original element-phosphorus-unit account over one interval; available and organic are chosen combined pools, without concentration, speciation or universal chemical-pathway claims.

03

Availability matters relative to a stated requirement

A nutrient can constrain production when its usable supply falls short relative to what the organisms require under the relevant conditions. Nitrogen and phosphorus limitation vary across settings; combined limitations can occur. A label such as freshwater or marine is not enough to decide the limiting nutrient of every system.

The original static capacity model assigns one new biomass unit a requirement of ten carbon units, two nitrogen units and one phosphorus unit. Available supplies are one hundred, twelve and four respectively. Dividing supply by requirement gives possible capacities ten, six and four. If these are the only constraints and all supplies are usable, the smallest capacity allows four new biomass units.

Four units use forty carbon, eight nitrogen and four phosphorus units, leaving sixty carbon and four nitrogen unused in this account. Those leftovers are not automatically additional production because phosphorus supply is exhausted. Real production also depends on energy, accessibility, losses, recycling, organismal composition and other conditions. This is an algebraic capacity model, not instructions for adding nutrients to an environment.

Three supplies constrain the same new biomass

Three supplies constrain the same new biomassSupplied carbon, nitrogen and phosphorus amounts are divided by their separate requirements before comparing biomass-unit capacities.Possible biomass units from this supplyCarbon10Nitrogen6Phosphorus4010Carbon: Possible biomass units from this supply 100/10 = 10;Element used in four biomass units 40; Element remaining 60Nitrogen: Possible biomass units from this supply 12/2 = 6; Elementused in four biomass units 8; Element remaining 4Phosphorus: Possible biomass units from this supply 4/1 = 4;Element used in four biomass units 4; Element remaining 0Smallest compatible biomass capacity: 4Only the stated fixed requirements and supplies constrain thistoy calculation
The graph compares derived biomass-unit capacities, not raw element amounts with different requirements.
Read the diagram in words

Carbon permits ten biomass units, nitrogen six and phosphorus four. The minimum is four. Those units use forty carbon, eight nitrogen and four phosphorus, leaving sixty, four and zero in their respective accounts.

Only the stated fixed requirements and supplies constrain this toy calculation
Separate element accountUsable element supplyElement units required per biomass unitPossible biomass units from this supplyElement used in four biomass unitsElement remaining
Carbon10010104060
Nitrogen122684
Phosphorus41440
Smallest compatible biomass capacity
Smallest compatible biomass capacity
4

Static original capacity calculation with fixed element requirements, fully usable supplies, no recycling or losses, and no other limiting condition. No actual stoichiometry, fertilisation experiment or environmental recommendation.

Worked example

Follow both transfers and requirements

Available phosphorus: 5 + 3 - 4 + 2 - 1 = 5. Organic phosphorus: 10 + 4 - 2 = 12. The fifteen-unit starting total becomes seventeen because external input three exceeds external output one by two.

For the capacity example, carbon permits 100/10 = 10 biomass units; nitrogen permits 12/2 = 6; phosphorus permits 4/1 = 4. Under the supplied constraints, production capacity is the minimum, four. This conclusion is conditional on the fixed requirements and usable pools.

Using those four biomass units consumes 40, 8 and 4 of the three element supplies. Subtracting from the initial 100, 12 and 4 gives remaining 60, 4 and 0. These different element accounts cannot be added as though they were interchangeable nutrient units.

Check your understanding

  1. Is nitrate uptake by a plant the same process as nitrogen fixation?

    Show reasoning

    No. Uptake and incorporation use an already available nitrogen form. Fixation converts molecular nitrogen into available reduced forms through organisms with the relevant capacity.

  2. Why does an unchanged five-unit available phosphorus stock not prove no uptake?

    Show reasoning

    Four units are taken up while input three and mineralisation two supply five and export removes one. Opposing interval transfers leave the stock unchanged.

  3. Why do leftover carbon sixty and nitrogen four not increase biomass beyond four in the capacity model?

    Show reasoning

    Every additional assigned biomass unit needs phosphorus as well as carbon and nitrogen. The supplied phosphorus is fully used at four. That result holds under the fixed requirements and other stated assumptions.

What to carry forward

Track element forms and compatible inventories; a limiting capacity belongs to an explicit requirement and supply, not an ecosystem label alone.

References

Resources supporting this lesson’s explanations and examples.

  1. Biology 2e (2018; chapter 46, sections 46.1–46.3)Mary Ann Clark, Matthew Douglas and Jung ChoiTextbook chaptersopenstax.orgRead source
  2. The microbial nitrogen-cycling network (Nature Reviews Microbiology 16(5):263–276, 2018; doi: 10.1038/nrmicro.2018.9)Marcel M. M. Kuypers, Hannah K. Marchant and Boran KartalResearch abstractnature.comRead source
  3. Global analysis of nitrogen and phosphorus limitation of primary producers in freshwater, marine and terrestrial ecosystems (Ecology Letters 10(12):1135–1142, 2007; doi: 10.1111/j.1461-0248.2007.01113.x)James J. Elser, Matthew E. S. Bracken, Elsa E. Cleland, Daniel S. Gruner, W. Stanley Harpole, Helmut Hillebrand, Jacqueline T. Ngai, Eric W. Seabloom, Jonathan B. Shurin and Jennifer E. SmithResearch abstractpubmed.ncbi.nlm.nih.govRead source