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Soil Health · Soil biological property

Soil Microorganisms

Also known as: Soil microbes, Soil microbiota

Soil microorganisms — bacteria, fungi, archaea, and protozoa — are the most numerous and diverse living component of soil. They drive decomposition and nutrient cycling, form key symbioses with plant roots, and help suppress some soil-borne pathogens.

Dated referenceLast reviewed: 2026-07-12Updated: 2026-07-12
Illustrative diagram · AgricultureID (original)

A single handful of healthy soil can contain an immense number of microorganisms across a huge diversity of species, most of which remain uncharacterized. This microbial community forms the base of the soil food web, mediating nearly every chemical transformation that organic residues and minerals undergo.

Beyond free-living decomposers, some soil microorganisms form close symbioses with plant roots — most notably mycorrhizal fungi and nitrogen-fixing rhizobia — that directly enhance plant nutrition, while others act as pathogens or as natural antagonists of pathogens.

What soil microorganisms are

Soil microorganisms include bacteria (the most numerous group by cell count), fungi (which can dominate microbial biomass through extensive hyphal networks), archaea, and protozoa. Each group occupies different ecological niches, from rapid decomposition of simple compounds by many bacteria to the breakdown of more resistant organic material by fungi.

Mycorrhizal fungi
Fungi that form symbiotic associations with plant roots, extending the root’s effective reach for water and nutrients, especially phosphorus.
Rhizobia
Bacteria that form nodules on the roots of legumes and fix atmospheric nitrogen into plant-available forms.
Antagonistic microorganisms
Microbes that suppress pathogens through competition, antibiosis, or direct parasitism, contributing to natural disease suppression.

Why soil microorganisms matter

Microbial decomposition and mineralization release nutrients locked in organic matter into forms plants can absorb, making microorganisms central to nutrient cycling. Mycorrhizal and rhizobial symbioses can substantially improve plant nutrient and water acquisition. Some microbial communities also suppress soil-borne pathogens through competition for resources, production of antagonistic compounds, or direct parasitism, contributing to natural disease resistance in well-managed soils.

How the microbial community is assessed

Microbial biomass carbon estimates the total living microbial mass in a sample, while soil respiration (carbon dioxide release) reflects overall metabolic activity. Phospholipid fatty acid (PLFA) analysis can characterize broad community composition, and DNA- or RNA-based sequencing methods provide detailed identification of which organisms are present and, in some cases, active.

Supporting beneficial soil microorganisms

Because microorganisms depend on organic carbon as an energy source, management that maintains a steady supply of residues and living roots, while minimizing unnecessary disturbance, tends to support a more active and diverse microbial community.

  • Maintain organic matter inputs through residues, cover crops, and organic amendments
  • Rotate diverse crops, including legumes, to support varied microbial symbioses
  • Reduce tillage intensity to protect fungal networks and microbial habitat
  • Consider microbial inoculants (such as rhizobial or mycorrhizal products) where appropriate for the crop and soil, following supplier and regional guidance

Relationships

Evidence-backed connections in the knowledge graph.

Scope & limitations

Geographic scope: General soil-science overview applicable worldwide; the composition and function of microbial communities vary greatly by climate, soil type, and management.

Climate context: Temperature and moisture regulate microbial activity rates and seasonal community dynamics.

  • The soil microbial community is highly diverse and site-specific; most species remain uncharacterized, and general statements cannot capture local variation.
  • Microbial measurements are sensitive to recent conditions and are best interpreted as trends over repeated sampling rather than single results.
  • Microbial inoculant performance varies with soil conditions, existing microbial populations, and crop, and is not guaranteed across all contexts.

Sources

This article draws on the following authoritative sources. See our sources & methodology for how they are selected.

  1. [1]USDA NRCS — Natural Resources Conservation Service (opens in a new tab)

    USDA Natural Resources Conservation Service (NRCS)

    Authoritative

    Cited for: Soil microorganisms and microbial indicators

    Type:
    Government agency
    Jurisdiction:
    United States
    Accessed:
    2026-07-12
  2. [2]FAO — Soils Portal (opens in a new tab)

    FAO Global Soil Partnership

    Authoritative

    Cited for: Soil microbial diversity and function

    Type:
    Intergovernmental organization
    Jurisdiction:
    Global
    Accessed:
    2026-07-12
  3. High

    Cited for: Global soil biological property context

    Type:
    Research institute
    Jurisdiction:
    Global
    Accessed:
    2026-07-12
  4. [4]Cornell CALS — Plant pathology and crop resources (opens in a new tab)

    Cornell University College of Agriculture and Life Sciences

    High

    Cited for: Soil microbial community assessment

    Type:
    University extension service
    Jurisdiction:
    United States (New York)
    Accessed:
    2026-07-12