Diatom
Diatoms are single-celled photosynthetic algae whose glass-like silica walls help define their form and ecological role. Found in marine and freshwater environments, they contribute to aquatic food webs and the cycling of silicon and carbon. Their abundance, physiology and sinking behavior vary among species and with environmental conditions.
Structure and diversity
Diatoms are microscopic algae in the group Bacillariophyta. Their cell covering, called a frustule, is built from hydrated silica and typically consists of two overlapping parts. Frustule shapes and surface patterns differ widely among lineages, making diatoms both ecologically diverse and visually distinctive. Some species are solitary; others form chains or colonies. Their life cycles involve cell division and size changes, and some species can form resting stages when conditions become unfavorable.
Habitats and ecological roles
Diatoms occur in oceans, lakes, rivers, wetlands and moist soils. As photosynthetic primary producers, they convert inorganic carbon into organic matter and support consumers in aquatic food webs. Their contribution is not uniform: local production and community composition depend on light, temperature, water movement and nutrients. Diatoms take up dissolved silicic acid to make their frustules, so silicon availability can influence their growth relative to phytoplankton that do not require silica.
Silica, carbon and sinking
When diatom cells or aggregates sink, they can transport organic matter and silica away from sunlit surface waters. This export links surface production to deeper ocean processes, although the fraction that reaches depth depends on grazing, aggregation, sinking and decomposition. Silica in frustules can dissolve and return to the water as silicic acid, where it may again become available for biological uptake. The timing and depth of dissolution affect how nutrients circulate through the water column.
Community effects and uncertainty
The ecological influence of a diatom community cannot be inferred from cell counts alone. Research on natural assemblages found that large cells could contribute disproportionately to short-term silica production, while growth rate became more important over longer periods. Diatoms are also not a single uniform response group: species differ in size, shell properties and environmental tolerances. Claims about their global production or responses to ocean change therefore depend on the method, location and time scale being considered.
Key facts
- Cell covering
- A silica-based structure called a frustule, commonly formed from two overlapping parts.
- Nutrient requirement
- Diatoms take up dissolved silicic acid to build their silica frustules.
- Ecosystem role
- They are photosynthetic primary producers and contribute to aquatic food webs and biogeochemical cycling.
- Export pathway
- Sinking cells and aggregates can carry organic carbon and silica from surface waters toward the ocean interior.
- Variation among taxa
- Cell size, growth rate and morphology affect silica production, so abundance alone does not determine a species' contribution.
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References
- 1.A Diatom Helix
Smithsonian Ocean · other · reliability: unverified · retrieved 29 October 2026
Supports: Describes a marine diatom, its silica cell wall, and roles in oxygen production and food webs.
- 2.Role of diatoms in regulating the ocean's silicon cycle
Global Biogeochemical Cycles (American Geophysical Union/Wiley) · other · reliability: unverified · retrieved 29 October 2026
Supports: Examines diatom dependence on silicic acid and links between diatom ecology, silicon cycling and carbon export.
- 3.Taxon-specific contributions to silica production in natural diatom assemblages
Limnology and Oceanography (Association for the Sciences of Limnology and Oceanography); available via PubMed Central · other · reliability: unverified · retrieved 29 October 2026
Supports: Reports that cell surface area and growth rates influence taxon-specific contributions to silica production in sampled diatom communities.
- 4.Unexpected global diatom decline in response to ocean acidification
Ocean Carbon & Biogeochemistry (US OCB) · other · reliability: unverified · retrieved 29 October 2026
Supports: Summarizes a proposed mechanism by which acidification may affect silica dissolution and projected diatom abundance; projections are scenario/model dependent.
References are suggested by the research engine and may be incomplete. Unverified URLs are omitted rather than guessed.
Article history
- Version 129 October 2026 · EditorCreated by Zapia