Diatoms are single-celled algae encased in ornate silica shells called frustules. Discover how these tiny organisms support ecosystems, shape oxygen cycles, and inspire biomimetic science.
Visit the dedicated Q&A page to discuss taxonomy, microscopy techniques, ecology, identification, and research methods around diatoms.
Go to Diatoms Q&ADiatoms are nature's most prolific artists — each species engineering a unique, nanometer-precise glass shell that no human technology has yet replicated.
Belonging to the class Bacillariophyceae, diatoms are photosynthetic microalgae found in virtually every aquatic environment on Earth — from polar oceans and tropical seas to freshwater lakes, rivers, and even damp soils.
Their defining feature is the frustule — an intricate two-part cell wall made of amorphous silicon dioxide (SiO₂·nH₂O), the same material as glass. The two overlapping halves (epitheca and hypotheca) fit together like a Petri dish, and together they create patterns of extraordinary geometric precision.
Far from mere curiosities, diatoms are ecological powerhouses: they account for roughly 20–25% of global net primary production and are responsible for nearly a quarter of the oxygen in every breath we take.
Discover the Types →Diatoms are among the most ecologically and economically important organisms on Earth, with capabilities that continue to astonish scientists.
Each frustule contains thousands of precisely spaced nanopores (areolae) arranged in species-specific geometric patterns — a natural photonic crystal.
Diatoms collectively fix more carbon dioxide than all the world's tropical rainforests combined, making them the planet's most important carbon sink.
Diatoms extract dissolved silicic acid from water and deposit it into their frustules at room temperature — a process chemists still cannot replicate efficiently.
When diatoms die, they sink, dragging captured carbon to the ocean floor in what scientists call the "biological pump" — a natural climate regulator.
Diatomaceous earth — fossilized frustules — is used in filtration, as a natural pesticide, in toothpaste, paints, and even dynamite (Nobel's first stabilizer).
With over 200,000 estimated species, diatoms are more genetically diverse than all vertebrate animals combined.
Diatom pore spacing can be as small as 100 nm — a precision achieved through protein scaffolds that act as molecular templates during cell wall formation.
The oldest diatom fossil records date to the Early Jurassic (~185 Mya). They survived all five major mass extinctions, thriving where other life perished.
All diatoms are classified into two fundamental groups based on the symmetry of their frustule — each group has evolved distinct ecological strategies.
Radially symmetrical — like a wheel or medallion viewed from above. Primarily marine and planktonic, centric diatoms drift freely in open water. Key genera include Coscinodiscus, Thalassiosira, and Cyclotella. Their circular frustules scatter light beautifully, creating iridescent displays.
Bilaterally symmetrical — elongated like a feather or canoe. Many possess a raphe, a groove that allows active gliding motility along surfaces. Found in freshwater and benthic marine environments. Key genera include Navicula, Nitzschia, and Pinnularia.
Many species form chains, ribbons, or star-shaped colonies by linking frustules with silica bridges or mucilage pads. Asterionella creates stunning rosettes; Melosira builds filaments. Colonial forms dominate spring phytoplankton blooms, colouring lakes and seas with living green–gold carpets.
Because silica resists decomposition, diatom frustules accumulate in sediments over geological time. These fossil assemblages — diatomite or diatomaceous earth — record past climate, salinity, and productivity. California's Lompoc deposit is over 300 metres thick and contains billions of trillion individual frustules.
Remove diatoms from the ocean and the biosphere collapses. Their ecological importance spans oxygen production, carbon sequestration, and feeding the entire marine food web.
Using sunlight and dissolved CO₂, diatoms produce roughly 20% of Earth's atmospheric oxygen — more than all tropical rainforests combined. A single diatom bloom can stretch thousands of square kilometres.
When diatom cells die, they sink — a process known as the "biological pump." This draws atmospheric carbon into deep ocean sediments, locking it away for millennia and regulating global climate.
Diatoms are the primary food source for zooplankton, krill, shellfish, and small fish. Their rich fatty acids (EPA and DHA) underpin the nutritional value of the entire marine food chain — including the fish on your plate.
Diatoms are the dominant biogeochemical drivers of the global silicon cycle, transforming dissolved silicic acid into biogenic silica and back again, influencing ocean chemistry and productivity worldwide.
Because different species thrive under different conditions, diatom assemblages in sediment cores act as precise environmental recorders — telling scientists about past temperatures, pH levels, and pollution events.
Convert sunlight to biomass, anchoring marine food webs globally.
Produce ~25% of Earth's net oxygen output every year.
Sequester gigatons of carbon in ocean sediments each year.
EPA/DHA fatty acids in diatoms fuel fish, seabirds, whales & humans.
Their fossils decode Earth's past climates with extraordinary resolution.
Used in drug delivery, biosensors, photovoltaics & nanotechnology.
The diatom is to the ocean what the grass is to the prairies — invisible to the naked eye, yet the foundation upon which all visible life depends.