What Is Plankton and Why Are They Important?

Plankton are a diverse collection of tiny organisms that drift within water bodies, unable to propel themselves against currents. The term originates from the Greek word for “wanderer” or “drifter,” accurately describing their mode of existence. These organisms form the foundation of aquatic life in both oceans and freshwater systems.

Understanding Plankton

Plankton are defined by their inability to swim strongly against water currents, rather than by their size or taxonomic classification. While many plankton are microscopic, often less than a millimeter in length, the group also includes larger organisms like some crustaceans and jellyfish that are still considered planktonic due to their limited swimming ability.

These organisms exist across a wide size spectrum, from femtoplankton (viruses, less than 0.2 micrometers) to megaplankton (large jellyfish, up to 2 meters). Plankton communities are found in the sunlit upper layers of water bodies, known as the euphotic zone, where light penetration supports photosynthetic life. Their distribution within these habitats is influenced by factors such as light availability, nutrient concentrations, and water temperature.

Major Plankton Types

Plankton are broadly categorized based on their ecological roles. Phytoplankton, derived from Greek words meaning “plant” and “wanderer,” are plant-like, autotrophic organisms that produce their own food through photosynthesis. Common types include diatoms, dinoflagellates, cyanobacteria, and coccolithophores. They contain chlorophyll and require sunlight, carbon dioxide, and nutrients to grow, similar to land plants.

Zooplankton, meaning “animal” and “wanderer,” are heterotrophic organisms that obtain energy by consuming others. This group includes microscopic animals like copepods, krill, and various larval stages of larger invertebrates and fish. Some zooplankton are primary consumers, feeding on phytoplankton, while others are secondary consumers that prey on other zooplankton. Bacterioplankton (bacteria) and virioplankton (viruses) also play roles in nutrient cycling and regulating other plankton populations.

Ecological Significance

Plankton form the fundamental basis of aquatic food webs in both marine and freshwater ecosystems. Phytoplankton serve as primary producers, converting sunlight into organic compounds, which then become the direct food source for zooplankton. This energy transfer cascades up the food chain, supporting a vast array of aquatic animals, from small fish and crustaceans to large filter-feeding organisms like baleen whales.

Beyond their role in food webs, phytoplankton are major producers of oxygen. Through photosynthesis, they release oxygen into the water, which then diffuses into the atmosphere. Scientists estimate that phytoplankton contribute more than half of the oxygen in Earth’s atmosphere. Their presence and activity are important for sustaining aquatic biodiversity and ecosystem health.

Global Impact of Plankton

Plankton influence global systems, extending beyond their immediate aquatic habitats. Phytoplankton play a role in the global carbon cycle by absorbing carbon dioxide from the atmosphere during photosynthesis. This process incorporates carbon into their cells. When these organisms die and sink to the deep ocean, or are consumed and their carbon is transferred through the food web, it helps transport carbon away from the surface.

This biological carbon pump helps regulate atmospheric carbon dioxide concentrations, influencing Earth’s climate patterns. Changes in plankton populations can affect global climate. Plankton also indirectly support human activities, particularly global fisheries, by forming the base of the food chain for many commercially important fish species. Scientific research relies on understanding plankton dynamics to assess ocean health and predict environmental changes.