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During photosynthesis, they assimilate carbon dioxide and release oxygen. If solar radiation is too high, phytoplankton may fall victim to photodegradation. Phytoplankton species feature a large variety of photosynthetic pigments which species-specifically enables them to absorb different wavelengths of the variable underwater light. [14]
Aquatic photosynthesis is the occurrence of photosynthesis in the aquatic environment, which includes the freshwater environment and the marine (saltwater) environment. . Organisms that perform photosynthesis in the aquatic environment include but are not limited to plants, algae, cyanobacteria, [1] coral, [2] phytoplankton (also known as micro
The marine carbon cycle. Carbon dioxide is taken up by phytoplankton for photosynthesis and incorporated into the marine food web. When plankton or predator dies, sedimentation of organic matter reaches the seafloor, where carbon can be buried and sequestered.
Marine primary production is the chemical synthesis in the ocean of organic compounds from atmospheric or dissolved carbon dioxide. It principally occurs through the process of photosynthesis , which uses light as its source of energy, but it also occurs through chemosynthesis , which uses the oxidation or reduction of inorganic chemical ...
Microalgae, capable of performing photosynthesis, are important for life on earth; they produce approximately half of the atmospheric oxygen [3] and use the greenhouse gas carbon dioxide to grow photoautotrophically. "Marine photosynthesis is dominated by microalgae, which together with cyanobacteria, are collectively called phytoplankton."
Inorganic nutrients and carbon dioxide are fixed during photosynthesis by phytoplankton, which both release dissolved organic matter (DOM) and are consumed by herbivorous zooplankton. Larger zooplankton - such as copepods - egest fecal pellets which can be reingested and sink or collect with other organic detritus into larger, more-rapidly ...
Calcium carbonate and carbon dioxide are produced from calcium and bicarbonate by the following chemical reaction: [100] Ca 2+ + 2HCO − 3 ⇌ CaCO 3 + CO 2 + H 2 O. Because coccolithophores are photosynthetic organisms, they are able to use some of the CO 2 released in the calcification reaction for photosynthesis. [101]
Ecosystem respiration is the production portion of carbon dioxide in an ecosystem's carbon flux, while photosynthesis typically accounts for the majority of the ecosystem's carbon consumption. [3] Carbon is cycled throughout the ecosystem as various factors continue to uptake or release the carbon in different circumstances.