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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 ...
Gross primary production (GPP) is the amount of chemical energy, typically expressed as carbon biomass, that primary producers create in a given length of time.Some fraction of this fixed energy is used by primary producers for cellular respiration and maintenance of existing tissues (i.e., "growth respiration" and "maintenance respiration").
There they decay and return to the dissolved state, but at greater ocean depths. The fertility of the oceans depends on the abundance of the nutrients, and is measured by the primary production, which is the rate of fixation of carbon per unit of water per unit time. "Primary production is often mapped by satellites using the distribution of ...
They produce 25–45% of the total primary production of organic material in the oceans, [58] [59] [60] owing to their prevalence in open-ocean regions when total phytoplankton biomass is maximal. [61] [62] Diatoms are enclosed in protective silica (glass) shells called frustules. They are classified by the shape of these glass cages in which ...
In oceans, most primary production is performed by algae. This is a contrast to on land, where most primary production is performed by vascular plants. Algae ranges from single floating cells to attached seaweeds, while vascular plants are represented in the ocean by groups such as the seagrasses and the mangroves.
Since primary production and phytoplankton biomass cannot currently be measured over entire ocean basins, scientists use chlorophyll α as a proxy for primary production. Modern satellite observations monitor and track global chlorophyll α abundances in the ocean via remote sensing. Higher chlorophyll concentrations generally indicate areas of ...
Most primary production in the ocean occurs via photosynthesis, by organisms called phototrophic primary producers. [14] Phototrophs are the foundation of most aquatic food webs, and primary production in the ocean accounts for about half of Earth's carbon fixation. [15]
As much as 25% of the primary production from phytoplankton in the global oceans may be recycled within the microbial loop through viral shunting. [121] The viral shunt is a mechanism whereby marine viruses prevent microbial particulate organic matter (POM) from migrating up trophic levels by recycling them into dissolved organic matter (DOM ...