Pyrenoids are sub-cellular micro-compartments found in chloroplasts of many algae, and in a single group of land plants, the hornworts. Pyrenoids are associated with the operation of a carbon-concentrating mechanism (CCM). Their main function is to act as centres of carbon dioxide (CO2) fixation, by generating and maintaining a CO2 rich environment around the photosynthetic enzyme ribulose-1,5-bisphosphate carboxylase/oxygenase (RuBisCO). Pyrenoids therefore seem to have a role analogous to that of carboxysomes in cyanobacteria.
Algae are restricted to aqueous environments, even in aquatic habitats, and this has implications for their ability to access CO2 for photosynthesis. CO2 diffuses 10,000 times slower in water than in air, and is also slow to equilibrate. The result of this is that water, as a medium, is often easily depleted of CO2 and is slow to gain CO2 from the air. Finally, CO2 equilibrates with bicarbonate (HCO3−) when dissolved in water, and does so on a pH-dependent basis. In sea water for example, the pH is such that dissolved inorganic carbon (DIC) is mainly found in the form of HCO3−. The net result of this is a low concentration of free CO2 that is barely sufficient for an algal RuBisCO to run at a quarter of its maximum velocity, and thus, CO2 availability may sometimes represent a major limitation of algal photosynthesis.
Pyrenoids were first described in 1803 by Vaucher (cited in Brown et al.). The term was first coined by Schmitz who also observed how algal chloroplasts formed de novo during cell division, leading Schimper to propose that chloroplasts were autonomous, and to surmise that all green plants had originated through the “unification of a colourless organism with one uniformly tinged with chlorophyll". From these pioneering observations, Mereschkowski eventually proposed, in the early 20th century, the symbiogenetic theory and the genetic independence of chloroplasts.
In the following half-century, phycologists often used the pyrenoid as a taxonomic marker, but physiologists long failed to appreciate the importance of pyrenoids in aquatic photosynthesis.
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L'anhydrase carbonique est une enzyme présente à la surface plasmique intracellulaire (liée à l'échangeur anionique AE1 Cl/HCO3) des globules rouges (ou hématies ou encore érythrocytes) qui transforme le en et inversement. La plupart des anhydrases carboniques contiennent un atome de zinc. C'est une des enzymes les plus rapides connues. Équation : + − + . Dans les reins, elle sert à libérer les protons . Dans les os compacts, l'anhydrase carbonique permet de maintenir les lacunes de Howship dans un milieu acide (pH=4,5) grâce à un apport en H+ Catégorie:EC 4.
vignette| Représentation simplifiée de la photorespiration et du cycle de Calvin. vignette| Schéma de la photorespiration à travers les organites impliqués. La photorespiration est l'ensemble des réactions mises en œuvre par les organismes photosynthétiques à la suite de l'activité oxygénase de la Rubisco. En effet, cette enzyme intervient le plus souvent à travers son activité carboxylase, par laquelle une molécule de dioxyde de carbone est fixée sur du ribulose-1,5-bisphosphate pour donner deux molécules de 3-phosphoglycérate qui sont métabolisées par le cycle de Calvin.
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