Cyanobacteria + general algae Flashcards
Sheath in Cyanobacterial cells. Thin electrondense layer, surrounding cells or groups of cells in a more or less adherent way. It can be observed both under the light and the electron microscope.
It is more frequent in the filamentous forms
Capsule generally consists of a thicker and more compact layer of the sheath, tightly associated with the cell surface.
It is more frequent in the coccoid forms.
(Cyanobacterial cell)
Slime is the polysaccharidic material that is found dispersed around the cyanobacterial cells, rapidly secreted externally.
Cyanobacterial cell is generally occupied for the most part by thylakoidal membranes (or thylakoids), whose spatial organization in the cytoplasm seems to have a taxonomic value.
Other cellular inclusions of cyanobacteria are carboxysomes; micro-compartments containing the enzymes carbonic anhydrase and Rubisco, where the carbon dioxide fixation occurs
In cyanobacteria: Formation of specialized , spore-like cells, much larger than the vegetative ones with thickened walls, called akinetes. Can accumulate and store various essential material, that allow the survival of cyanobacteria for many years when environmental conditions are not favorable for growth (drought, cold, lack of nutrients).
Planktonic cyanobacteria is able to perform vertical migration by buoyancy. This occurs by modulating the production of gas vesicles, favouring buoyancy or by the production of starch of the Cyanophyceae granules and cyanophycin, acting instead as ballast.
Pili in cyanobacteria.
Many coccoid forms achieve gliding motility through particular structures called pili
Many cyanobacterial species are a component of the marine phytoplankton, where in the presence of eutrophic waters, they are able to produce considerable biomass, causing real blooms, with the colouring of the water in green, brown or red.
Microbial mats are dense benthic communities of cyanobacteria, in which the different species are distributed vertically to form distinct layers, often recognizable to the naked eye due to the different colours, due to the pigments of the organisms that compose them.
Stromatolites are found all over the world and are thought to have been produced by “light loving” microorganisms.
In the Precambrian, stromatolites grew in a wide variety of habitats, from shallow coastal areas to deep water, where they gave rise to domes or branched columns.
The number of stromatolites dates back to a maximum of 700-800 million years, then suddenly declined.
Research suggest that this decrease is due to the evolution of numerous types of herbivorous gastropods, which fed on these covers
Cyanobacteria: Spirulina sp. (Oscillatoriales)
Cyanobacteria: Oscillatoria princeps (Oscillatoriales)
Cyanobacteria: Chroococcus sp. (Chroococcales
Cyanobacteria: Hapalosiphon hibernicus (Stigonematales)
Cyanobacteria: Nostoc sp. (Nostocales)