Photosynthesis The green sulfur bacteria use a Type I
reaction center for photosynthesis. Type I reaction centers are the bacterial
homologue of
photosystem I (PSI) in plants and
cyanobacteria. The GSB reaction centers contain
bacteriochlorophyll a and are known as P840 reaction centers due to the excitation wavelength of 840 nm that powers the flow of electrons. In green sulfur bacteria, the reaction center is associated with a large antena complex called the
chlorosome that captures and funnels light energy to the reaction center. The chlorosomes have a peak absorption in the
far red region of the spectrum between 720 and 750 nm because they contain bacteriochlorophyll c, d and e. A protein complex called the
Fenna-Matthews-Olson complex (FMO) is physically located between the chlorosomes and the P840 RC. The FMO complex helps efficiently transfer the energy absorbed by the antena to the reaction center. PSI and Type I reaction centers are able to reduce
ferredoxin (Fd), a strong reductant that can be used to reduce
NAD+ and fix . Once the reaction center (RC) has given an electron to Fd, it becomes an oxidizing agent (P840+) with a
reduction potential of around +300 mV. While this is not positive enough to strip electrons from water to synthesize (E
0 = +820 mV), it can accept electrons from other sources like ,
thiosulphate or ions. This transport of electrons from donors like to the acceptor Fd is called
linear electron flow, or
linear electron transport. The oxidation of sulfide ions leads to the production of sulfur as a waste product that accumulates as globules on the extracellular side of the membrane. These globules of sulfur give green sulfur bacteria their name. When sulfide is depleted, the
sulfur globules are consumed and further oxidized to sulfate. However, the pathway of sulfur oxidation is not well-understood. The intermediate is usually sulfur, which is deposited outside of the cell, and the end product is sulfate. The sulfur, which is deposited extracellularly, is in the form of sulfur globules, which can be later oxidized completely. The oxidation of thiosulfate to sulfate could be catalyzed by the enzymes in the {{chem2|SO_{x}|}} system. However it has several oxygen sensitive enzymes that limits its efficiency in aerobic conditions. Mixotrophy occurs during amino acid biosynthesis/carbon utilization and energy metabolism. The bacterium uses electrons, generated from the oxidation of sulfur, and the energy it captures from light to run the rTCA.
C. tepidum also exhibits use of both pyruvate and acetate as an organic carbon source.
Nitrogen fixation among green sulfur bacteria is generally typical of an anoxygenic phototroph, and requires the presence of light. Green sulfur bacteria exhibit activity from a
Type-1 secretion system and a ferredoxin-NADP+ oxidoreductase to generate reduced iron, a trait that evolved to support nitrogen fixation. Like purple sulfur bacteria, they can regulate the activity of nitrogenase post-translationally in response to ammonia concentrations. Their possession of
nif genes, even though evolutionarily distinct, may suggest their nitrogen fixation abilities arose in two different events or through a shared very distant ancestor. Examples of green sulfur bacteria capable of nitrogen fixation include the genus
Chlorobium and
Pelodictyon, excluding
P. phaeoclathratiforme.
Prosthecochloris aestuarii and
Chloroherpeton thalassium also fall into this category. Their fixation is widespread and plays an important role in overall nitrogen availability for ecosystems. Green sulfur bacteria living in coral reefs, such as
Prosthecochloris, are crucial in generating available nitrogen in the already nutrient-limited environment. ==See also==