Anoxygenic photosynthesis

During the Archean Era on Earth, the atmosphere lacked or was limited in oxygen, was highly abundant in iron, and had harmful ultraviolet (UV) rays due to a lack of an ozone layer. Sedimentary rock records in the ocean have suggested that anoxygenic photosynthesis evolved before oxygenic photosynthesis. One of the lines of evidence that suggests that the bacteria present during the Archean era were anoxygenic is because there was a lack of ferric iron minerals. As ferric minerals were not present, this suggests that oxygenic photosynthesis was not occurring, and oxygen was not being produced (i.e. anoxygenic). Instead of oxygen being the electron donor in the anoxygenic photosynthesis chemical reaction, hydrogen sulfide has been suggested instead. Serpentinizing hydrothermal vents have been present on the sea floor for 4.2 billion years, making it a long-standing Earth feature. Serpentinization, an ancient geochemical reaction within this feature, produces hydrogen-based compounds such as H2 and H2S. Chemolithoautotrophy where carbon dioxide is reduced to simple organic matter using H2 as an electron reducer is thought to have been the main process of primary production in this system prior to photosynthesis being developed. This made hydrogen a limiting factor in primary production. The electron transports chains found within anoxygenic photosynthetic bacteria involve cytochromes (heme) and quinones which are essential for the creation of chlorophyll (Chl). The biosynthesis of Chl is a pivotal step for the evolution of phototrophs. It is likely that the evolution of the critical photopigment developed in hydrothermal conditions where the ultraviolet rays that could be damaging to chlorophototrophs could not penetrate to that depth. The development of Chl helped lead to the development of two types of reaction centers (type I reaction center, RC1 & type II reaction center, RC 2). RC1 has been listed as a precursor to RC2, allowing for the for electrons to flow through ferredoxin, a small iron-sulfur protein, that transfers electrons and is in turn reduced to Fdred. This process allowed for chlorophototrophs to use H2S as an electron reducer, allowing for those organisms to move away from the dependency of H2. However all anoxygenic phototrophs use either RC1 or RC2. ==Bacteria==

Several groups of bacteria can conduct anoxygenic photosynthesis: green sulfur bacteria (GSB), Chloracidobacterium, heliobacteria, acidobacteriota, red and green filamentous phototrophs (FAPs e.g. Chloroflexia), and purple bacteria. Possibly also some members of Myxococcota, as they have been found to possess a photosynthesis gene cluster encoding a type-II reaction center with all enzymes and proteins required for photosynthesis. ==Pigments==

The photopigments used to carry out anaerobic photosynthesis are similar to chlorophyll but differ in molecular detail and peak wavelength of light absorbed. Bacteriochlorophylls a through g absorb electromagnetic radiation maximally in the near-infrared within their natural membrane milieu. This differs from chlorophyll a, the predominant plant and cyanobacteria pigment, which has peak absorption wavelength approximately 100 nanometers shorter (in the red portion of the visible spectrum). Predominantly found in anaerobic bacteria, they can be a major pigment used for anoxygenic photosynthesis.The quantity of light and the type of light that is absorbed is dependent on 1) the type of organism and 2) where the bacteriochlorophyll is located within the membrane. Generally however, bacteriochlorophyll absorb light at a spectrum between 800 and 1040 nm, for instance, green sulfur bacteria use BChl c through e at a range between 720 and 755 nm. ==Reaction centers==

There are two main types of anaerobic photosynthetic electron transport chains in bacteria. The type I reaction centers are found in GSB, Chloracidobacterium, and Heliobacteria, while the RC2 are found in FAPs and purple bacteria. Type I reaction centers The electron transport chain of green sulfur bacteria—such as is present in the model organism Chlorobaculum tepidum—uses the reaction center bacteriochlorophyll pair, P800/P840. The electron is transferred through a series of electron carriers and complexes until it is used to reduce NAD+ to NADH. Type II reaction centers Although the type II reaction centers are structurally and sequentially analogous to photosystem II (PSII) in plant chloroplasts and cyanobacteria, known organisms that exhibit anoxygenic photosynthesis do not have a region analogous to the oxygen-evolving complex of PSII. The electron transport chain of purple non-sulfur bacteria begins when the reaction center bacteriochlorophyll pair, P870, becomes excited from the absorption of light. Excited P870 will then donate an electron to bacteriopheophytin, which then passes it on to a series of electron carriers down the electron chain. In the process, it will generate an electrochemical gradient which can then be used to synthesize ATP. Molecular hydrogen in the bacterial environment is the usual electron donor. == See also ==