The first phototrophs were anoxygenic and likely used H₂S as electron donor for CO₂ fixation, generating elemental sulphur (S⁰) as a waste product. How could the first phototrophs have evolved at a time when life existed mostly near hydrothermal systems?
A clue came from the recent discovery of anoxygenic phototrophs living at hydrothermal vents in the complete darkness of the deep ocean. These phototrophs actually carry out photosynthesis using infrared radiation generated by the heat of hydrothermal vents.
Likewise, the first photosynthetic organisms likely lived in the dark, at hydrothermal vents where H₂S and infrared radiation were abundant. Diversification of anoxygenic phototrophs led to species that were able to use a range of electron donors including Fe²⁺, which was abundant throughout Earth’s early oceans.
The ability to use Fe²⁺ as an electron donor likely allowed early phototrophs to escape from hydrothermal systems and colonize shallow regions of Earth’s early oceans where light was abundant but where overlying water still provided protection from UV radiation.
The ability to use solar radiation as an energy source allowed phototrophs to diversify extensively. By 2.5-3.3 bya, the cyanobacterial lineage evolved a photosystem capable of oxygenic photosynthesis in which H₂O supplanted H₂S as the reductant for CO₂, thereby generating O₂ as a waste product.
About a billion years later, eukaryotic oxygen phototrophs appeared and can be seen in the microfossil record.
Which of the following chemical species played a crucial role in the early phototrophs' colonization in the shallow waters of Earth's early oceans?
Correct Answer: 3. Fe²⁺
Solution:"Diversification of anoxygenic phototrophs led to species that were able to use a range of electron donors including Fe²⁺, which was abundant throughout Earth's early oceans.
The ability to use Fe²⁺ as an electron donor likely allowed early phototrophs to escape from hydrothermal systems and colonize shallow regions..."
This clearly indicates that Fe²⁺ was the key electron donor that enabled colonization of shallow waters by early phototrophs.