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The most common form, oxygenic photosynthesis, turns carbon dioxide, water and sunlight into food.
The ability of cyanobacteria to perform oxygenic photosynthesis is highly significant.
Modern photosynthesis in plants and most photosynthetic prokaryotes is oxygenic.
This occurs by oxidation of water in the case of oxygenic photosynthesis.
In oxygenic photosynthesis, the first electron donor is water, creating oxygen as a waste product.
In nature, free oxygen is produced by the light-driven splitting of water during oxygenic photosynthesis.
Oxygenic photosynthesis is used by the primary producers-plants, algae, and cyanobacteria.
He also made significant contributions to the development of the Z-scheme of oxygenic photosynthesis.
Dioxygen complexes are the precursors to other families of oxygenic ligands.
The research focuses on harnessing oxygenic photosynthesis in cyanobacteria for sustainable energy production.
Earth's atmosphere starts to become oxygenic.
For oxygenic photosynthesis, both photosystems I and II are required.
Chlorophyll a is a specific form of chlorophyll used in oxygenic photosynthesis.
Chlorophototrophy can further be divided into oxygenic photosynthesis and anoxygenic phototrophy.
The net-reaction of all light-dependent reactions in oxygenic photosynthesis is:
The symbiosis evolved around 1500 million years ago and enabled eukaryotes to carry out oxygenic photosynthesis.
This is called oxygenic photosynthesis.
It is estimated that the appearance of oxygenic photosynthesis increased biological productivity by a factor of between 100 and 1,000.
The enzyme is present in organisms capable of oxygenic photosynthesis, which includes plants, algae, and cyanobacteria.
Oxygenic photosynthesis accounts for virtually all of the production of organic matter from non-organic ingredients.
If this is true, and given the time estimates here, the evolutionary innovation of oxygenic photosynthesis may have had a relatively rapid impact on the environment.
In plants, cyanobacteria and algae, oxygenic photosynthesis splits water, with oxygen produced as a waste product.
Archean 2-methyl-hopanes also might have been produced by ancestral cyanobacteria that predated oxygenic photosynthesis.
The lack of large terrestrial vertebrate predators and the highly oxygenic atmosphere at that time probably enabled them to grow so large.
Also, the origin of oxygenic photosynthesis may have occurred at some time later than the origin of cyanobacteria.
