"Photosynthetic microbes" refer to tiny living organisms that can use sunlight to produce energy through a process called photosynthesis.
Full definition
Along with weather and geologic processes on Earth removed carbon dioxide from the atmosphere, the expanding success
of photosynthetic microbes eventually created so much atmospheric oxygen and depleted methane and carbon dioxide levels to such an extent that the greenhouse effect may have become negligible around Year 2.1 billion, chilling the young Earth (Gabrielle Walker, New Scientist, 1999); and Evans and Kirschvink, 1997).
Venter and other scientists are experimenting
with photosynthetic microbes such as algae and cyanobacteria (sometimes referred to as blue - green algae).
Warmer waters also put them under stress, making them
expel photosynthetic microbes that provide most of their energy as well as their vibrant colours, leaving them a bleached white.
Some plants, such as soybeans, also store fats and can be used as fuel sources, but Bruce Rittmann, Vermaas's colleague at Arizona State, argues that
photosynthetic microbes produce nearly 250 times more fat per acre.
Unicellular photosynthetic microbes — phytoplankton — are responsible for virtually all oceanic primary production, which fuels marine food webs and plays a fundamental role in the global carbon cycle.
Huang's research addresses fundamental questions about the rules bacteria live by — for instance, what determines their shape and how different wavelengths of light affect the movement
of photosynthetic microbes (SN: 10/14/17, p. 17).
On the other hand, the hardy lichen partnership between fungi and
photosynthetic microbes has withstood the vicissitudes of time.
On the other hand, many anaerobic microbes including methanogens are easily poisoned by oxygen, and the recent discovery of banded sediments with rusted iron on Akilia Island in West Greenland suggests that oxygen - producing,
photosynthetic microbes (e.g., cyanobacteria) living on the surface of wet areas to gather sunlight may have developed by the end of this geologic period (3.85 billion years ago) despite continuing bombardment from space.
Even more crustal minerals were formed by plate tectonics with the help of lubricating ocean water, atmospheric oxygen from the successful development of
photosynthetic microbes, and land - based lichens (of algae and fungi) and mosses which were followed by deep - rooted plants that hastened the erosion and weathering of surface rocks with the help of biochemical action and the creation of soils as well as new clay minerals.
As I wrote in my first book on climate, in 1992, other life forms have had a big influence on the atmosphere (
photosynthetic microbes and plants, for instance), but they weren't aware of their potency.