6. In the face of constant competition for the limited
amounts of organic matter, certain bacteria (if we may now call
them that) found ways to enhance their survival by using metalloporphyrins
and similar delocalized ring molecules to absorb solar energy. Perhaps
at first the absorbed energy was used only as heat to accelerate
all reactions uniformly. Later, this electronic excitation of chlorophyll
molecules was coupled to the production of ATP and NADH. Two of
the best reducing agents that were available, H2
and H2S, were used to supply reducing
equivalents for making NADH. Carbohydrates were synthesized from
this ATP, NADH, and atmospheric CO2
by taking some of the reactions of gluconeogenesis and turning them
into the Calvin cycle. The stage of the present-day green and purple
sulfur bacteria had been reached.
7. Sulfate, although not a substance that would have been present
in quantity on the primitive Earth, was given off as a waste product
from bacterial photosynthesis. The ancestors of Desulfovibrio developed
the ability to squeeze a little more energy out of their foods by
oxidizing them with this sulfate. Colonies of green sulfur bacteria
and sulfate-respiring bacteria could have existed in close symbiotic
association, as they sometimes do today, passing oxidized and reduced
sulfur compounds back and forth and drawing their common support
from the sun. Respiration had been invented, although not the kind
that was to dominate the planet in later years.
8. The slow development of a citric acid cycle as an alternate
source of NADH gradually liberated the purple sulfur bacteria from
their dependence on H2S and noncyclic
photosynthesis. The ancestors of the purple nonsulfur bacteria arose,
which were dependent mainly on cyclic photophosphorylation for ATP
energy.
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