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As long as the original population group "1-A" dominates the numbers of organisms in the
theoretical planet's oceans, each "year" (actually 1000 saturation cycles) will see another
set of second-level groups being created. Since these population sizes are the same as the
first "year's", the numbers are already calculated. In calculating third-level groups, we
thus see that they come from "first-year 2-A", "second-year 2-A", "first-year 2-B",
"second-year 2-B", "first-year 2-C", and "second-year 2-C". It deserves an illustration:
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