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

