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\subsubsection{Complexity in Latitudinal Gradient}  Comparing the average of complexity for an annual cycle in the Artic to Tropical transect as latitudinal gradient, we can see that NL appears to represent a transition point for complexity values (Fig. **). At this point for Physico-chemical subsystem decreasing complexity goes from very high to highcategory (0.6909),  by reason of emergence increasing (0.75). Then, at the tropical lake the category of complexity goes retuns  to very high levelagain,  due to  the increasing of regularity self-organization (regularity in variables)  and their consequently emergence reduction. For limiting nutrients subsystem, complexity has a sinusoidal behavior going to very high goes from hig  at the Ar to fair in NH; high category is maintaining in NL and T. The transition point for NL is more evident from emergence values because emergence is almost 0.62 (fair category). Emergence starts in the low category in Ar and finish in T in the same category. This means, limiting nutrient change to a greater proportion at NL latitudes. For Biomass, the transition at NL point is more evident than other subsystems because complexity values reach the higher category of Ar-T transect (0,74; very high category). For Ar and NH biomass, complexity value was classified in the low category and for T in very low.