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\subsubsection{Complexity in the Limiting Nutrient Subsystem}  Limiting nutrients shown at the Arctic high changes in inflow silicates (SL), carbon dioxide in the inflow and planktonic Zones (ICD, PCD). Very High regularity in nitrogen at the 3 layers of lakes; high regularity in silicates, phosporous in plankctonic and bencthic zones (PS, BS, PP, BP). Also, planktonic detritus (PDt). In complexity terms very high category was for IS, PP,BP, CCD BCD  and planktonic and benthonic  detritus. For the NH, carbon dioxide (PCD) had very high emergence at planktonic zone and high in inflow and C** (CCD). benthic carbon dioxide (BCD).  In contrast, variables with very high self-organization were siliciates in planktonic and benthic zone, nitrogen and phosphorous in 3 layers were in (nitrogen in benthic was high S). Variables in the very high complexity category were inflow silicates (due to high E and low S), carbon dioxide in inflow and C**, and detritus. At the NL, due an increasing in the emergence of nitrogen and decreasing in the self-organization of detritus, 13 of the 16 variables of the limiting nutrient components was classified in very high and high complexity categories. Carbon dioxide in planktonic and C**, and benthic detritus because of their very high emergence were categorized as low complexity variables. At this point of the gradient Ar-T, complexity of the limiting nutrients subsystem has an important variation in terms of its increasing with respect of Ar and NH levels. This levels continuous its increment due the balance between emergence and self-organization values at the end of the gradient. This way, at the tropic lake a very high levels of complexity for the majority of variables are shown. Only a very high emergence of detritus were the exception.