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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 and detritus.
For the NH, carbon dioxide (PCD) had very high emergence at planktonic zone and high in inflow and C** (CCD). 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.
Due At the NL, due an increasing in the emergence of nitrogen and decreasing in the
S self-organization of
detritus detritus, 13 of the 16 variables of the limiting nutrient components was classified in very high and high complexity categories.
Variables that no reach the above level were due to their very high emergence like Carbon
Dioxide dioxide in planktonic and
C, C**, and
Benthic detritus. benthic detritus because of their very high emergence were categorized as low complexity variables. At this point of the gradient
Ar-T Ar-T, complexity
of the limiting nutrients subsystem has an important variation
that in terms of its increasing with respect of Ar and NH levels. This levels continuous its increment
of due the balance between emergence and self-organization
values at the end of the gradient. This
way in way, at the tropic
lake a very high levels of complexity for the majority of variables are shown. Only
the a very high emergence of detritus were the exception.
In consequence in the tropic limiting nutrients in general have positive autopoiesis defining more autonomy for adaptation.
In gradient Ar-T there are an increasing of very high complexity category for all variables, only IS having high complexity due to high emergence. From PCA
ordination, ordination for limiting nutrients at all lakes, the groups that can be identified
are Group were a first group representing
emergence: Detritus, Carbon Dioxide. Group emergence with detritus and carbon dioxide variables. A second group representing self-organization
Nitrogen in nitrogen and
Inflow Phosphorous. Group inflow phosphorous. A third group representing complexity
Silicates variables with silicates and
Phosphorous phosphorous in
Planktonic planktonic and
Benthic benthic zone.
\subsubsection{Complexity in Biomass Subsystem}