deletions | additions       diff --git a/Results.tex b/Results.tex  index 727e3bb..008bb54 100644  --- a/Results.tex  +++ b/Results.tex 
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For the NH, planktonic carbon dioxide (PCD= 9788.5 $\pm$ 2119.1) had very high emergence. Inflow and benthic carbon dioxide (ICD= 10005.7 $\pm$ 1418.2, BCD= 7571.1 $\pm$ 3150.3) were in high emergence category. In contrast, variables with very high self-organization were siliciates in planktonic and benthic zone (PS= 25257.32 $\pm$ 7025.4 BS= 25703.99 $\pm$ 7216.8), phosphorous in 3 layers (IP,PP and BP= 7.69 $\pm$ 2.26) and nitrogen in inflow and planktonic zone (IN and PN= 62.91 $\pm$ 15.1); nitrogen in benthic was high self-organization (79.21 $\pm$ 9.34). Variables in the very high complexity category were inflow silicates (IS), carbon dioxide in inflow and Benthos (ICD,BCD), and detritus (PDt,BDt).  At the NL, due an increasing in the emergence of nitrogen (143.4 $\pm$ 39.08) and decreasing in the self-organization of detritus (228989.6 $\pm$ 245332.9), 13 of the 16 variables of the limiting nutrient components was classified in very high and high complexity categories. Carbon dioxide in planktonic and benthic zones (PCD= 9746.7 $\pm$ 1477.7  and BCD=), BCD= 10888.03 $\pm$ 2105),  and benthic detritus (BDt=) because of their very high emergence (BDt= 457320.9 $\pm$ 126432.4)  were categorized as low complexity variables. variables because of their very high emergence.  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. From PCA ordination for limiting nutrients at all lakes, the groups that can be identified were a first group representing emergence with detritus and carbon dioxide variables. A second group representing self-organization in nitrogen and inflow phosphorous. A third group representing complexity variables with silicates and phosphorous in planktonic and benthic zone.  \subsubsection{Complexity in Biomass Subsystem}  At the Arctic, self-organization for all groups of phyto and zooplankton species in all zones, were high or very high. Only the low emergences of diatoms, diatoms (PD and BD = 185.4 $\pm$ 191.3),  cyanobacteria (PCy and BCy= 118.9 $\pm$ 169.3)  and green algae (PGA and BGA= 164.2 $\pm$ 160.6)  permits that these photosynthetic organisms reach very high levels of complexity and autopoiesis. This situation continuing in NH in spite of planktonic diatoms (PD= 281.12 $\pm$ 209.35)  and cyanobacteria (PCy= 162.9 $\pm$ 169.5)  reached the fair category of emergence. It means, the feature of this two types of lakes is their regularity. In a similar waythat  with limiting nutrient subsystem, when gradient Ar-T reaches the NL point, the dynamics of emergence and self-organization varies in considerable level. Here, the complexity of almost all variables were maximum due the balance in self-organization and emergence. Only, chlorophiceas, Only chlorophiceas (PCh= 6.2 $\pm$ 5.1),  benthic detritus (BDt= 3.8 $\pm$ 71.7)  and fishes ($\pm$)  in planktonic and benthic zones have regularity for all annual cycle. In contrast to the NL, the biomass subsystem in the tropic reflects very low complexity due the very high self-organization of the living taxa. Only planktonic and piscivorous fishes have very high and high complexity, respectively. 
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\subsection{Homeostasis}  \begin{tabbing}  Nombre \= Apellido \= Padron\\   Esteban \> Quito \> 80000\\   Elena \> Nito \> 80001\\   Olga \> Sana \> 80002\\   \end{tabbing}