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. 2018 Nov 27;9:2891. doi: 10.3389/fmicb.2018.02891

Table 2.

The Spearman’s coefficients (ρ) and the corresponding p-values between the CL500-11 maximum abundance and environmental measurements in each lake.

Surface area Surface elevation Water retention time Maximum depth Water volume Hypolimnetic temperature during stratification pH (min) pH (max) TN (min) TN (max) TP (min) TP (max)
p-value 0.136 0.459 0.657 0.025 0.034 0.107 0.004 0.251 0.270 0.432 0.104 0.022
ρ 0.355 -0.181 0.109 0.512 0.488 0.381 0.631 0.277 0.284 0.204 0.385 0.520

The original data used for the statistics are available in Supplementary Table S2. p-values lower than 0.05 are shown in bold. For pH, TN, and TP, minimum (min) and maximum (max) values recorded in each lake were separately used. TP measurements below detection limits were replaced with the value of the detection limit.