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. 2020 Jul 27;14(12):2951–2966. doi: 10.1038/s41396-020-0723-2

Table 1.

Features that imposed selection and dispersal limitation in the Paraná fluvial system during different hydrological phases based on the model selection for βNTI and RCbray analysis.

Hydrological phase Features imposing selection Features imposing dispersal limitation
Low water (LW) PCA1: DO, pH, CDOM molecular weight NA
PCA3: unmeasured abiotic variable
PCA4: unmeasured abiotic variable
Low water + sedimentological pulse (LWs) PCA1: SPR, nitrate NA
PCA3: pH + unmeasured abiotic variable
PCA11: pH, CDOM molecular weight
High water (HW) PCA1: conductivity, DO, CDOM molecular weight PCA2
PCA3
Extraordinary high water (eHW) PCA1: CDOM molecular weight, CDOM concentration NA
PCA5: SPR
PCA6: SPR

The PCA axes retained during model selection for βNTI were considered as imposing selection and those significant for RCbray as imposing dispersal limitation. Within each PCA significant for βNTI, strong loading was considered as a measure or unmeasured variable imposing selection. Loading values for each PCA axes are presented in Supplementary Table S4.

DO dissolved oxygen, SPR soluble reactive phosphorous, CDOM chromophoric dissolved organic matter, NA indicated that nonsignificant PCA axes were retained in RCbray model selection.