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. 2017 Mar 27;8:466. doi: 10.3389/fmicb.2017.00466

Figure 5.

Figure 5

(A) Principal component analysis with the different bacterial phyla. The first principal component (PC1) explained 26% of the variation and PC2 12%. Principal component analysis with the different archaeal groups from the first sampling site at Texcoco soil never flooded (Inline graphic), flooded once (Inline graphic), flooded twice (Inline graphic), three times (Inline graphic), six times (Inline graphic), seven times (Inline graphic), nine times (Inline graphic) or ten times (Inline graphic), second sampling site never flooded (Inline graphic), flooded once (Inline graphic), flooded twice (Inline graphic), flooded three times (Inline graphic), six times (Inline graphic), seven times (Inline graphic), nine times (Inline graphic) or ten times (Inline graphic), and third sampling site never flooded (Inline graphic), flooded once (Inline graphic), flooded twice (Inline graphic), flooded three times (Inline graphic), six times (Inline graphic), seven times (Inline graphic), nine times (Inline graphic) or ten times (Inline graphic). The first principal component (PC1) explained 22% of the variation and PC2 17%. (B) Principal coordinate analysis of the weighted UniFrac distances of the bacterial OTUs clustered at a 97% similarity. Legends of the figure are the same as (A).