Fig. 1: Changes in taxonomic diversity by soil layer during extended thaw incubation. | ISME Communications

Fig. 1: Changes in taxonomic diversity by soil layer during extended thaw incubation.

From: Genomic evidence that microbial carbon degradation is dominated by iron redox metabolism in thawing permafrost

Fig. 1

Beta diversity (A) ordination from principal coordinate analysis (PCoA) based on Bray-Curtis dissimilarity in the relative abundance of 16S rRNA amplicon sequence variants (ASVs) within each soil layer microbiome. Each point represents an individual sampling replicate from each soil layer collected at each incubation time point during the experiment (N = 27). B Venn diagram of unique and shared 16S ASVs for each soil layer microbiome. The total ASVs of each soil layer and those ASVs shared between soil layers are shown as counts. The relative abundance of ASVs associated with each count value is shown as a percentage in parentheses.

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