13 research outputs found

    Water chemical parameters from representative areas in the cave.

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    <p>SI<sub>calcite</sub> was calculated using the Merlak algorithm [<a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0180700#pone.0180700.ref037" target="_blank">37</a>].</p

    Representative sampling sites in the cave.

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    <p>A) Calcite raft deposit at Chaos (SO1); B) moonmilk deposit at Piredda Hall (SO2 & SO3); C) manganese oxide deposit at Water Tower site (SO6) and D) sampling of a limestone wall at location Shaft (SO4)</p

    Impact of human exploration on the microbial diversity in a hypogean system.

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    <p>The most abundant human associated genera (as previously described by The Human Microbiome Project Consortium) were used for this analysis and include <i>Lactobacillus</i>, <i>Propionibacterium</i>, <i>Streptococcus</i>, <i>Bacteroides</i>, <i>Corynebacterium</i>, <i>Staphylococcus</i>, <i>Moraxella</i>, <i>Haemophilus</i>, <i>Prevotella</i>, and <i>Veillonella</i>.</p

    Relative class abundance of A) the whole cave and B) separated into the different sampling sites.

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    <p>Phylogenetic groups accounting for ≤ 5% of all classified sequences are summarized in the artificial group “others” (Part B). Full relative class abundance is given in Supplementary <a href="http://www.plosone.org/article/info:doi/10.1371/journal.pone.0180700#pone.0180700.t003" target="_blank">Table 3</a>.</p

    Gene structure of putative <i>phrA</i> gene of <i>R. varieornatus</i>.

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    <p>(A) Exon-intron structures of <i>phrA</i> in <i>R. varieornatus</i> and <i>D. melanogaster</i>. (B) Amino acid sequence alignment of the <i>phrA</i> genes between <i>R. varieornatus</i> and <i>D. melanogaster</i>.</p
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