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Research Article

Metaproteomics reveals differential modes of metabolic coupling among ubiquitous oxygen minimum zone microbes

Alyse K. Hawley, Heather M. Brewer, Angela D. Norbeck, Ljiljana Paša-Tolić, and Steven J. Hallam
PNAS August 5, 2014 111 (31) 11395-11400; first published July 22, 2014; https://doi.org/10.1073/pnas.1322132111
Alyse K. Hawley
aDepartment of Microbiology and Immunology,
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Heather M. Brewer
bBiological and Computational Sciences Division, Pacific Northwest National Laboratory, Richland, WA 99352
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Angela D. Norbeck
bBiological and Computational Sciences Division, Pacific Northwest National Laboratory, Richland, WA 99352
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Ljiljana Paša-Tolić
bBiological and Computational Sciences Division, Pacific Northwest National Laboratory, Richland, WA 99352
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Steven J. Hallam
aDepartment of Microbiology and Immunology,
cGraduate Program in Bioinformatics, and
dGenome Sciences and Technology Training Program, University of British Columbia, Vancouver, BC, Canada V6T 1Z3; and
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  • For correspondence: shallam@mail.ubc.ca
  1. Edited by Edward F. DeLong, Massachusetts Institute of Technology, Cambridge, MA, and approved June 10, 2014 (received for review November 26, 2013)

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    Fig. 1.

    Hierarchical clustering of metaproteome by NSAF (see Methods) for detected proteins from Sep09 S2, S3, and S4 indicating compartments of the water column, with adjacent sparklines for oxygen (O2), nitrate (NO3−), and hydrogen sulfide (H2S) for each sample.

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    Fig. 2.

    Distribution and NSAF value of proteins involved in nitrogen and sulfur-based energy metabolism and inorganic carbon fixation for taxa abundant in the metaproteome. For metagenome (gray, Apr08 only) and metaproteome in upper oxycline (green), lower oxycline (teal), S/N transition zone (blue), and sulfidic zone (purple). See Table S4 for full list of protein names; Anx indicates anammox hydroxylamine oxidoreductase and hydrazine oxidoreductase proteins.

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    Fig. 3.

    Relative abundance of SUP05 genes and proteins in two overlapping SUP05 fosmid sequences (GQ351266 and GQ351267) (16). Metagenome (gray, Apr08 only) and metaproteome for the upper oxycline (green), lower oxycline (teal), S/N transition zone (blue), and sulfidic zone (purple). Selected SUP05 genes involved in denitrification (dark gray shading), sulfide oxidation (black shading), and putative hydroxylamine oxidoreductase (diagonal lines) are indicated. Protein abundance shown as summed NSAF values for all detected ORFs with top hit to a given SUP05 protein. Metagenome abundances shown as percentage of ORFs with top hit to a given SUP05 gene with sparklines for oxygen (O2), nitrate (NO3−), and hydrogen sulfide (H2S) for each sample.

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    Fig. 4.

    Proposed metabolic model based on metaproteomic observations for heterotrophic remineralization (brown) and energetic coupling (yellow dashed lines) of nitrogen (green), sulfur (red), and hydrogen (orange) based chemolithotrophic energy metabolism with carbon fixation (yellow star) for taxa abundant in the metaproteome. Line weight and arrow size indicate magnitude of metabolic activity. Gray lines, activity not occurring under given conditions; light gray taxa, reduced abundance and metabolic activity.

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Metaproteomics of coupled biogeochemical cycling
Alyse K. Hawley, Heather M. Brewer, Angela D. Norbeck, Ljiljana Paša-Tolić, Steven J. Hallam
Proceedings of the National Academy of Sciences Aug 2014, 111 (31) 11395-11400; DOI: 10.1073/pnas.1322132111

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Metaproteomics of coupled biogeochemical cycling
Alyse K. Hawley, Heather M. Brewer, Angela D. Norbeck, Ljiljana Paša-Tolić, Steven J. Hallam
Proceedings of the National Academy of Sciences Aug 2014, 111 (31) 11395-11400; DOI: 10.1073/pnas.1322132111
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