Evidence map›Paper›PMID 28729646›Full record

ArticleScientific reports2017

Climate oscillations reflected within the microbiome of Arabian Sea sediments.

William D Orsi, Marco J L Coolen, Cornelia Wuchter, Lijun He, Kuldeep D More, Xabier Irigoien, Guillem Chust, Carl Johnson, Jordon D Hemingway, Mitchell Lee and 2 more

Abstract read
In one paragraph

Article in Scientific reports, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 28 papers.

0numbers the graph read from it
0cells of the map it votes in
28citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

28 citing papers in PubMed.

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4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

12 authors.

William D OrsiMarine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, USA. w.orsi@lrz.uni-muenchen.de.
Marco J L CoolenMarine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, USA. marco.coolen@curtin.edu.au.
Cornelia WuchterMarine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, USA.
Lijun HeState Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai, 200062, China.
Kuldeep D MoreWestern Australia Organic and Isotope Geochemistry Centre (WA-OIGC), Department of Chemistry, Curtin University, Bentley, WA, 6102, Australia.
Xabier IrigoienAZTI - Marine Research, Herrera Kaia, Portualdea z/g, 20110, Pasaia (Gipuzkoa), Spain.
Guillem ChustAZTI-Tecnalia, Marine Research Division, Txatxarramendi ugartea z/g, 48395, Sukarrieta (Bizkaia), Spain.
Carl JohnsonMarine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, USA.
Jordon D HemingwayMarine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, USA.
Mitchell LeeMarine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, USA.
Valier GalyMarine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, USA.ORCID 0000-0003-0385-8443
Liviu GiosanGeology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, USA.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Selection of microorganisms in marine sediment is shaped by energy-yielding electron acceptors for respiration that are depleted in vertical succession. However, some taxa have been reported to reflect past depositional conditions suggesting they have experienced weak selection after burial. In sediments underlying the Arabian Sea oxygen minimum zone (OMZ), we performed the first metagenomic profiling of sedimentary DNA at centennial-scale resolution in the context of a multi-proxy paleoclimate reconstruction. While vertical distributions of sulfate reducing bacteria and methanogens indicate energy-based selection typical of anoxic marine sediments, 5-15% of taxa per sample exhibit depth-independent stratigraphies indicative of paleoenvironmental selection over relatively short geological timescales. Despite being vertically separated, indicator taxa deposited under OMZ conditions were more similar to one another than those deposited in bioturbated intervals under intervening higher oxygen. The genomic potential for denitrification also correlated with palaeo-OMZ proxies, independent of sediment depth and available nitrate and nitrite. However, metagenomes revealed mixed acid and Entner-Dourdoroff fermentation pathways encoded by many of the same denitrifier groups. Fermentation thus may explain the subsistence of these facultatively anaerobic microbes whose stratigraphy follows changing paleoceanographic conditions. At least for certain taxa, our analysis provides evidence of their paleoenvironmental selection over the last glacial-interglacial cycle.

Indexed as

ClimateMicrobiotaGeologic SedimentsMetagenomeMetagenomicsOceans and SeasRNA, Ribosomal, 16SSeawaterRNA, Ribosomal, 16S

Identifiers

PMID28729646
PMCPMC5519670

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Registered trials

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.