Evidence map›Paper›PMID 35314706›Full record

ArticleNature communications2022

Microbiomes in the Challenger Deep slope and bottom-axis sediments.

Ying-Li Zhou, Paraskevi Mara, Guo-Jie Cui, Virginia P Edgcomb, Yong Wang

Abstract read
In one paragraph

Article in Nature communications, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 51 papers.

0numbers the graph read from it
0cells of the map it votes in
51citing 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

51 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

5 authors.

Ying-Li Zhou *Institute of Deep-Sea Science and Engineering, Chinese Academy of Sciences, Sanya, Hainan, China.ORCID http://orcid.org/0000-0002-3757-0029
Paraskevi Mara *Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, USA.ORCID http://orcid.org/0000-0003-0072-0238
Guo-Jie CuiInstitute of Deep-Sea Science and Engineering, Chinese Academy of Sciences, Sanya, Hainan, China.
Virginia P EdgcombDepartment of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA, USA.ORCID http://orcid.org/0000-0001-6805-381X
Yong WangInstitute of Deep-Sea Science and Engineering, Chinese Academy of Sciences, Sanya, Hainan, China. wangyong@sz.tsinghua.edu.cn.ORCID http://orcid.org/0000-0003-3595-3867

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Hadal trenches are the deepest and most remote regions of the ocean. The 11-kilometer deep Challenger Deep is the least explored due to the technical challenges of sampling hadal depths. It receives organic matter and heavy metals from the overlying water column that accumulate differently across its V-shaped topography. Here, we collected sediments across the slope and bottom-axis of the Challenger Deep that enable insights into its in situ microbial communities. Analyses of 586 metagenome-assembled genomes retrieved from 37 metagenomes show distinct diversity and metabolic capacities between bottom-axis and slope sites. 26% of prokaryotic 16S rDNA reads in metagenomes were novel, with novelty increasing with water and sediment depths. These predominantly heterotrophic microbes can recycle macromolecules and utilize simple and complex hydrocarbons as carbon sources. Metagenome and metatranscriptome data support reduction and biotransformation of arsenate for energy gain in sediments that present a two-fold greater accumulation of arsenic compared to non-hadal sites. Complete pathways for anaerobic ammonia oxidation are predominantly identified in genomes recovered from bottom-axis sediments compared to slope sites. Our results expand knowledge of microbially-mediated elemental cycling in hadal sediments, and reveal differences in distribution of processes involved in nitrogen loss across the trench.

Indexed as

BacteriaMicrobiotaGeologic SedimentsHeterotrophic ProcessesMetagenomeWaterWater

Identifiers

PMID35314706
PMCPMC8938466

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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.