Evidence map›Paper›PMID 34459543›Full record

ArticleMicrobiologyOpen2021

Active microbial ecosystem in glacier basal ice fuelled by iron and silicate comminution-derived hydrogen.

Mario Toubes-Rodrigo, Sanja Potgieter-Vermaak, Robin Sen, Edda S Oddsdóttir, David Elliott, Simon Cook

Open access · goldAbstract read
In one paragraph

Article in MicrobiologyOpen, 2021. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 6 papers.

0numbers the graph read from it
0cells of the map it votes in
6citing papers in PubMed
1.0field-weighted citation impact, top 23% of its field
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

6 citing papers in PubMed, 10 citations in OpenAlex.

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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

6 authors at 5 institutions in 2 countries.

Mario Toubes-RodrigoAstrobiologyOU, Faculty of Science, Technology, Engineering and Mathematics, The Open University, Milton Keynes, UK.ORCID 0000-0001-7884-7285
Sanja Potgieter-VermaakDepartment of Natural Sciences, Ecology and Environment Research Centre, Manchester Metropolitan University, Manchester, UK.ORCID 0000-0002-1994-7750
Robin SenDepartment of Natural Sciences, Ecology and Environment Research Centre, Manchester Metropolitan University, Manchester, UK.ORCID 0000-0002-1914-2178
Edda S OddsdóttirIcelandic Forest Research, Reykjavik, Iceland.ORCID 0000-0002-7811-5719
David ElliottEnvironmental Sustainability Research Centre, University of Derby, Derby, UK.ORCID 0000-0001-9837-7890
Simon CookGeography and Environmental Science, University of Dundee, Dundee, UK.
Manchester Metropolitan University · GBInnovation Center Iceland · ISThe Open University · GBUniversity of Derby · GBUniversity of Dundee · GB

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The basal zone of glaciers is characterized by physicochemical properties that are distinct from firnified ice due to strong interactions with underlying substrate and bedrock. Basal ice (BI) ecology and the roles that the microbiota play in biogeochemical cycling, weathering, and proglacial soil formation remain poorly described. We report on basal ice geochemistry, bacterial diversity (16S rRNA gene phylogeny), and inferred ecological roles at three temperate Icelandic glaciers. We sampled three physically distinct basal ice facies (stratified, dispersed, and debris bands) and found facies dependent on biological similarities and differences; basal ice character is therefore an important sampling consideration in future studies. Based on a high abundance of silicates and Fe-containing minerals and, compared to earlier BI literature, total C was detected that could sustain the basal ice ecosystem. It was hypothesized that C-fixing chemolithotrophic bacteria, especially Fe-oxidisers and hydrogenotrophs, mutualistically support associated heterotrophic communities. Basal ice-derived rRNA gene sequences corresponding to genera known to harbor hydrogenotrophic methanogens suggest that silicate comminution-derived hydrogen can also be utilized for methanogenesis. PICRUSt-predicted metabolism suggests that methane metabolism and C-fixation pathways could be highly relevant in BI, indicating the importance of these metabolic routes. The nutrients and microbial communities release from melting basal ice may play an important role in promoting pioneering communities establishment and soil development in deglaciating forelands.

Indexed as

BacteriaCarbon CycleChemoautotrophic GrowthEcosystemExtremophilesGeologic SedimentsHydrogenIce CoverIronMethaneOxidation-ReductionRNA, Ribosomal, 16SSilicatesHydrogenIronMethaneRNA, Ribosomal, 16SSilicatescryosphereenvironmental microbiologyextremophilesglaciersmicrobial ecology

Identifiers

PMID34459543
PMCPMC8289488
OpenAlexW3184099201

What OpenQuestion holds

Textmetadata
LicenceCC BY
Read underepoch 390

Registered trials

None linked

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.