Evidence map›Paper›PMID 27555839›Full record

ArticleFrontiers in microbiology2016

Soil Fungal:Bacterial Ratios Are Linked to Altered Carbon Cycling.

Ashish A Malik, Somak Chowdhury, Veronika Schlager, Anna Oliver, Jeremy Puissant, Perla G M Vazquez, Nico Jehmlich, Martin von Bergen, Robert I Griffiths, Gerd Gleixner

Open access · goldAbstract read
In one paragraph

Article in Frontiers in microbiology, 2016. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 54 papers.

0numbers the graph read from it
0cells of the map it votes in
54citing papers in PubMed
23.8field-weighted citation impact, top 1% 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

54 citing papers in PubMed, 436 citations in OpenAlex.

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  12. Principal role of fungi in soil carbon stabilization during early pedogenesis in the high Arctic.Proceedings of the National Academy of Sciences of the United States of America · 2024
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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

10 authors at 3 institutions in 3 countries.

Ashish A MalikDepartment of Biogeochemical Processes, Max Planck Institute for BiogeochemistryJena, Germany; Centre for Ecology and HydrologyWallingford, UK.
Somak ChowdhuryDepartment of Biogeochemical Processes, Max Planck Institute for Biogeochemistry Jena, Germany.
Veronika SchlagerDepartment of Biogeochemical Processes, Max Planck Institute for Biogeochemistry Jena, Germany.
Anna OliverCentre for Ecology and Hydrology Wallingford, UK.
Jeremy PuissantCentre for Ecology and Hydrology Wallingford, UK.
Perla G M VazquezDepartment of Biogeochemical Processes, Max Planck Institute for Biogeochemistry Jena, Germany.
Nico JehmlichDepartment of Proteomics, Helmholtz Centre for Environmental Research Leipzig, Germany.
Martin von BergenDepartment of Proteomics, Helmholtz Centre for Environmental ResearchLeipzig, Germany; Department of Metabolomics, Helmholtz Centre for Environmental ResearchLeipzig, Germany; Institute of Biochemistry, Faculty of Biosciences, Pharmacy and Psychology, University of LeipzigLeipzig, Germany; Department of Life Sciences and Chemistry, Aalborg UniversityAalborg, Denmark.
Robert I GriffithsCentre for Ecology and Hydrology Wallingford, UK.
Gerd GleixnerDepartment of Biogeochemical Processes, Max Planck Institute for Biogeochemistry Jena, Germany.
Max Planck Institute for Biogeochemistry · DEUK Centre for Ecology & Hydrology · GBHelmholtz Centre for Environmental Research · DE

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Despite several lines of observational evidence, there is a lack of consensus on whether higher fungal:bacterial (F:B) ratios directly cause higher soil carbon (C) storage. We employed RNA sequencing, protein profiling and isotope tracer techniques to evaluate whether differing F:B ratios are associated with differences in C storage. A mesocosm (13)C labeled foliar litter decomposition experiment was performed in two soils that were similar in their physico-chemical properties but differed in microbial community structure, specifically their F:B ratio (determined by PLFA analyses, RNA sequencing and protein profiling; all three corroborating each other). Following litter addition, we observed a consistent increase in abundance of fungal phyla; and greater increases in the fungal dominated soil; implicating the role of fungi in litter decomposition. Litter derived (13)C in respired CO2 was consistently lower, and residual (13)C in bulk SOM was higher in high F:B soil demonstrating greater C storage potential in the F:B dominated soil. We conclude that in this soil system, the increased abundance of fungi in both soils and the altered C cycling patterns in the F:B dominated soils highlight the significant role of fungi in litter decomposition and indicate that F:B ratios are linked to higher C storage potential.

Indexed as

bacteriafungilitter decompositionproteomicsRNA sequencingsoil carbonstable isotopes

Identifiers

PMID27555839
PMCPMC4977315
OpenAlexW2508177270

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.