Evidence map›Paper›PMID 32503635›Full record

ArticleMicrobiome2020

Winter warming in Alaska accelerates lignin decomposition contributed by Proteobacteria.

Xuanyu Tao, Jiajie Feng, Yunfeng Yang, Gangsheng Wang, Renmao Tian, Fenliang Fan, Daliang Ning, Colin T Bates, Lauren Hale, Mengting M Yuan and 13 more

Open access · goldAbstract read
In one paragraph

Article in Microbiome, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 20 papers.

0numbers the graph read from it
0cells of the map it votes in
20citing papers in PubMed
7.4field-weighted citation impact, top 2% 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

20 citing papers in PubMed, 80 citations in OpenAlex.

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  17. A Synergistic Consortium Involved inApplied and environmental microbiology · 2021
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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

23 authors at 9 institutions in 2 countries.

Xuanyu TaoDepartment of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Jiajie FengDepartment of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Yunfeng YangState Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, 100084, China. yangyf@tsinghua.edu.cn.
Gangsheng WangDepartment of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Renmao TianDepartment of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Fenliang FanKey Laboratory of Plant Nutrition and Fertilizer, Ministry of Agriculture, Institute of Agricultural Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing, 100081, China.
Daliang NingDepartment of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Colin T BatesDepartment of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Lauren HaleDepartment of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Mengting M YuanDepartment of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Linwei WuDepartment of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA.
Qun GaoState Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, 100084, China.
Jiesi LeiState Key Joint Laboratory of Environment Simulation and Pollution Control, School of Environment, Tsinghua University, Beijing, 100084, China.
Edward A G SchuurCenter for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ, 86011, USA.
Julian YuCollege of Integrative Sciences and Arts, Arizona State University, Mesa, AZ, 85212, USA.
Rosvel BrachoSchool of Forest Resources and Conservation, Department of Biology, University of Florida, Gainesville, FL, 32611, USA.
Yiqi LuoCenter for Ecosystem Science and Society, Northern Arizona University, Flagstaff, AZ, 86011, USA.
Konstantinos T KonstantinidisSchool of Civil and Environmental Engineering, School of Biology, and Center for Bioinformatics and Computational Genomics, Georgia Institute of Technology, Atlanta, GA, 30332, USA.
Eric R JohnstonSchool of Civil and Environmental Engineering, School of Biology, and Center for Bioinformatics and Computational Genomics, Georgia Institute of Technology, Atlanta, GA, 30332, USA.
James R ColeCenter for Microbial Ecology, Michigan State University, East Lansing, MI, 48824, USA.
C Ryan PentonCollege of Integrative Sciences and Arts, Arizona State University, Mesa, AZ, 85212, USA.
James M TiedjeCenter for Microbial Ecology, Michigan State University, East Lansing, MI, 48824, USA.
Jizhong ZhouDepartment of Microbiology and Plant Biology, University of Oklahoma, Norman, OK, 73019, USA. jzhou@ou.edu.
University of Oklahoma · USArizona State University · USGeorgia Institute of Technology · USMichigan State University · USNorthern Arizona University · USTsinghua University · CNInstitute of Agricultural Resources and Regional Planning · CNState Key Joint Laboratory of Environment Simulation and Pollution Control · CNUniversity of Florida · US

Funding

National Natural Science Foundation of China 41430856National Natural Science Foundation of China 41825016National Natural Science Foundation of China 41877048U.S. Department of Energy DE-SC0004601U.S. Department of Energy DE-SC0010715
6 · The paper itself

Abstract

backgroundIn a warmer world, microbial decomposition of previously frozen organic carbon (C) is one of the most likely positive climate feedbacks of permafrost regions to the atmosphere. However, mechanistic understanding of microbial mediation on chemically recalcitrant C instability is limited; thus, it is crucial to identify and evaluate active decomposers of chemically recalcitrant C, which is essential for predicting C-cycle feedbacks and their relative strength of influence on climate change. Using stable isotope probing of the active layer of Arctic tundra soils after depleting soil labile C through a 975-day laboratory incubation, the identity of microbial decomposers of lignin and, their responses to warming were revealed.

resultsThe β-Proteobacteria genus Burkholderia accounted for 95.1% of total abundance of potential lignin decomposers. Consistently, Burkholderia isolated from our tundra soils could grow with lignin as the sole C source. A 2.2 °C increase of warming considerably increased total abundance and functional capacities of all potential lignin decomposers. In addition to Burkholderia, α-Proteobacteria capable of lignin decomposition (e.g. Bradyrhizobium and Methylobacterium genera) were stimulated by warming by 82-fold. Those community changes collectively doubled the priming effect, i.e., decomposition of existing C after fresh C input to soil. Consequently, warming aggravates soil C instability, as verified by microbially enabled climate-C modeling.

conclusionsOur findings are alarming, which demonstrate that accelerated C decomposition under warming conditions will make tundra soils a larger biospheric C source than anticipated. Video Abstract.

Indexed as

LigninProteobacteriaSoil MicrobiologyAlaskaBurkholderiaClimate ChangeHot TemperaturePermafrostSoilTundraLigninSoil

Identifiers

PMID32503635
PMCPMC7275452
OpenAlexW3033476358

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.