Evidence map›Paper›PMID 40770184›Full record

ArticleNature communications2025

Metal-driven anaerobic oxidation of methane and the Sturtian deglaciation.

Jun Hu, Sanzhong Li, Shui-Jiong Wang, Jörn Peckmann, Hongxiang Guan, Shao-Yong Jiang, Wei Chen, Huan Cui, Zheng Qin, Peng Liu and 9 more

Abstract read
PubMed Full text at PMC Publisher
In one paragraph

Article in Nature communications, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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

0 citing papers in PubMed.

No citing paper in PubMed yet.

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

19 authors.

Jun HuFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China.ORCID http://orcid.org/0000-0002-4143-2809
Sanzhong LiFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China. sanzhong@ouc.edu.cn.ORCID http://orcid.org/0000-0002-3436-2793
Shui-Jiong WangState Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (Beijing), Beijing, China. wsj@cugb.edu.cn.ORCID http://orcid.org/0000-0002-2111-0255
Jörn PeckmannFachbereich Erdsystemwissenschaften, Universität Hamburg, Hamburg, Germany.ORCID http://orcid.org/0000-0002-8572-0060
Hongxiang GuanFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China.
Shao-Yong JiangState Key Laboratory of Geological Processes and Mineral Resources, School of Earth Resources, China University of Geosciences, Wuhan, China.ORCID http://orcid.org/0000-0003-3921-739X
Wei ChenState Key Laboratory of Geological Processes and Mineral Resources, School of Earth Resources, China University of Geosciences, Wuhan, China.
Huan CuiDepartment of Geology, Kansas State University, Manhattan, KS, USA.ORCID http://orcid.org/0000-0003-0705-3423
Zheng QinState Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (Beijing), Beijing, China.
Peng LiuFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China.ORCID http://orcid.org/0000-0003-4175-504X
Yanhui SuoFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China.
Zhaoxia JiangFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China.
Dongyong LiFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China.
Nan WangFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China.
Xiaohui LiFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China.ORCID http://orcid.org/0000-0001-7227-0788
Yuan ZhongFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China.
Ruru LiFrontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE and College of Marine Geosciences, Ocean University of China, Qingdao, China.
Xi-Ming YangState Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences (Beijing), Beijing, China.
Kurt O KonhauserDepartment of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada.ORCID http://orcid.org/0000-0001-7722-7068

Funding

National Natural Science Foundation of China (National Science Foundation of China) 2172079 to J.H., 42121005 to S.Z.L., 41973010 to S.-J.W., 42488201 to W.J.X. and 42475052 to P.L
6 · The paper itself

Abstract

The Sturtian and Marinoan glaciations shaped Neoproterozoic palaeoenvironmental evolution. While methane emission likely intensified the Marinoan greenhouse effect, its role during the Sturtian glaciation-coinciding with widespread iron formations (IFs)-remains poorly understood. Here, we analysed bio-essential metals (Ni, Co, Zn), rare earth elements and yttrium (REY), Fe (δ

Identifiers

PMID40770184
PMCPMC12328600

What OpenQuestion holds

Textmetadata
LicenceCC BY-NC-ND
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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.