Evidence map›Paper›PMID 25246590›Full record

ArticleProceedings of the National Academy of Sciences of the United States of America2014

Iron oxides stimulate sulfate-driven anaerobic methane oxidation in seeps.

Orit Sivan, Gilad Antler, Alexandra V Turchyn, Jeffrey J Marlow, Victoria J Orphan

Open access · bronzeAbstract read
In one paragraph

Article in Proceedings of the National Academy of Sciences of the United States of America, 2014. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 19 papers.

0numbers the graph read from it
0cells of the map it votes in
19citing papers in PubMed
11.5field-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

19 citing papers in PubMed, 141 citations in OpenAlex.

  1. Article
  2. Article
  3. Article
  4. Tracing the Century-Long Evolution of Microplastics Deposition in a Cold Seep.Advanced science (Weinheim, Baden-Wurttemberg, Germany) · 2023
    Article
  5. Article
  6. A Reduced FJournal of bacteriology · 2022
    Article
  7. Article
  8. Article
  9. Editorial: Advances in Microbial Iron Cycling.Frontiers in microbiology · 2022
    Article
  10. Article
  11. Genomic Insights Into theFrontiers in microbiology · 2021
    Article
  12. Article
  13. Article
  14. Review
  15. Article
  16. Article
  17. Article
  18. Article
  19. Article
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 at 3 institutions in 3 countries.

Orit SivanDepartment of Geological and Environmental Sciences, Ben Gurion University of the Negev, Beer-Sheva 84105, Israel; oritsi@bgu.ac.il.
Gilad AntlerDepartment of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom; and.
Alexandra V TurchynDepartment of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom; and.
Jeffrey J MarlowDivision of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125.
Victoria J OrphanDivision of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125.
California Institute of Technology · USUniversity of Cambridge · GBBen-Gurion University of the Negev · IL

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Seep sediments are dominated by intensive microbial sulfate reduction coupled to the anaerobic oxidation of methane (AOM). Through geochemical measurements of incubation experiments with methane seep sediments collected from Hydrate Ridge, we provide insight into the role of iron oxides in sulfate-driven AOM. Seep sediments incubated with (13)C-labeled methane showed co-occurring sulfate reduction, AOM, and methanogenesis. The isotope fractionation factors for sulfur and oxygen isotopes in sulfate were about 40‰ and 22‰, respectively, reinforcing the difference between microbial sulfate reduction in methane seeps versus other sedimentary environments (for example, sulfur isotope fractionation above 60‰ in sulfate reduction coupled to organic carbon oxidation or in diffusive sedimentary sulfate-methane transition zone). The addition of hematite to these microcosm experiments resulted in significant microbial iron reduction as well as enhancing sulfate-driven AOM. The magnitude of the isotope fractionation of sulfur and oxygen isotopes in sulfate from these incubations was lowered by about 50%, indicating the involvement of iron oxides during sulfate reduction in methane seeps. The similar relative change between the oxygen versus sulfur isotopes of sulfate in all experiments (with and without hematite addition) suggests that oxidized forms of iron, naturally present in the sediment incubations, were involved in sulfate reduction, with hematite addition increasing the sulfate recycling or the activity of sulfur-cycling microorganisms by about 40%. These results highlight a role for natural iron oxides during bacterial sulfate reduction in methane seeps not only as nutrient but also as stimulator of sulfur recycling.

Indexed as

anaerobic respirationANME archaeadeep-seamethanotrophyredox

Identifiers

PMID25246590
PMCPMC4209987
OpenAlexW2111843680

What OpenQuestion holds

Textmetadata
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.