Evidence map›Paper›PMID 28332570›Full record

ArticleNature communications2017

Iron minerals within specific microfossil morphospecies of the 1.88 Ga Gunflint Formation.

Kevin Lepot, Ahmed Addad, Andrew H Knoll, Jian Wang, David Troadec, Armand Béché, Emmanuelle J Javaux

Abstract read
In one paragraph

Article in Nature communications, 2017. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 16 papers.

0numbers the graph read from it
0cells of the map it votes in
16citing 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

16 citing papers in PubMed.

  1. Article
  2. Article
  3. Article
  4. Primordial magnetotaxis in putative giant paleoproterozoic magnetofossils.Proceedings of the National Academy of Sciences of the United States of America · 2024
    Article
  5. Review
  6. Article
  7. Review
  8. Article
  9. Article
  10. Article
  11. Cyanobacteria evolution: Insight from the fossil record.Free radical biology & medicine · 2019
    Review
  12. Review
  13. A Field Guide to Finding Fossils on Mars.Journal of geophysical research. Planets · 2018
    Review
  14. Article
  15. Article
  16. 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

7 authors.

Kevin LepotLaboratoire d'Océanologie et de Géosciences, Université de Lille, CNRS UMR8187, Cité Scientifique, SN5, 59655 Villeneuve d'Ascq, France.ORCID 0000-0003-0556-0405
Ahmed AddadUnité Matériaux et Transformations, Université de Lille, CNRS UMR8207, Cité Scientifique C6, 59655 Villeneuve d'Ascq, France.
Andrew H KnollDepartment of Organismic and Evolutionary Biology, Harvard University, 26 Oxford Street, Cambridge, Massachusetts 02138, USA.
Jian WangCanadian Light Source Inc., University of Saskatchewan, 44 Innovation Boulevard, Saskatoon, Saskatchewan, Canada S7N 2V3.
David TroadecInstitut d'Electronique, de Micro-électronique et de Nanotechnologie, CNRS UMR8520, Avenue Poincaré, 59655 Villeneuve d'Ascq, France.
Armand BéchéElectron Microscopy for Material Science, University of Antwerp, Groenenborgerlaan 171, 2020 Antwerp, Belgium.
Emmanuelle J JavauxPaléobiogéologie, Paléobotanique &Paléopalynologie, UR Geology, Département de Géologie, Université de Liège, 14 Allée du 6 Août B18, Quartier Agora, 4000 Liège, Belgium.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Problematic microfossils dominate the palaeontological record between the Great Oxidation Event 2.4 billion years ago (Ga) and the last Palaeoproterozoic iron formations, deposited 500-600 million years later. These fossils are often associated with iron-rich sedimentary rocks, but their affinities, metabolism, and, hence, their contributions to Earth surface oxidation and Fe deposition remain unknown. Here we show that specific microfossil populations of the 1.88 Ga Gunflint Iron Formation contain Fe-silicate and Fe-carbonate nanocrystal concentrations in cell interiors. Fe minerals are absent in/on all organically preserved cell walls. These features are consistent with in vivo intracellular Fe biomineralization, with subsequent in situ recrystallization, but contrast with known patterns of post-mortem Fe mineralization. The Gunflint populations that display relatively large cells (thick-walled spheres, filament-forming rods) and intra-microfossil Fe minerals are consistent with oxygenic photosynthesizers but not with other Fe-mineralizing microorganisms studied so far. Fe biomineralization may have protected oxygenic photosynthesizers against Fe

Indexed as

FossilsGeologic SedimentsIronMicroscopy, Electron, Scanning TransmissionMineralsOntarioOxidation-ReductionOxygenPaleontologyPhotosynthesisIronMineralsOxygen

Identifiers

PMID28332570
PMCPMC5376642

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Registered trials

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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.