Evidence map›Paper›PMID 32047154›Full record

ArticleNature communications2020

Distinct iron cycling in a Southern Ocean eddy.

Michael J Ellwood, Robert F Strzepek, Peter G Strutton, Thomas W Trull, Marion Fourquez, Philip W Boyd

Open access · goldAbstract read
In one paragraph

Article in Nature communications, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 13 papers.

0numbers the graph read from it
0cells of the map it votes in
13citing papers in PubMed
12.1field-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

13 citing papers in PubMed, 89 citations in OpenAlex.

  1. Article
  2. Article
  3. Article
  4. Enhancing impacts of mesoscale eddies on Southern Ocean temperature variability and extremes.Proceedings of the National Academy of Sciences of the United States of America · 2023
    Article
  5. Article
  6. Review
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  8. Article
  9. Article
  10. Article
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  12. Article
  13. Anthropogenic Asian aerosols provide Fe to the North Pacific Ocean.Proceedings of the National Academy of Sciences of the United States of America · 2020
    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

6 authors at 3 institutions in 1 country.

Michael J EllwoodResearch School of Earth Sciences, Australian National University, Canberra, Australia. Michael.ellwood@anu.edu.au.ORCID http://orcid.org/0000-0003-4288-8530
Robert F StrzepekInstitute for Marine and Antarctic Studies, University of Tasmania, Hobart, Australia.ORCID http://orcid.org/0000-0002-6442-7121
Peter G StruttonInstitute for Marine and Antarctic Studies, University of Tasmania, Hobart, Australia.
Thomas W TrullCSIRO Oceans and Atmosphere, Hobart, Australia.
Marion FourquezInstitute for Marine and Antarctic Studies, University of Tasmania, Hobart, Australia.
Philip W BoydInstitute for Marine and Antarctic Studies, University of Tasmania, Hobart, Australia.ORCID http://orcid.org/0000-0001-7850-1911
University of Tasmania · AUAustralian National University · AUCSIRO Oceans and Atmosphere · AU

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Mesoscale eddies are ubiquitous in the iron-limited Southern Ocean, controlling ocean-atmosphere exchange processes, however their influence on phytoplankton productivity remains unknown. Here we probed the biogeochemical cycling of iron (Fe) in a cold-core eddy. In-eddy surface dissolved Fe (dFe) concentrations and phytoplankton productivity were exceedingly low relative to external waters. In-eddy phytoplankton Fe-to-carbon uptake ratios were elevated 2-6 fold, indicating upregulated intracellular Fe acquisition resulting in a dFe residence time of ~1 day. Heavy dFe isotope values were measured for in-eddy surface waters highlighting extensive trafficking of dFe by cells. Below the euphotic zone, dFe isotope values were lighter and coincident with peaks in recycled nutrients and cell abundance, indicating enhanced microbially-mediated Fe recycling. Our measurements show that the isolated nature of Southern Ocean eddies can produce distinctly different Fe biogeochemistry compared to surrounding waters with cells upregulating iron uptake and using recycling processes to sustain themselves.

Indexed as

Oceans and SeasAtmosphereCarbonChlorophyllIronMarine BiologyModels, BiologicalPhytoplanktonSeawaterTemperatureTrace ElementsCarbonChlorophyllIronTrace Elements

Identifiers

PMID32047154
PMCPMC7012851
OpenAlexW3005594733

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.