Evidence map›Paper›PMID 31492930›Full record

ArticleScientific reports2019

Flow-driven micro-scale pH variability affects the physiology of corals and coralline algae under ocean acidification.

S Comeau, C E Cornwall, C A Pupier, T M DeCarlo, C Alessi, R Trehern, M T McCulloch

Open access · goldAbstract read
In one paragraph

Article in Scientific reports, 2019. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 10 papers.

0numbers the graph read from it
0cells of the map it votes in
10citing papers in PubMed
6.6field-weighted citation impact, top 3% 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

10 citing papers in PubMed, 58 citations in OpenAlex.

  1. Article
  2. Article
  3. Article
  4. Article
  5. Experimental coral reef communities transform yet persist under mitigated future ocean warming and acidification.Proceedings of the National Academy of Sciences of the United States of America · 2024
    Article
  6. Article
  7. Dual-Lifetime Referencing (Sensors (Basel, Switzerland) · 2023
    Article
  8. Article
  9. Article
  10. Global declines in coral reef calcium carbonate production under ocean acidification and warming.Proceedings of the National Academy of Sciences of the United States of America · 2021
    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 at 2 institutions in 4 countries.

S ComeauThe University of Western Australia, Oceans Graduate School and Oceans Institute, 35 Stirling Highway, Crawley, 6009, Western Australia, Australia. comeau@obs-vlfr.fr.ORCID http://orcid.org/0000-0002-6724-5286
C E CornwallThe University of Western Australia, Oceans Graduate School and Oceans Institute, 35 Stirling Highway, Crawley, 6009, Western Australia, Australia.ORCID http://orcid.org/0000-0002-6154-4082
C A PupierThe University of Western Australia, Oceans Graduate School and Oceans Institute, 35 Stirling Highway, Crawley, 6009, Western Australia, Australia.ORCID http://orcid.org/0000-0003-3841-3516
T M DeCarloThe University of Western Australia, Oceans Graduate School and Oceans Institute, 35 Stirling Highway, Crawley, 6009, Western Australia, Australia.ORCID http://orcid.org/0000-0003-3269-1320
C AlessiThe University of Western Australia, Oceans Graduate School and Oceans Institute, 35 Stirling Highway, Crawley, 6009, Western Australia, Australia.
R TrehernThe University of Western Australia, Oceans Graduate School and Oceans Institute, 35 Stirling Highway, Crawley, 6009, Western Australia, Australia.
M T McCullochThe University of Western Australia, Oceans Graduate School and Oceans Institute, 35 Stirling Highway, Crawley, 6009, Western Australia, Australia.ORCID http://orcid.org/0000-0003-1538-1558
The University of Western Australia · AUCentre National de la Recherche Scientifique · FR

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

Natural variability in pH in the diffusive boundary layer (DBL), the discrete layer of seawater between bulk seawater and the outer surface of organisms, could be an important factor determining the response of corals and coralline algae to ocean acidification (OA). Here, two corals with different morphologies and one coralline alga were maintained under two different regimes of flow velocities, pH, and light intensities in a 12 flumes experimental system for a period of 27 weeks. We used a combination of geochemical proxies, physiological and micro-probe measurements to assess how these treatments affected the conditions in the DBL and the response of organisms to OA. Overall, low flow velocity did not ameliorate the negative effect of low pH and therefore did not provide a refugia from OA. Flow velocity had species-specific effects with positive effects on calcification for two species. pH in the calcifying fluid (pH

Indexed as

Oceans and SeasRheologyAcidsAnimalsAnthozoaCalcification, PhysiologicCarbonatesDiffusionEukaryotaHydrogen-Ion ConcentrationLightPhotosynthesisAcidsCarbonates

Identifiers

PMID31492930
PMCPMC6731248
OpenAlexW2971832474

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.