Evidence map›Paper›PMID 36437278›Full record

ArticleScientific reports2022

Local-scale feedbacks influencing cold-water coral growth and subsequent reef formation.

Guillem Corbera, Claudio Lo Iacono, Gonzalo Simarro, Jordi Grinyó, Stefano Ambroso, Veerle A I Huvenne, Furu Mienis, Marina Carreiro-Silva, Inês Martins, Beatriz Mano and 4 more

Open access · goldAbstract read
In one paragraph

Article in Scientific reports, 2022. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 1 paper.

0numbers the graph read from it
0cells of the map it votes in
1citing papers in PubMed
3.7field-weighted citation impact, top 7% 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

1 citing paper in PubMed, 26 citations in OpenAlex.

  1. 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

14 authors at 9 institutions in 6 countries.

Guillem CorberaInstitut de Ciències del Mar, CSIC, Barcelona, Spain. guillemcorb@gmail.com.
Claudio Lo IaconoInstitut de Ciències del Mar, CSIC, Barcelona, Spain. loiacono@icm.csic.es.
Gonzalo SimarroInstitut de Ciències del Mar, CSIC, Barcelona, Spain.
Jordi GrinyóInstitut de Ciències del Mar, CSIC, Barcelona, Spain.
Stefano AmbrosoInstitut de Ciències del Mar, CSIC, Barcelona, Spain.
Veerle A I HuvenneNational Oceanography Centre, Southampton, UK.
Furu MienisRoyal Netherlands Institute for Sea Research (NIOZ), Texel, The Netherlands.
Marina Carreiro-SilvaInstitute of Marine Research-Okeanos, University of Azores, Ponta Delgada, Portugal.
Inês MartinsInstitute of Marine Research-Okeanos, University of Azores, Ponta Delgada, Portugal.
Beatriz ManoInstitute of Marine Research-Okeanos, University of Azores, Ponta Delgada, Portugal.
Covadonga OrejasCentro Oceanográfico de Gijón, Instituto Español de Oceanografía (IEO-CSIC), Avenida Príncipe de Asturias 70 Bis, 33212, Gijón, Spain.
Ann LarssonUniversity of Gothenburg, Gothenburg, Sweden.
Sebastian HennigeSchool of GeoSciences, University of Edinburgh, Edinburgh, UK.
Andrea GoriInstitut de Ciències del Mar, CSIC, Barcelona, Spain.
Institut de Ciències del Mar · ESInstitut Català de Ciències del Clima · ESRoyal Netherlands Institute for Sea Research · NLUniversidade dos Açores · PTInstitute of Marine Research · PTInstituto Español de Oceanografía · ESNational Oceanography Centre · GBUniversity of Edinburgh · GBUniversity of Gothenburg · SE

Funding

HABISS Project 890815Horizon 2020 101028621Horizon 2020 678760
6 · The paper itself

Abstract

Despite cold-water coral (CWC) reefs being considered biodiversity hotspots, very little is known about the main processes driving their morphological development. Indeed, there is a considerable knowledge gap in quantitative experimental studies that help understand the interaction between reef morphology, near-bed hydrodynamics, coral growth, and (food) particle transport processes. In the present study, we performed a 2-month long flume experiment in which living coral nubbins were placed on a reef patch to determine the effect of a unidirectional flow on the growth and physiological condition of Lophelia pertusa. Measurements revealed how the presence of coral framework increased current speed and turbulence above the frontal part of the reef patch, while conditions immediately behind it were characterised by an almost stagnant flow and reduced turbulence. Owing to the higher current speeds that likely promoted a higher food encounter rate and intake of ions involved in the calcification process, the coral nubbins located on the upstream part of the reef presented a significantly enhanced average growth and a lower expression of stress-related enzymes than the downstream ones. Yet, further experiments would be needed to fully quantify how the variations in water hydrodynamics modify particle encounter and ion intake rates by coral nubbins located in different parts of a reef, and how such discrepancies may ultimately affect coral growth. Nonetheless, the results acquired here denote that a reef influenced by a unidirectional water flow would grow into the current: a pattern of reef development that coincides with that of actual coral reefs located in similar water flow settings. Ultimately, the results of this study suggest that at the local scale coral reef morphology has a direct effect on coral growth thus, indicating that the spatial patterns of living CWC colonies in reef patches are the result of spatial self-organisation.

Indexed as

AnthozoaAnimalsBiodiversityCoral ReefsFeedbackWaterWater

Identifiers

PMID36437278
PMCPMC9701764
OpenAlexW4310027118

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.