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

dc.contributor.authorCorbera, Guillem
dc.contributor.authorLo Iacono, Claudio
dc.contributor.authorSimarro, Gonzalo
dc.contributor.authorGrinyó, Jordi
dc.contributor.authorAmbroso, Stefano
dc.contributor.authorHuvenne, Veerle A.I.
dc.contributor.authorMienis, Furu
dc.contributor.authorCarreiro-Silva, Marina
dc.contributor.authorMartins, Inês
dc.contributor.authorMano, Beatriz
dc.contributor.authorOrejas, Covadonga
dc.contributor.authorLarsson, Ann
dc.contributor.authorHennige, Sebastian
dc.contributor.authorGori, Andrea
dc.date.accessioned2023-03-06T16:01:52Z
dc.date.available2023-03-06T16:01:52Z
dc.date.issued2022-11-27
dc.date.updated2023-03-06T16:01:52Z
dc.description.abstractDespite 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.
dc.format.extent14 p.
dc.format.mimetypeapplication/pdf
dc.identifier.idgrec730240
dc.identifier.issn2045-2322
dc.identifier.urihttps://hdl.handle.net/2445/194715
dc.language.isoeng
dc.publisherNature Publishing Group
dc.relation.isformatofReproducció del document publicat a: https://doi.org/10.1038/s41598-022-24711-7
dc.relation.ispartofScientific Reports, 2022, vol. 12, p. 20389
dc.relation.urihttps://doi.org/10.1038/s41598-022-24711-7
dc.rightscc-by (c) Corbera, Guillem et al., 2022
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.sourceArticles publicats en revistes (Biologia Evolutiva, Ecologia i Ciències Ambientals)
dc.subject.classificationEcologia dels esculls coral·lins
dc.subject.classificationBiodiversitat
dc.subject.otherCoral reef ecology
dc.subject.otherBiodiversity
dc.titleLocal‐scale feedbacks influencing cold‐water coral growth and subsequent reef formation
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion

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