Evidence map›Paper›PMID 41258168›Full record

ArticleScientific reports2025

Sediment grain size and bedform morphology and dynamics shape benthic community heterogeneity in submarine dune fields.

Nathan Chauvel, Théo Dufresne, Sophie Le Bot, Pierre Weill, Aurore Raoux, Jean-Philippe Pezy

Abstract read
In one paragraph

Article in Scientific reports, 2025. 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
–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

1 citing paper in PubMed.

  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

6 authors.

Nathan ChauvelNormandie Université, UNICAEN, UNIROUEN, CNRS, M2C, Caen, 14000, France. nathan.chauvel@unicaen.fr.
Théo DufresneNormandie Université, UNICAEN, UNIROUEN, CNRS, M2C, Mont-Saint-Aignan, 76821, France.
Sophie Le BotNormandie Université, UNICAEN, UNIROUEN, CNRS, M2C, Mont-Saint-Aignan, 76821, France.
Pierre WeillNormandie Université, UNICAEN, UNIROUEN, CNRS, M2C, Caen, 14000, France.
Aurore RaouxNormandie Université, UNICAEN, UNIROUEN, CNRS, M2C, Caen, 14000, France.
Jean-Philippe PezyNormandie Université, UNICAEN, UNIROUEN, CNRS, M2C, Caen, 14000, France.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The distribution of benthic communities is governed by a multitude of interacting ecological processes. Among these factors, sediment grain size is generally considered as a key structuring factor for benthic communities in the eastern English Channel. However, grain size often oversimplifies the true complexity of the substrate, as the presence of bedforms such as submarine dunes adds another layer of complexity to this relationship. This study utilizes bathymetric, grain size, and macrofauna benthic data collected during four surveys conducted between 2014 and 2016 at the planned site of the Dieppe-Le Tréport offshore wind farm. The significance of these sedimentary characteristics for benthic community structure was examined through multivariate analyses and trophic group studies. The results revealed significant heterogeneity in the benthic communities within dune fields. The troughs and adjacent nondune areas, which are primarily composed of coarse sediments (gravels), support a diverse community dominated by deposit feeders and filter feeders. In contrast, the stoss and lee sides of the dunes present a much less diverse community dominated by predators and scavengers. The mechanisms driving this structuring are discussed, with an emphasis on sediment dynamics and trophic processes.

Indexed as

BedformsDune morphodynamicsMarine renewable energyMorphologicalOffshore wind farmTrophic interactions

Identifiers

PMID41258168
PMCPMC12630921

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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.