Evidence map›Paper›PMID 39562430›Full record

ArticleThe Journal of animal ecology2025

Reconstruction of long-term sublethal effects of warming on a temperate coral in a climate change hotspot.

Marina J Vergotti, Juan P D'Olivo, Thomas C Brachert, Pol Capdevila, Joaquim Garrabou, Cristina Linares, Philipp M Spreter, Diego K Kersting

Abstract read
In one paragraph

Article in The Journal of animal ecology, 2025. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 4 papers.

0numbers the graph read from it
0cells of the map it votes in
4citing 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

4 citing papers in PubMed.

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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

8 authors.

Marina J VergottiInstitut für Geologische Wissenschaften, Freie Universität Berlin, Berlin, Germany.ORCID 0000-0001-7443-2015
Juan P D'OlivoUnidad Académica de Sistemas Arrecifales, Instituto de Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Puerto Morelos, Mexico.
Thomas C BrachertInstitut für Erdsystemforschung und Fernerkundung, Universität Leipzig, Leipzig, Germany.
Pol CapdevilaDepartament de Biologia Evolutiva, Ecologia i Ciències Ambientals, Facultat de Biologia, Universitat de Barcelona (UB), Barcelona, Spain.
Joaquim GarrabouInstitut de Ciències del Mar (ICM), Consejo Superior de Investigaciones Científicas (CSIC), Barcelona, Spain.
Cristina LinaresDepartament de Biologia Evolutiva, Ecologia i Ciències Ambientals, Facultat de Biologia, Universitat de Barcelona (UB), Barcelona, Spain.ORCID 0000-0003-3855-2743
Philipp M SpreterInstitut für Erdsystemforschung und Fernerkundung, Universität Leipzig, Leipzig, Germany.
Diego K KerstingInstituto de Acuicultura Torre de la Sal, Consejo Superior de Investigaciones Científicas (CSIC), Ribera de Cabanes, Spain.

Funding

Deutsche Forschungsgemeinschaft 401447620Horizon 2020 Framework Programme 869710ICREA AcademiaSevero Ochoa Centre of Excellence" CEX2019-000928-SSpanish Ministry of Science and Innovation PEICTI 2021-2023Spanish Ministry of Science and Innovation RYC2021-033576-ISpanish Ministry of Sciencie, Inovation and Universities PID2022-137539OA-C22
6 · The paper itself

Abstract

The impact of warming on zooxanthellate corals is widespread, from tropical to temperate seas, with its associated mortalities causing global concern. The temperate coral Cladocora caespitosa is the only zooxanthellate coral with reef building capacity in the Mediterranean Sea, a climate change hotspot with warming rates triple the global average. During the past two decades, C. caespitosa populations have suffered severe mortality events associated with marine heatwaves (MHWs). However, with monitoring efforts beginning, at best, in the 2000s, the occurrence of MHWs before that period, as well as the sublethal effects of these events remain poorly understood. Here, we use sclerochronology to reconstruct the histories of past stress events and long-term sublethal effects on C. caespitosa in three locations along a latitudinal gradient within the NW Mediterranean Sea, each with different environmental conditions. Skeletal extension, density and calcification rates were compared with the in situ seawater temperature of each site to assess their relationship. Furthermore, we assessed the occurrence of skeletal growth anomalies to reconstruct stress events between 1991 and 2021, a period that encompasses the onset and evolution of warming-related mass mortality events in the NW Mediterranean Sea. Our results reveal a positive association between calcification and temperature, following a latitudinal temperature gradient. However, the evolution of the likelihood distribution of growth rates in the warmest site (Columbretes Islands) since the 1990s indicates a decrease in linear extension and calcification rates during the most recent years. With the increase in the frequency of MHWs and growth anomalies during the last decade, this decline suggests recurrent physiological stress events. These results unravel information on the long-term impacts of warming on coral growth and highlight the potential of applying sclerochronology to reconstruct the sublethal effects of warming using C. caespitosa.

Indexed as

AnthozoaClimate ChangeGlobal WarmingHot TemperatureAnimalsCoral ReefsMediterranean SeaStress, PhysiologicalCladocora caespitosamarine heatwavesMediterranean Seapaleo‐reconstructionsclerochronologysublethal effectstemperate coral

Identifiers

PMID39562430
PMCPMC11730637

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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.