Evidence map›Paper›PMID 42802139›Full record

ArticleGlobal change biology2026

Projecting Impacts of Marine Heatwaves and Their Effects on Long-Term Changes in Marine Ecosystems Over the 21st Century.

Vianney Guibourd de Luzinais, William W L Cheung, Thomas Frölicher, Laurent Bopp, Gabriel Reygondeau, Didier Gascuel

Abstract read
In one paragraph

Article in Global change biology, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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

0 citing papers in PubMed.

No citing paper in PubMed yet.

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.

Vianney Guibourd de LuzinaisUMR Dynamics and Sustainability of Ecosystems: From Source to Sea (DECOD), Institut Agro, Ifremer, INRAE, Rennes, France.ORCID https://orcid.org/0000-0001-9071-6069
William W L CheungInstitute for the Oceans and Fisheries, The University of British Columbia, Vancouver, British Columbia, Canada.ORCID https://orcid.org/0000-0001-9998-0384
Thomas FrölicherClimate and Environmental Physics, University of Bern, Bern, Switzerland.
Laurent BoppLaboratoire de Météorologie Dynamique, LMD-IPSL, École Normale Supérieure, Université PSL, École Polytechnique, Institut Polytechnique de Paris, Sorbonne Université, CNRS, Paris, France.ORCID https://orcid.org/0000-0003-4732-4953
Gabriel ReygondeauRosenstiel School of Marine, Atmospheric, and Earth Science, University of Miami, Miami, Florida, USA.ORCID https://orcid.org/0000-0001-9074-625X
Didier GascuelUMR Dynamics and Sustainability of Ecosystems: From Source to Sea (DECOD), Institut Agro, Ifremer, INRAE, Rennes, France.ORCID https://orcid.org/0000-0001-5447-6977

Funding

NSERC Discovery GrantRégion BretagneSSHRC Grant through the Solving-FCB Partnership
6 · The paper itself

Abstract

Marine heatwaves (MHWs) are increasing in frequency, duration and intensity under climate change. Although current MHWs trigger broad ecological impacts, such as coral bleaching, mass mortality of seagrass meadows, and declines in important fish stocks, the cascading effects of MHWs on ecosystem structure and functions in the 21st century remain unclear. In this study, we utilise a global biomass flow modelling framework to analyse these impacts. Leveraging climate projections from two Earth system models (ESMs), we project marine food webs dynamics at a spatial resolution of 1° latitude and longitude for the global ocean under a high-emission 'no mitigation' scenario, two MHW baseline definitions (fixed vs. moving baseline), and five organismal acclimation capacity scenarios to MHWs. We project that MHWs exacerbate declines in total consumer biomass under intensifying Global Warming Level (GWL), with spatial variations. Globally, under a scenario assuming a fixed baseline, MHWs' additional biomass decline increases with GWL at a rate ranging from 1.3% to 6.7% biomass loss per Celsius degree of warming, according to best-to-worst acclimation capacity scenarios to MHWs. Furthermore, the projected impacts of MHWs on marine biomass vary across the food web, with higher trophic levels being impacted by 0.8% more than lower trophic level compartments. Moreover, under a scenario that assumes a moving baseline, reflecting marine communities' capacity to adapt or acclimatise to climate change, the projected biomass loss from MHWs is reduced by an average of 3.7% per °C of global warming compared to fixed baseline simulations. We conclude that it is essential to incorporate extreme temperature events into climate change impact and risk assessments and examine the potential role of adaptive capacities of marine communities to inform robust climate responses and adaptations for biodiversity and fisheries. We emphasise that limiting global warming to below +2°C would significantly reduce MHWs' impacts.

Indexed as

Climate ChangeEcosystemFood ChainAnimalsAquatic OrganismsBiomassGlobal WarmingModels, TheoreticalOceans and Seas

Identifiers

PMID42802139
PMCPMC13616748

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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.