Coral Reefs News

Pacific coral reef shows historic increase in climate resistance

Photo Credit: Ocean Image Bank / Jayne Jenkins

Coral reefs in one part of the Pacific Ocean have likely adjusted to higher ocean temperatures which could reduce future bleaching impacts of climate change, new research reveals.

Photo Credit - Ocean Image Bank // Tracey Jennings

A Newcastle University-led study focused on the Pacific Island nation of Palau and has shown that historic increases in the thermal tolerance of coral reefs are possible. The results demonstrate how this capacity could reduce future bleaching impacts if  are cut down.

Drawing on decades of field observations, the scientists modeled many possible future coral bleaching trajectories for Palauan reefs, each with a different simulated rate of thermal tolerance enhancement. They found that if coral thermal tolerance continues to rise throughout the 21st century at the most-likely historic rate, significant reductions in bleaching impacts are possible.

Published in the journal, Nature Communications, the results affirm the scientific consensus that the severity of future coral bleaching depends on carbon emissions reductions. High-frequency bleaching can be fully mitigated at some reefs under low-to-middle emissions scenarios where, for example, the Paris Agreement commitments are fulfilled. However, such bleaching impacts are unavoidable under high emissions scenarios where society continues to rely on fossil-fueled development.

“Our study indicates the presence of an ecological resilience to , yet also highlights the need to fulfil Paris Agreement commitments to effectively preserve coral reefs,” said lead author, Liam Lachs, whom is a part of Newcastle University’s Coralassist lab.

“We quantified a natural increase in coral thermal tolerance over decadal time scales which can be directly compared to the rate of ocean warming. While our work offers a glimmer of hope, it also emphasizes the need for continued action on reducing carbon emissions to mitigate climate change and secure a future for these vital ecosystems.”

Photo Credit: Ocean Image Bank // Jordan Robins

Study co-author, Dr. James Guest, of Newcastle University’s School of Natural and Environmental Sciences, added, “We know that coral reefs can increase their overall thermal tolerance over time by acclimatization, genetic adaptation or shifts in community structure, however we know very little about the rates at which this is occurring. This study uses data from a remote Pacific coral reef system and estimates the rate of increase in tolerance since the late 1980s. The results provide some hope that reefs can keep up with increasing temperatures, but only if strong action is taken on climate change.”

This study was the result of a collaborative visit the lead author undertook in 2021 to work with Professor Simon Donner’s Climate and Coastal Ecosystems Laboratory at the University of British Columbia, Canada.

“This study shows the potential for some coral reefs to become more resilient to future climate change-fueled heat waves,” Prof. Donner said. “That resilience, however, can also come at a cost, in terms of reduced reef diversity and growth. Without sharp cuts in  over the next two to three decades, the reefs in the Pacific won’t provide the resources and protection from waves that Pacific peoples have depended upon for centuries.”

Photo Credit: Ocean Image Bank // Gabriel Barathieu

The future of coral reefs

Coral reefs harbor remarkable levels of biodiversity, yet also face unprecedented declines due to marine heat waves and resulting mass coral bleaching and mortality events. To persist under climate change, coral communities need to endure progressively more intense and frequent marine heat waves.

The rate at which the thermal tolerance of  can increase naturally and whether this can match the pace of ocean warming has remained largely unknown. To fill this knowledge gap and offer insights into the future resilience of coral communities, the team from Newcastle University investigated historic mass bleaching events, with a focus on the case study of Palau, a remote Pacific coral reef system.

The study also tested different levels of global action to mitigate climate change and reduce carbon emissions, investigating four emissions scenarios and their impact on future coral bleaching projections.

The findings reveal that the thermal tolerance of corals in Palau has likely increased at a rate of 0.1°C per decade since the late 1980s. This increase suggests that natural mechanisms, such as genetic adaptation or acclimatization of corals or their symbiotic microalgae, could have contributed to the enhancement of coral thermal tolerance.

Study co-author Prof. Peter Mumby of the University of Queensland and Palau International Coral Reef Center reflects that “some of the upcoming challenges will be to disentangle which mechanisms have driven these potential shifts in tolerance, and to understand the possibility of continued future increases in thermal tolerance.”

Future projections of accumulated heat stress (greyscale upper panels; DHW—degree heating weeks) and mass coral bleaching conditions (lower panels) are shown for four shared socioeconomic pathways (SSP) with Paris Agreement (a, SSP1–2.6), middle-of-the-road (b, SSP2–4.5), middle-high (c, SSP3–7.0), and worst-case (d, SSP5–8.5) emissions scenarios. Ensemble projections are based on downscaled sea surface temperatures from 17 Global Circulation Models (GCMs). High-frequency bleaching is considered to occur when at least two bleaching events (i.e., DHW events >8 °C-weeks) are projected to occur in any given decade. Projections of DHW (upper panels, greyscale shading) and bleaching (lower panels, lines) are shown for four simulated increases in thermal tolerance: 0.0, 0.1, 0.2, and 0.3 °C/decade (coloured lines). A fixed thermal tolerance (yellow dashed line) is the null hypothesis, the most-likely historic rate of change in thermal tolerance according to the most parsimonious model is 0.1 °C/decade (bold line), and more rapid shifts beyond the most-likely historic rate are also shown (purple and blue dashed lines). DHW is displayed as an ensemble mean across all GCMs, while bleaching trajectories are shown as the ensemble mean ± SE. Source data are provided as a Source Data file. DOI: 10.1038/s41467-023-40601-6

More information: Open Access, Liam Lachs et al, Emergent increase in coral thermal tolerance reduces mass bleaching under climate change, Nature Communications (2023). DOI: 10.1038/s41467-023-40601-6

Journal information: Nature Communications

Source: Slightly adapted from Newcastle University Press Release

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