Context of the issue
Shallow-water coral reefs are among the most biodiverse and functionally important marine ecosystems in the world. However, these systems are highly sensitive to ocean warming, and projections indicate that more than 99% could be lost within the next 50 years under continued climate change. Such declines would lead to substantial losses in biodiversity, ecosystem functioning, and the provision of critical ecosystem services. Mesophotic coral ecosystems (MCEs) are light-dependent ecosystems that occur at depths of approximately 30–150 m. These ecosystems develop under reduced light availability compared with shallow coral reefs, yet they support diverse and structurally complex coral assemblages. MCEs provide many of the same ecosystem services as shallow-water reefs, including the support of marine biodiversity, fisheries productivity, and climate regulation. As shallow-water coral reefs continue to be impacted by climate change, MCEs may play a role in sustaining coral reef biodiversity and ecosystem functioning across depth gradients. However, the effect of climate change on MCEs remains understudied, representing a significant gap in our knowledge despite the potentially pivotal importance of MCEs to the biodiversity and functioning of marine ecosystems.
For many years, it was assumed that MCEs may be protected from warming oceans by cooler, more stable conditions found at these deeper depths. However, recent observations, including our own work in the Indian Ocean, have shown that warming can extend far deeper than expected. During the 2019 Indian Ocean Dipole event, we observed widespread coral bleaching at depths of 60–90 m, linked to warming at depth caused by changes in ocean structure. This raises questions about the resilience of MCEs to future climate change and their ability to support biodiversity, ecosystem function and ecosystem service provision as shallow water reefs decline.