Coral skeleton in Maldives reveals sea levels sped up from 1959, far earlier than believed

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This microatoll held clues about sea level rise in the Indian Ocean since the 1930s. The fossil coral has live coral on the outer margin.

This microatoll holds clues about sea level rise in the Indian Ocean since the 1930s. The fossil coral has live coral on the outer margin.

PHOTO: NUS

Follow topic:
  • A Maldivian coral fossil reveals Indian Ocean sea levels accelerated from 1959, earlier than previously known using satellite/tide data.
  • Between 1930 and 2019, sea levels rose 30cm, with acceleration linked to global warming and winds causing faster ocean heat absorption.
  • The data will improve sea level projections and coastal protection, benefiting Singapore's flood models. NUS aims to study fossils near Singapore improving forecasting.

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SINGAPORE - The Indian Ocean’s sea levels began accelerating from 1959, far earlier than previously thought, according to Singapore scientists who studied a coral fossil discovered in the Maldives.

Sea levels in the central Indian Ocean rose by 30cm between 1930 and 2019. This started with an annual rise of 1.42mm since 1930, before it accelerated to 3.44mm per year from 1959. Between 1992 and 2019, it rose 4.39mm per year.

These findings were published in scientific journal Nature Communications in July.

The century-old white, chalky fossil – called a microatoll – stores the memories of the Indian Ocean.

It records sea level rise each year because its skeleton grows layer by layer sideways, similar to how trees form rings. Each layer captures details about the ocean at that time, such as temperature, salt levels, and even sea level.

Such sea level archives are valuable because most existing records are from satellite data and tide gauges that go back only to the late 20th century. Most records from the central tropical locations in the Indian Ocean date back only up to 30 years.

“What we’ve now got is 60 more years of sea level records, which we never had in this part of the world. The Indian Ocean basin seemed to respond quite quickly to climate change,” said Professor Paul Kench from the National University of Singapore’s Department of Geography.

Professor Paul Kench using a handsaw to cut a cross-section of the coral fossil.

PHOTO: NUS

In 2019, he led a research team from his department and Nanyang Technological University (NTU) to visit the Maldives, where they found the 2.7m-wide coral fossil, which resembles a table, and brought back a cross-section of it for study.

The microatoll resides in the shallow waters of the Maldives’ Huvadhoo atoll.

An aerial view of the Mahutigalaa reef platform at the Maldives’ Huvadhoo atoll.

PHOTO: NUS

The microatoll has a small patch of living stony coral encrusting its outer edge and surface. Microatolls can grow only to the height of the lowest sea level, as exposure to air kills them. Once the corals reach sea level, they continue to grow sideways and can therefore retain a record of sea level change.

An X-ray of the cross-section of the fossil, showing annual growth bands moving sideways.

PHOTO: NUS

The acceleration in the rise of sea level in the Maldives from the 1950s is caused by global warming and shifting wind patterns.

Strong winds blowing across the Indian Ocean brought cool water from the deep to the surface. Cooler waters have a greater capacity to absorb heat. When water heats up, its volume expands and contributes to sea level rise.

“This created a period where heat was being absorbed into the ocean surface a lot faster,” Prof Kench said.

A long-term record of rising seas can help to improve sea level rise projections, and optimise the design of nature-based protection measures, such as mangroves and beaches, added the coastal scientist.

Long-term sea level patterns are key data for running models on coastal flooding.

A cross-section of the carved-out sample of the microatoll, in Prof Kench’s office.

ST PHOTO: SHABANA BEGUM

Scientists using the data would be able to refine and “recalibrate their models of sea level behaviour for the whole Indian Ocean basin, and have a much improved accuracy in future predictions”, said Prof Kench.

The Indian Ocean covers approximately 30 per cent of the world’s ocean area and supports around 30 per cent of the global population.

Sea level data is critical for the region, given the abundance of low-lying coastal areas and islands, and heightened sea level risks to coastal communities and ecosystems, stated the paper.

While Singapore is far away from the Maldives and Indian Ocean, Prof Kench said: “Whatever we’re observing in the central Indian Ocean has consequences for South-east Asia and Singapore… it’s all connected.”

The Strait of Malacca opens to the Andaman Sea, which is part of the Indian Ocean.

By 2100, Singapore’s sea level is projected to rise by up to 1.15m. According to data from the Tanjong Pagar tide gauge, the average sea level has risen by around 14cm between 1989 and 2024.

Singapore is building a coastal-inland flood model that can simulate the dual effects of extreme sea levels and floods within land, based on the latest climate projections.

The findings unveiled by the coral fossil in the Maldives can help countries optimise how they harness nature to protect their coastlines, said Prof Kench, who has spent several years doing fieldwork in the Maldives.

He explained: “The Indian Ocean and South-east Asia have been responding to sea level rise for 70 years already. A lot of the physical changes we see in the landscapes over the decades have already been induced by sea level rise. But a lot of adaptation measures don’t really acknowledge that adjustment.”

For example, mangrove forests or their sediments can be further studied to find out how they have been responding to sea level rise since 1959. This can help conservationists fine-tune how mangroves can be harnessed as nature-based shields, including where to plant them. The complex roots of mangroves trap sediment from the tides, allowing them to keep pace with rising seas.

“At the moment, there’s a tendency to plant mangroves everywhere and hope they work, because there hasn’t been better knowledge about them,” said Prof Kench.

NTU professor of coastal science Adam Switzer, who was not involved in the study, said: “New sea level insights from coral records like these are helping South-east Asia and Singapore sharpen climate models and unlock smarter, nature-based solutions, like reef and mangrove restoration, to build resilient coastlines for the future.”

Singapore has ancient microatolls as well, in places such as Sentosa and the Southern Islands. The ones at Lazarus Island and Pulau Tekukor are around 7,000 years old.

Prof Kench said the local fossils are slightly more difficult to analyse because the nutrient-rich waters here and marine creatures have broken down their surfaces. This makes the skeleton’s annual bands more difficult to detect.

To reconstruct sea level changes closer to home, Prof Kench visited a fossil-rich archipelago off Sulawesi, Indonesia, in mid-August.

He brought back some coral samples to put an initial age on them, and will return to the site next April to dissect a couple of micro­atolls.

“We’re sandwiched by both Indonesia and Malaysia. If we can get sea level records from those two locations, that’s going to be a record for Singapore... adds another level of improvement to our sea level prediction capabilities,” he added.

Prof Switzer added: “In a world increasingly shaped by AI (artificial intelligence) and computer models, traditional field-collected data like this remains the heartbeat of discovery.”

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