Reading the Ocean’s Past to Understand Our Climate Future

Edith Zhao2026, Affiliate Research

Extreme close up of tiny, mottled, gem-like shells of various shapes (spiral, circular, long) and colors ranging from white to yellow to a dark orange. They are shiny under the light and on a dark background. Foraminifera shells from coral sand. Hurgada, Egypt.
Image by Alexmar, licensed via Adobe Stock (Education License).

To understand how Earth’s climate is changing, we first need to understand how it has changed before. One of the best tools for doing that sits at the bottom of the ocean — tiny, fossilized shells of microscopic, single celled creatures called foraminifera. A new study published in the journal Palaeogeography, Palaeoclimatology, Palaeoecology takes a closer look at how reliably these shells can tell us about ancient ocean temperatures, specifically in the Indian Ocean.

Elisabeth Sikes, RCEI Affiliate, Professor in the Department of Marine and Coastal Sciences at Rutgers University, is a co-author on the study alongside lead author Ryan Glaubke, a PhD student in the Department of Marine and Coastal Sciences, and colleagues from the University of Maine and Old Dominion University.

When foraminifera are alive, the ratio of magnesium to calcium in their shells changes with water temperature. After they die and sink to the seafloor, those shells preserve a record in their shell chemistry of ocean conditions was like when they were alive — like a natural thermometer frozen in time. But the tool only works well if we know exactly how to read it, and that depends on having accurate “calibration” equations — essentially, conversion charts that translate shell chemistry into temperature.

The authors analyzed shells from 115 locations across the Indian Ocean to build and test these calibration equations for four species of foraminifera. Their key finding: for the two species studied, a simple linear relationship to temperature works best. More complex equations that also account for ocean acidity or salt content didn’t improve the results enough to justify their added complexity.

“More accurate calibrations based on empirical data mean better reconstructions of past ocean temperatures, and that’s directly useful for climate modeling. If we can more precisely portray how the Indian Ocean has warmed and cooled over thousands of years, we can better test and refine the climate models that inform today’s policy decisions.”, said Sikes

The Indian Ocean is a major driver of global weather patterns, including monsoons that affect billions of people. More accurate records of how that ocean has behaved in the past can sharpen our predictions about how it — and the climate system as a whole — may behave in the future.

You can read the full study here: https://doi.org/10.1016/j.palaeo.2025.113190

This article was written with assistance from Artificial Intelligence, was reviewed and edited by Kenneth Tam, and was reviewed by Elisabeth Sikes, a co-author on the study.