Andrea Dutton from University of Florida and colleagues from University of Michigan in the US utilised a new technique of analysis to reconstruct Antarctic ocean temperatures that support the idea that the combined impacts of volcanic eruptions and an asteroid impact brought about one of Earth's biggest mass extinctions 66 million years ago.
Researchers used a recently developed technique called the carbonate clumped isotope paleothermometer to analyse the chemical composition of fossil shells in the Antarctic Ocean.
One event was related to volcanic eruptions in India, and the other, tied to the impact of an asteroid or comet on the Yucatan Peninsula in Mexico, they said.
To create their new temperature record, which spans 3.5 million years at the end of the Cretaceous and the start of the Paleogene Period, researchers analysed the isotopic composition of 29 remarkably well-preserved shells of clam-like bivalves collected on Antarctica's Seymour Island.
Scientists have shown that the K-Pg boundary contains iridium, also found in asteroids, meteorites and comets, bolstering the theory that an asteroid killed most of the creatures of the Cretaceous Period.
Researchers studied the fossilised remains of Seymour Island bivalves with the hope of reconstructing past climate change across this critical interval of time.
However, the only experimental evidence available at the time showed a combined signal of temperature and salinity of the coastal waters, without being able to isolate the temperature signal on its own.
The data show two significant temperature spikes. The first corresponds to the eruption of the Deccan traps flood basalts, researchers said.
The other lines up exactly with the asteroid impact, which, in turn, may have sparked a renewed phase of volcanism in India, they said.
Both events are associated with extinction events of nearly equal magnitude on Seymour Island, Antarctica, researchers said.
The findings were published in the journal Nature Communications.
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