The study, published in the journal Science Advances, details a record of volcanism preserved along the mid-ocean ridges, which mark the oceanic boundaries of tectonic plates.
The evidence comes from changes in the strength of gravity above the seafloor.
The findings by researchers at University of Oregon in the US point to a pulse of accelerated worldwide volcanic activity that includes enhanced eruptions at India's Deccan Traps after the Chicxulub impact.
The Deccan Traps region has been in and out of the dinosaur debate. Rare volcanic events at such a scale are known to cause catastrophic disturbances to Earth's climate, and, when they occur, they are often linked to mass extinctions.
Huge volcanic events can eject so much ash and gas into the atmosphere that few plants survive, disrupting the food chain and causing animals to go extinct.
Progressively improving dating methods indicate that the Deccan Traps volcanoes already were active when the meteor struck.
Resulting seismic waves moving through the planet from the meteor strike probably fuelled an acceleration of those eruptions.
"Our work suggests a connection between these exceedingly rare and catastrophic events, distributed over the entire planet," said Leif Karlstrom, a professor at University of Oregon.
"The meteorite's impact may have influenced volcanic eruptions that were already going on, making for a one-two punch," said Karlstrom.
That team, which included Karlstrom, suggested that the meteorite may have modulated distant volcanism by generating powerful seismic waves that produced shaking worldwide.
Similar to the impacts that normal tectonic earthquakes sometimes have on wells and streams, Karlstrom said, the study proposed that seismic shaking liberated magma stored in the mantle beneath the Deccan Traps and caused the largest eruptions there.
The new findings extend this eruption-triggering in India to ocean basins worldwide.
Disclaimer: No Business Standard Journalist was involved in creation of this content
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