The discovery, the first meteorite impact described within the British Paleogene Igneous Province (BPIP), raises questions about the impact and its possible connection to Paleogene volcanic activity across the North Atlantic.
Simon Drake, an associate lecturer in geology at Birkbeck University of London, zeroed in on a meter-thick layer at the base of a 60.0 million-year-old lava flow.
"We thought it was an ignimbrite (a volcanic flow deposit)," said Drake.
However, when researchers analysed the rock using an electron microprobe, they discovered that it contained rare minerals straight from outer space: vanadium-rich and niobium-rich osbornite.
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What is more, the osbornite is unmelted, suggesting that it was an original piece of the meteorite.
The team also identified reidite, an extremely high pressure form of zircon which is only ever associated in nature with impacts, along with native iron and other exotic mineralogy linked to impacts such as barringerite.
A second site, seven kilometres away, proved to be a two-meter-thick ejecta layer with the same strange mineralogy.
So far, Drake has collected samples from another site on Skye that also yield strange mineralogy, including another mineral strikingly similar to one found in comet dust.
He said that it was surprising that the ejecta layer had not been identified before, as the Isle of Skye is famously well-trampled by geologists.