Mercury Rising: New evidence that volcanism triggered the late Devonian extinction

The team analyzed rocks from Morocco, Germany, and northern Russia, all dating from the same short geologic interval 372 million years ago, just before the Frasnian-Famennian boundary. In addition to being spread across two continents, the rocks varied from black shale, grey shale, to limestone, and ranged from a few centimeters to a few meters thick. Yet they all shared one particularly striking characteristic: a sharp mercury peak hundreds of times higher than background.

In other mass extinctions, elevated mercury has been closely linked to big-time volcanic episodes. In fact, points out Racki, mercury has become to Earth-based catastrophes what iridium is to extraterrestrial-based ones. "Mercury as a geochemical fingerprint of volcanism appears decisive in the new stage of mass extinction studies," he says.

"Now we can say that all of the 'Big Five' mass extinctions coincide with major volcanic events," adds co-author Paul Wignall, with the University of Leeds in England. "Until our discovery, this (late Devonian extinction) was the major exception."

So far, the actual smoking gun -- a large region of age-appropriate volcanic rocks -- has yet to be unearthed. Racki suggests that the leading candidate may be in Russia, although telltale volcanic rocks have apparently either been eroded away or deeply buried.

That absence actually provides another take-away from the study, says Wignall. "It's possible to discover evidence for giant volcanic episodes, using trace metals in sediments, even when the lavas themselves may have long vanished," he says.