Continent-Spanning Swaths of Cooled Magma Could Hold the Key to Mass Extinctions

Geologists look to LIPs to better understand what caused massive die-offs in the planet's past.

By Eric Betz
Jan 3, 2019 12:00 AMDec 2, 2019 7:04 PM
Volcano - Microstocker2
(Credit: microstocker2/123rf)

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The Transantarctic Mountains split our planet’s southernmost continent into east and west, at times rising more than 14,000 feet high. Today, it’s a barren landscape of inhospitable rock and ice. But for the scientists who hike and camp this rocky spine, it’s also a portal to another Earth.

Park University paleobotanist Patty Ryberg and her colleagues are uncovering the fossilized remains of a lush forest that thrived in the Antarctic Circle some 260 million years ago during the Permian period. One type of tree, called glossopterids, dominated much of a supercontinent. Then they vanished in a geological instant.

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