News Release

Oxygen came late to ocean depths during Paleozoic

Thallium isotopes show O2 levels rose and fell at the ocean floor long after marine animals appeared and diversified half billion years ago, according to study of ancient marine sediments exposed by river cuts in Canada's Yukon

Peer-Reviewed Publication

University of Utah

Peel River upper canyon

image: 

A group of geologists that includes co-authors Justin Strauss and Tiffani Fraser examine Silurian strata of the Tetlit Formation exposed on the Peel River, Yukon Territory in 2015.

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Credit: Erik Sperling, Stanford University

Thallium isotopes show O2 levels rose and fell at the ocean floor long after marine animals appeared and diversified half billion years ago, according to study of ancient marine sediments exposed by river cuts in Canada's Yukon


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