Taxonomy term

In the Pacific Northwest, oozing volcanic basalts erupted over the landscape during the middle Miocene, layering a sequence of 43 distinct strata, comprising roughly 350 individual flows, up to 2 kilometers thick over roughly 210,000 square kilometers. The timeline over which all that rock, known as the Columbia River Basalt Group (CRBG), piled up — and the pace at which it did so — hasn’t been as clear as scientists would like, in part because prior dates for the lava flows have come with large uncertainties. But in a new study in Science Advances, researchers have reduced those uncertainties and shown that the vast majority of the massive CRBG was deposited in less than a million years.

Two distinct images come to mind when I think of Warren Huff, my former doctoral adviser: one in which he is enthusiastically teaching and mentoring students both in and out of the classroom, and one in which he is sitting around a fire, playing guitar and leading a group of geologists in science-themed sing-alongs. Both images encapsulate the kind of person he is: a leading scholar in the field of clay mineralogy who lives life with gusto.

In the Southern Ocean surrounding Antarctica, complex and dynamic interactions among the atmosphere, cryosphere, and surface and deep ocean waters play an important role in climate. Although it covers only a quarter of Earth’s oceanic surface area, the Southern Ocean — with its cold temperatures and carbon-sucking algal blooms — has been estimated to take up 40 percent of anthropogenic carbon dioxide emissions. However, new data collected by a fleet of autonomous floating sensors show that the Southern Ocean is taking up significantly less carbon than scientists thought.

Errant asteroids and toxic emissions from volcanic eruptions are the usual suspects in mass extinctions. But during the Ordovician, it was a million-year stretch of cooling ushered in by proliferating algae that triggered a worldwide glaciation and extinction event, according to a new study.