Mass extinction

Writing for The Guardian, Prof. Daniel Rothman examines the history of Earth’s mass extinctions and how Earth seems to experience “a cascade of disruptions when stressed beyond a tipping point." Rothman writes that: “If we do not significantly cut back CO2 emissions, then we risk passing the threshold before the end of the present century.” He adds, “let us not contribute to the risk of a sixth extinction. Efforts to limit CO2 emissions now may pay dividends further into the future than we can imagine.”

Wall Street Journal reporter Atish Patel highlights new MIT research indicating that volcanic activity may have contributed to the extinction of the dinosaurs. Patel explains that the findings suggest “dinosaurs were already in decline, suffering from the climate change prompted by the volcanic eruptions.”

Researchers have uncovered evidence that volcanic activity could have contributed to the extinction of dinosaurs, reports Joel Achenbach for The Washington Post. Prof. Sam Bowring says the eruption “began just prior to the extinction and continued throughout.” 

Financial Times reporter Clive Cookson highlights the work of MIT researchers in identifying a new culprit for the Earth’s largest mass extinction. While volcanic activity did contribute to the extinction, Cookson reports, MIT researchers found the main cause was methane-producing microbes.

The Huffington Post reports on new research from MIT that indicates microbes may have been responsible for Earth’s largest mass extinction. The “Great Dying,” which took place 252 million years ago, wiped out 90 percent of all species.

“These microbes of death were so small, that 1 billion of them could fit in a thimble-full of ocean sediment, and yet, they were almost responsible for killing off all the life on our planet,” writes Los Angeles Times reporter Deborah Netburn about new research from MIT that indicates microbes may be responsible for the end-Permian mass extinction.

“A microbial feeding frenzy may have fueled the biggest mass extinction in Earth's history,” writes Tia Ghose for CBS News about new research by Professor Daniel Rothman and Gregory Fournier that suggests microbes may be responsible for the Earth’s largest mass extinction.

Washington Post reporter Fred Barbash highlights new MIT research that shows that a microbe called “Methanosarcina” triggered the largest mass extinction in Earth’s history.

Reporting for NPR’s Morning Edition, Christopher Joyce features new work by Professor Daniel Rothman that indicates the world’s largest mass extinction may have been caused by microbes.

MIT researchers have found evidence that methane-producing microbes may have triggered the largest mass extinction in Earth’s history, reports Will Dunham for Reuters.

Nature reporter Chelsea Ward reports that a team from MIT led by Professor Daniel Rothman has found that, “Methane-belching microbes may have been behind the 'Great Dying', a mass-extinction event that wiped out some 90% of all species on Earth about 252 million years ago.”

The Guardian highlights new research by Professor Daniel Rothman that suggests microbes may be responsible for the end-Permian extinction. As reported by The Guardian, “Analysis of geological carbon deposits reveals a significant boost in levels of carbon-containing gases – either carbon dioxide or methane – at the time of the mass extinction.”

In a Scientific American podcast, Cynthia Graber reports on new findings from MIT researchers that show the End Permian extinction, the largest mass extinction, was the fastest mass extinction.

New York Times reporter Carl Zimmer examines Sam Bowring’s work to understand the largest mass extinction of animal life. Zimmer reports that Bowring found the extinction lasted less than 60,000 years, which could help researchers identify what triggered the die-off.

Becky Oskin writes in Scientific American about new research from MIT’s Department of Earth, Atmospheric and Planetary Science that pinpoints the duration of Earth’s worst mass-extinction. The work could help researchers identify what triggered the die-off.