Jan 23, 2020 16:13 UTC

A new research suggests that "massive gas bursts emitted by volcanoes about 66 million years ago probably couldn’t have caused a mass extinction event that spelled doom for all nonbird dinosaurs".

On January 17, Researchers report: "Data on ancient temperatures, combined with simulations of the shifting carbon cycle in the ocean, lend support to the hypothesis that a giant asteroid impact was primarily responsible for the die-off".

About three-quarters of Earth’s plant and animal species were killed off during the extinction event at the end of the Cretaceous Period. Sediment deposits linked to the giant asteroid impact, which struck Chicxulub in what now Mexico’s Yucatan peninsula, form a layer known as the “KPg” boundary. This boundary marks the transition from the Cretaceous to the Paleogene Period, and implicates the asteroid strike in the extinction event.

But the Deccan Traps eruptions, which spewed as much as 500,000 cubic kilometers of lava across much of what’s now western India, also occurred within a million years of the extinction. Figuring out the true killer has been challenging, because the precise timing of the Deccan Traps eruptions has been uncertain. Scientists previously have focused on dating the rocks — either zircon crystals embedded within ash layers between flows of lava, or outcrops of the lava itself. Those efforts have resulted in a range of different dates for the eruptions, some before and some after the extinction.

Furthermore, the real dino killer wouldn’t have been the lava — it would have been the volcanic gases: carbon dioxide heating the planet or sulfur dioxide acidifying the oceans. Pincelli Hull, a paleoceanographer at Yale University says “It’s the outgassing that’s important, but it’s really hard to pin that down”.

Sudden, huge bursts of CO2 and sulfur dioxide have climate-altering power — and could have come either from the asteroid impact or from the eruptions. So pinning down the timing of Deccan Traps outgassing could help solve the longstanding debate.

Hull and her colleagues turned to the temperature record preserved in sediment cores from the bottom of the ocean, and created a timeline of global temperature shifts spanning several hundred thousand years before, during and after the extinction event. The researchers then examined five different scenarios for when the Deccan Traps may have erupted, and compared them with the known temperature data.

Hull’s team found that only two of the scenarios matched the observed temperature data,— and neither scenario could have caused the extinction. In one scenario, the bulk of the eruptions occurred several hundred thousand years before the KPg, causing a blip of intense warming that was over long before the actual die-off. In the second scenario, half of the eruptions occurred before the KPg, and half after. But the temperature data suggest that any climate-altering impact immediately after the KPg would largely have been muted by shifts in the ocean carbon cycle.

Those shifts are related to calcareous plankton, tiny, floating, carbonate shell-building creatures. Plankton arose during the Mesozoic Era, but became especially abundant when the Cretaceous began about 145 million years ago. They were so ubiquitous, in fact, that their life cycle profoundly altered the ocean’s carbon cycle during the Cretaceous. The sinking shells were responsible for as much as half of the global transfer of carbon from the surface ocean to the deep during the Cretaceous, keeping the carbon cycle humming.

The KPg extinction wiped out almost all plankton, so the dissolved calcium carbonate stayed where it was in the surface ocean waters. Calcium carbonate is also a powerful buffer against acidification, which occurs when the ocean absorbs excess CO2 from the atmosphere. So even if the second scenario does explain the die-off, and the volcanoes emitted more CO2 after the extinction, the oceans likely neutralized a lot of it, muting its effect on global temperatures.

In other words, Hull says, “the mass extinction so affected global ecosystems that it hid the outgassing.”

Courtney Sprain, a geoscientist at the University of Florida in Gainesville says "the new study used really unique methods to try to answer that question” about what caused the mass extinction event. “Their conclusions about the timing of the outgassing make sense.”

Sprain adds "That doesn’t necessarily mean that previous geochemical dates determined for the Deccan Traps lava flows were incorrect. She believes that the same technological advances that made high-precision dating of the Deccan Traps possible were also responsible for revealing that there might have been a lag between lava flows and outgassing.

Courtney Sprain says "understanding why there might be a timing difference between lava and gas bursts is an active area of research in volcanology, there are still quite a few questions about how any volcanic system erupts.”

Written by: Carolyn Gramling

Courtesy: sciencenews.org

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