Ancient die-off greater than the dinosaur extinction

Ancient die-off greater than the dinosaur extinction
Rocks from the Belcher Islands in Hudson Bay, Canada, from which doctoral candidate Malcolm Hodgskiss collected barite samples dating 2.02 to 1.87 billion years old. Credit: Malcolm Hodgskiss

Clues from Canadian rocks formed billions of year ago reveal a previously unknown loss of life even greater than that of the mass extinction of the dinosaurs 65 million years ago, when Earth lost nearly three-quarters of its plant and animal species.

Rather than prowling animals, this die-off involved miniscule microorganisms that shaped the Earth's atmosphere and ultimately paved the way for those larger animals to thrive.

"This shows that even when biology on Earth is comprised entirely of microbes, you can still have what could be considered an enormous die-off event that otherwise is not recorded in the ," said Malcolm Hodgskiss, co-lead author of a new study published in Proceedings of the National Academy of Sciences.

Invisible clues

Because this preceded complex life, researchers cannot simply dig up fossils to learn what was living 2 billion years ago. Even clues left behind in mud and rocks can be difficult to uncover and analyze.

Instead, the group turned to barite, a mineral collected from the Belcher Islands in Hudson Bay, Canada, that encapsulates a record of in the atmosphere. Those samples revealed that Earth experienced huge changes to its biosphere—the part of the planet occupied by living organisms—ending with an enormous drop in life approximately 2.05 billion years ago that may also be linked to declining .

"The fact that this geochemical signature was preserved was very surprising," Hodgskiss said. "What was especially unusual about these barites is that they clearly had a complex history."

Looking at the Earth's productivity through provides a glimpse into how life is likely to behave over its entire existence—in addition to informing observations of atmospheres on planets outside our solar system.

"The size of the biosphere through geologic time has always been one of our biggest questions in studying the history of the Earth," said Erik Sperling, an assistant professor of geological sciences at Stanford who was not involved with the study. "This new proxy demonstrates how interlinked the biosphere and levels of oxygen and carbon dioxide in the atmosphere are."

Biological angle

This relationship between the proliferation of life and has given researchers new evidence of the hypothesized "oxygen overshoot." According to this theory, photosynthesis from ancient microorganisms and the weathering of rocks created a huge amount of oxygen in the atmosphere that later waned as oxygen-emitting organisms exhausted their nutrient supply in the ocean and became less abundant. This situation is in contrast to the stable atmosphere we know on Earth today, where the oxygen created and consumed balances out. The researchers' measurements of oxygen, sulfur and barium isotopes in barite support this oxygen overshoot hypothesis.

The research helps scientists hone their estimates of the size of the oxygen overshoot by revealing the significant biological consequences of oxygen levels above or below the capacity of the planet.

"Some of these oxygen estimates likely require too many microorganisms living in the ocean in Earth's past," said co-lead author Peter Crockford, a postdoctoral researcher at the Weizmann Institute of Science and Princeton University. "So we can now start to narrow in on what the composition of the could have been through this biological angle."

Co-authors include researchers from Nanjing University, the University of Colorado Boulder and Woods Hole Oceanographic Institution.

Explore further

What delayed Earth's oxygenation?

More information: Malcolm S. W. Hodgskiss et al, A productivity collapse to end Earth's Great Oxidation, Proceedings of the National Academy of Sciences (2019). DOI: 10.1073/pnas.1900325116
Citation: Ancient die-off greater than the dinosaur extinction (2019, August 29) retrieved 18 September 2019 from
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Aug 29, 2019
ending with an enormous drop in life approximately 2.05 Gy

Vredefort impact ~2.023 Gy.

Aug 29, 2019
The GOE likely caused two die offs, first when oxygen pressure raised and all organisms were anaerobic, later this one when oxygen pressure sank and many organisms were aerobic. But the 80 % extinction rate they see is not too bad, the Big One end-Permian had 90 % land animals die IIRC.

Also, the era in between is interesting since the oxygen level was close to when animals evolved much later and they see similar fossil preservation in shales/shale analogs of putative complex multicellulars including possible track burrows. (Which if fact, would have gone totally extinct later, but yield more data on the robustness of complex lineages and animals in particular.)

Aug 30, 2019
The evidence may be strong, but the hypothesis needs more gin.

Aug 30, 2019
The monkey needs more bananas. Taking the monkey out of the bush is easy, taking the bush out of Antigoracle monkey is not.

Aug 30, 2019
A short overview of a data set supporting a solid theory that has been in use many years now.
Neither new or controversial to any involved.
So what is with these outright weird comments? This is far from rocket science.

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