Clues from Canadian rocks formed billions of years ago reveal a previously unknown loss of life even greater than that of the mass extinction of the dinosaurs 65 million years ago. The Earth lost nearly three-quarters of its plant and animal species in a huge die-off in the ancient biosphere.
Rather than prowling animals, this die-off involved minuscule microorganisms that shaped the Earth’s atmosphere and ultimately paved the way for those larger animals to thrive. Malcolm Hodgskiss, the co-lead author of a new study published in Proceedings of the National Academy of Sciences, said:
“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 fossil record.”
Invisible clues to the mass die-off
Because this time period 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 oxygen in the atmosphere.
This photograph shows 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. (Image: Malcolm Hodgskiss)
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, which may also be linked to declining oxygen levels. Hodgskiss said:
“The fact that this geochemical signature was preserved was very surprising.
“What was especially unusual about these barites is that they clearly had a complex history.”
Looking at the Earth’s productivity through ancient history 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. Erik Sperling, an assistant professor of geological sciences at Stanford who was not involved with the study, said:
“The size of the biosphere through geologic time has always been one of our biggest questions in studying the history of the Earth.
“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 atmospheric oxygen 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 contrasts 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. Peter Crockford, a postdoctoral researcher at the Weizmann Institute of Science and Princeton University, said:
“Some of these oxygen estimates likely require too many microorganisms living in the ocean in Earth’s past.
“So we can now start to narrow in on what the composition of the atmosphere could have been through this biological angle.”
Provided by: Danielle Torrent Tucker, Stanford University [Note: Materials may be edited for content and length.]
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