The researchers unearthed the answer to that question in ancient sedimentary rocks from central Australia.
With new technology they were able to look at the rocks differently, removing contaminants that had previously hidden molecules.
By crushing the rocks, they could extract ancient molecules.
“What we found was quite spectacular and was really, totally unexpected,” Professor Brocks said.
“We found out that these molecules of more complicated algae increased in a big burst around 650 million years ago.”
And being able to pinpoint that timeframe was the key to their breakthrough.
“The reason why that is so exciting is it is just before animals appeared and also exciting because it happened after the biggest climatic catastrophe in Earth’s history.”
Melting ‘Snowball Earth’ triggered algae explosion
That climatic catastrophe was a global thawing of what Professor Brocks calls a “Snowball Earth”.
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Which begs the question “which algae”?
The full article in Nature shines a light on which chemicals. Steroids (steranes) with up to 30 carbon atoms. The distribution is compared with that in “a Phanerozoic oil”.
Looking up what the heck a “sterane” is, it seems to be a chemical derived from cholesterol. So whet they’re looking for here is the presence of cholesterol and similar chemicals in rocks.
Are these found in algae? Yes. “Eleven species of Caribbean marine algae (red, green, and brown) were investigated for their cholesterol content. All of them were found to contain this sterol. Consistent with previously reported results, all five red algae contained large quantities of cholesterol. However, the two brown algae and three of the four green algae in our study also contained significant quantities of cholesterol.”
“In eukaryotes, sterols such as cholesterol modulate membrane order, yet they are not typically found in prokaryotes. The structurally similar bacterial hopanoids exhibit similar ordering properties as sterols in vitro”.
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http://www.nature.com/nature/journal/vaop/ncurrent/full/nature23457.html
The transition from dominant bacterial to eukaryotic marine primary productivity was one of the most profound ecological revolutions in the Earth’s history, reorganizing the distribution of carbon and nutrients in the water column and increasing energy flow to higher trophic levels. But the causes and geological timing of this transition, as well as possible links with rising atmospheric oxygen levels1 and the evolution of animals, remain obscure.
Here we present a molecular fossil record of eukaryotic steroids demonstrating that bacteria were the only notable primary producers in the oceans before the Cryogenian period (720–635 million years ago). Increasing steroid diversity and abundance marks the rapid rise of marine planktonic algae (Archaeplastida) in the narrow time interval between the Sturtian and Marinoan ‘snowball Earth’ glaciations, 659–645 million years ago. We propose that the incumbency of cyanobacteria was broken by a surge of nutrients supplied by the Sturtian deglaciation.
The ‘Rise of Algae’ created food webs with more efficient nutrient and energy transfers, driving ecosystems towards larger and increasingly complex organisms. This effect is recorded by the concomitant appearance of biomarkers for sponges and predatory rhizarians, and the subsequent radiation of eumetazoans in the Ediacaran period.
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Well, that all makes sense, unless of course the rise in primitive cholesterol levels was due to either animals or to the bacteria that were the common ancestors of animals and plants.