Novel hypothesis on why animals diversified on Earth

By Birgitte Svennevig, birs@sdu.dk, 1/18/2018

Life on Earth was dominated by microbes for roughly 4 billion years when multicellular life suddenly – then in the form of animals in robust ecosystems – made a vigorous entry. Why animals diversified so late and so dramatically has remained unresolved and is a matter of hot debate.

Fossilised trilobites (Photo: Wikipedia).

The diversification of animals occurred over a geologically short period of time and is known as the Cambrian explosion. Many geologists have assumed that the Cambrian explosion was triggered by an increase of atmospheric oxygen.

However, a causal relationship between the Cambrian explosion and increasing atmospheric oxygen lacks convincing evidence.

Historic focus on high oxygen

Indeed, research over the last years weaken the support for a correlation between the Cambrian explosion and increasing atmospheric oxygen. For example, dramatic changes in atmospheric oxygen are noted both before and after the Cambrian, but not specifically when animal diversification took off. 

Continents and ocean on Earth when animals diversified dramatically in the Cambrian (Illustration: Christopher Scotese).

Simple animals are furthermore noted to require surprisingly low oxygen levels, which would have been met well before the Cambrian.

“A heated hunt for the geochemical evidence that oxygen increased when animals diversified goes on but, after decades of discussion, it seems worthwhile to consider the development of multicellularity also from other angles”, says geobiologist Emma Hammarlund, PhD and researcher at the division for translational cancer research at Lund University and guest researcher at the Nordic Center for Earth Evolution at the University of Southern Denmark.

Tumors are successful versions of multicellularity, also at low oxygen

In order to understand more about the conditions for multicellular life, Emma Hammarlund contacted tumor biologist, Professor Sven Påhlman at the Department of Laboratory Medicine at Lund University, who has explored the importance of low oxygen concentrations, or so-called hypoxia, in the tumor setting for nearly two decades.

“I wanted to learn what tumor scientists observe on a daily basis, in terms of tissue growth and how it relates to oxygen. Tumours are after all, and unfortunately, successful versions of multicellularity”, explains Emma Hammarlund.

Emma Hammarlund (Photo: Michael Yde Katballe/SDU).

The team, including also tumor biologist Dr. Kristoffer von Stedingk at Lund University’s Paediatrics division, tackled the historic question of why animals developed so late and dramatically with novel clues from the field of tumour biology.

A shared success factor

Specifically, they tested whether the same molecular tools exploited by many tumors – to maintain stem cell properties – could also be relevant to the success of animals in the Cambrian explosion. Vertebrate tissue with oxygenated blood neighboring cells with stem cell properties, a yet unexplored paradox (Photo: Sofie Mohlin).

Cells with stem cell properties are vital for all multicellular life in order to regenerate tissue. For example, cells in the wall of human small intestine are replaced every 2-4 days, through the division of stem cells.

“Hypoxia is generally seen as a threat, but we forget that oxygen shortage in precise periods and settings also is a prerequisite for multicellular life. Our stem cells are the ones that form new tissue, and they are extremely sensitive to oxygen. The stem cells therefore have various systems for dealing with the effects of both oxygen and oxygen shortage, which is clear in the case of tumors”, explains Sven Påhlman.

Tumor cells in oxygen environment

This same ability, according to the authors, is one of the keys that also made animals so successful.

Life and rocks in one picture (Photo: Emma Hammarlund).

“The ability to construct stem cell properties despite high oxygen levels, so called ‘pseudohypoxia’, is present also in our normal vertebrate tissue. Therefore, we flip the perspective on the oxic setting: While low oxygen is generally unproblematic for animal cells, the oxic settings pose a fundamental challenge for complex multicellularity. Without additional tools, the oxic setting makes tissue-specific stem cells mature too early”, says Sven Påhlman.

A biological revolution

The new hypothesis holds that the dramatic diversification of animals resulted from a revolution within the animals’ own biology, rather than in the surrounding chemistry on Earth’s surface.

A view that fits with other geobiological observations, such that environments with ‘enough’ oxygen have been present on Earth since long before the Cambrian explosion.

The hypothesis also has implications for how animals may have varying capacities to live in oxygenated environments, and perhaps even for how we see cancer as an evolutionary consequence of our ability to live in oxygenated niches.

Bringing geobiology and cancer research together

Taking an evolutionary approach is unusual for cancer researchers, even though the development of tumors is generally seen as an evolutionary process.

In an unusual collaboration, research within geobiology and tumor biology provide insight to animal diversification on Earth (Illustration: Emma Hammarlund).

Similarly, geobiological research rarely apply the cellular perspective. But having combined their expertise, both Emma Hammarlund and Sven Påhlman are surprised that we have not previously wondered about our paradoxical ability to renew tissue in the oxic setting.

“Surely, many people who would intuitively disagree. But once you flip the perspective on the oxic niche and start to consider it as challenging for stem cell properties and tissue renewal, then puzzling observations from distant fields starts to fit together. And you can’t turn back”, concludes Sven Påhlman.

About the Cambrian Explosion

The Cambrian explosion is a generic term for the event in the history of the Earth when animal species first started to diversify. From here on, animal fossils start to appear in the rock record and the Eon of visible life (Phanerozoic) begins on our planet.

The diversification is pronounced in the time period known as the Cambrian, beginning at 543 million years ago, even if the process stretched over a longer period. During the Cambrian explosion, most of the animal groups (phyla) developed and the diversity of species increased dramatically over a few tens of millions of years, which is a short period in the context of geological time.

Ref:  ‘Refined control of cell stemness allowed animals to evolve in the oxic realm’ by Emma U. Hammarlund, Kristoffer von Stedingk and Sven Påhlman. Journal: Nature Ecology and Evolution.