A new evaluation of geological history might help resolve the riddle of the ‘Cambrian explosion’, the rapid diversification of animal life in the fossil record 530 million years ago. The sudden burst of new life is also called ‘Darwin's dilemma’ because it appears to contradict Charles Darwin's hypothesis of gradual evolution by natural choice.

The Cambrian explosion is one of the most significant events in Earth's 4.5-billion-year history. The surge of evolution led to the sudden appearance of almost all modern animal groups. Fossils from the Cambrian explosion document the rapid evolution of life on Earth, but its cause has been a mystery.

A paper by Professor Ian Dalziel from The University of Texas at Austin's Jackson School of Geosciences, published in the November issue of Geology,  suggests a major tectonic event may have triggered the rise in sea level and other environmental changes that accompanied the apparent burst of life.

"At the boundary between the Precambrian and Cambrian periods, something big happened tectonically that triggered the spreading of shallow ocean water across the continents, which is clearly tied in time and space to the sudden explosion of multicellular, hard-shelled life on the planet," said Dalziel.

Beyond the sea level rise itself, the ancient geological and geographic changes probably led to a build-up of oxygen in the atmosphere and a change in ocean chemistry, allowing more complex life-forms to evolve, explained Dalziel.

The paper is the first to integrate geological evidence from five present-day continents – North America, South America, Africa, Australia and Antarctica – in an attempt to address the paleogeography of that critical time. Dalziel proposes that present-day North America was still attached to the southern continents until some time into the Cambrian.

Current reconstructions of the globe's geography during the early Cambrian show the ancient continent of Laurentia – the ancestral core of North America – as already having separated from the supercontinent Gondwanaland at that time.

In contrast, Dalziel suggests the development of a deep oceanic gateway between the Pacific and Iapetus (ancestral Atlantic) oceans, immediately preceding the global sea level rise, which isolated Laurentia in the early Cambrian.

"The reason people didn't make this connection before was because they hadn't looked at all the rock records on the different present-day continents," Dalziel said. The rock record in Antarctica, for example, comes from the very remote Ellsworth Mountains.

"People have wondered for a long time what rifted off there, and I think it was probably North America, opening up this deep seaway," Dalziel said. "It appears ancient North America was initially attached to Antarctica and part of South America, not to Europe and Africa, as has been widely believed."

Although the new analysis adds to evidence suggesting a massive tectonic shift caused the seas to rise more than half a billion years ago, Dalziel said more research is needed to determine whether this new chain of paleogeographic events can truly explain the sudden rise of multicellular life in the fossil record.

"I'm not claiming this is the ultimate explanation of the Cambrian explosion," Dalziel said. "But it may help to explain what was happening at that time."

Our editors found this article on the physics.org website where you can read more on this topic. The image of the Dickinsonia Costata fossil is by Verisimilus and released under the GNU Free Documentation License.