The changing Earth through deep time — Gondwana, with Ordovician and Silurian events

Earth begins half a billion years ago, in the Cambrian, and ends at the last Ice Age. Between them: a planet rearranging itself — continents gathering and breaking apart, the slow tearing away of Antarctica, and the arrival of a familiar shoreline. Somewhere in that passage, almost imperceptibly, the world stirs and fills — glimpsed rather than dwelt on, a horizon crossed in passing. Deep geological time, rendered at a scale where even life is just one more change in the land.

Theme

Earth's deep unfolding. Geological time, and the slow becoming of a living world.

What you see

Between the ignition of the Sun, where Laniakea ends, and the first frame of Earth lie some four billion years that Numen does not show: the planet’s formation and the birth of the Moon, the first life, the oxygen coming into the air, the long snowball glaciations. It is a deliberate ellipsis. Earth begins about 540 million years ago, in the Cambrian — where the fossil record fills with complex life, and where the palaeogeographic models the globe is built from begin.

The centre wall is a globe, and every frame of it is a reconstruction. The surface is built from the PALEOMAP palaeo-elevation models (Scotese & Wright, 2018) — the height of the land and the depth of the sea across the last 540 million years — reconstructed through time with the PALEOMAP plate model (Scotese, 2016), in 2,161 steps a quarter of a million years apart. The continents are not drawn by hand. They go where the reconstruction puts them.

The colours are climate: temperature, rainfall, snow and sea ice from palaeoclimate simulations run for each stage (Valdes, Scotese & Lunt, 2021), so ice spreads where the model froze and deserts open where it dried. A few things are choices rather than measurements — the height of the ice, how far the sea falls at the end — and so is the pace. Time slows as it nears the present, so the last 66 million years are not over in a blink.

Australia begins inside Gondwana, a shallow seaway across its heart. On the side walls, moments from the fossil and geological record surface and pass, each riding a scrolling axis of deep time at its age — fifty-one of them in all. The images are imagined: generated from descriptions of the record, not photographs of it.

The globe about 450 million years ago, a shallow seaway across the interior, with Ordovician event cards on the side walls
About 450 million years ago · the Larapintine Seaway, and the ice that brings the first great extinction

Ice comes and goes. Three hundred million years ago Gondwana lies under the greatest ice of the journey — the white is where the climate model froze.

The globe about 300 million years ago, Gondwana under ice
About 300 million years ago · Gondwana at its greatest extent of ice

An inland sea floods the interior. Australia is still joined to Antarctica, and forests — and the dinosaurs that lived in them — endure months of polar dark inside the Antarctic Circle.

The globe about 110 million years ago, an inland sea across Australia, still joined to Antarctica
About 110 million years ago · the Eromanga Sea; polar forests inside the Antarctic Circle

Then Australia tears away. The Southern Ocean opens behind it, a current closes around the pole, and Antarctica freezes. The continent drifts north into warmer latitudes and a drying heart.

The globe about 40 million years ago, Australia separating from Antarctica
45 to 34 million years ago · the Southern Ocean opens; Antarctica freezes

At the end the sea falls, the shelf is laid bare, and Australia, New Guinea and Tasmania are one land — Sahul. No people appear in Earth. At the last, only footprints on a shore.

The globe at the last Ice Age, Australia, New Guinea and Tasmania joined as Sahul
The last Ice Age · Sahul

Sources

Numen is an artwork. Most of its imagery is original; some is derived from the scientific data, simulations and images credited above, transformed into new work. We have tried to identify and credit every source. If you believe something has not been credited properly, please get in touch.