26 reconstructions

Lost Worlds

Supercontinents, drowned lands and the days that changed the planet

The Earth has not always looked the way it does from space today. Its continents have joined into supercontinents and broken apart again. Its oceans have frozen, its climate has swung between deep ice and searing heat, and whole stretches of land have sunk beneath the sea. None of this was ever seen by anyone, but it left traces that can be read.

This collection follows those traces. Pangaea and Gondwana are reconstructed from the way coastlines fit together, from matching rocks and fossils on continents now oceans apart, and from the magnetism frozen into ancient lava. Zealandia, a continent almost entirely under water, has been mapped from rocks dredged up from the seafloor. Doggerland, the land that once joined Britain to Europe, is known from seismic surveys, peat and tools brought up by trawlers, and DNA from seabed cores.

Some of these places are moments rather than lands: the asteroid that struck Chicxulub 66 million years ago, the volcanic floods behind the Great Dying, the burst of animal life in the Cambrian, and the times, around 700 million years ago, when ice may have reached the equator. Others are closer to our own time: the ice sheets of the last glacial maximum, the Sahara when it was green, and the Mediterranean, which fell far below today’s level and then refilled. The oldest of all, the Hadean, is known almost entirely from tiny grains of a mineral called zircon.

The paintings show these worlds as current studies reconstruct them. Exact coastlines, the colour of the land and the sky are rarely known, and the note under the facts on every page says what each picture is based on.

Start here

About 4 567 to 4 031 million years ago Hadean eon Earth's first half-billion years, named after hell but probably already wet, under a Moon three times as wide About 2.46 to 2.06 billion years ago Great Oxidation Event The slow, unsteady rise of oxygen in the air, released by microbes about 2.4 billion years ago Formed about 1.26 to 0.9 billion years ago, broke apart from about 750 million Rodinia A supercontinent of bare rock with North America at its heart, assembled about a billion years ago About 750 to 190 million years ago Panthalassa One ocean over most of the planet, whose floor has vanished without trace except for scraps stuck onto the continents About 717 to 635 million years ago Snowball Earth The times, about 700 million years ago, when ice may have reached the equator and covered the whole planet Formed about 600 million years ago, broke apart from 184 million Gondwana The great southern continent, where forests once grew close to the South Pole About 575 to 538.8 million years ago Ediacaran biota Fronds, ribbed ovals and tiny worms that covered the sea floor before the Cambrian animals arrived About 539 to 519 million years ago Cambrian explosion The burst, about 539 million years ago, when many of the main kinds of animals appear in the fossil record 358.86 to 298.9 million years ago Carboniferous period Sixty million years of equatorial coal swamps and southern ice sheets, when four-limbed animals began to breed away from water About 335 to 175 million years ago Pangaea Nearly all the land on Earth in one piece, surrounded by a single vast ocean for 160 million years About 252 million years ago The Great Dying The worst mass extinction in Earth's history, when volcanoes in Siberia nearly ended life on the planet About 250 to 14 million years ago Tethys Ocean The tropical ocean that once split the continents, now folded into mountains from the Alps to the Himalaya About 215 to 56 million years ago, as a continent of its own Laurasia The northern continent of North America, Europe and Asia, cut off from Gondwana and then broken in two by the Atlantic Sank from about 85 to 25 million years ago Zealandia A continent of about five million square kilometres, almost all of it under the sea About 66.3 to 65.6 million years ago Deccan Traps Lava that flooded western India as the age of dinosaurs ended, and an argument still running over how much it mattered 66 million years ago Chicxulub crater The buried scar of the asteroid that ended the age of dinosaurs, 66 million years ago About 5.97 to 5.33 million years ago Messinian salinity crisis The Mediterranean cut off from the ocean and left to evaporate, its level falling, in recent estimates, by anything from 600 m to over 2 km About 5.33 million years ago Zanclean flood The Atlantic breaking through at Gibraltar to refill a sea that had shrunk to lakes, perhaps within a few years Land on and off from about 2.4 million years ago; last drowned by about 7 000 years ago Sundaland The lowland, now under shallow seas, that joined Borneo, Java and Sumatra to mainland Asia through much of the Ice Age About 74 000 years ago Toba eruption The largest eruption of the past 2 million years, which left a caldera about 100 km long in northern Sumatra Exposed about 35 700 to 11 000 years ago Beringia The vanished land between Asia and Alaska, where the first Americans waited out the Ice Age About 26 500 to 19 000 years ago Last Glacial Maximum The coldest stretch of the last Ice Age, when ice stood more than 3 km high over Canada and the sea lay about 120 to 130 m lower Drowned between about 10 000 and 7 000 years ago Doggerland The lost land that joined Britain to Europe, home to hunters until the sea rose over it About 20 000 to 14 000 years ago Missoula floods A glacial lake that kept bursting through its ice dam and emptying across Washington towards the Pacific About 14 500 to 5 000 years ago Green Sahara The Sahara as a land of grass, lakes and fishers, which came to an end about 5 000 years ago About 12 900 to 11 700 years ago Younger Dryas A sudden return to near-glacial cold in the north, just as the last Ice Age was ending