THE world’s ultimate jigsaw puzzle will be missing a couple of pieces when it is next put together. A Pangaea-like supercontinent is forecast to form in 250 million years, but a new model predicts that superplumes rising from hotspots deep in the Earth’s mantle will keep South America and Antarctica from re-merging with the other continents.

Supercontinents form, break apart, then form again every few hundred million years. Geophysicists have traced the process back to early in Earth’s history by measuring magnetic fields in ancient rocks, and some have attempted to extrapolate from the present motion of the plates the likely shape of the next supercontinent.

That supercontinent is already beginning to form: Africa is slowly colliding with Europe, and the fringes of Australia have begun to collide with Asia. Most future projections have it that the Pacific will close as its crust continues to sink beneath Asia to the west and North America to the east, and that South America and Antarctica will eventually join the ultra-slow-motion train wreck to form a supercontinent variously dubbed “Amasia” or “Novopangaea”. An alternative scenario, proposed by Christopher Scotese of the University of Texas at Arlington, predicts that the Atlantic, not the Pacific, will close, reconnecting the east coast of North America to Africa to form “Pangea Proxima“.

Neither of these predictions takes into account two massive warm zones in the mantle, 2800 kilometres beneath Africa and the south Pacific. Evidence is growing that these superplumes are too important to ignore, though. They each appear to elevate the crust above them by 1 or 2 kilometres – enough to affect plate motion.


The hotspots appear to have formed hundreds of millions of years ago, says Masaki Yoshida of the Japan Agency for Marine-Earth Science and Technology in Yokosuka. They may even be remnants of the Earth’s primordial mantle, according to a recent study that also suggested the hotspots are behind the appearance of large volcanic provinces that co-occurred with many mass extinction events (New Scientist, 30 July, p 8).

Now Yoshida and Madhava Santosh of Kochi University, Japan, have modelled how convection in the mantle – including the superplumes – will drive plate motion over the next 250 million years. They report that the two plumes will deflect both South America and Antarctica. That will keep the Pacific open, with South America staying in the south and Antarctica remaining near the South Pole (Terra Nova, DOI: 10.1111/j.1365-3121.2011.01018.x).

They are the first ones to make a quantified model of the effects of the plumes, says Kent Condie at the New Mexico Institute of Mining and Technology in Socorro. “You’re not going to ride a continent up over one of these upwellings.”