![Image 1 — The New Core Paradox: what powered Earth's magnetic field before the inner core existed? [OC]](https://preview.redd.it/2kqn1la3vbkh1.jpg?width=1179&format=pjpg&auto=webp&s=f299138c28c81bf9737ea19271fe8bb2aebbfb48)
![Image 2 — The New Core Paradox: what powered Earth's magnetic field before the inner core existed? [OC]](https://preview.redd.it/2ax0zla3vbkh1.jpg?width=1179&format=pjpg&auto=webp&s=957136cd1b085254d1070d05e111c2f81874d768)
![Image 3 — The New Core Paradox: what powered Earth's magnetic field before the inner core existed? [OC]](https://preview.redd.it/5x0ziua3vbkh1.jpg?width=1179&format=pjpg&auto=webp&s=e96b58b384ab78b049dfe23cdd51e95abb2a9681)
![Image 4 — The New Core Paradox: what powered Earth's magnetic field before the inner core existed? [OC]](https://preview.redd.it/75sg6ma3vbkh1.jpg?width=1225&format=pjpg&auto=webp&s=33216bd8f57f7f73706bf8932b213261aaadbddf)
![Image 5 — The New Core Paradox: what powered Earth's magnetic field before the inner core existed? [OC]](https://preview.redd.it/vs6z5la3vbkh1.jpg?width=1345&format=pjpg&auto=webp&s=2f11d0676ff0dcfacc5cb93e2fc82e353ceb1fc6)
The New Core Paradox: what powered Earth's magnetic field before the inner core existed? [OC]
Earth's magnetic field is at least 3.5 billion years old. Earth's inner core might be less than 1 billion. So what powered the dynamo for the missing two-and-a-half billion years?
Today the geodynamo runs mostly on crystallisation. As the solid inner core slowly freezes out of the liquid outer core, it releases latent heat and buoyant light elements, and that stirs the surrounding iron into convection. Moving conductive fluid, magnetic field. Simple enough, except the inner core is a latecomer, and the field is ancient.
The problem got sharper in 2012, when new calculations of iron's conductivity at core pressures came back two to three times higher than the values everyone had been using. Higher conductivity means more heat escapes the core by simple conduction instead of driving convection, which shrinks the energy available to run a dynamo. Peter Olson named the result the "new core paradox" in 2013.
Candidate fixes exist. Magnesium oxide or silica may have precipitated out of the young core, releasing buoyancy the way inner-core freezing does now. A dynamo may have operated in a molten silicate layer at the base of the mantle instead. And a 2019 study of 565-million-year-old rocks found the field at roughly a tenth of today's strength, hinting the dynamo nearly failed just before the inner core began to freeze.
None of it is settled. In 2016, two teams published conductivity measurements in the same issue of Nature, one high enough to keep the paradox alive, one low enough to dissolve it.