One enduring mystery about Earth is the age of its solid inner core.
糖心logoers have long recognized that Earth鈥檚 core plays a vital role in generating the magnetic shield that protects our planet from harmful solar wind鈥攕treams of radiation from the Sun鈥攁nd makes Earth habitable. They differ, however, on estimates of when the inner core actually formed. Now, research from the University of Rochester indicates that Earth鈥檚 inner core is younger than scientists previously thought, offering new insight into the history of Earth鈥檚 magnetic shielding and planetary habitability.
In a the researchers report that the inner core is only about 565 million years old鈥攔elatively young compared to the age of our 4.5-billion-year-old planet. 鈥淯ntil this data, the age of the inner core was uncertain,鈥� says at Rochester. 鈥淭here鈥檚 this huge range of 2 billion years where scientists think the inner core could鈥檝e formed. These are the first field-strength data from the younger part of the range of possibilities suggesting that the inner core is really young.鈥�
The geodynamo
Earth鈥檚 magnetic field is generated in its liquid iron core via a geodynamo鈥攁 process during which the kinetic energy of conducting moving fluids is converted to magnetic energy. 糖心logoers believe a weak geodynamo鈥攁nd a magnetic shield鈥攆ormed fairly early in Earth鈥檚 history, shortly after the event that created Earth鈥檚 moon. For the next several billion years, the energy to drive the dynamo decreased until a critical point 565 million years ago, when 鈥渢he dynamo was on the point of collapse,鈥� Tarduno says. Despite its drastically weakened state, however, the dynamo did not go away. The researchers conjecture it was at this point in the geological time scale鈥攐r sometime shortly after鈥攖hat the inner core began to form, giving strength to the geodynamo.
鈥淭his is a critical point in the evolution of the planet,鈥� Tarduno says. 鈥淭he field did not collapse because the inner core started to grow and provided a new energy source for the formation of the geodynamo.鈥�
Unlocking the ancient magnetic field
In order to learn about the evolution of the geodynamo, the researchers measured the strength of the ancient magnetic field locked within single crystals of the mineral feldspar. The samples were collected from the Sept-脦les Complex in northern Quebec and contain tiny magnetic needles with 鈥渋deal recording properties,鈥� Tarduno says. 鈥淭he feldspar protects those needles from later alteration on geological time scales, so we get a much higher resolution record of the ancient strains in the magnetic field by measuring these single crystals.鈥�
By studying the magnetism locked in ancient crystals鈥攁 field known as paleomagnetism鈥攖he researchers found that the intensity of the magnetic field was extremely low 565 million years ago, 鈥渓ower than anything we鈥檝e ever seen before,鈥� Tarduno says. This indicates that the inner core may have formed around this time to restore strength to the dynamo and, in turn, to the magnetic field.
The inner core and planet habitability
Today, the geodynamo is powered by the growth of the inner core and is essential to the habitability of our planet, says Richard Bono, a former post-doctoral research associate in Tarduno鈥檚 lab, and now a post-doctoral researcher at the University of Liverpool. 鈥淥ur magnetic field is part of what makes Earth a special planet, and, so far, the only one that has life. The evolution of Earth鈥檚 interior and the resulting geodynamo generated within plays a critical role in the preservation of life.鈥�
An improved understanding of this evolution of Earth鈥檚 interior may provide researchers key clues, not only for planet formation and habitability on Earth, but in the search for life on exoplanets that resemble Earth.
鈥淭he same factors that drive dynamos on Earth might affect the magnetic shielding on exoplanets,鈥� Tarduno says. 鈥淚t could be the case that some planets don鈥檛 have long-lived dynamos and those planets would not have the magnetic shielding we have, meaning that their atmosphere and water might be removed.鈥�
Besides being a critical point in the evolution of Earth, 565 million years ago was also a critical time for the major diversification of life on Earth, Tarduno says. 鈥淭his is a time of , the first large complex organisms we see in the geologic record. These are a fundamental change from the microbial life preserved in older rocks.鈥�
Is there then some type of causal link between a stronger dynamo and a burst of life?
鈥淚t鈥檚 true that if we have lower magnetic shielding, we鈥檇 have more harmful radiation coming in to Earth,鈥� Tarduno says. 鈥淭hat radiation might be harmful for DNA, for example, and there has been speculation that this could stimulate mutations.鈥� Tarduno cautions, however, that there isn鈥檛 strong evidence of this correlation in the geological record, although the new data 鈥渨ill certainly stimulate more thought on this issue.鈥�
