Scotland’s Ancient Lava Flows Reveal Earth's Magnetic Field Weakens Every 200 Million Years
09:13 GMT 20.08.2021 (Updated: 10:00 GMT 30.11.2022)
© Photo : Aubert et al./IPGP/CNRS Photo libraryA simulation of the Earth’s magnetic field
© Photo : Aubert et al./IPGP/CNRS Photo library
The Earth’s magnetic field is generated in the planet's core and contained within a region of space known as the magnetosphere by the action of the solar wind. This field is largely that of a dipole: it has one North pole and one South pole, with periods of variation, when the planet’s field can undergo a decrease in strength.
Dr Louise Hawkins and colleagues at the University of Liverpool performed thermal and microwave examination on the rock samples from ancient lava flows in Strathmore and Kinghorn in Scotland.
Finally! The last piece of work from my PhD is out. If you were a fan of the Mesozoic dipole low, then let me introduce you to its older sibling, the Mid-Paleozoic dipole low. https://t.co/GyxvmhgAYC with @PaleomagMichael @CourtneySprain @andybiggin— Dr Louise Hawkins (@lhawkinsgeomag) August 17, 2021
Analysis of the valuable rock samples confirmed that Earth's magnetic field, which starts in the molten core of the planet and extends into the vacuum of space, registered a quarter of its current strength between 332 and 416 million years ago. The researchers have dubbed this the Mid-Paleozoic dipole low.
The Mesozoic Dipole Low (MPDL), another similar period of low magnetic field around 120 million years ago, was identified by researchers 30 years ago.
The new findings feed into the theory, dating back to 2012, that the geomagnetic field periodically weakens - approximately every 200 million years. In the previous study, the field data was from the last 300 million years.
Molten iron and other metals in the outside core are what comprise Earth’s magnetic field. These create electromagnetic currents - the dynamo action – which offers all life on our planet protection from solar radiation. However, overtime, this unstable field fluctuates in terms of both strength and direction.
Understandably, at moments when the geomagnetic field strength is at its lowest, solar radiation showers its negative impact on Earth. This was the case with the mass extinction of 50 percent of animals and plants at the Devonian-Carboniferous boundary 359 million years ago. At the time, there was a spike in radiation levels, similar to those during the MPDL.
Dr Hawkins, lead author of the research, was cited as saying:
“This dataset compliments other studies we have worked on over the last few years, alongside our colleagues in Moscow and Alberta that fit between the ages of these two locations. Our findings also provide further support that a weak magnetic field is associated with pole reversals, while the field is generally strong during a Superchron, which is important as it has proved nearly impossible to improve the reversal record prior to 300 million years ago.”
Both the current findings and pending research might help explain future behaviour of the Earth’s geomagnetic field, and how it will affect life on our planet in the years to come.