Marine sediments record variations in the Earth's magnetic field

The beryllium isotope. Be forms in the atmosphere under the action of cosmic rays, which are partially deflected by the Earth's magnetic field. The strength of the field therefore affects the production of ¹⁰Be. The isotope is washed out of the atmosphere by rain shortly after it forms and sticks to mineral grains that settle onto the sea floor. Three sediment cores were extracted from the bottom of the Indian and Pacific oceans and analyzed with the aim of comparing ¹⁰Be concentrations with those of ⁹Be, which originates in the Earth's crust. This ratio was used to estimate the atmospheric production rate of ¹⁰Be at the millennial scale over a period of 850,000 years. The production rate was indeed found to change in line with variations in the magnetic field, which were already known from paleomagnetic methods whose reliability needed testing.

Episodes of overproduction of ¹⁰Be correspond to collapses of the Earth's magnetic field, including those associated with its most recent reversal known, the Brunhes-Matuyama reversal 770,000 years ago. Falls in the strength of the magnetic field also coincide with excursions, failed reversals in which the poles finally return to their initial position. Such phenomena occur every 20,000 to 50,000 years, with the most recent one taking place 41,500 years ago. After several attempted reversals, the Earth's magnetic field might well resume this behavior. Indeed, direct measurements of the magnetic field reveal a rapid decrease in the field, initiated 2,500 years ago. If this continues in the future, it could create conditions favorable to a new excursion, or even a reversal, in two or three thousand years' time. 

Funding for this study was provided by the French National Research Agency ANR (MAGORB Program) and the European Research Council (EDIFICE). The researchers taking part in the study are members of the Centre de Recherche et d'Enseignement de Géosciences de l'Environnement (CNRS/Aix-Marseille Université/IRD/Collège de France), the Institut de Physique du Globe de Paris (CNRS/IPGP/Université Paris Diderot) and the Laboratoire des Sciences du Climat et de l'Environnement (CNRS/UVSQ/CEA).