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- W3043256472 abstract "Significance Earth’s magnetic field is generated in the outer core by convecting liquid iron and protects the atmosphere from solar wind erosion. The most substantial anomaly in the magnetic field is in the South Atlantic (SA). An important conjecture is that this region could be a site of recurring anomalies because of unusual core−mantle conditions, but this has not previously been tested on geological timescales. With paleodirectional data from rocks from Saint Helena, an island in the SA, we show that the directional behavior of the magnetic field in the SA did indeed vary anomalously between ∼8 million and 11 million years ago. This supports the hypothesis of core−mantle interaction being manifest in the long-term geomagnetic field behavior of this region." @default.
- W3043256472 created "2020-07-23" @default.
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- W3043256472 date "2020-07-20" @default.
- W3043256472 modified "2023-10-09" @default.
- W3043256472 title "Elevated paleomagnetic dispersion at Saint Helena suggests long-lived anomalous behavior in the South Atlantic" @default.
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- W3043256472 doi "https://doi.org/10.1073/pnas.2001217117" @default.
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