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Dissecting the Jurassic monster polar shift: Paleomagnetic analyses of Middle–Late Jurassic sedimentary rocks from Ethiopia

Subject Area Palaeontology
Geophysics
Term from 2021 to 2024
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 465492305
 
Final Report Year 2024

Final Report Abstract

According to a preliminary selection of key paleomagnetic poles from the literature, from 160 to 148 Ma the continents bordering the Atlantic and the Pacific plate underwent a simultaneous clockwise rotation of 30° around a common equatorial Euler pole located near the Bay of Benin (offshore west Africa). This event is referred to as the ‘Jurassic monster polar shift’ (JUMPS). In order to dissect this major geodynamic event, we performed a paleomagnetic investigation of key localities in two cratonic area, namely NE Africa and Europe. Upper Jurassic sedimentary rocks were sampled near Dejen (Ethiopia) and at the Ebermannstadt quarry near Bamberg (Franconian Alb, Germany). Three sites were sampled near Dejen: DJ01, DJ02, and DJ03, for a total of 246 samples collected and oriented in the field. Paleomagnetic results from Site DJ01 and DJ02 were combined in a single dataset as they belong to the same rock body. Comparing the obtained paleomagnetic pole with reference data from the literature, it appears to be closer to the early Cretaceous (Aptian-Albian) part of the global apparent polar wander path (APWP). Because of the uncertainty of the age assignation (despite the information from the literature), the samples sediments are currently under inspection for calcareous nannofossil content. Data from Site DJ03 appear to have been remagnetized during younger times, likely early Cenozoic. At Ebermannstadt, analysis on 107 collected samples resulted in a total of 79 paleomagnetic directions of generally low quality. Nevertheless, the calculated paleomagnetic pole falls plotted in an African reference frame appears to picture an early stage of the JUMPS.

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