New archaeomagnetic data recovered from the study of celtiberic remains from central Spain (Numantia and Ciadueña, 3rd-1st centuries BC). Implications on the fidelity of the Iberian paleointensity database

The new archaeointensity data disagrees with previous results from Iberian ceramics which were not corrected for the ATRM effect. On the contrary, they are in agreement with the most recent French paleointensity curve and the latest European intensity model; both based on a selection of high quality paleointensity data. This result reinforces the idea that the puzzling scatter often observed in the global paleointensity database is likely due to differences in the laboratory protocols. Further data from well-established laboratory protocols are still necessary to delineate confidently the evolution of the geomagnetic palaeofield during the first millennium BC.