In this work, we present 16 directional and 27 intensity high‐quality values from Iberia. Moreover, we have updated the Iberian archeomagnetic catalogue published more than 10 years ago with a considerable increase in the database. This has led to a notable improvement of both temporal and spatial data distribution. A full vector paleosecular variation curve from 1000 BC to 1900 AD has been developed using high‐quality data within a radius of 900 km from Madrid. A hierarchical bootstrap method has been followed for the computation of the curves. The most remarkable feature of the new curves is a notable intensity maximum of about 80 μT around 600 BC, which has not been previously reported for the Iberian Peninsula. We have also analyzed the evolution of the paleofield in Europe for the last three thousand years and conclude that the high maximum intensity values observed around 600 BC in the Iberian Peninsula could respond to the same feature as the Levantine Iron Age Anomaly, after travelling westward through Europe.
Pretendemos con esta breve nota dar a conocer la existencia de tres fragmentos de bronce pertenecientes a un nuevo ejemplar de casco Montefortino. El contexto de su localización y sus características decorativas lo acercan a los individuos recuperados en las necrópolis del sudeste peninsular, distanciándolo un tanto de los ejemplares catalanes conocidos hasta el momento. The aim of this note is to present three bronze fragments from a new Montefortino helmet. From its localisation context and decorative characteristics, we maintain a relation between this helmet and others found in the southeastern Iberian cemeteries, placing this helmet far from the catalonian examples. PALABRAS CLAVE-KEY WORDS Casco Montefortino. Ibérico Tardío. Ustrinum. Ajuar funerario. Necrópolis de incineración. Montefortino helmet. Late Iberian. Ustrinum. Grave goods. Incineration cemetery.
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