Geomagnetic excursions in late Brunhes time, European long-core data

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Scientific paper

Numerous geomagnetic polarity anomalies, i.e., excursions and flips, have been reported within the Brunhes Normal Polarity Epoch. The evaluation of their reality and geographic validity remains a problem. We report here the results from two continual sequences of lacustrine deposits covering the last 140 000 years. Several polarity anomalies are recorded. Some may be of global validity, some of regional European validity and some of no validity and representing local disturbances. The recorded excursions seem to represent different causal mechanisms; rapid destructions into a quadrupole field (about 12 500 years bp), tilted dipole fields (about 30 000-35 000 years bp), and irregular destruction of the dipole field (about 100 000-125 000 years bp).

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