10Be and relative paleointensity signals across the last geomagnetic reversal

Two techniques can be used to determine the evolution of the geomagnetic field intensity in the past. The first one relies on records of relative paleointensity (RPI) in sediments. Although they remain relatively sparse detailed records of 10Be production (expressed in terms of 10Be/9Be) provide an alternative approach. However integration of 10Be within the sediment is not better understood than the magnetization process, and therefore paleofield studies should greatly benefit from the integration of both datasets. In order to achieve this goal, it is crucial to compare and analyze the signals over a common time period. We selected five sedimentary cores from the Indian, Pacific and Atlantic Oceans and focused on the last reversal which is characterized by the largest intensity changes. Since 10Be is homogenized in the atmosphere, the same amount of 10Be should be recorded everywhere. We found different amounts of 10Be at each site during the last reversal which appear roughly correlated with accumulation rate. In contrast the 10Be amplitude is similar at all locations while higher amplitude signals are expected for low deposition rates. Taking advantage of the distribution of tektites layers, the beryllium signals have been deconvolved, but this procedure did not strikingly change the results. Despite atmospheric mixing we wonder whether 10Be production was slightly different at each location in presence of a multipolar transitional field. The comparison between the 10Be and RPI signals reveals large similarities but also puzzling differences. In particular, the relationship between the two signals is not the same during periods of stable polarity as during the transitional interval. A precursor with low intensity is present in several RPI records but not clearly marked on the beryllium records. We also addressed the question of a possible offset between the two signals that would be indicative of a delayed magnetization acquisition. After correlating and rescaling all records at the same common depth, the unique offset between RPI and 10Be was found in one core from the equatorial Pacific. Summarizing we wonder whether it is justified to match RPI and 10Be records over periods of higher 10Be production and lowest RPI. This is not without consequences when stacking records.