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    Archeomagnetic and paleomagnetic dating

    noted non-trivial differences between some stacks for the past 40 ka and stated these differences were outside measurement errors or errors of the stacking procedures.The provision of a substantial amount of relative paleointensity and chronological data will allow refinement of such stacks over the past 50 ka, and corresponding rock magnetic data may aid in understanding if remanence acquisition processes vary among sediments from different environments.Its objective is to catalogue data that will improve our understanding of changes in the geomagnetic field, physical environments, and climate.

    Several databases provide paleomagnetic, rock magnetic, and chronological data; however, none that are currently maintained exclusively catalogue data from sediments over the past 50 ka.Furthermore, additional excursion-like behavior has been noted at distinctly different times, e.g., the Hilina Pali/Tianchi excursion (Coe et al.), the time span was restrictive and the number of sediment records used for the modeling limited.Providing more comprehensive data will enable a rigorous assessment of the factors that may influence these records and allow more realistic uncertainties to be assigned.To learn more about the mechanisms that generate the geomagnetic field, it is necessary to understand variations in the field over different time scales.

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