According to Geoscience world, Gail's study represents the first dated terrestrial record at the Pliocene-Pleistocene boundary with sufficient resolution to link lake cycles ( a climate proxy ) to astronomic forcing and the geochronometry of the sequence was determined using the paleomagnetic record ( top of subchron CN2, 1.785 Ma ), the ages of two tuffs ( Tuff IB and Tuff IF ), and sedimentation rates.
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