The last major reversal of the Earth’s magnetic field, the Matuyama–Brunhes boundary (MBB), dated at 0.78Ma, is widely identified in Australian and New Zealand Pleistocene deposits. In New Zealand, the MBB is precisely located in shallow marine sediments of Wanganui Basin, where it corresponds with the base of the New Zealand Putikian Substage. A combination of marine biostratigraphy, sequence ...