[8][9] The apparent duration at any particular location can vary by an order of magnitude, depending on geomagnetic latitude and local effects of non-dipole components of the Earth's field during the transition.
[3] The Brunhes–Matuyama reversal is a marker for the Global Boundary Stratotype Section and Point (GSSP) defining the base of the Chibanian Stage and Middle Pleistocene Subseries at the Chiba section, Japan, which was officially ratified in 2020 by the International Union of Geological Sciences.
[10][11] It is useful in dating ocean sediment cores and subaerially erupted volcanics.
There is a highly speculative theory that connects this reversal event to the large Australasian strewnfield (c. 790,000 years ago),[12] although the causes of the two are almost certainly unconnected and only coincidentally happened around the same time.
[citation needed] Adding to the data is the large African Bosumtwi impact event (c. 1.07 million years ago) and the later Jaramillo reversal (c. 1 million years ago), another pair of events which has not gone unnoticed.