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The Arctic Ocean is divided into the Amerasia Basin and the Eurasia Basin by the Lomonosov Ridge (Figure 1a ). While it is well accepted that the Eurasia Basin has been spreading along the Gakkel Ridge since the late Paleocene-early Eocene (e.g., Brozena et al., 2003) , the model of the opening of the Amerasia Basin is still debated (e.g.,doi:10.1029/2021gc010033 fatcat:lsmecdrhhzahdpx6tuotqzk6sm