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<p><strong>Abstract.</strong> We present a new marine chronostratigraphy from a high-accumulation rate Arctic Ocean core at the intersection of the Lomonosov Ridge and the Siberian margin, spanning the last &#8764;30&#8201;kyr. The chronology was derived using a combination of bulk <sup>14</sup>C dating and stratigraphic correlation to Greenland ice-core records. This was achieved by applying an appositely developed Markov chain Monte Carlo algorithm fordoi:10.5194/gchron-2019-16 fatcat:mx2e4enhyfcmrnc5oi6frcx22u