“…In particular, the long half‐life of 129 I (15.7 Ma) and 236 U (23.4 Ma) along with their conservative behavior (Aldahan et al., 2007; Sakaguchi et al., 2012), high concentration relative to natural sources and well‐defined but differing transient release histories into the northeast Atlantic domain (Casacuberta et al., 2018; Christl et al., 2015; Wefing et al., 2021), make them ideal tracers for investigating oceanic transport processes in the Arctic Ocean and SPNA (e.g., Casacuberta & Smith, 2023 and references therein). Recent developments in Accelerator Mass Spectrometry (AMS) have made it possible to measure these radionuclides in concentrations in the order of 1 × 10 6 at/kg of seawater (Casacuberta et al., 2016) with uncertainties of less than 3% (Christl et al., 2013, 2023; Vockenhuber et al., 2015), which is crucial for distinguishing natural from anthropogenic levels of 236 U.…”