| Summary: | High-temperature melting in mantle plumes produces voluminous eruptions that are often temporally coincident with mass extinctions. Paleocene Baffin Island lavas—products of early Iceland mantle plume activity—are exceptionally well characterized geochemically but have poorly constrained stratigraphy, geochronology, and eruptive tempos. To provide better geologic context, we measured seven stratigraphic sections of the volcanic deposits and collected paleomagnetic data from 38 sites in the lavas and underlying Cretaceous sediments (Quqaluit Fm.). The average paleomagnetic pole from this study does not overlap with the expected pole for a stable North American locality at 60 Ma, yet the data have sufficient dispersion to average out secular variation. After ruling out other possibilities, we find that the picrites were probably erupted during a polarity transition, over less than 5 kyr. If so, the average eruption interval was ∼67 years per flow for the thickest sequence of exposed lavas. We also calculate that the flood basalts had a minimum total volume of ∼176 km³ (excluding submerged lavas in Baffin Bay). This implies a minimum eruption rate of ∼0.035 km³ yrâ»Â¹, which is similar to rates found in West Greenland lavas but less than rates found in larger flood basalts. Despite this, the Baffin and West Greenland lavas temporally correlate with the 'End C27n event' (a period of ∼2° C global warming) and may be its underlying cause. © 2022 American Geophysical Union. Accepted manuscript online: 15 August 2022. Manuscript accepted: 11 July 2022. Manuscript revised: 07 July 2022. Manuscript received: 17 September 2021. Maryse Mahy of the Parks Canada Nunavut Field Unit, the Qikiqtani Inuit Association, and the Nunavut Research Institute assistedwith permitting and logistics.Morris Kuniliusee providedvigilant bearmonitoring. Stephane Caron(Hélicopters Panorama LTÉE) and Arctic KingdomInc.provided transportation andlogistical support, respectively. Discussions with Joseph Kirschvink and use of ...
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