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Magnetic record of deglaciation using FORC‐PCA, sortable‐silt grain size, and magnetic excursion at 26 ka, from the Rockall Trough (NE Atlantic)

Core MD04‐2822 from the Rockall Trough has apparent sedimentation rates of ∼ 1 m/kyr during the last deglaciation (Termination I). Component magnetization directions indicate a magnetic excursion at 16.3 m depth in the core, corresponding to an age of 26.5 ka, implying an excursion duration of ∼350 years. Across Termination I, the mean grain size of sortable silt implies reduced bottom‐current velocity in the Younger Dryas and Heinrich Stadial (HS)−1A, and increased velocities during the Bølling‐Allerød warm period. Standard bulk magnetic parameters imply fining of magnetic grain size from the mid‐Younger Dryas (∼12 ka) until ∼ 8 ka. First‐order reversal curves (FORCs) were analyzed using ridge extraction to differentiate single domain (SD) from background (detrital) components. Principal component analysis (FORC‐PCA) was then used to discriminate three end members corresponding to SD, pseudo‐single domain (PSD), and multidomain (MD) magnetite. The fining of bulk magnetic grain size from 12 to 8 ka is due to reduction in concentration of detrital (PSD + MD) magnetite, superimposed on a relatively uniform concentration of SD magnetite produced by magnetotactic bacteria. The decrease in PSD+MD magnetite concentration from 12 to 8 ka is synchronized with increase in benthic δ13C, and with major (∼70 m) regional sea‐level rise, and may therefore be related to detrital sources on the shelf that had reduced influence as sea level rose, and to bottom‐water reorganization as Northern Source Water (NSW) replaced Southern Source Water (SSW).