A geochemical mechanism for >10 m apparent downward offsets of magnetic reversals inferred from comparison of two Scotia Sea drill sites

• Main Authors: Reilly, BT, Tauxe, L, Brachfeld, SA, Kenlee, B, Gutjahr, M, Dale, AW, Hernández-Almeida, I, Hemming, S, Bailey, I, Zheng, X, Cheu, D, Taglienti, R, Weber, ME, Raymo, ME, Williams, T
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2024
• Subjects: paleomagnetism; Scotia Sea; magnetic reversals; Iceberg Alley; geochemistry; Matuyama-Brunhes; Pirie Basin; Dove Basin; porewater; International Ocean Discovery Porgram
• Online Access: http://hdl.handle.net/10871/136582

This is the author accepted manuscript. Data availability: All shipboard generated data can be accessed through the IODP LIMS database (Weber 488 et al., 2021b; 2021c; 2021d; https://web.iodp.tamu.edu/LORE/). Magnetic data are available 489 through the MagIC database (Weber et al., 2019; Reilly et al., 2024a). Additional data and rock 490 magnetic data files are available through the Zenodo database (Reilly et al., 2024b). We document an apparent downward displacement of the Matuyama-Brunhes magnetic reversal by ~20 meters at Scotia Sea International Ocean Discovery Program Site U1538 (Pirie Basin) by comparison with the well-defined paleomagnetic record at nearby Site U1537 (Dove Basin). Detailed stratigraphic correlation between the two sites is possible due to similar lithologic variations. However, the two sites have distinctly different porewater geochemistry. Notably, Site U1538 indicates a greater demand for electron acceptors to oxidize organic carbon and Fe2+ enrichment below the depth of SO42- depletion. Magnetic parameters indicate enrichment of an authigenic magnetic mineral with strong remanence properties around the depth of SO42- depletion (~46 meters at Site U1538) relative to magnetic parameters at correlative depths at Site U1537. Fe2+ enrichment below the depth of SO42- depletion is not predicted based on the energetically favorable order of electron acceptors for microbial respiration but is documented here and in other depositional settings. This indicates Fe2+ production exceeds the production of H2S by SO42- reduction, providing a geochemical environment that favors production and preservation of ferrimagnetic remanence-bearing iron sulfides over paramagnetic pyrite and, thus, a mechanism for deep chemical remanent magnetization acquisition at depths of tens of meters. The influence of authigenic ferrimagnetic iron sulfides on paleomagnetic signals can be difficult to demonstrate with magnetic properties alone, so this finding has implications for evaluating the fidelity of ...