Isolating Detrital and Diagenetic Signals in Magnetic Susceptibility Records From Methane‐Bearing Marine Sediments
نویسندگان
چکیده
Volume-dependent magnetic susceptibility (κ) is commonly used for paleoenvironmental reconstructions in both terrestrial and marine sedimentary environments where it reflects a mixed signal between primary deposition secondary diagenesis. In the environment, κ strongly influenced by abundance of ferrimagnetic minerals regulated sediment transport processes. Post-depositional alteration H2S, however, can dissolve titanomagnetite, releasing reactive Fe that promotes pyritization subsequently decreases κ. Here, we provide new approach isolating detrital identifying intervals diagenetic driven organoclastic sulfate reduction (OSR) anaerobic oxidation methane (AOM) methane-bearing sediments offshore India. Using correlation heavy mineral proxy from X-ray fluorescence data (Zr/Rb) unaltered sediments, predict identify decreased κ, which correspond to increased total sulfur content. Our rapid, high-resolution method overprinted resulting titanomagnetite due H2S production sediments. addition, organic carbon, sulfur, authigenic carbonate δ13C measurements indicate OSR AOM drive observed loss, but drives greatest Overall, our enhance insight into paleo-positions sulfate-methane transition zone, past enhancements or paleo-methane seepage, role iron oxide on sink, with consequences influencing development chemosynthetic biological communities at seeps.
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ژورنال
عنوان ژورنال: Geochemistry Geophysics Geosystems
سال: 2021
ISSN: ['1525-2027']
DOI: https://doi.org/10.1029/2021gc009867