Title | A Depth-Transect of Ocean Deoxygenation During the Paleocene-Eocene Thermal Maximum: Magnetofossils in Sediment Cores From the Southeast Atlantic |
Authors | Xue, Pengfei Chang, Liao Dickens, Gerald R. Thomas, Ellen |
Affiliation | Peking Univ, Lab Orogen Belts & Crustal Evolut, Sch Earth & Space Sci, Beijing, Peoples R China Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Peoples R China Trinity Coll Dublin, Dept Geol, Dublin, Ireland Yale Univ, Dept Earth & Planetary Sci, New Haven, CT USA Wesleyan Univ, Dept Earth & Environm Sci, Middletown, CT USA |
Keywords | ROCK MAGNETIC COMPONENTS COMET IMPACT TRIGGER ORGANIC-CARBON FLUX DEEP-SEA MAGNETOTACTIC BACTERIA PALAEOCEANOGRAPHIC CHANGES CIRCULATION CHANGES BIOGENIC MAGNETITE REMANENCE CURVES ABUNDANCE |
Issue Date | Aug-2022 |
Publisher | JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH |
Abstract | The Paleocene-Eocene Thermal Maximum (PETM, similar to 56 Ma) presents a past analog for future global warming. Previous studies provided evidence for major loss of dissolved oxygen during the PETM, although understanding the degree and distribution of oxygen loss poses challenges. Magnetofossils produced by magnetotactic bacteria are sensitive to redox conditions in sediments and water columns, and have been used to reconstruct paleoredox conditions over a range of geological settings. Here, we present records of well-preserved magnetofossils from cores along Walvis Ridge in the Southeast Atlantic that span the PETM across a depth transect (similar to 1,500-3,600 m paleodepth). Hysteresis, isothermal remanent magnetization curves, first-order reversal curve diagrams, and low-temperature magnetic measurements document large variations in magnetic properties of magnetofossils, which relate to time and water depth. Abundant magnetofossil grains are present within the studied sediments, and their morphologies change with paleodepth, as shown by transmission electron microscope observations. Magnetofossils from samples within the PETM onset at the deeper sites (similar to 2,600-3,600 m paleodepth) have lower coercivity values, a higher oxidation degree, and smaller grain sizes than those from shallower sites (similar to 1,500-1,800 m paleodepth), likely reflecting changes in paleoredox conditions at different paleodepths. We use the magnetofossil records to reconstruct relative changes in dissolved oxygen content at different water depths through the PETM, and suggest that ocean deoxygenation likely expanded downwards in the early stages of the PETM. We thus demonstrate the value of magnetofossil records for paleoenvironmental reconstructions over time and space, particularly for sediments that lack carbonate fossils. |
URI | http://hdl.handle.net/20.500.11897/650559 |
ISSN | 2169-9313 |
DOI | 10.1029/2022JB024714 |
Indexed | SCI(E) |
Appears in Collections: | 地球与空间科学学院 造山带与地壳演化教育部重点实验室 |