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Prof. Ferre' Seminar

UL Lafayette, School of Geosciences Seminar Series
Friday, February 5th, 2021, 1:00 pm CT


Dr. Eric Ferré
Director and Professor
School of Geosciences
University of Louisiana at Lafayette



Most geologists learn during their first field trips that the color of sediments is a primary indication of syn-depositional environmental conditions of the past on our planet. While this is largely true, as a first approximation, it might be wise to consider other factors capable of affecting mineral assemblages in formations where basinal fluids percolate after deposition. During a recent International Ocean Discovery Expedition (IODP), we drilled through sediments showing alternating red and green sedimentary beds. Shipboard results, from deep Miocene marine sediments in the South China Sea, at IODP Site U1502, exemplify such post-depositional fluid-rock interactions. Petrographic, rock magnetic and paleomagnetic data on cores show that the red coloration comes from an early, basin-wide, pervasive diagenetic oxidation event (with hematite). In contrast, the green beds host a pyrrhotite-magnetite mix resulting from fluid-driven reduction. The dense sulfidic stockwork in the basaltic basement underlying these Miocene sediments is the main source of the reducing fluids. Drilling deep holes that target basin basements can thus provide useful information on the transfer of fluids, thermal energy and chemical components from the basement to the overlying sedimentary layers, and the impacts of these processes on subseafloor biogeochemical conditions.


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