Browsing by Author "Pujatti, Simone"

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    Iron oxidation and porosity generation in serpentinized abyssal peridotite
    (Elsevier, 2024-06-21) Pujatti, Simone; Sevgen, Serhat; Phelps, Patrick; Tutolo, Benjamin
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    The Controls of Porosity on Mineral Alteration Processes in the Shallow Oceanic Lithosphere at Slow-Spreading Ridges
    (2023-03-20) Pujatti, Simone; Tutolo, Benjamin Michael; Lecumberri-Sanchez, Pilar; Pattison, David Robert Maitlan; Nair, Rajeev Kumar Sasidharan; Lauer, Rachel Mollie; Tutolo, Benjamin Michael; Shugar, Daniel H
    Porosity exerts strong controls on mineral replacement and alteration processes mediated by the action of fluids. These processes are ubiquitous in the Earth’s crust, but even more so within the oceanic lithosphere, an environment saturated by infiltrating fluids that can range in composition from hot hydrothermal fluids to low-temperature seawater. This thesis presents examples of fluid-rock interactions that affect mafic and ultramafic lithologies recovered via drilling from the subseafloor of the slow-spreading Mid-Atlantic Ridge. These reactions are enabled by the presence of pores that provide flow pathways for fluids to reach the reaction front of altering minerals. Chapter 2 explores the genesis of petrographic textures observed in samples recovered from the Trans-Atlantic Geotraverse, a hydrothermal sulfide mound that shows black smoker activity. The textures form due to the replacement of anhydrite by pyrite under the action of hot hydrothermal fluids generated via heating of seawater entrained within the oceanic crust, and involved growth of quartz into open space. Intensive investigation of the observed textures detailed in this Chapter provides a mechanistic explanation for the attainment of the sulfur isotopic signatures found in sulfide precipitate within the hydrothermal mound. In Chapter 3, tomographic analysis of serpentinized peridotite at nanometer and micrometer scales reveals the presence of dissolution pores located at the grain boundaries of olivine, which show significant connectivity, suggesting that soluble Mg and Si sourced from the dissolution of olivine are exported to seawater, affecting its chemical budget, alkalinity, and consequently the coupled carbonate-silicate cycle. Chapter 4 tests the hypothesis that the porosity and Fe3+ contents of serpentinized peridotite increase with increasing serpentinization degree, suggested by correlations between density and magnetic susceptibility of serpentinites established in earlier work. The hypothesis was tested by applying statistical analysis to geochemical and porosity data collected on serpentinite samples recovered from 10 different drilling sites, revealing complex alteration patterns that involve seafloor weathering processes and thus extend beyond the transformation imparted by serpentinization reactions. Together, the scientific investigations conducted in this thesis demonstrate the importance and complexities of porosity generation and evolution during alteration of the shallow oceanic lithosphere.
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    Weathering-driven porosity generation in altered oceanic peridotites
    (Elsevier, 2023-01-23) Pujatti, Simone; Plümper, Oliver; Tutolo, Benjamin M.
    Ultramafic rocks exposed at low and ultra-slow spreading mid-ocean ridges represent a significant and extremely reactive portion of the oceanic lithosphere. Thus, mechanistic understanding of the processes by which seawater infiltrates into and reacts with these rocks is essential for constraining their contribution to the chemistry of the oceans and the coupled carbonate-silicate cycle. Recent observations indicate that nanoscale processes contribute to seawater-driven alteration of ultramafic rocks, but conventional petrographic and tomographic observations of the associated physical features are challenging to link to these nanoscale features. Moreover, multiple generations and varying conditions of fluid infiltration often obscure the relative roles of higher-temperature serpentinization, where most chemical constituents are essentially immobile, and lower-temperature weathering reactions, where observations suggest the release of massive amounts of magnesium. Here we bridge these scales and investigate the specific role of weathering processes in dissolution-driven porosity generation by integrating focused ion beam scanning electron microscopy (FIB-SEM) nanotomography and micro-computed X-ray tomography (μ-CT) imaging of the pore structures preserved in drill cores of serpentinized oceanic peridotites. Relict olivine crystals in all imaged samples contain abundant etch pits, and those in the higher-resolution FIB-SEM imagery show the presence of channel-like dissolution structures. The pore channels preferentially affect olivine along grain boundaries and show anisotropic distribution likely controlled by crystallographic features. The pores formed via olivine dissolution are interpreted to result from dissolution of serpentinized peridotite at conditions where serpentine and carbonate precipitation are kinetically inhibited, i.e., at weathering conditions. Importantly, the calculated connectivity of the imaged pore structures increases as the scale of investigation increases, suggesting that weathering-driven olivine dissolution facilitates further seawater infiltration and olivine dissolution, a positive feedback that can sustain continued magnesium extraction until the rocks are ultimately cut off from seawater circulation via sedimentation. Thus, while much attention has been directed towards constraining geochemical fluxes from the higher-temperature alteration of ultramafic rocks, our results suggest that mineral dissolution, and hence elemental fluxes, are significant at the lower temperatures of seafloor weathering. Our data thus provide mechanistic evidence of the physical process contributing to the observed Mg loss from weathered oceanic peridotites.
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    Weathering-driven porosity generation in altered oceanic peridotites
    (Elsevier, 2023-01) Pujatti, Simone; Plümper, Oliver; Tutolo, Benjamin M.
    Ultramafic rocks exposed at slow and ultra-slow spreading mid-ocean ridges represent a significant and extremely reactive portion of the oceanic lithosphere. Thus, mechanistic understanding of the processes by which seawater infiltrates into and reacts with these rocks is essential for constraining their contribution to the chemistry of the oceans and the coupled carbonate-silicate cycle. Recent observations indicate that nanoscale processes contribute to seawater-driven alteration of ultramafic rocks, but conventional petrographic and tomographic observations of the associated physical features are challenging to link to these nanoscale features. Moreover, multiple generations and varying conditions of fluid infiltration often obscure the relative roles of higher-temperature serpentinization, where reactions are mostly isochemical, and lower-temperature weathering reactions, where observations suggest the release of massive amounts of magnesium. Here we bridge these scales and investigate the specific role of weathering processes in dissolution-driven porosity generation by integrating focused ion beam scanning electron microscopy nanotomography and micro-computed X-ray tomography imaging of the pore structures preserved in drill cores of serpentinized oceanic peridotites. Relict olivine crystals in all imaged samples contain abundant etch pits, and those in the higher-resolution FIB-SEM imagery show the presence of channel-like dissolution structures. The pore channels preferentially affect olivine along grain boundaries and show anisotropic distribution likely controlled by crystallographic features. The pores formed via olivine dissolution are interpreted to result from dissolution of serpentinized peridotite at conditions where serpentine and carbonate precipitation are kinetically inhibited, i.e., at weathering conditions. Importantly, the calculated connectivity of the imaged pore structures increases as the scale of investigation increases, suggesting that weathering-driven olivine dissolution facilitates further seawater infiltration and olivine dissolution, a positive feedback that can sustain continued magnesium extraction until the rocks are ultimately cut off from seawater circulation via sedimentation. Thus, while much attention has been directed towards constraining geochemical fluxes from the higher-temperature alteration of ultramafic rocks, our results support literature studies suggesting that mineral dissolution, and hence elemental fluxes, are significant at the lower temperatures of seafloor weathering. Our data thus provide mechanistic evidence of the physical process contributing to the observed elemental loss from weathered oceanic peridotites.