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              <p>This study aims to experimentally constrain the water storage capacities of olivine and wadsleyite at a depth near 410 km (12-14 GPa) under water-saturated conditions, as a function of temperature, oxygen fugacity, and the presence of carbon (molar H / C of 2). Experiments have been conducted in the multi-anvil press, with sealed double capsules to preserve fluids, at 1200 to 1400 &lt;SUP&gt;∘&lt;/SUP&gt;C and three different oxygen fugacities fixed at the rhenium-rhenium oxide buffer (RRO), nickel-nickel oxide buffer (NNO), and iron-wüstite (IW) for oxidizing, intermediate, and reducing conditions, respectively. The water contents of minerals were measured by Raman spectroscopy that allows a very small beam size to be used and were cross-checked on a few samples with NanoSIMS analyses. &lt;P /&gt;We observe an effect, although slight, of fO&lt;SUB&gt;2&lt;/SUB&gt; on the water storage capacity of both wadsleyite and olivine and also on their solidus temperatures. At 1200 &lt;SUP&gt;∘&lt;/SUP&gt;C, the storage capacity of the nominally anhydrous minerals (NAMS) increases with increasing oxygen fugacity (from the IW to the RRO buffer) from 1 wt % to 1.5 wt % H&lt;SUB&gt;2&lt;/SUB&gt;O in wadsleyite and from 0.1 wt % to 0.2 wt % in olivine, owing to the increase in H&lt;SUB&gt;2&lt;/SUB&gt;O / H&lt;SUB&gt;2&lt;/SUB&gt; speciation in the fluid, whereas at 1400 &lt;SUP&gt;∘&lt;/SUP&gt;C the storage capacity decreases from 1 wt % to 0.75 wt % H&lt;SUB&gt;2&lt;/SUB&gt;O in wadsleyite and down to 0.03 wt % for olivine. At high temperature, the water storage capacity is lowered due to melting, and the more oxidized the conditions are the more the solidus is depressed. Still, at 1400 &lt;SUP&gt;∘&lt;/SUP&gt;C and IW, wadsleyite can store substantial amounts of water: 0.8 wt % to 1 wt % H&lt;SUB&gt;2&lt;/SUB&gt;O. The effect of carbon is to decrease water storage capacity in both wadsleyite and olivine by an average factor 2 at 1300-1400 &lt;SUP&gt;∘&lt;/SUP&gt;C. The trends in water storage as a function of fO&lt;SUB&gt;2&lt;/SUB&gt; and C presence are confirmed by NanoSIMS measurements. The solidus at IW without C is located between 1300 and 1400 &lt;SUP&gt;∘&lt;/SUP&gt;C in the wadsleyite stability field and drops to temperatures below 1300 &lt;SUP&gt;∘&lt;/SUP&gt;C in the olivine stability field. With the addition of C, the solidus is found between 1200 and 1300 &lt;SUP&gt;∘&lt;/SUP&gt;C in both olivine and wadsleyite stability fields.</p>
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