“…Deep-sea sensors are efficient tools for observing local geochemistry, allowing real-time monitoring of certain key chemical variables such as pH, dissolved H 2 , H 2 S, CH 4 , CO 2 , and dissolved inorganic nutrients ( Luther et al, 2001 ; Moore et al, 2009 ; Petersen et al, 2011 ; Wankel et al, 2011 ; Perner et al, 2013 ; Daniel et al, 2020 ; Gros et al, 2021 ; Liang et al, 2021 ; Mowlem et al, 2021 ). However, technical limitations require that various chemical parameters still have to be determined ex situ ( Mowlem et al, 2021 ). Although in situ filtration allows reduction of chemical alteration caused by precipitation and/or adsorption of some dissolved elements during transit from the seafloor to the ship’s research laboratory, it is evident that the most representative data on deep-sea fluid chemistry would be provided by direct in situ measurements ( Sievert and Vetriani, 2012 ; Cotte et al, 2015 ).…”