“…Z C was chosen as a metric primarily because thermodynamic or kinetic relationships with redox potential have been implicated in a variety of natural processes. Examples include the predicted energetic favorability of amino acids biosynthesis in submarine hydrothermal vents (Amend and Shock, 1998), preservation and degradation of organic matter in sediments and soils (Likens, 2010;LaRowe and Van Cappellen, 2011;Boye et al, 2017), oxidation rates of atmospheric organic aerosols (Kroll et al, 2011(Kroll et al, , 2015, and evolutionary convergence on proteomes inferred from metagenomes of microbial communities in natural systems Shock, 2011, 2013;Dick, 2014;Dick et al, 2019;Fones et al, 2019), in aerobic and anaerobic nitrogen-fixing bacteria and archaea (Poudel et al, 2018), and in human cancer tissue (Dick, 2016(Dick, , 2017. Further, several of these studies have implicated Z C as a useful proxy for biosynthetic costs predicted from redox geochemistry (Amend and Shock, 1998;Dick and Shock, 2013;Dick et al, 2019).…”