“…Since Leg 190, drastic advances in cell separation and enumeration technologies for sediment core samples have lowered the MQL by a factor of ~10,000 (e.g., Kallmeyer, 2011;Morono et al, 2009Morono et al, , 2013Morono et al, , 2014Morono and Inagaki, 2010). Likewise, the new capacities offered in the "omics" era for elucidation of taxonomic composition (e.g., Inagaki et al, 2006;Sogin et al, 2006), metabolic activity, and function at single-cell to community levels (e.g., Biddle et al, 2008;Lloyd et al, 2013;Orsi et al, 2013), as well as new molecularisotopic techniques that link biomass to substrate pools (e.g., Biddle et al, 2006;Morono et al, 2011;Wegener et al, 2012) and central metabolic intermediates to distinct geomicrobiological processes (e.g., Heuer et al, 2006Heuer et al, , 2009Zhuang et al, 2014;Wang et al, 2015), allow entirely new approaches to study microbial life close to the limit of the deep biosphere.…”