“…The study of the release of methane from thermogenic and biogenic seeps in the world's oceans (and lakes) has expanded from simple recognition of the extent of the sources to efforts to characterize methane release mechanisms and quantify fluxes. These efforts include studies of: the exchange across the sediment water interface (Tryon and Brown, 2004;Kastner and MacDonald, 2006), bubble fluxes using bottom imaging (Leifer and MacDonald, 2003;Leifer, 2010;Thomanek et al, 2010;Römer et al, 2019;Di et al, 2020;Johansen et al, 2020), bubble fluxes using acoustic imaging (Weber et al, 2014), dissociation of hydrates (Lapham et al, 2010;Lapham et al, 2014), and inferred fluxes to the seafloor based on shallow thermal gradients (Smith et al, 2014). We now know that methane bubble release rates can vary on time scales of seconds, minutes, hours, and days (e.g., Greinert 2008;Leifer, 2019 (and references therein); Johansen et al, 2020).…”