“…7B), as the hydrologically-closed depression becomes filled with water (R.H.M. White, 1992;Németh, 2001;Martin and Németh, 2005;Gernon et al, 2008;Pirrung et al, 2008;Kano and Ohguchi, 2009-this volume). Maar lake successions typically fineupward from coarse breccias to finer-grained lacustrine sediments containing deltaic sequences, basin floor fans, and turbidites (White, 1992;Németh, 2001;Pirrung et al, 2003), sometimes culminating in anoxic, varved sediments (Giresse et al, 1991;Mingram, 1998).…”