“…Modern microbialites have been extensively studied using lipid biomarker analysis, gene sequencing, isotopic analysis, growth experiments, and microelectrode measurements from a wide range of sites, including Shark Bay in Western Australia (Allen, Neilan, Burns, Jahnke, & Summons, 2010;Goh et al, 2009;Grice et al, 2014;Ruvindy, White, Neilan, & Burns, 2015;Wong, Smith, Visscher, & Burns, 2015;Wong et al, 2017), the Bahamas (Andres & Pamela Reid, 2006;Baumgartner et al, 2006;Dupraz, Fowler, Tobias, & Visscher, 2013;Mobberley et al, 2015;Paerl, Steppe, & Reid, 2001;Reid et al, 2000;Visscher et al, 1998), Yellowstone National Park USA (Jahnke et al, 2004;Osburn, Sessions, Pepe-Ranney, & Spear, 2011;Pepe-Ranney et al, 2012), Pavilion Lake in British Columbia Canada (Brady, Laval, Lim, & Slater, 2014;Russell et al, 2014;White et al, 2016), the Antarctic McMurdo Ice Shelf (Jungblut, Allen, Burns, & Neilan, 2009), and Alchichica, Mexico (Breitbart et al, 2009;Couradeau et al, 2011). The study of modern microbialites enhances our understanding of ancient analogs by connecting explicit biosignatures such as DNA and RNA sequences and aqueous geochemistry to those that are preserved over geologic time such as carbonate morphology and lipid biomarkers.…”