“…The substrate revolution triggered feedback loops between organisms and the environment that destroyed the simple, gently graded uniform Ediacaran microbial mat habitats and replaced them with increasingly complex, fragmented, heterogeneous, dynamic Cambrian habitats (Budd & Jackson, 2016; Erwin & Tweedt, 2012; Mangano & Buatois, 2017). Over tens of millions of years, simple ecosystems containing animals that ate microbial slime were transformed into ecosystems containing recognizable modern animal phyla and complex food webs resembling modern inshore marine ecosystems (Fox, 2016; Frood, 2008). Most modern animal phyla, most of which have nervous systems, appear in the fossil record before 500 Ma (Budd & Jackson, 2016; Darroch, Smith, Laflamme, & Erwin, 2018; Droser et al, 2017; Marshall, 2006; Schiffbauer et al, 2016).…”