“…Allogenic successions are much more common in the fossil record of hard substrate communities. For example, hardground communities can develop through several stages in response to early diagenetic cementation of the substrate (Goldring and Kazmierczak, 1974;Gruszczynski, 1979Gruszczynski, , 1986Walker and Diehl, 1986;Goldring, 1995), cave faunas can change over time with increasing sedimentation and restriction of the environment (Wilson, 1998), and reefs and bioherms respond to changes in sea levels and climate (Toomey and Cys, 1979;Crame, 1980;Williams, 1980;Nakazawa, 2001). Physical changes primarily control these successions, but biotic interactions such as larval recruitment strategies and competition are still critical.…”