TIERING AND ENCRUSTATION IN THE MODERN ROCKY INTERTIDAL – EFFECT OF ENVIRONMENTAL CHANGE AND IMPLICATIONS FOR PALEO-COMMUNITIES
Encrustation rate of the rocky shore is correlated with intertidal height; bare substrate is more common in upper intertidal (Spearman’s rho = 0.29, alpha 0.05 = 0.19). Similarly, both species richness (rho = -0.59) and the rate of tiering (encrustation of an organism on another organism, rho = -0.29) decreases with intertidal height; diversity and tiering are lower in the upper intertidal. Personal observations of the size and length of macroalgae also supports this trend; longer/broader forms are found lower in the intertidal. The only significant correlation between wave energy and encrustation/tiering is a negative relationship with the number of tiers (levels of encrustation, such as an epibiont on an epibiont on a host, rho = -0.21); fewer tiers are observed in the upper intertidal.
Given the strong relationship between species composition and intertidal height, it naturally follows that encrustation and tiering increase with diversity. However, it is surprising that the large-scale pattern (wave-exposure) did not correlate with encrustation patterns – except in that more complex tiers of encrustation are only observed in lower energy settings. These results provide interesting hypotheses to test in fossil ecosystems where encruster-host dynamics provide a unique window into in-situ ecological interactions.