Intertidal exposure zones: A way to subdivide the shore

Abstract

A new way of subdividing the shore is described and Doty's concept of critical tide levels (CTLs), on which the scheme is based, is revised. The various cycles of the tide (e.g., daily, monthly, and annual cycles) define several different orders of CTL at which the duration of continuous exposure or submergence increases abruptly by a discrete interval, the magnitude of which is determined by cycle period. Contrary to popular belief, most CTLs are common to all tidal types (i.e., mixed, semi-diurnal, and diurnal) and thus they can be used as reference levels for cross-comparing different intertidal regions, regardless of tidal type. CTLs naturally subdivide the intertidal region into discrete exposure zones, here called the atmozone, amphizone, and aquazone, which have upper and lower subzones. The amphizone, the intertidal core, experiences exposure and submergence extremes in terms of hours (⩽ 1 lunar day). The overlying lower atmozone and underlying upper aquazone experience exposure and submergence extremes, respectively, of the order of days (⩾2 to ≈10 days), while in the upper atmozone and lower aquazone extremes are measured in months or years (> ≈20 days). In most intertidal environments (tidal flats, saltmarshes, brackish marshes, and sheltered rocky shores) CTLs (including exposure zone boundaries) probably limit some biological zones. For tidal flats experiencing large tidal ranges it is possible that biological zones in the fringes of the intertidal region shift in response to long-term fluctuations in the levels of CTLs, due to the effects of the 18.6 year soli-lunar cycle.