No abstract

Extensive partial mortality of intertidal corals was observed at the Houtman Abrolhos Islands, Western Australia, associated with extended and recurrent daytime low water levels from September to November 2018. Branching Acropora corals on shallow leeward reef platforms were emersed during the middle of day during the Austral spring due to diurnal tidal influences, seasonal mean sea-level minima associated with the southward flowing Leeuwin Current and interannual variability related to the El Niño-Southern Oscillation. Pre-emersion total live coral cover was estimated to be * 35%, dominated by Acropora (* 24%). Post-emersion, live Acropora cover decreased to 11.1% (± 1.5 SE) and total cover to 21.7% (± 0.8 SE). Mortality of non-acroporid corals which were lower in the water column was not observed. Partial coral mortality associated with seasonal low tides and interannual variability in mean sea level is a universal process and under-reported driver of temporal variability in coral cover on intertidal reef platforms.

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In August 2009, eight large Porites corals were relocated prior to dredging works at Cocos (Keeling) Islands. In March 2020, relocated colonies were found to have survived and grown, demonstrating that large Porites colonies growing on unconsolidated substrates can be relocated successfully if moved swiftly to a similar habitat to their source.

Sea level exerts a fundamental influence on the intertidal zone, where organisms are subject to immersion and emersion at varying timescales and frequencies. While emersed, intertidal organisms are exposed to atmospheric stressors which show marked diurnal and seasonal variability, therefore the daily and seasonal timing of low water is a key determinant of survival and growth in this zone. Using the example of shallow coral reefs, the coincidence of emersion with selected stressors was investigated for eight locations around the Australian coastline. Hourly water levels (1992 – 2016) from a high-resolution sea level hindcast (http://sealevelx.ems.uwa.edu.au), were linked to maximum surface solar radiation data from the Copernicus ERA5 atmospheric model and minimum atmospheric temperature observations from the Australian Bureau of Meteorology to identify seasonal patterns and historical occurrence of coral emersion mortality risk. Local tidal characteristics were found to dictate the time of day when low water, and therefore emersion mortality risk occurs, varying on a seasonal and regional basis. In general, risk was found to be greatest during the Austral spring when mean sea levels are lowest and a phase change in solar tidal constituents occurs. For all Great Barrier Reef sites, low tide occurs close to midday during winter and midnight in the summer, which may be fundamental factor supporting the historical bio-geographical development of the reef. Interannual variability in emersion mortality risk was mostly driven by non-tidal factors, particularly along the West Coast where El Niño events are associated with lower mean sea levels. This paper highlights the importance of considering emersion history when assessing intertidal environments, including shallow coral reef platform habitats, where critical low water events intrinsically influence coral health and cover. The study addresses a fundamental knowledge gap in both the field of water level science and intertidal biology in relation to the daily timing of low tide, which varies predictably on a seasonal and regional basis.