Abstract

Over the past several decades, coral reef ecosystems have experienced recurring bleaching events. These events were predominantly caused by thermal anomalies, which vary widely in terms of severity and spatio-temporal distribution. Acropora corals, highly prominent contributors to the structural complexity of Pacific coral reefs, are sensitive to thermal stress. Response of Acropora corals to extremely high temperature has been well documented. However, studies on the effects of moderately high temperature on Acropora corals are limited. In the summer of 2016, a moderate coral bleaching event due to moderately high temperature was observed around Sesoko Island, Okinawa, Japan. The objective of this study was to examine thermal tolerance patterns of Acropora corals, across reefs with low to moderate thermal exposure (degree heating weeks ~2–5°C week). Field surveys on permanent plots were conducted from October 2015 to April 2017 to compare the population dynamics of adult Acropora corals 6 months before and after the bleaching events around Sesoko Island. Variability in thermal stress response was driven primarily by the degree of thermal stress. Wave action and turbidity may have mediated the thermal stress. Tabular and digitate coral morphologies were the most tolerant and susceptible to thermal stress, respectively. Growth inhibition after bleaching was more pronounced in the larger digitate and corymbose coral morphologies. This study indicates that Acropora populations around Sesoko Island can tolerate short-term, moderate thermal challenges.

Highlights

  • Coral reef ecosystems worldwide are being challenged by increasing global and local anthropogenic stress

  • Degree heating weeks (DHW) reached above the significant bleaching level of 4 ̊C-weeks only at Sesoko Station (1.4 to 5.4 ̊C-weeks, Fig 2)

  • To preserve coral larval sources and sinks, corals located on reefs where the temperature is low, which are remote from local disturbances like crown of thorns starfish (COTS) predation and construction activity should be selected for the conservation

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Summary

Introduction

Coral reef ecosystems worldwide are being challenged by increasing global and local anthropogenic stress. Stressors can affect individual performance, community species composition, and ecosystem function [1,2,3,4]. Coral bleaching is caused by the collapse of the mutualistic relationship between host corals and their symbiotic algae and it is a major threat to the health and survival of coral reefs. Bleaching occurs mainly in response to rising average sea surface temperature (SST) with strong irradiance [5,6,7,8].

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