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Coral community resilience to successive years of bleaching in Kāne‘ohe Bay, Hawai‘i

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Abstract

The Hawaiian Islands are at the northern edge of coral reef distributions, and corals found there are exposed to large seasonal temperature changes. Historically, coral bleaching in the Hawaiian Islands was extremely rare and had only occurred in 1996. However, in the summers of both 2014 and 2015, successive bleaching events occurred in Kāne‘ohe Bay, O‘ahu. Seawater temperatures were above 28 °C for approximately 1 month in 2014 and 3 months in 2015 and peaked above 30 °C in both years. Patterns of bleaching did not vary among the three sites within Kāne‘ohe Bay. Severe bleaching and paling covered 77 and 55% of reefs in 2014 and 2015, respectively. Different species showed a range of susceptibility with 80–100% of Pocillopora spp. bleaching in both years, but less than 50% bleaching of Porites compressa and Montipora capitata in Kāne‘ohe Bay. Less than 1% of the encrusting coral Leptastrea purpurea colonies bleached in both years. Sixty individual colonies of P. compressa and M. capitata and 28 colonies of Pocillopora damicornis were tagged and monitored for rates of bleaching, recovery and mortality throughout the two-year period. Most of the colonies that bleached recovered their symbionts within 3–4 months, though P. compressa visually recovered more rapidly than M. capitata and P. damicornis. Cumulatively, 19% of P. damicornis, 10% of M. capitata and no P. compressa died by May 2016. Partial mortality within a colony did not occur in 2014, but impacted 13% of the colonies in 2015, with P. damicornis and M. capitata having higher rates of partial mortality than P. compressa. Relatively, low susceptibility in the dominant species and low rates of mortality combined with rapid rates of recovery show coral resilience to anomalously high temperatures in Kāne‘ohe Bay, O‘ahu.

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Acknowledgements

Special thanks to Laura Nunez-Pons, Chris Wall, Josh Levy, Ross Cunning, Drew Fant and Taylor Whitman for their extensive help with the field monitoring. Thank you to my committee members, Amy Moran, Robert Toonen, David Carlon and Philip Williams and two anonymous reviewers for their extensive reading and comments on this dissertation chapter. This is contribution number 1805 of the Hawai‘i Institute of Marine Biology.

Funding

The Watson T. Yoshimoto and Alison Kay Fellowship from the University of Hawaii to RRW partially funded this research, and the Graduate Student Organization provided funding for RRW to present this data at the SICB meeting in 2016. RRW was funded by a STAR Fellowship Assistance Agreement# FP917660 awarded by the US Environmental Protection Agency (EPA). It has not been formally reviewed by EPA. The views expressed in this manuscript are solely those of the authors, and EPA does not endorse any products or commercial services mentioned in this publication.

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Figure S1

Temperature regime at three reefs in Kāne‘ohe Bay from October 2014 to December 2015. Thick lines are rolling weekly means, and thin lines represent individual daily means. Reef 44 is in the northern section of Kāne‘ohe Bay and is represented by the green line, reef 25 is in the middle of the bay and is represented by the purple line and the reef at HIMB is in the southern section of the bay and is represented in gray. All temperatures were collected with a HOBO pendent logger that was held at a depth of 2 meters. There was a statistical difference in temperature among the reefs with a mean of 26.0 °C for the reef at HIMB which was less than the mean of 26.1 °C at reef 44 (p = 0.004) and 26.1 °C at reef 25 (p = 0.001) (PDF 17 kb)

Figure S2

Light regime at three reefs in Kāne‘ohe Bay from October 2014 to December 2015. Lines represent the mean daily light integrals, and there was a significant difference in the light environment (p < 0.001), with reef 25 having the lowest light levels. Line colors and reefs are the same as described in Figure S1 (PDF 15 kb)

Figure S3

Sediment regime at three reefs in Kāne‘ohe Bay from October 2014 to December 2015. There was no significant difference in the rate of sedimentation among the reefs (p = 0.064). Line colors and reefs are the same as described in Figure S1 (PDF 5 kb)

Figure S4

Inorganic nutrient concentrations at three reefs in Kāne‘ohe Bay from October 2014 to January 2016. A. The concentration of phosphorus. B. The concentration of nitrate + nitrite. C. The concentration of ammonia. D. The concentration of silicate. There were significant differences in the concentrations of nutrients among the reefs for phosphorus (p = 0.001), nitrate and nitrite (p < 0.001), ammonia (p = 0.08), but no differences for silicate (p = 0.183). Line colors and reefs are the same as described in Figure S1 (PDF 9 kb)

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Ritson-Williams, R., Gates, R.D. Coral community resilience to successive years of bleaching in Kāne‘ohe Bay, Hawai‘i. Coral Reefs 39, 757–769 (2020). https://doi.org/10.1007/s00338-020-01944-4

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