Successive marine heatwaves cause disproportionate coral bleaching during a fast phase transition from El Nino to La Nina

被引:43
|
作者
Dalton, Steven J. [1 ,2 ]
Carroll, Andrew G. [3 ,4 ]
Sampayo, Eugenia [1 ]
Roff, George [1 ]
Harrison, Peter L. [3 ]
Entwistle, Kristina [3 ]
Huang, Zhi [4 ]
Salih, Anya [5 ]
Diamond, Sandra L. [6 ]
机构
[1] Univ Queensland, Australian Res Council Ctr Excellence Coral Reef, Sch Biol Sci, St Lucia, Qld 4072, Australia
[2] Southern Cross Univ, Natl Marine Sci Ctr, POB 4321, Coffs Harbour, NSW 2450, Australia
[3] Southern Cross Univ, Marine Ecol Res Ctr, POB 157, Lismore, NSW 2480, Australia
[4] Geosci Australia, Natl Earth & Marine Observat Branch, GPO Box 378, Canberra, ACT 2601, Australia
[5] Western Sydney Univ, Confocal Bioimaging Facil, Hawkesbury Campus,POB 1797, Penrith, NSW 2751, Australia
[6] Western Sydney Univ, Sch Sci & Hlth, Hawkesbury Campus,POB 1797, Penrith, NSW 2751, Australia
关键词
Climate change; Ocean warming; Southern oscillation index; High-latitude reefs; Resilience; Lord Howe Island; GREAT-BARRIER-REEF; LORD-HOWE-ISLAND; CLIMATE-CHANGE; SCLERACTINIAN CORALS; CUMULATIVE IMPACT; GENETIC DIVERSITY; HIGH-LATITUDE; MORTALITY; PATTERNS; COMMUNITIES;
D O I
10.1016/j.scitotenv.2020.136951
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The frequency and intensity of marine heatwaves that result in coral bleaching events have increased over recent decades and led to catastrophic losses of reef-building corals in many regions. The high-latitude coral assemblages at Lord Howe Island, which is a UNESCO listed site is the world southernmost coral community, were exposed to successive thermal anomalies following a fast phase-transition of the record-breaking 2009 to 2010 warm pool El Nino in the Central Pacific to a strong La Nina event in late 2010. The coral community experienced severe and unprecedented consecutive bleaching in both 2010 and 2011. Coral health surveys completed between March 2010 and September 2012 quantified the response and recovery of approximately 43,700 coral colonies to these successive marine heatwaves. In March 2010, coral bleaching ranged from severe, with 99% of colonies bleached at some shallow lagoon sites, to mild at deeper reef slope sites, with only 17% of individuals affected. Significant immediate mortality from thermal stress was evident during the peak of the bleaching event. Overall, species in the genera Pocillopora, *Whom. Seriatopora and Ponies were the most affected, while minimal bleaching and mortality was recorded among members of other coral families (e.g. Acroporidae, Dendrophylfidae & Merulinidae). Surviving corals underwent a subsequent, but much less intense, thermal anomaly in 2011 that led to a disproportionate bleaching response among susceptible taxa. While this observation indicates that the capacity of thermally susceptible high-latitude corals to acclimatize to future ocean warming may be limited, particularly if bleaching events occur annually, our long-term survey data shows that coral cover at most sites recovered to pre-bleaching levels within three years in die absence of further thermal anomalies. Crown Copyright (C) 2020 Published by Elsevier B.V. All rights reserved.
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页数:12
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