Deoxygenation following coral spawning and low-level thermal stress trigger mass coral mortality at Coral Bay, Ningaloo Reef

IF 2.7 2区 生物学 Q1 MARINE & FRESHWATER BIOLOGY
Zoe T. Richards, Lewis Haines, Claire Ross, Sophie Preston, Troy Matthews, Anthony Terriaca, Ethan Black, Yvette Lewis, Josh Mannolini, Patrick Dean, Vincent Middleton, Ben Saunders
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引用次数: 0

Abstract

Oxygen depletion is well recognized for its role in the degradation of tropical coral reefs. Extreme acute hypoxic events that lead to localized mass mortality and the formation of ‘dead zones’ (a region where few or no organisms can survive due to a lack of oxygen) are particularly concerning as they can result in wide-ranging losses of biodiversity, ecosystem productivity and functioning, economic prosperity, and wellbeing. In March of 2022, the annual coral spawning event at Bills Bay (Coral Bay, Ningaloo Reef, Western Australia) coincided with elevated seawater temperature, calm weather conditions and a flood tide resulting in coral spawn becoming trapped in Bills Bay. Immediately after, there was a mass fish kill, which is believed to have been caused by local eutrophication resulting in severe oxygen depletion. The impact the deoxygenation and thermal stress event had on benthic communities has not yet been quantified; hence, the principal aim of this study is to document the extent of change that occurred in the benthic communities before and after the 2022 coral spawning event over a spatial gradient from the nearshore to mid-reef. Percent coral cover in the Bay decreased from 55.62 ± 2.26% in 2016–2018 and 70.44 ± 5.24% in 2021 to 1.16 ± 0.51% in 2022. Over the same period, the percent cover of turf algae increased from 27.40 ± 2.00% in 2016–2018 and 24.66 ± 6.67% in 2021 to 78.80 ± 3.06% in 2022, indicating a dramatic phase shift occurred at Bills Bay. The abundance of healthy coral colonies recorded on replicated belt transects at nine sites declined from 3452 healthy individuals in 2018 to 153 individuals in 2022 and coral generic richness decreased by 84.61%, dropping from 26 genera in 2018 to 4 genera in 2022. Previously dominant genera such as Acropora, Montipora and Echinopora, were extirpated from survey sites. Isolated colonies of massive Porites spp. and encrusting Cyphastrea sp. survived the event and understanding the mechanisms underpinning their greater survivorship is an important area of future research. Long-term monitoring is recommended to track the community recovery process and improve our understanding of the longer-term implications of this acute mortality event on the ecological, socio-economic and cultural values of Ningaloo Reef.

Abstract Image

珊瑚产卵后脱氧和低水平热应力引发宁格鲁礁珊瑚湾珊瑚大量死亡
氧气耗尽在热带珊瑚礁退化中的作用已得到公认。极端严重的缺氧事件会导致局部大规模死亡,并形成 "死亡区"(由于缺氧,很少或没有生物能够存活的区域),这尤其令人担忧,因为它们会导致生物多样性、生态系统生产力和功能、经济繁荣和福祉的广泛丧失。2022 年 3 月,比尔斯湾(西澳大利亚宁格鲁礁珊瑚湾)一年一度的珊瑚产卵活动恰逢海水温度升高、天气平静和洪潮泛滥,导致珊瑚产卵被困在比尔斯湾。紧接着,鱼类大量死亡,据信这是由于当地富营养化导致氧气严重不足造成的。脱氧和热应力事件对底栖生物群落的影响尚未量化;因此,本研究的主要目的是记录 2022 年珊瑚产卵事件前后底栖生物群落在从近岸到中礁的空间梯度上发生的变化程度。海湾的珊瑚覆盖率从 2016-2018 年的 55.62 ± 2.26% 和 2021 年的 70.44 ± 5.24% 降至 2022 年的 1.16 ± 0.51%。同期,草皮藻类覆盖率从 2016-2018 年的 27.40 ± 2.00%、2021 年的 24.66 ± 6.67%增至 2022 年的 78.80 ± 3.06%,表明比尔斯湾发生了剧烈的阶段性变化。在 9 个地点的重复带状横断面上记录的健康珊瑚群丰度从 2018 年的 3452 个健康个体下降到 2022 年的 153 个,珊瑚属丰富度下降了 84.61%,从 2018 年的 26 个属下降到 2022 年的 4 个属。以前的优势种属,如 Acropora、Montipora 和 Echinopora,已从调查地点灭绝。大体量的 Porites 属和包壳 Cyphastrea sp.的孤立群落在这次事件中幸存下来,了解它们更强的生存能力的机制是未来研究的一个重要领域。建议进行长期监测,以跟踪群落恢复过程,并更好地了解这一严重死亡事件对宁格鲁礁生态、社会经济和文化价值的长期影响。
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来源期刊
Coral Reefs
Coral Reefs 生物-海洋与淡水生物学
CiteScore
6.80
自引率
11.40%
发文量
111
审稿时长
4-8 weeks
期刊介绍: Coral Reefs, the Journal of the International Coral Reef Society, presents multidisciplinary literature across the broad fields of reef studies, publishing analytical and theoretical papers on both modern and ancient reefs. These encourage the search for theories about reef structure and dynamics, and the use of experimentation, modeling, quantification and the applied sciences. Coverage includes such subject areas as population dynamics; community ecology of reef organisms; energy and nutrient flows; biogeochemical cycles; physiology of calcification; reef responses to natural and anthropogenic influences; stress markers in reef organisms; behavioural ecology; sedimentology; diagenesis; reef structure and morphology; evolutionary ecology of the reef biota; palaeoceanography of coral reefs and coral islands; reef management and its underlying disciplines; molecular biology and genetics of coral; aetiology of disease in reef-related organisms; reef responses to global change, and more.
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