The Bouraké semi-enclosed lagoon (New Caledonia). A natural laboratory to study the life-long adaptation of a coral reef ecosystem to climate change-like conditions

F. Maggioni, M. Pujo-Pay, J. Aucan, C. Cerrano, B. Calcinai, C. Payri, F. Benzoni, Y. Letourneur, R. Rodolfo-Metalpa
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引用次数: 3

Abstract

Abstract. According to current experimental evidence, coral reefs could disappear within the century if CO2 emissions remain unabated. However, recent discoveries of diverse and high cover reefs that already thrive under extreme conditions seem to contradict these projections. Volcanic CO2 vents, semi-enclosed lagoons and mangrove estuaries are unique study sites where one or more ecologically relevant parameters for life in the oceans are close or even worse than currently projected for the year 2100. These natural analogues of future conditions hold new hope for the future of coral reefs and provide unique natural laboratories to explore how reef species could keep pace with climate change. To achieve this, it is essential to characterize their environment as a whole, and accurately consider all possible environmental factors that may differ from what is expected in the future and that may possibly alter the ecosystem response. In this study, we focus on the semi-enclosed lagoon of Bouraké (New Caledonia, SW Pacific Ocean) where a healthy reef ecosystem thrives in warm, acidified and deoxygenated water. We used a multi-scale approach to characterize the main physical-chemical parameters and mapped the benthic community composition (i.e., corals, sponges, and macroalgae). The data revealed that most physical and chemical parameters are regulated by the tide, strongly fluctuate 3 to 4 times a day, and are entirely predictable. The seawater pH and dissolved oxygen decrease during falling tide and reach extreme low values at low tide (7.2 pHT and 1.9 mg O2 L−1 at Bouraké, vs 7.9 pHT and 5.5 mg O2 L−1 at reference reefs). Dissolved oxygen, temperature, and pH fluctuates according to the tide of up to 4.91 mg O2 L−1, 6.50 °C, and 0.69 pHT units on a single day. Furthermore, the concentration of most of the chemical parameters was one- to 5-times higher at the Bouraké lagoon, particularly for organic and inorganic carbon and nitrogen, but also for some nutrients, notably silicates. Surprisingly, despite extreme environmental conditions and altered seawater chemical composition, our results reveal a diverse and high cover community of macroalgae, sponges and corals accounting for 28, 11 and 66 species, respectively. Both environmental variability and nutrient imbalance might contribute to their survival under such extreme environmental conditions. We describe the natural dynamics of the Bouraké ecosystem and its relevance as a natural laboratory to investigate the benthic organism’s adaptive responses to multiple stressors like future climate change conditions.
Bouraké半封闭式泻湖(新喀里多尼亚)。一个研究珊瑚礁生态系统终身适应气候变化条件的自然实验室
摘要根据目前的实验证据,如果二氧化碳排放量不减,珊瑚礁可能在本世纪内消失。然而,最近发现的多样性和高覆盖率的珊瑚礁似乎与这些预测相矛盾,这些珊瑚礁已经在极端条件下茁壮成长。火山二氧化碳排放口、半封闭泻湖和红树林河口是独特的研究地点,在这些地方,海洋中生命的一个或多个生态相关参数接近甚至比目前预测的2100年更糟。这些未来条件的天然类似物为珊瑚礁的未来带来了新的希望,并为探索珊瑚礁物种如何跟上气候变化提供了独特的自然实验室。为了实现这一点,必须将其环境作为一个整体进行表征,并准确考虑所有可能与未来预期不同的环境因素,这些因素可能会改变生态系统的反应。在这项研究中,我们关注的是Bouraké(新喀里多尼亚,西太平洋)的半封闭泻湖,在那里,健康的珊瑚礁生态系统在温暖、酸化和脱氧的水中蓬勃发展。我们使用多尺度方法来表征主要的物理化学参数,并绘制了海底群落组成图(即珊瑚、海绵和大型藻类)。数据显示,大多数物理和化学参数都受到潮汐的调节,每天强烈波动3到4次,完全可以预测。海水pH值和溶解氧在退潮期间降低,在退潮时达到极低值(7.2 pHT和1.9 毫克 氧气 L−1在Bourake,vs 7.9 pHT和5.5 毫克 氧气 参考珊瑚礁处的L−1)。溶解氧、温度和pH值根据高达4.91的潮汐而波动 毫克 氧气 L−1,6.50 °C和0.69 pHT单位。此外,Bouraké泻湖的大多数化学参数的浓度都高出一到五倍,特别是有机和无机碳和氮,但也有一些营养物质,尤其是硅酸盐。令人惊讶的是,尽管环境条件极端,海水化学成分发生了变化,但我们的研究结果显示,大型藻类、海绵和珊瑚的群落多样性高,分别占28种、11种和66种。环境变异性和营养失衡都可能有助于它们在这种极端环境条件下的生存。我们描述了Bouraké生态系统的自然动力学及其作为自然实验室的相关性,以研究海底生物对多种压力源(如未来气候变化条件)的适应性反应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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