Nir Orit, Gruber David F, Shemesh Eli, Glasser Eliezra, Tchernov Dan
Marine Biology Department, The Leon H. Charney School of Marine Sciences, University of Haifa, Haifa, Israel.
Department of Natural Sciences, City University of New York, Baruch College, New York, New York, United States of America ; American Museum of Natural History, Sackler Institute of Comparative Genomics, New York, New York, United States of America.
PLoS One. 2014 Jan 15;9(1):e84968. doi: 10.1371/journal.pone.0084968. eCollection 2014.
Coral bleaching occurs when environmental stress induces breakdown of the coral-algae symbiosis and the host initiates algae expulsion. Two types of coral bleaching had been thoroughly discussed in the scientific literature; the first is primarily associated with mass coral bleaching events; the second is a seasonal loss of algae and/or pigments. Here, we describe a phenomenon that has been witnessed for repeated summers in the mesophotic zone (40-63 m) in the northern Red Sea: seasonal bleaching and recovery of several hermatypic coral species. In this study, we followed the recurring bleaching process of the common coral Stylophora pistillata. Bleaching occurred from April to September with a 66% decline in chlorophyll a concentration, while recovery began in October. Using aquarium and transplantation experiments, we explored environmental factors such as temperature, photon flux density and heterotrophic food availability. Our experiments and observations did not yield one single factor, alone, responsible for the seasonal bleaching. The dinoflagellate symbionts (of the genus Symbiodinium) in shallow (5 m) Stylophora pistillata were found to have a net photosynthetic rate of 56.98-92.19 µmol O2 cm(-2) day(-1). However, those from mesophotic depth (60 m) during months when they are not bleached are net consumers of oxygen having a net photosynthetic rate between -12.86 - (-10.24) µmol O2 cm(-2) day(-1). But during months when these mesophotic corals are partially-bleached, they yielded higher net production, between -2.83-0.76 µmol O2 cm(-2) day(-1). This study opens research questions as to why mesophotic zooxanthellae are more successfully meeting the corals metabolic requirements when Chl a concentration decreases by over 60% during summer and early fall.
当环境压力导致珊瑚与藻类的共生关系破裂,宿主开始排出藻类时,珊瑚白化现象就会发生。科学文献中已对两种类型的珊瑚白化进行了深入讨论;第一种主要与大规模珊瑚白化事件有关;第二种是藻类和/或色素的季节性损失。在此,我们描述了一种在红海北部中光层(40 - 63米)连续多个夏季都能观察到的现象:几种造礁珊瑚物种的季节性白化和恢复。在本研究中,我们追踪了常见珊瑚鹿角杯形珊瑚反复出现的白化过程。白化发生在4月至9月,叶绿素a浓度下降了66%,而恢复始于10月。我们通过水族箱和移植实验,探究了温度、光子通量密度和异养食物可利用性等环境因素。我们的实验和观察结果表明,没有一个单一因素能单独导致季节性白化。浅海(5米)鹿角杯形珊瑚中的甲藻共生体(共生藻属)的净光合速率为56.98 - 92.19 μmol O2 cm(-2) 天(-1)。然而,中光层深度(60米)的共生体在未白化的月份是氧气的净消费者,净光合速率在 -12.86 - (-10.24) μmol O2 cm(-2) 天(-1)之间。但在这些中光层珊瑚部分白化的月份,它们产生了更高的净产量,在 - 2.83 - 0.76 μmol O₂ cm(-2) 天(-1)之间。这项研究提出了一些研究问题,即为何在夏季和初秋叶绿素a浓度下降超过60%时,中光层虫黄藻能更成功地满足珊瑚的代谢需求。