State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen, 361102, PR China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou), Guangzhou, 511458, PR China.
State Key Laboratory of Marine Environmental Science, College of Ocean and Earth Sciences, Xiamen University, Xiamen, 361102, PR China; Xiamen Key Laboratory of Urban Sea Ecological Conservation and Restoration (USER), Xiamen University, Xiamen, 361102, PR China.
Mar Environ Res. 2023 Jul;189:106044. doi: 10.1016/j.marenvres.2023.106044. Epub 2023 Jun 5.
From July to August 2022, scleractinian coral communities in China's Greater Bay Area (GBA) in the northern South China Sea (nSCS) experienced an unprecedented bleaching event, despite the fact that coral communities in this area are often considered coral thermal refugia due to their high latitude distribution. Field surveys of six sites covering three main coral distribution areas of the GBA revealed that coral bleaching occurred at all sites. Bleaching was more severe in shallow water (1-3 m) than in deep water (4-6 m), as indicated by both percent bleached cover (51.80 ± 10.04% vs. 7.09 ± 7.37%) and bleached colonies (45.86 ± 11.22% vs. 6.58 ± 6.53%). Coral genera Acropora, Favites, Montipora, Platygyra, Pocillopora, and Porites showed high susceptibility to bleaching, and Acropora and Pocillopora suffered high post-bleaching mortality. In the three areas surveyed, analysis of oceanographic data detected marine heatwaves (MHWs) during the summer, with mean intensities between 1.62 and 1.97 °C and durations between 5 and 22 days. These MHWs were primarily driven by increased shortwave radiation due to strong western Pacific Subtropical High (WPSH), combined with reduced mixing between the surface and deep upwelling waters due to reduced wind speed. Comparing with histological oceanographic data showed that the 2022 MHWs were unprecedented, and there was a significant increase in the frequency, intensity, and total days of MHWs during 1982-2022. Furthermore, the heterogeneous distribution of summer MHW characteristics indicates that the coastal upwelling may modulate the spatial distribution of summer MHWs in nSCS through its cooling effect. Overall, our study indicates that MHWs may have affected the structure of the subtropical coral communities in the nSCS, and impaired their potential as thermal refugia.
2022 年 7 月至 8 月,南海北部(nSCS)中国大湾区(GBA)的石珊瑚群落经历了一次前所未有的白化事件,尽管该地区的珊瑚群落由于高纬度分布通常被认为是珊瑚热避难所。对覆盖 GBA 三个主要珊瑚分布区的六个地点的实地调查显示,所有地点都发生了珊瑚白化。浅水区(1-3 米)的白化程度比深水区(4-6 米)严重,表现为白化覆盖百分比(51.80±10.04%比 7.09±7.37%)和白化珊瑚(45.86±11.22%比 6.58±6.53%)。石珊瑚属 Acropora、Favites、Montipora、Platygyra、Pocillopora 和 Porites 对白化的敏感性较高,Acropora 和 Pocillopora 在白化后死亡率较高。在所调查的三个区域中,对海洋学数据的分析检测到夏季发生了海洋热浪(MHWs),平均强度在 1.62 到 1.97°C 之间,持续时间在 5 到 22 天之间。这些 MHWs 主要是由于西太平洋副热带高压(WPSH)导致的短波辐射增加,以及风速降低导致表面和深层上升流之间的混合减少所致。与组织学海洋学数据的比较表明,2022 年的 MHW 是前所未有的,1982-2022 年期间,MHW 的频率、强度和总天数都显著增加。此外,夏季 MHW 特征的异质分布表明,沿岸上升流可能通过其冷却效应调节南海北部夏季 MHW 的空间分布。总体而言,我们的研究表明,MHWs 可能影响了南海北部亚热带珊瑚群落的结构,并损害了它们作为热避难所的潜力。