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细菌不是地中海珊瑚巴塔哥尼亚石珊瑚(Oculina patagonica)白化的主要原因。

Bacteria are not the primary cause of bleaching in the Mediterranean coral Oculina patagonica.

作者信息

Ainsworth T D, Fine M, Roff G, Hoegh-Guldberg O

机构信息

Centre for Marine Studies, and the ARC Centre of Excellence for Coral Reef Studies, The University of Queensland, St Lucia, Queensland, Australia.

出版信息

ISME J. 2008 Jan;2(1):67-73. doi: 10.1038/ismej.2007.88. Epub 2007 Dec 6.

DOI:10.1038/ismej.2007.88
PMID:18059488
Abstract

Coral bleaching occurs when the endosymbiosis between corals and their symbionts disintegrates during stress. Mass coral bleaching events have increased over the past 20 years and are directly correlated with periods of warm sea temperatures. However, some hypotheses have suggested that reef-building corals bleach due to infection by bacterial pathogens. The 'Bacterial Bleaching' hypothesis is based on laboratory studies of the Mediterranean invading coral, Oculina patagonica, and has further generated conclusions such as the coral probiotic hypothesis and coral hologenome theory of evolution. We aimed to investigate the natural microbial ecology of O. patagonica during the annual bleaching using fluorescence in situ hybridization to map bacterial populations within the coral tissue layers, and found that the coral bleaches on the temperate rocky reefs of the Israeli coastline without the presence of Vibrio shiloi or bacterial penetration of its tissue layers. Bacterial communities were found associated with the endolithic layer of bleached coral regions, and a community dominance shift from an apparent cyanobacterial-dominated endolithic layer to an algal-dominated layer was found in bleached coral samples. While bacterial communities certainly play important roles in coral stasis and health, we suggest environmental stressors, such as those documented with reef-building corals, are the primary triggers leading to bleaching of O. patagonica and suggest that bacterial involvement in patterns of bleaching is that of opportunistic colonization.

摘要

当珊瑚与其共生体之间的内共生关系在压力下瓦解时,珊瑚白化现象就会发生。在过去20年里,大规模珊瑚白化事件有所增加,并且与海水温度升高的时期直接相关。然而,一些假说认为,造礁珊瑚白化是由细菌病原体感染所致。“细菌白化”假说基于对入侵地中海的珊瑚——巴塔哥尼亚石珊瑚(Oculina patagonica)的实验室研究,并进一步产生了诸如珊瑚益生菌假说和珊瑚全基因组进化理论等结论。我们旨在利用荧光原位杂交技术绘制珊瑚组织层内的细菌种群图谱,以研究巴塔哥尼亚石珊瑚在年度白化期间的自然微生物生态,结果发现,在以色列海岸线的温带岩石礁上,这种珊瑚在没有希氏弧菌(Vibrio shiloi)存在或其组织层没有细菌侵入的情况下发生了白化。在白化珊瑚区域的内石层发现了细菌群落,并且在白化珊瑚样本中发现,群落优势从明显以蓝藻为主的内石层转变为以藻类为主的层。虽然细菌群落肯定在珊瑚的稳定和健康中发挥着重要作用,但我们认为,环境压力因素,如那些在造礁珊瑚中记录到的压力因素,是导致巴塔哥尼亚石珊瑚白化的主要触发因素,并表明细菌在白化模式中的作用是机会性定殖。

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