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海水温度升高导致皮壳状珊瑚藻的微生物群落发生变化,这可能对珊瑚幼虫的附着产生影响。

Elevated seawater temperature causes a microbial shift on crustose coralline algae with implications for the recruitment of coral larvae.

机构信息

Australian Institute of Marine Science, Townsville, Queensland, Australia.

出版信息

ISME J. 2011 Apr;5(4):759-70. doi: 10.1038/ismej.2010.152. Epub 2010 Oct 14.

Abstract

Crustose coralline algae (CCA) are key reef-building primary producers that are known to induce the metamorphosis and recruitment of many species of coral larvae. Reef biofilms (particularly microorganisms associated with CCA) are also important as settlement cues for a variety of marine invertebrates, including corals. If rising sea surface temperatures (SSTs) affect CCA and/or their associated biofilms, this may in turn affect recruitment on coral reefs. Herein, we report that the CCA Neogoniolithon fosliei, and its associated microbial communities do not tolerate SSTs of 32 °C, only 2-4 °C above the mean maximum annual SST. After 7 days at 32 °C, the CCA exhibited clear signs of stress, including bleaching, a reduction in maximum quantum yield (F(v)/F(m)) and a large shift in microbial community structure. This shift at 32 °C involved an increase in Bacteroidetes and a reduction in Alphaproteobacteria, including the loss of the primary strain (with high-sequence similarity to a described coral symbiont). A recovery in F(v)/F(m) was observed in CCA exposed to 31 °C following 7 days of recovery (at 27 °C); however, CCA exposed to 32 °C did not recover during this time as evidenced by the rapid growth of endolithic green algae. A 50% reduction in the ability of N. fosliei to induce coral larval metamorphosis at 32 °C accompanied the changes in microbiology, pigmentation and photophysiology of the CCA. This is the first experimental evidence to demonstrate how thermal stress influences microbial associations on CCA with subsequent downstream impacts on coral recruitment, which is critical for reef regeneration and recovery from climate-related mortality events.

摘要

石珊瑚藻(CCA)是主要的造礁初级生产者,已知它们能诱导许多珊瑚幼虫的变态和定殖。珊瑚礁生物膜(特别是与 CCA 相关的微生物)也是多种海洋无脊椎动物(包括珊瑚)的重要定殖线索。如果不断上升的海水表面温度(SST)影响 CCA 和/或其相关生物膜,这可能反过来又会影响珊瑚礁的定殖。在此,我们报告石珊瑚藻 Neogoniolithon fosliei 及其相关微生物群落无法耐受 32°C 的 SST,仅比年平均最高 SST 高 2-4°C。在 32°C 下 7 天后,CCA 表现出明显的应激迹象,包括白化、最大光量子产量(F(v)/F(m))降低以及微生物群落结构的重大转变。这种在 32°C 下的转变涉及到变形菌门(Bacteroidetes)的增加和α变形菌门(Alphaproteobacteria)的减少,包括主要菌株的损失(与描述的珊瑚共生体具有高度相似的序列)。暴露于 31°C 下 7 天后,CCA 中观察到 F(v)/F(m)的恢复;然而,暴露于 32°C 下的 CCA 在这段时间内没有恢复,这表现在内生绿藻的快速生长上。在 32°C 下,N. fosliei 诱导珊瑚幼虫变态的能力降低了 50%,这伴随着 CCA 微生物学、色素沉着和光生理的变化。这是首次有实验证据表明热应激如何影响 CCA 上的微生物共生体,随后对珊瑚定殖产生下游影响,这对珊瑚礁的再生和从与气候相关的死亡事件中恢复至关重要。

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