Department of Biology, Pennsylvania State University, University Park, PA, USA.
Proc Biol Sci. 2010 Oct 7;277(1696):2925-34. doi: 10.1098/rspb.2010.0385. Epub 2010 May 5.
Mutualisms between reef-building corals and endosymbiotic dinoflagellates are particularly sensitive to environmental stress, yet the ecosystems they construct have endured major oscillations in global climate. During the winter of 2008, an extreme cold-water event occurred in the Gulf of California that bleached corals in the genus Pocillopora harbouring a thermally 'sensitive' symbiont, designated Symbiodinium C1b-c, while colonies possessing Symbiodinium D1 were mostly unaffected. Certain bleached colonies recovered quickly while others suffered partial or complete mortality. In most colonies, no appreciable change was observed in the identity of the original symbiont, indicating that these partnerships are stable. During the initial phases of recovery, a third species of symbiont B1(Aiptasia), genetically identical to that harboured by the invasive anemone, Aiptasia sp., grew opportunistically and was visible as light-yellow patches on the branch tips of several colonies. However, this symbiont did not persist and was displaced in all cases by C1b-c several months later. Colonies with D1 were abundant at inshore habitats along the continental eastern Pacific, where seasonal turbidity is high relative to offshore islands. Environmental conditions of the central and southern coasts of Mexico were not sufficient to explain the exclusivity of D1 Pocillopora in these regions. It is possible that mass mortalities associated with major thermal disturbances during the 1997-1998 El Niño Southern Oscillation eliminated C1b-c holobionts from these locations. The differential loss of Pocillopora holobionts in response to thermal stress suggests that natural selection on existing variation can cause rapid and significant shifts in the frequency of particular coral-algal partnerships. However, coral populations may take decades to recover following episodes of severe selection, thereby raising considerable uncertainty about the long-term viability of these communities.
造礁石珊瑚与其共生虫黄藻之间的互利共生关系对环境压力特别敏感,但它们所构建的生态系统却经受住了全球气候变化的重大波动。2008 年冬季,加利福尼亚湾发生了一次极端冷水事件,使携带热敏感共生体 Symbiodinium C1b-c 的石珊瑚属 Pocillopora 白化,而携带 Symbiodinium D1 的珊瑚礁则基本未受影响。某些白化的珊瑚礁很快恢复,而其他珊瑚礁则遭受部分或完全死亡。在大多数珊瑚礁中,原始共生体的身份没有明显变化,这表明这些共生关系是稳定的。在恢复的初始阶段,第三种共生体 B1(Aiptasia),与入侵海葵 Aiptasia sp. 所携带的共生体在遗传上完全相同,机会性地生长,并在几个珊瑚礁的分支尖端呈现出浅黄色斑块。然而,这种共生体并没有持续存在,几个月后,所有情况下都被 C1b-c 取代。在东太平洋大陆沿岸的近岸栖息地,D1 丰富存在,与近海岛屿相比,季节性浊度较高。墨西哥中南部海岸的环境条件不足以解释 D1 Pocillopora 在这些地区的排他性。可能是 1997-1998 年厄尔尼诺南方涛动期间与主要热干扰相关的大规模死亡事件使这些地区的 C1b-c 共生体灭绝。Pocillopora 共生体对热应激的不同反应表明,对现有变异的自然选择可以导致特定珊瑚藻共生关系的频率发生快速而显著的变化。然而,珊瑚种群可能需要数十年才能从严重选择事件中恢复,从而对这些群落的长期生存能力产生相当大的不确定性。