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海洋酸化降低了有孔虫藻对珊瑚附着的诱导作用。

Ocean acidification reduces induction of coral settlement by crustose coralline algae.

机构信息

Australian Institute of Marine Science, PMB 3, Townsville Mail Centre, Townsville, Qld, 4810, Australia.

出版信息

Glob Chang Biol. 2013 Jan;19(1):303-15. doi: 10.1111/gcb.12008. Epub 2012 Sep 25.

DOI:10.1111/gcb.12008
PMID:23504741
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3597258/
Abstract

Crustose coralline algae (CCA) are a critical component of coral reefs as they accrete carbonate for reef structure and act as settlement substrata for many invertebrates including corals. CCA host a diversity of microorganisms that can also play a role in coral settlement and metamorphosis processes. Although the sensitivity of CCA to ocean acidification (OA) is well established, the response of their associated microbial communities to reduced pH and increased CO2 was previously not known. Here we investigate the sensitivity of CCA-associated microbial biofilms to OA and determine whether or not OA adversely affects the ability of CCA to induce coral larval metamorphosis. We experimentally exposed the CCA Hydrolithon onkodes to four pH/pCO2 conditions consistent with current IPCC predictions for the next few centuries (pH: 8.1, 7.9, 7.7, 7.5, pCO2 : 464, 822, 1187, 1638 μatm). Settlement and metamorphosis of coral larvae was reduced on CCA pre-exposed to pH 7.7 (pCO2  = 1187 μatm) and below over a 6-week period. Additional experiments demonstrated that low pH treatments did not directly affect the ability of larvae to settle, but instead most likely altered the biochemistry of the CCA or its microbial associates. Detailed microbial community analysis of the CCA revealed diverse bacterial assemblages that altered significantly between pH 8.1 (pCO2  = 464 μatm) and pH 7.9 (pCO2  = 822 μatm) with this trend continuing at lower pH/higher pCO2 treatments. The shift in microbial community composition primarily comprised changes in the abundance of the dominant microbes between the different pH treatments and the appearance of new (but rare) microbes at pH 7.5. Microbial shifts and the concomitant reduced ability of CCA to induce coral settlement under OA conditions projected to occur by 2100 is a significant concern for the development, maintenance and recovery of reefs globally.

摘要

石莼藻是珊瑚礁的一个重要组成部分,因为它们可以为珊瑚礁结构积累碳酸盐,并作为许多无脊椎动物包括珊瑚的附着基质。石莼藻上栖息着多种微生物,这些微生物也可以在珊瑚附着和变态过程中发挥作用。虽然石莼藻对海洋酸化(OA)的敏感性已得到充分证实,但之前并不知道其相关微生物群落对降低 pH 值和增加 CO2 的反应。在这里,我们研究了石莼藻相关微生物生物膜对 OA 的敏感性,并确定 OA 是否会对石莼藻诱导珊瑚幼虫变态的能力产生不利影响。我们通过实验将石莼藻 Hydrolithon onkodes 暴露于四种与未来几个世纪内 IPCC 预测一致的 pH/pCO2 条件下(pH:8.1、7.9、7.7、7.5,pCO2:464、822、1187、1638 μatm)。在 6 周的时间里,暴露在 pH7.7(pCO2 = 1187 μatm)及以下的石莼藻上,珊瑚幼虫的附着和变态减少了。进一步的实验表明,低 pH 值处理并没有直接影响幼虫附着的能力,而是很可能改变了石莼藻的生物化学性质或其微生物伙伴。对石莼藻的详细微生物群落分析表明,细菌群落存在多样性,并且在 pH8.1(pCO2 = 464 μatm)和 pH7.9(pCO2 = 822 μatm)之间发生了显著变化,随着 pH 值降低和 pCO2 值升高,这种趋势仍在继续。微生物群落组成的变化主要是由于不同 pH 值处理之间优势微生物的丰度变化,以及在 pH7.5 时出现的新(但罕见)微生物。在预计到 2100 年将发生的 OA 条件下,微生物的变化以及石莼藻诱导珊瑚附着的能力降低,是全球珊瑚礁的发展、维持和恢复的一个重大问题。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/57f1a727b880/gcb0019-0303-f5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/a848bf1a56df/gcb0019-0303-f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/a463242d5c2b/gcb0019-0303-f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/377f17d241f1/gcb0019-0303-f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/eca2a9f9b7f3/gcb0019-0303-f4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/57f1a727b880/gcb0019-0303-f5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/a848bf1a56df/gcb0019-0303-f1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/a463242d5c2b/gcb0019-0303-f2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/377f17d241f1/gcb0019-0303-f3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/eca2a9f9b7f3/gcb0019-0303-f4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2d29/3597258/57f1a727b880/gcb0019-0303-f5.jpg

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