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The ancient evolutionary origins of Scleractinia revealed by azooxanthellate corals

机译:偶氮黄藻珊瑚揭示了巩膜藻的古老进化起源

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Background Scleractinian corals are currently a focus of major interest because of their ecological importance and the uncertain fate of coral reefs in the face of increasing anthropogenic pressure. Despite this, remarkably little is known about the evolutionary origins of corals. The Scleractinia suddenly appear in the fossil record about 240 Ma, but the range of morphological variation seen in these Middle Triassic fossils is comparable to that of modern scleractinians, implying much earlier origins that have so far remained elusive. A significant weakness in reconstruction(s) of early coral evolution is that deep-sea corals have been poorly represented in molecular phylogenetic analyses. Results By adding new data from a large and representative range of deep-water species to existing molecular datasets and applying a relaxed molecular clock, we show that two exclusively deep-sea families, the Gardineriidae and Micrabaciidae, diverged prior to the Complexa/Robusta coral split around 425 Ma, thereby pushing the evolutionary origin of scleractinian corals deep into the Paleozoic. Conclusions The early divergence and distinctive morphologies of the extant gardineriid and micrabaciid corals suggest a link with Ordovician "scleractiniamorph" fossils that were previously assumed to represent extinct anthozoan skeletonized lineages. Therefore, scleractinian corals most likely evolved from Paleozoic soft-bodied ancestors. Modern shallow-water Scleractinia, which are dependent on symbionts, appear to have had several independent origins from solitary, non-symbiotic precursors. The Scleractinia have survived periods of massive climate change in the past, suggesting that as a lineage they may be less vulnerable to future changes than often assumed.
机译:背景技术巩膜珊瑚由于其生态重要性和面对不断增加的人为压力的不确定性,目前是人们关注的焦点。尽管如此,对珊瑚的进化起源知之甚少。巩膜藻突然出现在约240 Ma的化石记录中,但是这些中三叠纪化石中所见的形态变化范围与现代的巩膜藻相当,这意味着迄今为止尚不清楚的更早的起源。早期珊瑚演化重建的一个显着弱点是,深海珊瑚在分子系统发育分析中的代表性很低。结果通过将来自广泛的代表性深水物种的新数据添加到现有的分子数据集中并应用轻松的分子钟,我们显示出两个专有的深海科,Gardineriidae和Micrabaciidae,在Complexa / Robusta珊瑚之前分叉了大约在425 Ma左右分裂,从而将巩膜珊瑚的进化起源推向了古生代。结论现有的gardineriid和micrabaciid珊瑚的早期散布和独特的形态表明与奥陶纪的“ scleractiniamorph”化石有联系,而这些化石以前被认为代表着灭绝的人类动物骨架化世系。因此,Scleractinian珊瑚最有可能是从古生代的软体祖先演化而来的。依赖共生体的现代浅水巩膜菌似乎有多个独立的,非共生的前体起源。过去,Scleractinia在大规模的气候变化中幸免于难,这表明,作为一个世系,Scleractinia对未来变化的脆弱性可能比通常想象的要小。

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