Draisma Stefano G A, van Reine Willem F Prud'homme, Sauvage Thomas, Belton Gareth S, Gurgel C Frederico D, Lim Phaik Eem, Phang Siew Moi
Institute of Ocean & Earth Sciences, University of Malaya, Kuala Lumpur, 50603, Malaysia.
Naturalis Biodiversity Center, P.O. Box 9517, Leiden, 2300 RA, The Netherlands.
J Phycol. 2014 Dec;50(6):1020-34. doi: 10.1111/jpy.12231. Epub 2014 Oct 9.
The siphonous green algal family Caulerpaceae includes the monotypic genus Caulerpella and the species-rich genus Caulerpa. A molecular phylogeny was inferred from chloroplast tufA and rbcL DNA sequences analyzed together with a five marker dataset of non-caulerpacean siphonous green algae. Six Caulerpaceae lineages were revealed, but relationships between them remained largely unresolved. A Caulerpella clade representing multiple cryptic species was nested within the genus Caulerpa. Therefore, that genus is subsumed and Caulerpa ambigua Okamura is reinstated. Caulerpa subgenus status is proposed for the six lineages substantiated by morphological characters, viz., three monotypic subgenera Cliftonii, Hedleyi, and Caulerpella, subgenus Araucarioideae exhibiting stolons covered with scale-like appendages, subgenus Charoideae characterized by a verticillate branching mode, and subgenus Caulerpa for a clade regarded as the Caulerpa core clade. The latter subgenus is subdivided in two sections, i.e., Sedoideae for species with pyrenoids and a species-rich section Caulerpa. A single section with the same name is proposed for each of the other five subgenera. In addition, species status is proposed for Caulerpa filicoides var. andamanensis (W.R. Taylor). All Caulerpa species without sequence data were examined (or data were taken from species descriptions) and classified in the new classification scheme. A temporal framework of Caulerpa diversification is provided by calibrating the phylogeny in geological time. The chronogram suggests that Caulerpa diversified into subgenera and sections after the Triassic-Jurassic mass extinction and that infra-section species radiation happened after the Cretaceous-Tertiary mass extinction.
管藻目绿藻科包括单型属拟蕨藻属和物种丰富的蕨藻属。基于叶绿体tufA和rbcL DNA序列,并结合非管藻目绿藻的五个标记数据集,推断出一个分子系统发育树。揭示了六个管藻科谱系,但它们之间的关系在很大程度上仍未解决。一个代表多个隐存种的拟蕨藻分支嵌套在蕨藻属内。因此,该属被归并,冈村蕨藻被重新恢复。根据形态特征,为六个谱系提出了蕨藻亚属的地位,即三个单型亚属,克利夫顿蕨藻亚属、赫德利蕨藻亚属和拟蕨藻亚属,南洋杉蕨藻亚属的匍匐茎上覆盖着鳞片状附属物,轮叶蕨藻亚属的特征是轮状分枝模式,以及被视为蕨藻核心分支的蕨藻亚属。后一个亚属又细分为两个组,即具有蛋白核的种类的景天蕨藻组和一个物种丰富的蕨藻组。为其他五个亚属分别提出了一个同名的组。此外,还提出了安达曼蕨藻变种(W.R. 泰勒)的物种地位。对所有没有序列数据的蕨藻物种进行了检查(或数据取自物种描述),并按照新的分类方案进行了分类。通过在地质时间中标定系统发育树,提供了蕨藻多样化的时间框架。时间树状图表明,蕨藻在三叠纪 - 侏罗纪大灭绝之后分化为亚属和组,而组内物种辐射发生在白垩纪 - 古近纪大灭绝之后。