Craveiro Sandra C, Calado António J, Daugbjerg Niels, Moestrup Øjvind
GeoBioSciences, GeoTechnologies and GeoEngineering (GeoBioTec) Research Unit and Departamento de Biologia, Universidade de Aveiro, P-3810-193 Aveiro, PortugalPhycology Laboratory, Department of Biology, University of Copenhagen, Øster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.
J Phycol. 2009 Oct;45(5):1175-94. doi: 10.1111/j.1529-8817.2009.00739.x. Epub 2009 Sep 28.
The name Peridinium palatinum Lauterborn currently designates a freshwater peridinioid with 13 epithecal and six cingular plates, and no apical pore complex. Freshwater dinoflagellate floras classify it in Peridinium group palatinum together with P. pseudolaeve M. Lefèvre. General ultrastructure, flagellar apparatus, and pusular components of P. palatinum were examined by serial section TEM and compared to P. cinctum (O. F. Müll.) Ehrenb. and Peridiniopsis borgei Lemmerm., respectively, types of Peridinium and Peridiniopsis. Partial LSU rDNA sequences from P. palatinum, P. pseudolaeve and several peridinioids, woloszynskioids, gymnodinioids, and other dinoflagellates were used for a phylogenetic analysis. General morphology and tabulation of taxa in group palatinum were characterized by SEM. Differences in plate numbers, affecting both the epitheca and the cingulum, combine with differences in plate ornamentation and a suite of internal cell features to suggest a generic-level distinction between Peridinium group palatinum and typical Peridinium. The branching pattern of the phylogenetic tree is compatible with this conclusion, although with low support from bootstrap values and posterior probabilities, as are sequence divergences estimated between species in group palatinum, and typical Peridinium and Peridiniopsis. Palatinus nov. gen. is proposed with the new combinations Palatinus apiculatus nov. comb. (type species; syn. Peridinium palatinum), P. apiculatus var. laevis nov. comb., and P. pseudolaevis nov. comb. Distinctive characters for Palatinus include a smooth or slightly granulate, but not areolate, plate surface, a large central pyrenoid penetrated by cytoplasmic channels and radiating into chloroplast lobes, and the presence of a peduncle-homologous microtubular strand. Palatinus cells exit the theca through the antapical-postcingular area.
目前,腭梨甲藻(Peridinium palatinum Lauterborn)指的是一种淡水梨甲藻,具有13块上壳板和6块环沟板,且无顶孔复合体。淡水甲藻区系将其与伪平滑梨甲藻(P. pseudolaeve M. Lefèvre)一同归入腭梨甲藻组(Peridinium group palatinum)。通过连续切片透射电子显微镜对腭梨甲藻的一般超微结构、鞭毛器和液泡成分进行了研究,并分别与梨甲藻属(Peridinium)的模式种环纹梨甲藻(P. cinctum (O. F. Müll.) Ehrenb.)以及梨甲藻状藻属(Peridiniopsis)的模式种博氏梨甲藻状藻(Peridiniopsis borgei Lemmerm.)进行了比较。利用腭梨甲藻、伪平滑梨甲藻以及几种梨甲藻、沃氏藻、裸甲藻和其他甲藻的部分大亚基核糖体DNA序列进行了系统发育分析。通过扫描电子显微镜对腭梨甲藻组类群的一般形态和板式进行了表征。上壳和环沟板数量的差异,以及板饰和一系列细胞内部特征的差异,表明腭梨甲藻组与典型的梨甲藻属在属级水平上存在区别。系统发育树的分支模式与这一结论相符,尽管自展值和后验概率的支持度较低,腭梨甲藻组内物种之间以及典型的梨甲藻属和梨甲藻状藻属之间的序列分歧也是如此。现提出新属梨甲藻属(Palatinus nov. gen.),并给出新组合尖顶梨甲藻(Palatinus apiculatus nov. comb.)(模式种;同物异名腭梨甲藻)、光滑尖顶梨甲藻变种(P. apiculatus var. laevis nov. comb.)和伪平滑梨甲藻(P. pseudolaevis nov. comb.)。梨甲藻属的独特特征包括板表面光滑或略有颗粒状,但无网纹,一个大的中央蛋白核被细胞质通道穿透并延伸到叶绿体叶中,以及存在一条与柄同源的微管链。梨甲藻属细胞通过反顶环沟后区域离开壳套。