Abstract

The morphogenesis of two hypotrich ciliates, Notohymena antarctica Foissner, 1996 and Engelmanniella mobilis (Engelmann, 1862) Foissner, 1982, were investigated using protargol staining. The main events of the oxytrichid Notohymena antarctica during binary fission are as follows: (1) the oral primordium of the opisthe is formed apokinetally left of transverse cirrus II/1; (2) six streaks of frontal-ventral-transverse cirral anlagen are segmented in the ordinary pattern 1: 3: 3: 3: 4: 4 from left to right, which form three frontal, four frontoventral, one buccal, three ventral, two pretransverse ventral and five transverse cirri; (3) marginal anlagen are formed intrakinetally and the right marginal anlagen develop much earlier than those on the left. Phylogenetic analyses based on SSU rDNA sequence data indicate that Notohymena is monophyletic. A remarkable morphogenetic feature in E. mobilis is the mode of formation of the right marginal rows. In this paper, we clarified that the right marginal anlagen of E. mobilis are formed and develop to the right of the parental outer right marginal row, and that the grandparental (inner) right marginal row and great-grand parental (the outermost) left marginal row are resorbed. It is the first time to report a population of E. mobilis with comprehensive information, i.e. the morphology, ontogeny and molecular sequence.

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