A new fossil diatom, Stephanodiscus kusuensis sp. nov., is described from a diatomite deposit from the Kusu Basin, Oita Prefecture Japan. Radiometric age estimates of the strata in which the taxon occurs are 400-500 kyr. The new species is distinct from all other known species of Stephanodiscus because it possesses a highly pronounced double concentric undulation and two distinct arrangements of central strutted processes. Cladistic analysis is used to identify the phylogenetic position of this taxon with respect to other Stephanodiscus species. © 2006 Japanese Society of Phycology.
CITATION STYLE
Julius, M. L., Curtin, M., & Tanaka, H. (2006). Stephanodiscus kusuensis, sp. nov a new Pleistocene diatom from Southern Japan. Phycological Research, 54(4), 294–301. https://doi.org/10.1111/j.1440-1835.2006.00436.x
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