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Origin of the plastid in the anomalously pigmented dinoflagellate Gymnodinium mikimotoi (Gymnodiniales, Dinophyta) as inferred from phylogenetic analysis based on the gene encoding the large subunit of form I‐type RuBisCO

The dinoflagellate Gymnodinium mikimotoi Miyake et Kominami ex Oda possesses an anomalously pigmented plastid which contains 19′‐hexanoyloxyfucoxanthin, 19′‐butanoyloxyfucoxanthin and fucoxanthin instead of peridinin as the major carotenoids. Previously, we have shown that the plastid of G. mikimotoi belongs to the rhodoplast lineage as inferred from phylogenetic analyses based on the amino acid sequences deduced from psbA and psaA and the nucleotide sequence of the plastid small subunit ribosomal RNA. Furthermore, in the present study, we cloned and sequenced an additional representative plastid gene, rbcL, encoding the large subunit of ribulose 1–5 bisphosphate carboxylase/oxygenase (RuBisCO LSU) from G. mikimotoi. The amino acid sequence deduced from the rbcL gene of G. mikimotoi apparently revealed the conventional form I RuBisCO LSU, which is present in most photosynthetic organisms, and not the divergent form II existing in typically pigmented dinofl age Nates with plastids containing peridinin as the main carotenoid. This finding supports the hypothesis that the origins of the plastids in G. mikimotoi and peridinin‐type dinoflagellates are not related to each other. Molecular phylogenetic analysis based on the amino acid sequence deduced from the rbcL gene further showed that the plastid of G. mikimotoi belongs to the rhodoplast lineage. In particular, G. mikimotoi clustered with haptophytes in the phylogenetic tree. From this result, two hypotheses with respect to the origin of the plastid in G. mikimotoi can be proposed: G. mikimotoi may have engulfed a haptophyte‐like cell (tertiary symbiosis) or englulfed a rhodophyte‐like cell that was closely related to the origin of the plastid in the haptophyte (secondary symbiosis).