The marine microalgal class Bolidophyceae is a sister group to the diatoms and includes motile naked (bolidomonad) cells and nonmotile siliceous plate‐bearing (parmalean) cells. The bolidomonad cell possesses two unequal flagella, a long one bearing mastigonemes (tubular hairs) and a shorter smooth one, with the basal apparatus reduced to basal bodies. The parmalean cell wall is composed of 5–8 interlocking siliceous plates, which exhibit distinct dorsal, ventral, shield and girdle plate morphologies. Both cell types have a chloroplast (including the major carotenoid fucoxanthin and chlorophylls
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) with a girdle lamella, Golgi body, nucleus, mitochondrion and large vacuole. The group currently includes approximately 30 taxa, mostly described from high latitudes, although some tropical species also have been reported. Parmalean algae reach high absolute abundances in the spring, but later in the summer, they sink to the pycnocline (a layer of maximum water density difference) – a strategy similar to the centric diatoms. Their rare occurrences in sediment trap and surface sediments suggest that the siliceous plates are mostly recycled in the photic zone, yet plates of parmalean algae have been discovered in older sediments, although their true stratigraphic distribution remains unknown.
Key Concepts
Recent gene sequence analyses have shown that the genus
Bolidomonas
is polyphyletic, forming several clades, one of which includes the Parmales, resulting in all
Bolidomonas
species being transferred to
Triparma
.
The Bolidophyceae is a sister group to the diatoms, with similar cell features and pigment composition.
Bolidomonad cells are motile and naked, while the nonmotile parmalean cells are covered by 5–8 silicified plates, consisting of three or four types (shield, girdle, ventral and/or dorsal), arranged in a particular pattern and with distinct morphology, which defines each genus.
At present, the ploidy level or life cycle has not been identified; however, it is possible that the nonmotile silica plate‐bearing cells are diploid and alternate with a naked bolidomonad‐like flagellate haploid stage.
Naked bolidomonads appear to be present throughout the World's oceans, while most parmalean taxa inhabit high latitude areas, although tropical taxa also exist.
Studies have shown the parmalean ecology is similar to that of the centric diatoms, with assemblages remaining in their silicified form throughout the year and sinking to the pycnocline in the summer.
Remains of parmalean cells found in the fossil record suggest at least an early Cenozoic origin.
If the bolidophytes are haplodiplontic and represent an ancestral stage to the diplontic diatoms, then future molecular clock calculations should reveal a much older origin, possibly as old as the late Paleozoic (as diatoms are believed to have diverged around the Permian–Triassic boundary).