Subcellular location and composition of the wall and secreted extracellular sulphated polysaccharides/proteoglycans of the diatomStauroneis amphioxys Gregory

Summary

Extracellular polysaccharide/proteoglycan (EPS) mucilages play a crucial role in maintaining the structure of the extensive algal sheets that appear along the undersurface of nearshore Antarctic sea ice during the austral spring. In this study we have determined the composition and ultrastructural location of a family of novel sulphated polysaccharides/proteoglycans from the pennate ice diatomStauroneis amphioxys Gregory. They occur as soluble EPS in the culture supernatant, as an intercellular mucilage sheet, and as components of a distinct organic layer (diatotepum) underlying the silicious cell wall. The ultrastructural location and quantitative extraction of the mucilage EPS and the major diatotepum polysaccharides with hot water and alkali, respectively, was monitored by light and electron microscopy. The EPS and wall components were purified by Ultrafiltration, anion exchange and gel filtration chromatographies, and their monosaccharide composition was determined by gas-chro-matography mass spectrometry. The soluble and mucilage EPS, and major diatotepum polysaccharides/proteoglycans had an apparent molecular mass greater than 2 × 10⁶ Da on gel. They contained a similar complex monosaccharide composition that includes glucuronic acid and galactose as the major sugars and significant levels of rhamnose, fucose, arabinose, xylose, mannose, glucose and the mono-O-methylated monosaccharides 3-O-methylrhamnose, 3-O-methylfucose, 3-O- and 4-O-methylxylose. The ratios of Gal to GlcA, which together account for 45% of the monosaccharides, varied from 0.8 (in the soluble EPS) to 2.3 (in diatotepum polysaccharides). The level of sulphation also varied from 5–15% (w/w), with the mucilage EPS being the most highly sulphated. The soluble EPS also contains a small amount of protein (ca. 5%, v/w) which cochromatographs with the polysaccharide during gel filtration and anion exchange chromatographies suggesting that it may be a sulphated proteoglycan. They are clearly distinct from a sulphated glucuronomannan that remained in the alkali-insoluble fraction and may be tightly associated with the silica wall components. The amount of mucilage EPS increased during logarithmic growth but decreased during stationary phase, when most of the EPS was found in the soluble pool. These changes correlate with the breakdown of the mucilage sheet and dispersal of diatom colonies during stationary growth. Interestingly, the soluble EPS from stationary-growth cultures was indistinguishable from the mucilage EPS of logarithmic- or stationary-phase cells, suggesting that the dissolution of the intercellular mucilage was not due to a change in EPS composition. The possibility that cell motility may be required for mucilage formation and the significance of these polysaccharides in the under-ice community is discussed.