Streptococcus sanguis colonizes several human oral surfaces, including both hard and soft tissues. Large salivary mucin-like glycoproteins bearing sialic acid residues are known to bind various S.sanguis strains. However, the molecular basis for the adhesion of S.sanguis to human buccal epithelial cells (HBEC) has not been established. The present study shows that S.sanguis OMZ 9 binds to exfoliated HBEC in a sialic acid-sensitive manner. The desialylation of such cells invariably abolishes adhesion of S.sanguis OMZ 9 to the cell surface. A soluble glycopeptide bearing short sialylated O-linked carbohydrate chains behaves as a potent inhibitor of the attachment of S.sanguis OMZ 9 to exfoliated HBEC. The resialylation of desialylated HBEC with CMP-sialic acid and Gal beta 1,3GalNAc alpha 2,3-sialyltransferase specific for O-glycans restores the receptor function for S.sanguis OMZ 9, whereas a similar cell resialylation with the Gal beta 1,4GlcNAc alpha 2,6-sialyltransferase specific for N-glycans is without effect. Finally, the same resialylation reaction carried out with CMP-9-fluoresceinyl-sialic acid as a substrate yields exfoliated HBEC bearing fluorescence on a single 23 kDa protein, when using the alpha 2,3-sialyltransferase as the catalyst. The latter finding demonstrates that this 23 kDa cell surface glycoprotein bears NeuNAc alpha 2-3Gal beta 1-3GalNAc O-linked sugar chains, a carbohydrate sequence which is recognized by S.sanguis OMZ 9 on exfoliated HBEC. In similar experiments carried out with a buccal carcinoma cell line termed SqCC/Y1, S.sanguis OMZ 9 did not attach in great numbers to such cultured cells, and these cells were shown to not express membrane glycoprotein bearing alpha 2,3-sialylated O-linked carbohydrate chains.
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http://dx.doi.org/10.1093/glycob/5.1.97 | DOI Listing |
Mar Environ Res
January 2025
Université de Bordeaux, CNRS Bordeaux INP, EPOC, UMR 5805, F-33600, Pessac, France.
The western Indian continental shelf (eastern Arabian Sea) exhibits contrasting biogeochemical features. This area becomes highly productive due to summer monsoon-driven coastal upwelling in the south and winter monsoon-induced convective mixing in the north. Additionally, in the northern self, the eastern boundary of the Oxygen Minimum Zone (OMZ) persists but is absent in the south.
View Article and Find Full Text PDFJ Fluoresc
January 2025
School of Science, Jiangnan University, Wuxi, 214122, China.
In this study, nitrogen-doped carbon nanodots (N-CDs) with temperature and fluorescence sensing were prepared via hydrothermal method using L-lysine and ethylenediamine as precursors. The synthesized N-CDs exhibited spherical morphology with sizes ranging from 2.8 to 5.
View Article and Find Full Text PDFMar Environ Res
December 2024
CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China; Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, 266071, China.
This study analyzed the relationship between the oxygen minimum zone (OMZ) and various types of carbon, such as POC, DOC, and DIC, in the Y3 seamount area in the Western Pacific. The results indicated that the OMZ was located at 200-1000 m and a threshold of 100 μmol/kg was established for this area of the Western Pacific. The DOC and POC changed drastically out of OMZ while they were relatively stable within the OMZ due to the low oxygen.
View Article and Find Full Text PDFProc Natl Acad Sci U S A
December 2024
Department of Global Ecology, Carnegie Institution for Science, Stanford, CA 94305.
Microorganisms in marine oxygen minimum zones (OMZs) drive globally impactful biogeochemical processes. One such process is multistep denitrification (NO→NO→NO→NO→N), which dominates OMZ bioavailable nitrogen (N) loss and nitrous oxide (NO) production. Denitrification-derived N loss is typically measured and modeled as a single step, but observations reveal that most denitrifiers in OMZs contain subsets ("modules") of the complete pathway.
View Article and Find Full Text PDFMar Pollut Bull
December 2024
Bharathidasan University, Tiruchirappalli, Tamilnadu, India.
Eutrophication of marine ecosystems is a global problem, particularly in a changing climate and the spreading of Oxygen Minimum Zones (OMZs). The eastern Arabian Sea has both seasonal and permanent/perennial OMZs, but our understanding of the fauna there is extremely poor. So, this study investigated the composition and physiological status (alive or dead) of zooplankton (copepods) in the two OMZs.
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