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Molecular surveys of marine picoeukaryotes have revealed a large number of sequences unrelated to cultured organisms, such as those forming the marine stramenopile (MAST)-4 clade. Recent FISH (fluorescent in situ hybridization) data have shown that MAST-4 cells are uncultured heterotrophic flagellates of 2–3 μm in size that have a global distribution in non-polar marine waters. However, FISH is time-consuming and hard to apply to the many samples generated during oceanographic cruises, so we developed a real-time quantitative polymerase chain reaction (Q-PCR) protocol to determine rapidly the abundance of this group using environmental DNA. We designed a primer set targeting the 18S rRNA genes (rDNA) of MAST-4 and optimized and calibrated the Q-PCR protocol using a plasmid with the target sequence as insert. The Q-PCR was then applied to quantify MAST-4 rDNA molecules along three marine transects, longitudinal in the Indian Ocean, latitudinal in the Drake Passage and coastal–offshore in the Mediterranean Sea, and to a temporal study in a Mediterranean Sea coastal station. MAST-4 was detected in all samples processed (averaged abundances between 500 and 1000 rDNA molecules ml−1) except in mesopelagic and Antarctic samples, where it was virtually absent. In general, it was more abundant in the coast than offshore and in the deep chlorophyll maximum than at surface. A comparison of Q-PCR and FISH signals in well-controlled microbial incubations indicated that MAST-4 cells have around 30 copies of the rDNA operon. This Q-PCR assay quickly yielded quantitative data of uncultured MAST-4 cells and confirmed their wide distribution and putative ecological importance. [ABSTRACT FROM AUTHOR]

Members of the class Epsilonproteobacteria are known to be of major importance in biogeochemical processes at oxic-anosic interfaces. In pelagic redoxclines of the central Battic Sea, an uncultured epsilonproteobacterium related to Sulfurimonas denitrificans was proposed to play a key rote in chemolithotrophic denitrification (I. Brettar, M. Labrenz, S. Flavier. J. Bötel, H. Kuosa, R. Christen, and M. G. Höfle, AppI. Environ. Microbiol. 72:1364-1372, 2006). In order to determine the abundance, activity, and vertical distribution of this bacterium in high-resolotion profiles, 16S rRNA cloning and catalyzed reporter deposition and fluorescence in situ hybridization CARD-FISH) and quantitative PCR measurements were carried out. The results showed that 21% of the derived clone sequences, which in the present study were grouped together under the name GD17, had >99% similarity to the uncultured epsilonproteobacterium. A specific gene probe against GD17 (S-*-Sul-0090-a-4-18) was developed and used for enumeration hy CARD-FISH. In different pelagic redoxclines sampled during August 2003, May 2005, and February 2006, GD17 cells were always detected from the lower oxic area to the sulfidic area. Maximal abundance was detected around the chemocline, where sulfide and nitrate concentrations were close to the detection limit. The highest GD17 numbers 12 × 105 cells ml-1), representing up to 15% of the total bacteria, were comparable In those reported for Epsilonproteobacteria in pelagic redoxclines of the Black Sea and the Cariaco Trench (X. Lin, S. G. Wakeham, I. F. Putnam, Y. M. Astor, M. I. Scranton, A. Y. Chistoserdov, and G. T. Taylor, AppI. Environ. Microbiol. 72:2679-2690, 2006). However, in the Baltic Sea redoxclines, Epsilonproteobacteria consisted nearly entirely of cells belonging to the distinct GD17 group. This suggested that GD17 was the best-adapted epsilonproteobacterium within this ecological niche. [ABSTRACT FROM AUTHOR]