2017
DOI: 10.1039/c7ob00357a
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Metabolism of 2,3-dihydroxypropane-1-sulfonate by marine bacteria

Abstract: Both enantiomers of the sulfoquinovose breakdown product 2,3-dihydroxypropane-1-sulfonate, an important sulfur metabolite produced by marine algae, were synthesised in a S-labelled form and used in feeding experiments with marine bacteria. The labelling was efficiently incorporated into the sulfur-containing antibiotic tropodithietic acid and sulfur volatiles by the algal symbiont Phaeobacter inhibens, but not into sulfur volatiles released by marine bacteria associated with crustaceans. The ecological implica… Show more

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Cited by 15 publications
(14 citation statements)
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“…A similar series of γ-lactones spanning from pentan-4-olide ( 14) to dodecan-4olide (20), in addition to 3-methylbutan-4-olide ( 21) and 4-methylhex-5-en-4-olide (22), was detected in strain-specific patterns, with almost all of these compounds present in C. marinus; only C. halophilus did not emit lactones. Furans included furan-2-ylmethanol (23), furfural (24), and 2-acetylfuran (25). Cyclohexanol ( 26) was observed only once in C. marinus, and aromatic compounds included benzyl alcohol (27), benzaldehyde (28) and salicylaldehyde ( 29), acetophenone (30) and o-aminoacetophenone (31), 2-phenylethanol (32), and phenylacetone (33).…”
Section: Headspace Analysismentioning
confidence: 99%
See 1 more Smart Citation
“…A similar series of γ-lactones spanning from pentan-4-olide ( 14) to dodecan-4olide (20), in addition to 3-methylbutan-4-olide ( 21) and 4-methylhex-5-en-4-olide (22), was detected in strain-specific patterns, with almost all of these compounds present in C. marinus; only C. halophilus did not emit lactones. Furans included furan-2-ylmethanol (23), furfural (24), and 2-acetylfuran (25). Cyclohexanol ( 26) was observed only once in C. marinus, and aromatic compounds included benzyl alcohol (27), benzaldehyde (28) and salicylaldehyde ( 29), acetophenone (30) and o-aminoacetophenone (31), 2-phenylethanol (32), and phenylacetone (33).…”
Section: Headspace Analysismentioning
confidence: 99%
“…It has already been pointed out in the 1970s and 1980s that atmospheric DMS is important for the global sulfur cycle [20] and influences the climate on Earth, known as CLAW hypoth-esis according to the authors' initials (Carlson, Lovelock, Andreae, Warren) [21], which underpins the relevance of this algal-bacterial interaction. Isotopic labeling experiments demonstrated that also in laboratory cultures roseobacter group bacteria efficiently degrade DMSP into sulfur volatiles [22,23], but also from other sulfur sources including 2,3-dihydroxypropane-1-sulfonic acid (DHPS, Scheme 1C) labeling was efficiently incorporated into sulfur volatiles [24,25]. Notably, DHPS is produced in large quantities by the marine diatom Thalassiosira pseudonana [26], and diatoms from this genus live in symbiotic relationship with bacteria of the roseobacter group [27].…”
Section: Introductionmentioning
confidence: 99%
“…8 DHPS is the substrate for a range of bacterial biomineralization processes that cleave the carbon−sulfur bond to liberate inorganic sulfite, 3 sulfate, 9 or sulfide 10 or that lead to assorted secondary metabolites. 11 For instance, the Desulfovibrio sp. strain DF1 from anaerobic sewage sludge converts DHPS to hydrogen sulfide, 10 while Roseobacter in marine environments convert DHPS to bisulfite.…”
Section: ■ Introductionmentioning
confidence: 99%
“…It is present in up to millimolar intracellular concentrations in eukaryotic marine phytoplankton, including the highly abundant diatoms (2,8), which are estimated to contribute ∼20% of the total global primary production (9). These phytoplankton use sulfate, present at ∼30 mM levels in seawater to synthesize a variety of organosulfur compounds including DHPS and sulfoquinovose, Secretion or cell lysis makes these compounds available for degradation by marine heterotrophic bacteria, accounting for a large component of the flux of organic carbon in the surface oceans (8,10).…”
mentioning
confidence: 99%