Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5161867 | Organic Geochemistry | 2010 | 6 Pages |
Abstract
Bacterial communities often develop with distinct metabolisms in hot springs using various chemical substrates. The carbon and hydrogen isotopic compositions of characteristic lipid biomarkers such as C16:1 and C20:1 fatty acids (FAs) have been determined in a bacterial mat at the Naruko hot spring, Japan. The C20:1 FA is extremely enriched in 13C (â0.5â°) and derives from hydrogen-oxidizing bacteria which fix carbon via the reversed tricarboxylic acid cycle. On the other hand, the C16:1 FA has a δ13C value of â36.8â°, consistent with an origin in sulfur-oxidizing bacteria utilizing the Calvin cycle for carbon fixation. The C20:1 FA is more depleted in D (â469â°) by ca. 300â° than the C16:1 FA (â173â°), suggesting a D-depleted hydrogen pool (NADH or NADPH) for lipid synthesis by the hydrogen-oxidizing bacteria. The distinct δ13C-δD distribution of lipid biomarkers is useful for clarifying the metabolic pathways between different organisms in a bacterial ecosystem in hot springs.
Related Topics
Physical Sciences and Engineering
Chemistry
Organic Chemistry
Authors
Hiroshi Naraoka, Tomoko Uehara, Satoshi Hanada, Takeshi Kakegawa,