Open AccessPolar lipid ester‐linked fatty acid composition of Lake Vechten seston: an ecological application of lipid analysis
Author(s) -
Fredrickson H.L.,
Cappenberg T.E.,
Leeuw J.W.
Publication year - 1986
Publication title -
fems microbiology letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.899
H-Index - 151
eISSN - 1574-6968
pISSN - 0378-1097
DOI - 10.1111/j.1574-6968.1986.tb01751.x
Subject(s) - seston , chromatium , water column , fatty acid , polyunsaturated fatty acid , environmental chemistry , biology , chemistry , biochemistry , phytoplankton , ecology , photosynthesis , nutrient
In order to relate the benthic lipid composition to possible sources in the water column, the sestonic communities of a monomictic lake were profiled using their saponifiable polar lipid fatty acids, which were identified by capillary gas chromatography‐mass spectrometry (GC‐MS). The epilimnion, dominated by the dinoflagellate alga Ceratium hirundella , was characterized by C 20:5 and C 22:6 polyunsaturated fatty acids. The photic anoxic metalimnion supported a radically different community, dominated by photosynthetic sulfur‐oxidizing bacteria ( Chromatium and Chloronema spp.) and a Synechococcus ‐like cyanobacterium, and was characterized by high concentrations of C 16 and C 18 monounsaturated fatty acids. The fatty acid compositions of the hypolimnetic seston and the sediment were qualitatively similar to that of the metalimnion. Methyl‐branched acids, commonly found in eubacteria, increased with depth in the water column. The concentrations of several unusual fatty acids found in Desulfovibrio spp. Desulfobacter spp. and Desulfotomaculum spp. were inversely related to sulfate concentration in the metalimnion. After the water column mixed in the winter, steep gradients of respiratory terminal electron acceptors developed in the surface sediment and were reflected in the polar lipid fatty acid compositions. The results show that fatty acids derived from the membranes of epilimnetic phytoplankton were efficiently metabolized in the oxic portion of the water column. The fatty acids synthesized by prokaryotic microorganisms at and below the oxycline dominated the sediment. The polar lipid fatty acid composition of the sediment showed seasonal changes which can be associated with concentrations of terminal electron acceptors of microbial respiration, and thus with physiologically distinct bacterial groups.