A new method for the rapid analysis of 1H-Pyrrole-2,5-diones (maleimides) in environmental samples by two-dimensional gas chromatography time-of-flight mass spectrometry
Journal of chromatography. A, Jan 26, 2016
Maleimides (1H-Pyrrole-2,5-diones) are monopyrrolic pigment derivatives with specific alkyl side ... more Maleimides (1H-Pyrrole-2,5-diones) are monopyrrolic pigment derivatives with specific alkyl side chains that can be directly linked to their tetrapyrrole precursors, most notably chlorophylls and bacteriochlorophylls. These compounds can be used as palaeoenvironmental indicators such as algal productivity and redox conditions in ancient and modern aquatic systems. Here, we present a new method using two-dimensional gas chromatography time-of-flight mass spectrometry (GC×GC-ToF-MS), which enables the rapid analysis of maleimides in complex mixtures and different matrices (e.g. sediments and soils), therefore largely simplifying the previous intricate maleimide purification protocol. This method also reduces the potential for bias associated with partial losses due to low recovery and the high volatility of maleimides. The maleimide distributions and concentrations obtained by GC×GC-ToF-MS were reproducible and in agreement with the previously used purification procedure followed by a...
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Papers by Sabine Lengger
microorganisms in aquatic environments, however, their
metabolism in marine sediments is still debated. Labeling
studies in marine sediments have previously been undertaken,
but focused on complex organic carbon substrates
which Thaumarchaeota have not yet been shown to take up.
In this study, we investigated the activity of Thaumarchaeota
in sediments by supplying different 13C-labeled substrates
which have previously been shown to be incorporated into archaeal
cells in water incubations and/or enrichment cultures.
We determined the incorporation of 13C-label from bicarbonate,
pyruvate, glucose and amino acids into thaumarchaeal
intact polar lipid-glycerol dibiphytanyl glycerol tetraethers
(IPL-GDGTs) during 4–6 day incubations of marine sediment
cores from three sites on the Iceland shelf. Thaumarchaeal
intact polar lipids, in particular crenarchaeol, were detected
at all stations and concentrations remained constant or
decreased slightly upon incubation. No 13C incorporation in
any IPL-GDGT was observed at stations 2 (clay-rich sediment)
and 3 (organic-rich sediment). In bacterial/eukaryotic
IPL-derived fatty acids at station 3, contrastingly, a large
uptake of 13C label (up to + 80‰ ) was found. 13C was
also respired during the experiment as shown by a substantial
increase in the 13C content of the dissolved inorganic
carbon. In IPL-GDGTs recovered from the sandy sediments
at station 1, however, some enrichment in 13C (1–4‰ )
was detected after incubation with bicarbonate and pyruvate.
The low incorporation rates suggest a low activity of Thaumarchaeota
in marine sediments and/or a low turnover rate
of thaumarchaeal IPL-GDGTs due to their low degradation
rates. Cell numbers and activity of sedimentary Thaumarchaeota
based on IPL-GDGT measurements may thus have
previously been overestimated.
CONCLUSIONS: Structures of O4 species in OSPW have been identified. This confirms pathways of microbial biodegradation, which were only postulated previously, and may be a further indication that remediation of OSPW toxicity can occur by natural microbial action. The presence and abundance of these diacids might therefore be useful as a measure of biodegradation and weathering.