1997
DOI: 10.1016/s0146-6380(97)00063-6
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Potential palaeoenvironmental information of C24 to C36 mid-chain diols, keto-ols and mid-chain hydroxy fatty acids; a critical review

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Cited by 163 publications
(141 citation statements)
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“…The polar fraction was analyzed, after silylation of alcohols to the trimethyl silyl (TMS) derivatives, with gas chromatography-mass spectrometry 150 (GC-MS). Fractional abundances of the long chain alkyl diols were calculated from relevant peak areas of mass chromatograms obtained using selected ion monitoring (SIM) of m/z 299, 313, 327, 341 and 355, which represent characteristic fragment ions of the relevant diols (Versteegh et al, 1997). Differences in the contribution of the selected ions to the total mass spectra (m/z 50-800) of saturated and unsaturated long chain alkyl diols were taken into 155 account as described by Rampen et al (2009).…”
Section: Methodsmentioning
confidence: 99%
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“…The polar fraction was analyzed, after silylation of alcohols to the trimethyl silyl (TMS) derivatives, with gas chromatography-mass spectrometry 150 (GC-MS). Fractional abundances of the long chain alkyl diols were calculated from relevant peak areas of mass chromatograms obtained using selected ion monitoring (SIM) of m/z 299, 313, 327, 341 and 355, which represent characteristic fragment ions of the relevant diols (Versteegh et al, 1997). Differences in the contribution of the selected ions to the total mass spectra (m/z 50-800) of saturated and unsaturated long chain alkyl diols were taken into 155 account as described by Rampen et al (2009).…”
Section: Methodsmentioning
confidence: 99%
“…However, the role of eustigmatophytes as a source of marine long chain alkyl diols remains unclear. Reports of eustigmatophyte algae in marine environments are sparse and the long chain alkyl diol composition of marine eustigmatophytes does not match those of marine sediments (Volkman et al, 1992;Versteegh et al, 1997; Rampen et al, 60 2012). Despite uncertainties concerning their sources, recent work has indicated a strong correlation between sea surface temperatures (SST) and the fractional abundances of C28 1,13-, C30 1,13-and C30 1,15-diols in marine sediments.…”
Section: Introductionmentioning
confidence: 99%
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“…Versteegh et al, 1997;Sinninghe Damsté et al, 2003;Rampen et al, 2007Rampen et al, , 2008Rampen et al, , 2014aRampen et al, , 2014bZhang et al, 2011;Romero-Viana et al, 2012;de Bar et al, 2016;Lattaud et al, 2017a). They are composed of long n-alkyl chains with chain lengths of mainly C 28 to C 32 and contain alcohol groups at C 1 and at a mid-chain position, most notably between positions C 12 to C 15 (Versteegh et al, 1997).…”
Section: Introductionmentioning
confidence: 99%