The Handbook of Environmental Chemistry
DOI: 10.1007/10683826_8
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Lipid and Phenolic Biomarkers in Marine Ecosystems: Analysis and Applications

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Cited by 155 publications
(154 citation statements)
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“…It met the QA criteria prescribed for consistent external calibrations, low blanks, and precise replicate analysis. Relative standard deviations or coefficients of variation (CV) are ∼10% [6,7] and Iatroscan values for aquatic samples are routinely ∼90% of those obtained by gravimetry and other methods [6][7][8]. Gravimetric values tend to be higher, probably because the Iatroscan will determine only non-volatile lipids and because there is always the possibility of the inclusion of nonlipid material in gravimetric determinations.…”
Section: Lipid Analysesmentioning
confidence: 99%
“…It met the QA criteria prescribed for consistent external calibrations, low blanks, and precise replicate analysis. Relative standard deviations or coefficients of variation (CV) are ∼10% [6,7] and Iatroscan values for aquatic samples are routinely ∼90% of those obtained by gravimetry and other methods [6][7][8]. Gravimetric values tend to be higher, probably because the Iatroscan will determine only non-volatile lipids and because there is always the possibility of the inclusion of nonlipid material in gravimetric determinations.…”
Section: Lipid Analysesmentioning
confidence: 99%
“…Therefore our calculation of the levels of bacterial contribution was based on sum of i15:0, a15:0, i15:0, i17:0, a17:0, 17:0 and 19:0 FAs, the levels were found to be in the range of 19.98% and 33.48% with a mean value of 25.30% which is highest comparison with other contribution at the study area ( Figure 5) In many aquatic environments, there is interest in determining the extent of contribution from terrestrial plants. Even numbered, saturated long-chain FAs >C24 in aquatic sediments are typically associated with an input of OM from terrestrial higher plants (Parish et al, 2000;Camacho-Ibar et al, 2003;Al-mutlaq et al, 2008).The sum of C24-C32 (ΣC24-C32) concentrations of long chain FAs (LCFAs) were calculated ( Conclusions 1-The relatively low TOC content determined for the Shatt Al-Arab estuary and north west Arabian Gulf sediments may be due to its characteristic.…”
Section: Resultsmentioning
confidence: 97%
“…Other FAs reported to be produced by both aerobic and anaerobic bacteria are 15:0 and 17:0 (Parish et al, 2000). The sum of these FAs has been used to estimate the bacterial contribution to reveries and estuarine systems (Harvey and Marko, 1997;Parish et al, 2000).…”
Section: Resultsmentioning
confidence: 99%
“…The fatty acids of the mentioned sea-ice diatoms also consist mainly of C 14:0 , C 16:0 , C 16:1n-7 and C 20:5n-3 , similar to diatoms from temperate environments (Volkman et al, 1989;Viso and Marty, 1993). The ratio of AC 16:1 /C 16:0 as a general diatom indicator was proposed by Claustre et al (1988 -89) and values >1.6 have been used as evidence for diatom-derived fatty acid contributions in diverse aquatic systems, including the cold environment (Budge and Parrish, 1998;Parrish et al, 2000;Budge et al, 2001;Ramos et al, 2003). This is supported by comparisons of C 16:1 /C 16:0 ratios among different taxonomic classes of marine microalgae (Viso and Marty, 1993;Zhukova and Aizdaicher, 1995).…”
Section: Fatty Acidsmentioning
confidence: 88%