1987
DOI: 10.3354/meps040275
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Microphytobenthos from two subtidal sediments from North Brittany. II. Variations of pigment compositions and concentrations determinded by HPLC and conventional techniques

Abstract: Pigment composition and concentration of 2 temperate subtidal sediments, a mud and a sand from North Brittany, were studied using HPLC and conventional fluorometric methods. Pigment diversity, found using HPLC, was considerable, particularly in the mud (around 15 identified pigments). Pigment composition in the sand was dominated by Bacillariophyceae pigments, whereas in the mud pigments characteristic of Chlorophyceae were also found. Freeze-drying significantly reduces pigment concentrations.

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Cited by 54 publications
(34 citation statements)
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“…The complete absence of chl b in our samples excludes the possibility that Chlorophyceae and/or Euglenophyceae contributed to the microphytobenthic community of this intertidal mudflat. This is an important characteristic since chl b has been frequently detected in coastal sediments (Riaux-Gobin et al 1987, Klein & RiauxGobin 1991, but our observations corroborate those of Barlow et al (1990), who studied sediments of salt marshes in the same area (46" 10' N, 1" 15' W). Lutein, which is associated with chl b (Jeffrey 1974), was not detected in our samples whereas 1 unidentified peak might be zeaxanthin, which has been proposed as a taxonomic marker of Cyanophyceae (Guillard et al 1985, Gieskes et al 1988).…”
Section: Qualitative Analysissupporting
confidence: 82%
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“…The complete absence of chl b in our samples excludes the possibility that Chlorophyceae and/or Euglenophyceae contributed to the microphytobenthic community of this intertidal mudflat. This is an important characteristic since chl b has been frequently detected in coastal sediments (Riaux-Gobin et al 1987, Klein & RiauxGobin 1991, but our observations corroborate those of Barlow et al (1990), who studied sediments of salt marshes in the same area (46" 10' N, 1" 15' W). Lutein, which is associated with chl b (Jeffrey 1974), was not detected in our samples whereas 1 unidentified peak might be zeaxanthin, which has been proposed as a taxonomic marker of Cyanophyceae (Guillard et al 1985, Gieskes et al 1988).…”
Section: Qualitative Analysissupporting
confidence: 82%
“…There were nevertheless large amounts of degraded p~gments which probably derived from the breakdown of autochthonous material. We have indeed detected many forms of phaeopigment a, which is consistent with findings of other studies concerning sediment (Brown et al 1981, Riaux-Gobin et al 1987, Klein et Riaux-Gobin 1991, Yacobi et al 1991. The 4 phaeophorbides, which represented about 7 5 % of total phaeopigments, are markers for macrobenthic deposit-feeding processes (Bianchi et al 1988(Bianchi et al , 1993 and more generally for metazoan grazing activity (Brown et al 1981, Welschmeyer & Lorenzen 1985, Abele-Oeschger et al 1992 Based on their order of elution and retention times, the 2 major phaeophorbides a-like:, and a-like, (accounting for about 50 % of total phaeophorbides) correspond very likely to the phaeophorbides a-like in Hawkins et al (1986) study and to phaeophorbides a, and a3 reported by Plante-Cuny et al (1993).…”
Section: Qualitative Analysissupporting
confidence: 81%
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“…It is known (Daemen 1985) that for Dutch estuarine sediments the method of Lorenzen (1967) overestimates chl a content by ca 30% compared with results of HPLC. However, in the late 1970s the HPLC technique (Riaux-Gobin et al 1987) was not available to separate chl a from other pigments in estuarine areas. This was the main reason for application of a conversion procedure to obtain the best possible estimate of the chl a in vital microphytobenthos.…”
Section: Applied Methods and Proceduresmentioning
confidence: 99%