Photosynthetic pigments in 37 species (65 strains) of Haptophyta: implications for oceanography and chemotaxonomy

By M. Zapata, S. W. Jeffrey, S. Wright, F. Rodríguez, J. Garrido, L. Clementson. 2004

270 citations recorded by the source corpus.

Subfields: Ecology, Molecular Biology, Oceanography

View Paper: https://www.semanticscholar.org/paper/8f8e9afaf1b5d9c7bc923c31a833b1899ab94836

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In Ecology

1. J. Lavaud
2. Koen Sabbe
3. A. Alderkamp
4. J. Stefels
5. André Cattrijsse
6. N. Dijkman
7. Suzanne Roy
8. Ian Probert

In Molecular Biology

1. Geir Johnsen
2. R. J. Visser
3. A. Alderkamp
4. J. Stefels
5. J. Lavaud
6. S. Fraga
7. C. de Vargas
8. Suzanne Roy

In Oceanography

1. Geir Johnsen
2. A. Alderkamp
3. Jens C. Nejstgaard
4. J. Lavaud
5. Ian Probert
6. N. Dijkman
7. A. Penna
8. S. Fraga

Citations in the corpus

• Microzooplankton grazing and phytoplankton growth in marine mesocosms with increased CO 2 levels (2008, background): “A 19’-hexanoyloxyfucoxanthin-like peak, which was regarded typical for prymnesiophytes or even specific for coccolithophorids (Zapata et al., 2004), was found in the samples, corresponding to 4-keto-19’-hexanoyloxyfucoxanthin (4-keto-hex) recently reported by Airs and Llewellyn (2006).”
• CHARACTERIZATION OF NW MEDITERRANEAN KARLODINIUM SPP. (DINOPHYCEAE) STRAINS USING MORPHOLOGICAL, MOLECULAR, CHEMICAL, AND PHYSIOLOGICAL METHODOLOGIES 1 (2006, result): “Simultaneous synthesis of the two chl c2-MGDG pigments by K. armiger tracks the chloroplast pigments’ composition of this species to the pigment Type 7 (Chrysochromulina-type) of Haptophyta, similar to the results obtained for Karenia brevis (Zapata et al. 2004).”
• Molluscan assemblages of seagrass-covered and bare intertidal flats on the Banc d'Arguin, Mauritania, in relation to characteristics of sediment and organic matter (2008, background): “Fucoxanthin is generally used as a marker pigment for diatoms but can also be present in other taxonomic groups (Chrysophyceae, Raphidophyceae and Prymnesio-phycea) (Jeffrey and Vesk, 1997; Zapata et al., 2004).”
• On the description of Tisochrysis lutea gen. nov. sp. nov. and Isochrysis nuda sp. nov. in the Isochrysidales, and the transfer of Dicrateria to the Prymnesiales (Haptophyta) (2013, background): “…published information that shows that D. inornata and Imantonia rotunda are very similar in ultrastructure (Green and Pienaar 1977; Edvardsen et al. 2000) and pigment signatures (Jeffrey and Wright 1994; Zapata et al. 2004), and the fact that neither produces alkenones (Marlowe et al 1984).”
• Spatial variation in phytoplankton dynamics in the Belgian coastal zone of the North Sea studied by microscopy, HPLC-CHEMTAX and underway fluorescence recordings (2006, background): “19′–hexanoyloxyfucoxanthin concentrations in Phaeocystis strains, however, tend to be highly variable ( Zapata et al., 2004 ).”
• Emergence of brown tides caused by Aureococcus anophagefferens Hargraves et Sieburth in China (2012, background): “Based on the pigment composition and content, the causative species could be tentatively identified as a pelagophyte, haptophyte or silicoflagellate (Edvardsen et al., 2007; Zapata et al., 2004).”
• Pigment-based chloroplast types in dinoflagellates (2012, methodology): “Comparing molar pigment ratios of haptophytes from pigmentary groups 6, 7 and 8 (sensu Zapata et al. 2004) with Hex-fuco-containing dinoflagellates, the values chl c3:chl a, chl c2:chl a, chl c3:chl c2 and total chl c: total fuco are consistently higher in haptophytes relative to dinoflagellates of…”
• Photoacclimation in phytoplankton: implications for biomass estimates, pigment functionality and chemotaxonomy (2006, background): “1e) posessed Chl c2-MGDG [14:0/18:4] (Garrido et al. 2000; Zapata et al. 2004).”
• An optimized method for automated analysis of algal pigments by HPLC (2006, background): “Furthermore, an increasing amount of unknown analogue products of chlorophyll c's and fucoxanthins are being described (see Zapata et al., 2004 and references therein) and most of them elute at very similar retention times.”
• Can photoinhibition control phytoplankton abundance in deeply mixed water columns of the Southern Ocean? (2010, background): “The initial database included a Southern Ocean data set containing prasinophytes, cryptophytes, two types of diatoms (one with a pigment ratio specific for Pseudonitzschia and one for Antarctic diatoms without Chl c3), chlorophytes, and two types of haptophytes (type 6 with a pigment ratio specific ”
• Phospholipid-derived fatty acids as chemotaxonomic markers for phytoplankton: application for inferring phytoplankton composition (2006, background): “19’-hexanoyloxyfucoxanthin is a well-known biomarker pigment for Phaeocystis sp. (Zapata et al. 2004).”
• Composition and significance of picophytoplankton in Antarctic waters (2009, methodology): “Most Fuco was probably contributed by the diatoms seen in EM samples, but could also have other sources such as type 1 haptophytes (sensu Zapata et al. 2004).”
• Pigments and photoacclimation processes (2011, background): “From the ratios between photosynthetic pigments, distinct pigment-groups have been defined in the Prasinophyceae (e.g., Hooks et al., 1988; Egeland et al., 1995; Zingone et al., 2002) or in the haptophyta (e.g., Stolte et al., 2000; Zapata et al., 2004).”