HPLC Detection and Antioxidant Capacity Determination of Brown, Red and Green Algal Pigments in Seaweed Extracts

This study was carried out to determine the main pigments in some different selected seaweeds and to reveal their antioxidant potential regarding the ever-increasing demand for utilization of marine pigments in human health and nutrition. The individual amounts of algal pigments were found by reverse phase high-performance liquid chromatography (HPLC) and their total antioxidant capacities (TAC) by two spectrophotometric TAC assays, namely: CUPRAC (CUPric ion Reducing Antioxidant Capacity) and ABTS/TEAC (2,2′-azinobis [3-ethyl benzo thiazoline-6-sulfonate])/(trolox equivalent antioxidant capacity). These two tests gave the same rank order for TAC. The TAC of HPLC-quantified compounds accounted for a relatively much lower percentage of the observed CUPRAC capacities of seaweed extracts, namely ranging from 11 to 68% for brown, from 4 to 41% for red and from 3 to 100% for green species, i.e., some TAC originated from chromatographically unidentified compounds. Fucoxanthin, chlorophyll a, and pheophytin a compounds were major pigments in brown algae. The relative carotenoid contents in red marine algae were generally lower than those of chlorophylls. Overall total quantities were quite low compared with those of brown species. In general, chlorophyll a and chlorophyll b were chiefly present in green algae, but β-carotene, violaxanthin and siphonaxanthin were also detected substantially higher in some species of green algae such as Caulerpa racemosa var. cylindracea and Codium fragile.

PIGMENT CONTENT IN PHYTOPLANKTON, EPIPHYTON AND BOTTOM SEDIMENTS OF LAKE NERO

This article presents new data of spectrophotometric determination of pigment concentrations in phytoplankton, epiphyton and bottom sediments of the shallow highly productive Lake Nero based on survey materials in summer 2017. The average concentrations of chlorophyll a were 73.5±6.1 μg/L in phytoplankton and 40.7±21.4 mg/m2 of substrate in epiphyton, the sum of chlorophyll a with pheopigments in bottom sediments was 313±20.6 μg/g dry sediment. These values are comparable to those in the previous observation years. The parameters of pigment degradation were characterized by low values in the functioning communities of phytoplankton and epiphyton and reached the highest values in bottom sediments. The spatial distribution of algal pigments depended on the presence of macrophyte thickets. Overgrowing of the territory with macrophytes affected the content of pigments in phytoplankton negatively but the pigment accumulation in bottom sediments positively. The trophic state of the lake remains hypertrophic, as in previous years of observation.

Algal pigments distribution and phytoplankton group assemblages in the coastal transitional environment – Boka Kotorska Bay (Southeastern Adriatic Sea)

Prisutnost zajednica fitoplanktona i rasprostranjenost pigmenata utvrđivani su u tranzicijskim vodama Bokokotorskog zaljeva. Uzorci su prikupljeni četiri puta na tri lokaliteta u unutrašnjosti Zaljeva u periodu između travnja 2008. i ožujka 2009. godine. Mikroskopskom analizom utvrđeno je da fitoplankton čine morske dijatomeje, dinoflagelati, kriptofiti, klorofiti i kokolitoforidi. Pored fukoksantina kao dominantnog biomarkerskog pigmenta, bili su zastupljeni i aloksantin, 19′-heksanoiloksifukoksantin, peridinin i klorofil b‏. Fukoksantin i aloksantin su pokazali značajnu korelaciju sa klorofilom a kao indikatorom biomase fitoplanktona tijekom čitavog perioda ispitivanja. U studenom 2008. godine, dijatomeje su nadjačale kokolitoforide, koji su vjerovatno efikasno apsorbirali nutrijente tijekom perioda u kojem je njihova dostupnost bila smanjena. Kao rezultat smanjenog unosa nutrijenata, u ljetnom periodu, zajednicu fitoplanktona u Bokokotorskom zaljevu sačinjavali su uglavnom morski dinoflagelati, kriptofiti i klorofiti.

Algal pigments in Hornsund (Svalbard) sediments as biomarkers of Arctic productivity and environmental conditions

Pigments (chloropigments-a and carotenoids) in sediments and macroalgae samples, collected in Hornsund, in July 2015 and July 2016, were analysed (HPLC) in this work. In spite of the aerobic conditions and the periodic intensive solar irradiation in the Arctic environment, neither of which favour pigment preservation in water column and surface sediments, our results indicate that these compounds can provide information about phytoplankton composition, primary production and environmental conditions in this region. The sum of chloropigments-a, a marker of primary production, in the Hornsund sediments varied from 0.40 to 14.97 nmol/g d.w., while the sum of carotenoids ranged from 0.58 to 8.08 nmol/g d.w. Pheophorbides-a and pyropheophorbides-a made up the highest percentage in the sum of chloropigments-a in these sediments, supplying evidence for intensive zooplankton and/or zoobenthos grazing. Among the carotenoids, fucoxanthin and its derivatives (19’-hexanoyloxyfucoxanthin and 19’-hexanoyloxy-4-ketofucoxanthin) contributed the highest percentage, which points to the occurrence mainly of diatoms and/or haptophytes in the water. The pigment markers show that the input of macroalgae to the total biomass could be considerable only in the intertidal zone.