Supercritical carbon dioxide extraction of bioactive compounds from microalgae and volatile oils from aromatic plants

A discussion of the most interesting results obtained in our laboratories, during the supercritical CO(2) extraction of bioactive compounds from microalgae and volatile oils from aromatic plants, was carried out. Concerning the microalgae, the studies on Botryococcus braunii and Chlorella vulgaris were selected. Hydrocarbons from the first microalgae, which are mainly linear alkadienes (C(23)-C(31)) with an odd number of carbon atoms, were selectively extracted at 313 K increasing the pressure up to 30.0 MPa. These hydrocarbons are easily extracted at this pressure, since they are located outside the cellular walls. The extraction of carotenoids, mainly canthaxanthin and astaxanthin, from C. vulgaris is more difficult. The extraction yield of these components at 313 K and 35.0 MPa increased with the degree of crushing of the microalga, since they are not extracellular. On the other hand, for the extraction of volatile oils from aromatic plants, studies on Mentha pulegium and Satureja montana L were chosen. For the first aromatic plant, the composition of the volatile and essential oils was similar, the main components being the pulegone and menthone. However, this volatile oil contained small amounts of waxes, which content decreased with decreasing particle size of the plant matrix. For S. montana L it was also observed that both oils have a similar composition, the main components being carvacrol and thymol. The main difference is the relative amount of thymoquinone, which content can be 15 times higher in volatile oil. This oxygenated monoterpene has important biological activities. Moreover, experimental studies on anticholinesterase activity of supercritical extracts of S. montana were also carried out. The supercritical nonvolatile fraction, which presented the highest content of the protocatechuic, vanilic, chlorogenic and (+)-catechin acids, is the most promising inhibitor of the enzyme butyrylcholinesterase. In contrast, the Soxhlet acetone extract did not affect the activity of this enzyme at the concentrations tested. (C) 2011 Elsevier B.V. All rights reserved.

Induction of liver monooxygenases by annatto and bixin in female rats

Annatto or urucum is an orange-yellow dye obtained from Bixa orellana seeds. It has been used as a natural dye in a variety of food products, drugs and cosmetics, and also in Brazilian cuisine as a condiment ('colorau'). Bixin, a carotenoid devoid of provitamin A activity, is the main pigment found in annatto. Some carotenoids (canthaxanthin, astaxanthin and ß-Apo-8'-carotenal) are known to be potent inducers of CYP1A1, a property not shared by others (ß-carotene, lycopene and lutein). Little is known, however, about the CYP1A1-inducing properties of bixin and annatto. The present study was performed to determine the effects of an annatto extract (28% bixin) and bixin (95% pure) on rat liver monooxygenases. Adult female Wistar rats were treated by gavage with daily doses of annatto (250 mg/kg body weight, which contains approximately 70 mg bixin/kg body weight), bixin (250 mg/kg body weight) or the vehicle only (corn oil, 3.75 g/kg body weight) for 5 consecutive days, or were not treated (untreated control). The activities of aniline-4-hydroxylase (A4H), ethoxycoumarin-O-deethylase (ECOD), ethoxy- (EROD), methoxy- (MROD), pentoxy- (PROD) and benzyloxy- (BROD) resorufin-O-dealkylases were measured in liver microsomes. Annatto (250 mg/kg containing 70 mg bixin/kg) induced EROD (3.8x), MROD (4.2x), BROD (3.3x) and PROD (2.4x). Bixin (250 mg/kg) was a weaker inducer of EROD (2.7x), MROD (2.3x) and BROD (1.9x) and did not alter PROD, A4H or ECOD activities. These results suggest that constituents of the extract other than bixin play an important role in the induction of CYP1A and CYP2B observed with annatto food colorings.

Biomarker pigment signatures in Cochin back water system e A tropical estuary south west coast of India

Sedimentary biomarker pigments around Cochin estuary situated in the southwest coast of India were determined by HPLC. Fucoxanthin, an indicator of diatom was observed to be the most abundant carotenoid pigment in the estuary. Dinoflagellate derived carotenoid pigment peridinin was confined in the southern part of estuary and zeaxanthin pigment indicative of cyanobacteria were more found in sites influenced by anthropogenic activities. One compound having close similarity to fucoxanthin was also detected. Alloxanthin (cryptophyceae), chl b (green algae), canthaxanthin, neoxanthin, lutein and peridinin isomer were also detected by spectra and corresponding algal class were identified. The highest concentration of chl a (11.01 mg g 1) found near to the anthropogenic affected area while the lowest chl a (0.65 mg g 1) was recorded in industrial area. Degradation products of chl a, such as pheophorbide and pheophytin were observed and principal mode of mechanism of degradation were derived. Higher pheopigments content than chl a, reflects a density trapping of dead cells and early degradation of phytopigments from grazing activities

Evaluation of Rhodocyclus gelatinosus biomass for broiler pigmentation

We evaluated the influence of dietry inclusion of corn gluten meal, apocartenoic acid ethyl ester (APO-EE), canthaxanthin, and Rhodocylus gelatinosus R-1 biomass on broiler carcass color. These oxycarotenoid sources were used as pigment supplements to a basal ration containing yellow corn as the sole source of xnathophylls. Objective color values of L (lightness),C (chroma), and h (hue) were measured on skin and meat surfaces of broiler carcasses. on both surfaces, R. gelatinosus R-1 biomass oxycarotenoids enhanced the chroma values (color saturation), as compared to yellow corn xanthophylls, and tended to provide yellowness to broiler carcasses, whereas the APO-EE and canthaxanthin tended to provide redness. At the concentrations studied, R. gelatinosus R-1 biomass oxycarotenoids were less effective than APO-EE and canthaxanthin in enhancing color saturation. Lightness, chroma, and blue values did not differ significantly between males and females. However, skin showed significantly higher color saturation than meat in breast and thigh portions of the carcass.

Quality of egg yolks after oxycarotenoids supplementation in hens' diets

Oxycarotenoids concentration in layer hens’ feed may be increased whenever the consumer market demands for more pigmented egg yolks. Oxycarotenoids present in Rubrivivax gelatinosus biomass grown in industrial wastewater have already proved their ability on enhancing yolk color. Moreover, there is a current interest on the antioxidant properties that some carotenoids may provide to food and health. So, in this experiment, we investigated the effects of oxycarotenoids supplementation in hens´ diets on yolk composition and stability to rancidity. Hy line hens aging 19 weeks were individually housed in wire cages equipped with feeders and drinkers. After 15 days receiving a corn basal diet nutritionally balanced, they were assigned to four different treatments, with six replicates, that lasted for 28 days: T1 – basal diet (control), T2 – basal diet + 1.5 mg/kg canthaxanthin, T3 – basal diet + 4.5 g/kg freeze dried R. gelatinosus biomass and T4 - basal diet + 4.5 g/kg spray dried R. gelatinosus biomass. Eggs laid on the last 5 days of rearing were collected; the yolks were separated, analyzed for pH and then freeze dried for the further analyses. Proximate composition was determined after drying and the rancidity (TBRAS method) was investigated at 0, 30 and 60 days of storage at room temperature/dark conditions. Yolks that received the oxycarotenoids had the lowest moisture content and the highest protein contents (P < 0.05). Lipids and pH were the same for all treatments (P > 0.05) and ashes only were higher for T2 (P < 0.05). All treatments that received oxycarotenoids had lower TBARS than control group and, among them, oxycarotenoids from spray dried R. gelatinosus biomass were the most effective to prevent rancidity (P < 0.05). So, we concluded that the use of R. gelatinosus biomass in hens feed brings positive effects to the yolk quality, since protein content is increased and conservation is increased due to decreased water content and lipid oxidation.

Yolks color definition by supplementing yellow and red xanthophylls to hen's diets

Egg yolk color may be controlled both by the concentration and the type of xanthophylls added to diets, with the aim of meeting consumers demand. The objectives of this work were to study how yellow and red xanthophylls present in laying hens` diets influence yolks colors and find the concentrations of these ingredients that meet the regional consumer desire. A factorial design 5 x 3 with 5 concentrations of yellow xanthophylls (lutein + zeaxantin 40%; 1.0, 1.25, 1.5, 1.75 and 2.0 mg/hen/d) and 3 concentrations of red xanthophylls (canthaxantin 10%; 0, 0.35, 0.7 mg/hen/d) was used. After a 30 d period receiving corn basal diets and water ad libitum, 60 White Dekalbe hens were distributed to receive the 15 dietary treatments in 4 replicates. Diets were provided daily at 110 g, during 21 d under 16 h light/8 h dark. Yolks colors were evaluated daily using the CIE L, a, b color space and the Roche color index. After the color stabilization, data were analyzed by ANOVA, regression analysis and Response Surface Methodology (MRS). Global acceptance for the Roche colors was evaluated with a 5 points hedonic scale and data were analyzed by Friedman and Dunn tests. Significance was established at 95% (P < 0.05). Regression analysis showed that the red xanthophylls content was the most important factor that defined L, a and b values for yolk color (P < 0.0001; square function), although its effect was significantly affected by the yellow xanthophylls contents (P = 0.0277; P < 0.0001; P = 0.0002 for L, a, b, respectively), providing evidence for a synergistic effect and not for a saturation effect. MRS showed that the highest redness of yolks was reached with 1.5 mg/hen/d of yellow and 0.5 mg/hen/d of red xanthophylls. So, higher supplementations aiming at increasing yolk color would bring an unnecessary cost to the ration. The most accepted yolk color scored 9, which corresponded to mean color attributes L = 65; a = 16; and b = 64. MRS showed that these values could be reached with combinations of yellow:red xanthophylls like 1.0:0.15 or 1.5:0.1 mg/ hen/d or simply with the yellow xanthophylls at 2.0 mg/hen/d. So, it was concluded that both yellow and red xanthophylls are important to define yolks color; that high amounts of xanthophylls are unnecessary to bring changes to color; and that Brazilian consumer requires yolks color attainable with few amounts of red xanthophylls or only with the yellow ones.

Nachweis und Charakterisierung der Ketocarotinoidakkumulation in Zygosporen des Modellorganismus Chlamydomonas reinhardtii

Ketocarotinoide sind in den Dauerstadien vieler Grünalgen anzutreffen und aufgrund ihres hohen antioxidativen Potentials vermutlich von großer Bedeutung für deren Überleben unter ungünstigen Umweltbedingungen. Daneben ist die Aufnahme von Ketocarotinoiden im Zuge der Nahrungskette für verschiedene Tiere lebensnotwendig. Trotz zahlreicher Untersuchungen des Biosynthesewegs der Ketocarotinoide, vorwiegend in der Grünalge Haematococcus pluvialis, sind viele grundlegende Aspekte der Synthese nicht verstanden. Dazu zählt neben dem genauen Reaktionsmechanismus des ketolierenden Enzyms ß-Carotin-Ketolase (BKT) vor allem der noch nicht aufgeklärte Zusammenhang zwischen Lipidsynthese und Ketocarotinoidakkumulation. Nach der Entdeckung eines zur BKT aus H. pluvialis homologen Gens in einer EST-Datenbank des Modellorganismus Chlamydomonas reinhardtii wurden im Rahmen der vorliegenden Forschungsarbeit die als orange-rot beschrieben Zygosporen von C. reinhardtii als mögliches ketocarotinoidhaltiges Zellstadium untersucht. Dabei wurden für C. reinhardtii erstmals Ketocarotinoide in Konzentrationen bis zu einem Femtomol pro Zelle nachgewiesen und mittels HPLC-Analytik, chemischer Derivatisierung und Massenspektrometrie zweifelsfrei identifiziert. Es wurden, in aufsteigender Quantität, drei Ketocarotinoide detektiert: Canthaxanthin, Astaxanthin und 4-Ketolutein. Letzteres wurde bisher selten in anderen ketocarotinoidakkumulierenden Organismen beschrieben und stellt, im Gegensatz zu den vom ß-Carotin abgeleiteten Pigmenten Astaxanthin und Canthaxanthin, ein Pigment des α-Carotin-Zweiges dar. Astaxanthin und 4-Ketolutein wurden vor allem in Form von Pigment-Fettsäureestern nachgewiesen. Mit Hilfe von Paarungsansätzen mit der lor1-Mutante, die keine α-Carotinoide synthetisieren kann, und Vergleichen mit Ketocarotinoiden aus H. pluvialis konnte gezeigt werden, dass 4 Ketolutein nur als Monoacylester in der Alge vorliegt, während Astaxanthin sowohl als Monoacyl- wie auch als Diacylester anzutreffen ist. Ketocarotinoide wurden innerhalb der ersten 14 Tage der Zygotenreife gebildet. Transmissionselektronenmikroskopische Aufnahmen der Zygoten dokumentierten, dass damit ein starker Umbau der Zelle einherging, der sich vor allem in der Reduktion des Chloroplasten und der Bildung von Lipidtröpfchen darstellte. Letztere nahmen bei reifen Zygosporen den größten Teil des Zelllumens ein und wurden mittels dünnschichtchromatografischer Analysen als Neutralfette identifiziert. Der sinkende Zellgehalt an Carotinoiden im Zuge der Zygosporenreifung und Inhibitorexperimente an reifenden Zygoten mittels Norflurazon zeigten, dass für die Ketocarotinoidakkumulation keine Neusynthese von Carotinoiden nötig ist und lassen die Hypothese zu, dass C. reinhardtii die im Zuge der Chloroplastenreduktion freigesetzten Photosynthese-Carotinoide als Substrate für die Ketocarotinoidsynthese verwendet. Physiologische Bedeutung könnte den Ketocarotinoiden vor allem beim Schutz der Speicherlipide vor Peroxidation durch reaktive Sauerstoffspezies zukommen. Diese Reservestoffe stellen die Energieversorgung während des Auskeimens der Zellen sicher. Durch den im Rahmen der vorliegenden Forschungsarbeit dokumentierten Nachweis der Ketocarotinoidakkumulation in C. reinhardtii können die Ketocarotinoidsynthese und vor allem der Zusammenhang von Lipid- und Ketocarotinoidakkumulation zukünftig mit Hilfe der für diesen Modellorganismus vorliegenden umfangreichen molekulargenetischen Methoden detailliert untersucht werden.

Identifizierung und Quantifizierung der Ketocarotinoide in Dauerstadien von Grünalgen und Ketocarotinoidbiosynthese im Modellorganismus Chlamydomonas reinhardtii

Grünalgen bilden zur Überdauerung schlechter Umweltbedingungen Ruhestadien, die sich durch Ausbildung einer festen Zellwand, die Reduktion des Plastiden und die starke Akkumulation von Speicherfetten und Ketocarotinoiden im Zytosol auszeichnen. Obwohl Ketocarotinoide in Grünalgen seit über vierzig Jahren beforscht werden, gab es hierzu noch wenige molekularbiologische Untersuchungen. Im Vorfeld meiner Promotion wurde durch unsere Arbeitsgruppe entdeckt, dass auch der molekular gut zugängliche Modellorganismus Chlamydomonas reinhardtii im Zygotenstadium große Mengen an Ketocarotinoiden bildet. Neben dem zu erwartenden Ketocarotinoid Astaxanthin fanden wir große Mengen des bisher nur in einer Grünalge beschriebenen 4-Ketoluteins. Vorversuche ließen die Vermutung aufkommen, dass dieses Pigment bei der Untersuchung der Pigmentausstattung in Dauerstadien von vielen Grünalgen bisher übersehen wurde. rnIn der vorliegenden Arbeit wurde daher zunächst die Pigmentzusammensetzung von Dauerstadien der bereits gut untersuchten Grünalgen Muriella zofingiensis und Scenedesmus rubescens durch Vergleich mit dem Ketocarotinoidmuster aus Dauerstadien von C. reinhardtii und Fritschiella tuberosa reevaluiert und dabei erstmals das Vorkommen signifikanter Mengen an 4-Ketolutein nachgewiesen. Außerdem zeigte sich, dass die als bisheriger Modellorganismus der Ketocarotinoidbiosynthese in Grünalgen sehr gut untersuchte Alge Haematococcus pluvialis eher eine Ausnahme darstellt, da ihre Dauerstadien als einzige der hier untersuchten Algen nur minimale Mengen von 4 Ketolutein aufwiesen. Diese Beobachtungen machen es sehr wahrscheinlich, dass die Fähigkeit zur Bildung von 4-Ketolutein unter den Grünalgen wesentlich weiter verbreitet ist als bisher angenommen. Das sekundäre Carotinoid 4-Ketolutein kam in den Dauerstadien der Grünalgen neben seiner freien Form ausschließlich als Monoacylester vor, im Gegensatz zu Astaxanthin, das als mono- und diacylierte Form auftrat. rnÜber die Analyse der Pigmentausstattung hinaus konnten die entscheidenden Schritte des Synthesewegs der Ketocarotinoide in C. reinhardtii durch funktionelle Charakterisierung der beteiligten Enzyme in Bakterien aufgeklärt werden. Als Basis für die Charakterisierungen wurde ein umfangreiches Portfolio von carotinogenen E. coli-Bakterien etabliert, darunter α Carotin und Lutein produzierende Stämme, die bisher nicht zur Verfügung standen. Das wurde durch die Klonierung der Lycopinzyklase (OluLCY) aus der Grünalge Ostreococcus lucimarinus möglich, die eine Sonderolle unter den Zyklasen einnimmt, da sie die Lycopin-β-Zyklase und Lycopin-ε-Zyklase in einem Fusionsenzym vereint. Vorteile dieses Fusionsenzyms sind die Expressionskontrolle durch nur einen Promotor und die weitgehend konstante Stöchiometrie seiner Produkte α-Carotin und β-Carotin, was die OluLCY für die biotechnologische Anwendung prädestiniert.rnDie funktionelle Charakterisierung der Carotinoidbiosyntheseenzyme aus C. reinhardtii umfasste das Schlüsselenzym der Ketocarotinoidbiosynthese, die β-Carotin-Ketolase (BKT), sowie die Carotinoid-Hydroxylasen CHYB, CYP97A5 und CYP97C3. Dabei wurde für das BKT-Enzym aus C. reinhardtii nachgewiesen, dass es nicht nur die Ketolierung von β Carotin zu Canthaxanthin und von Zeaxanthin zu Astaxanthin, sondern auch die Bildung der von α-Carotin abgeleiteten Ketocarotinoide wie 4-Keto-α-Carotin und 4 Ketolutein katalysieren kann.rn

Pigment, carbohydrate and protein content of microbial mats from northern Victoria Land lake sediments

The composition of algal pigments and extracellular polymeric substances (EPS) was determined in microbial mats from two lakes in Victoria Land (Continental Antarctica) with different lithology and environmental features. The aim was to expand knowledge of benthic autotrophic communities in Antarctic lacustrine ecosystems, providing reference data for future assessment of possible changes in environmental conditions and freshwater communities. The results of chemical analyses were supported by microscopy observations. Pigment profiles showed that filamentous cyanobacteria are dominant in both lakes. Samples from the water body at Edmonson Point had greater biodiversity, fewer pigments and lower EPS ratios than those from the lake at Kar Plateau. Differences in mat composition and in pigment and EPS profile between the two lakes are discussed in terms of local environmental conditions such as lithology, ice-cover and UV radiation. The present study suggests that a chemical approach could be useful in the study of benthic communities in Antarctic lakes and their variations in space and time.

Water chemistry, and pigments and geochemistry of sediments from northern Victoria Land lakes

Total concentrations of algal pigments, organic C, C, N, P and S were determined in surface sediments from the littoral zone of 21 lakes in ice-free areas of northern Victoria Land (Antarctica) with different climatic and environmental conditions. Concentrations of major ions and nutrients were also determined in water samples from the same lakes. The latter samples had extremely variable chemical compositions; however, all the lakes resulted oligotrophic. Pigment concentrations in surface sediments were comparable to those reported for other Antarctic lakes and lower than those in oligotrophic lakes at lower latitudes. Cyanophyta, Chlorophyta and Bacillariophyta were the main taxa identified. These taxa correspond to those reported in previous microscopy-based studies on Antarctic phytoplankton and phytobenthos. Discriminant Function Analysis and Canonical Correspondence Analysis of data indicate that the distribution of pigments in these Victoria Land lakes depends mainly on their geographical location (particularly the distance from the sea) and nutrient status.

Site characteristics, sediment geochemistry and pigment concentration of northern Victoria Land lakes

Antarctic ice-free areas contain lakes and ponds that have interesting limnological features and are of wide global significance as early warning indicators of climatic and environmental change. However, most limnological and paleolimnological studies in continental Antarctica are limited to certain regions. There are several ice-free areas in Victoria Land that have not yet been studied well. There is therefore a need to extend limnological studies in space and time to understand how different geological and climatic features affect the composition and biological activity of freshwater communities. With the aim of contributing to a better limnological characterization of Victoria Land, this paper reports data on sedimentary pigments (used to identify the main algal taxa) obtained through a methodology that is more sensitive and selective than that of previous studies. Analyses were extended to 48 water bodies in ice-free areas with differing lithology, latitude, and altitude, and with different morphometry and physical, chemical, and biological characteristics in order to identify environmental factors affecting the distribution and composition of freshwater autotrophic communities. A wider knowledge of lakes in a limnologically important region of Antarctica was obtained. Cyanophyta was found to be the most important algal group, followed by Chlorophyta and Bacillariophyta, whereas latitude and altitude are the main factors affecting pigment distribution.

Geochemistry of tetrapyrrole, tetraterpenoid, and perylene pigments in sediments from the Gulf of California

Results and discussion cover pigment analyses of 36 sediment samples recovered by Deep Sea Drilling Project Leg 64, and six samples from the Leg 64 site-survey cruise in the Guaymas Basin (Scripps Institution of Oceanography, Leg 3). Pigments investigated were tetrapyrroles, tetraterpenoids, and the PAH compound perylene. Traces of mixed nickel and copper ETIO-porphyrins were ubiquitous in all sediment samples, except for the very surface (i.e., <2 m sub-bottom), and their presence is taken as an indication of minor influxes of previously oxidized allochthonous (terrestrial) organic matter. Phorbides and chlorins isolated from Site 479 sediment samples (i.e., the oxygen-minimum locale, northeast of the Guaymas Basin) well represent the reductive diagenesis ("Treibs Scheme"; see Baker and Palmer, 1978; Treibs, 1936) of chlorophyll derivatives. Three forms of pheophytin-a, plus a variety of phorbides, were found to give rise to freebase porphyrins, nickel phylloerythrin, and nickel porphyrins, with increasing depth of burial (increasing temperature). Sediments from Sites 481, 10G, and 18G yielded chlorophyll derivatives characteristic of early oxidative alterations. Included among these pigments are allomerized pheophytin-a, purpurin-18, and chlorin-p6. The high thermal gradient imposed upon the late Quaternary sediments of Site 477 greatly accelerated chlorophyll diagenesis in the adjacent overlying sediments, that is, the production of large quantities of free-base desoxophylloerythroetioporphyrin (DPEP) occurred in a section (477-7-5) presently only 49.8 meters sub-bottom. Present depth and age of these sediments are such that only chlorins and phorbides would be expected. Carotenoid (i.e., tetraterpenoids) concentrations were found to decrease rapidly with increasing sub-bottom depth. Less deeply buried sediments (e.g., 0-30 m) yielded mixtures of carotenes and oxygen-substituted carotenoids. Oxygencontaining (oxy-, oxo-, epoxy-) carotenoids were found to be lost preferentially with increased depth of burial. Early carotenoid diagenesis is suggested as involving interacting reductions and dehydrations whereby dehydro-, didehydro-, and retro-carotenes are generated. Destruction of carotenoids as pigments may involve oxidative cleavage of the isoprenoid chain through epoxy intermediates, akin to changes in the senescent cells of plants. Perylene was found to be a common component of the extractable organic matter from all sediments investigated. The generation of alkyl perylenes was found to parallel increases in the existing thermal regime at all sites. Igneous sills and sill complexes within the sediment profile of Site 481 altered (i.e., scrambled) the otherwise straightforward thermally induced alkylation of perylene. The degree of perylene alkylation is proposed as an indicator of geothermal stress for non-contemporaneous marine sediments.