BULLETIN OF MARINE SCIENCE, 67(2): 821–830, 2000 CORAL REEF PAPER UV-ABSORBING COMPOUNDS IN THREE SPECIES OF CARIBBEAN ZOOXANTHELLATE CORALS: DEPTH DISTRIBUTION AND SPECTRAL RESPONSE J. E. Corredor, A. W. Bruckner, F. Z. Muszynski, R. A. Armstrong, R. García and J. M. Morell ABSTRACT We examined the ultraviolet (UV) absorption spectra (280–400 nm) of coral tissue extracts and the concentration and composition of mycosporine-like amino acids (MAA) in three common Caribbean reef-building corals using UV spectroscopy and high-pressure liquid chromatography. Two of the species examined Porites astreoides (green morphotype) and Acropora cervicornis are widely distributed ranging from <1.0 to over 25 m depth, while the third, Mycetophyllia ferox, is a plating species usually confined to the deeper parts of the reef. UV absorption spectra (280–400 nm) of coral tissue extracts in seawater exhibited absorption maxima between 320 and 340 nm and protein-specific absorption in general decreased with depth. A. cervicornis and P. astreoides exhibited hypsochromic displacement in their UV-absorption spectra relative to M. ferox, denoting greater capacity per mole unit MAA for absorption of the shorter, more energetic, and thus more harmful radiation. MAA content of M. ferox was the lowest of the three species examined, approximately one tenth that of P. astreoides across the depth range examined. In all three species, mycosporine–glycine showed the least variation with depth while content of other MAAs varied substantially. Knowledge of the ability of corals and other marine organisms to chemically screen their tissues from harmful ultraviolet (UV) light dates to the work of MacMunn (1903) who reported the presence of “dark pigments that have the property of arresting the ultraviolet and violet rays of light”. With regard to the photoprotective role of these ‘pigments’, MacMunn noted that “they probably act as a screen, protecting the delicate organisms from the irritating effects of the rays of short wave-length”. Subsequently, Margalef (1959) reported the presence of an unidentified compound with high absorption at low wavelengths in reef building corals growing in shallow waters of southwest Puerto Rico; again recognizing that such compounds might serve as a defense against the biological effects of UV radiation. It was not, however, until the rediscovery of these compounds in corals of the Great Barrier Reef by Shibata (1969) that modern work on their chemical nature, taxonomic distribution and ecological significance came about. These compounds are now recognized as ‘mycosporine-like amino acids’ (MAAs) a group of cyclohexenone/ amino acid-based water-soluble compounds believed to arise from the shikimic acid biosynthetic pathway. MAAs are abundant in benthic marine invertebrates exposed to high fluxes of UV radiation, particularly in the reef building corals which are sessile and restricted to shallow depths within the euphotic zone. Dunlap and Shick (1998) have provided an extensive and up-to-date review of the biochemistry and environmental role of MAAs in coral reef organisms. Reef-building corals exhibit substantial variability in the concentration of these UVabsorbing compounds with depth. MAA content is usually greatest in shallow waters presumably as a response to increased UV fluxes (Dunlap and Chalker, 1986; Dunlap et al., 1986; Gleason and Wellington, 1993). The distribution of these photoprotective com821 822 BULLETIN OF MARINE SCIENCE, VOL. 67, NO. 2, 2000 pounds within a single colony also responds to differences in the incident light flux with higher concentrations on the upper part of the corallum and lower concentrations in the shaded portions (MacMunn, 1903; Muszynski et al., 1998). MAA suites and total concentrations vary among species or even between two color morphs of a single species (Gleason, 1993). To assess the capacity for UV screening of the different coral species, we examined the UV-absorption characteristics of coral extracts and the composition and concentration of MAAs in three common Caribbean reef-building corals from a reef off La Parguera, Puerto Rico. The species Porites astreoides (green morphotype), Acropora cervicornis and Mycetophyllia ferox were selected based on their abundance and vertical distribution. Two of the species examined are widely distributed from <1.0 to over 25 m depth, while the third, M. ferox, is a plating species usually limited to the deeper parts of the reef (Colin, 1978). In order to approximate the in vivo optical spectra of the coral MAAs, we re-suspended dried extracts in filtered offshore seawater and recorded their absorption spectra. These extracts were further characterized by high-pressure liquid chromatograhy. We report significant differences in both the position and magnitude of absorption maxima from different taxa as well as differences in MAA suite between species and within species along the depth gradient. MATERIALS AND METHODS SAMPLING PROCEDURE.—Coral samples were obtained at San Cristobal reef off La Parguera, on the southwest coast of Puerto Rico. Sampling was performed on 12 April 1997 except for the shallow (1.5 m) samples of A. cervicornis which were collected on 21 February 1997. Total MAA concentration and composition were examined in coral colonies at three depths (1.5, 5 and 10 m). At each depth, replicate coral tissue samples were taken from three colonies of each species, for a total of 18 samples (nine colonies, two samples per colony). M. ferox was rare at 1.5 m depth. Only one colony of this species was found oriented horizontally and exposed to direct incident light; samples were taken from this colony as well as two colonies oriented vertically and shaded by reef rock. We have previously demonstrated that MAA composition and content can vary up to five-fold within an individual coral specimen according to the orientation of the surface sampled relative to solar irradiation (Muszynski et al., 1998). To avoid such variability, we adopted the following sampling strategy: For all massive and plating species, samples were taken from the center of the horizontal upper surface. Two 3.5 cm2 cores were removed from three separate colonies of each coral species using a pneumatic drill and a carbide-tipped hole saw. Each core was cut into two equal portions with a high-speed rotary tool. For the coral A. cervicornis, one sample consisted of the top 10 cm of a vertically oriented branch approximately 15–20 cm in overall length; three vertical branches were collected from each coral. Samples were transported to the laboratory in individual containers submerged in seawater and shaded from direct sunlight. SAMPLE EXTRACTION.—All samples were extracted sequentially in four 10 ml volumes of 20% tetrahydrofuran in methanol (MeOH/THF) within 2 h of collection. Core sections were initially extracted for 20 h at 4°C, followed by three additional 20 min extractions at room temperature. Samples were then centrifuged at 5000 rpm for 5 min. The supernatant was decanted for MAA analysis and the solid fraction was used for determination of total protein. PROTEIN ANALYSIS.—Total protein was determined with a Bio-Rad DC protein assay kit using bovine gamma globulin as a standard. The solid portion of each sample was heated in 3 ml 1N NaOH for 30 min at 90°C, cooled to room temperature and neutralized with 3 ml 1N HCl prior to reagent addition. Absorption was recorded at 750 nm using a Hewlett-Packard 8452-A diode array spectrophotometer. CORREDOR ET AL.: CARIBBEAN CORALS DEPTH UV SPECTRAL RESPONSE 823 WHOLE EXTRACT ABSORPTION SPECTRA.—Capacity for light absorption of coral species was assessed using the MeOH/THF extract and extracts re-dissolved in seawater. Aliquots of the extract (5 ml) were evaporated to dryness in a rotary evaporator and re-dissolved in 5 ml filtered offshore seawater to simulate the ionic strength of the intracellular fluids. The re-dissolved extracts were passed through a C-8 Sep-Pak cartridge and MAAs retained in the cartridge were eluted with an additional 5 ml seawater. The combined extracts were then scanned in a 1 cm quartz cell using a HP8452 diode array spectrophotometer. Resulting data were normalized to protein content. Seawater exhibits higher pH and ionic strength than intracellular fluids and both pH and ionic strength can affect the absorption spectrum and magnitude of organic solutes (Görög, 1995). Consequently, the suitability of seawater for simulating the intracellular millieu was examined by varying the salinity and pH of representative extracts from P. astreoides re-dissolved in seawater over ranges encompassing the physiological ranges. MAA ANALYSIS.—MAAs were separated by reversed-phase isocratic HPLC using a LC-10AT Shimadzu liquid chromatograph and a C-8 column (Upchurch α-Chrom) following a protocol modified from Dunlap and Chalker (1986). For each sample, 4 ml of supernatant was evaporated under vacuum and re-suspended in 4 ml 0.1% aqueous acetic acid and 10% methanol. Non-polar photosynthetic pigments were removed with a maxi-clean C-18 SepPak solid-phase extraction cartridge (900 mg), the filtrate was diluted appropriately (1:1 to 1:10), and sub-samples of 600 μL were injected across a 200 μL injection loop at a flow rate of 0.2 ml.min −1. MAA elution was monitored between 250 and 400 nm by diode array. DATA HANDLING.—MAAs were identified by comparison of their absorption maxima and retention time to those of known compounds. Compounds were quantified as described previously (Muszynski et al., 1998) using absorption coefficients for mycosporine-glycine e310 = 28,100 (Ito and Hirata, 1977), for shinorine e334 = 44,668 (Tsujino et al., 1980), palythine e320 = 36,200 (Takano et al., 1978), and e330 = 43,500 for asterina 330 and palythinol (Gleason, 1993). UV absorption and MAA content were normalized to protein content (Chalker et al., 1983) for statistical analysis. Between species differences, and depth variability within species were assessed by analysis of variance. A two-factor ANOVA was used to determine if the total concentration of UV absorbing compounds varied significantly among species and depths. For M. ferox from 1.5 m a single factor ANOVA was used to examine for differences in MAA concentration between the horizontally and vertically oriented, partially shaded colonies. OPTICAL PROPERTIES.—Seawater absorption within the La Parguera reef complex was measured at an adjacent reef (Laurel reef) on five occasions between December 1997 and January 1999. We used a submersible Optronics OL-754 spectroradiometer with a 100 mm integrating sphere attached to a 11 m quartz fiber optic cable. Diffuse attenuation coefficients were calculated for each 2 nm band between 300 and 700 nm. Average daily sea-level UV irradiation for five channels of the UVA/UVB region (305, 320, 340 and 380 nm) is routinely monitored at La Parguera using a Biospherical Instruments GUV-511C radiometer. Estimates of daily UV irradiation at 320 nm were obtained by averaging observations over the week of sampling. RESULTS UV absorption spectra (280–400 nm) of coral tissue extracts re-dissolved in seawater exhibited UV-absorption maxima between 320 nm and 340 nm and absorption in general decreased with depth (Fig. 1). Both the wavelength of maximum absorption and the total absorption varied significantly within species. In shallow water (ca 1.5 m) P. astreoides had the highest absorption (mean = 0.08 cm−1 mg protein−1; SD = 0.029) and A. cervicornis had intermediate values (0.038 ± 0.007 cm−1 mg protein−1), while M. ferox exposed to ambient light at 1.5 m demonstrated the lowest overall ability to absorb UV radiation (0.0109 ± 0.0067 cm−1 mg protein−1). 824 BULLETIN OF MARINE SCIENCE, VOL. 67, NO. 2, 2000 Figure 1. Absorption spectra of protein-normalized MAA tissue extracts (re-dissolved in seawater) of A. cervicornis, M. ferox and P. astreoides from 1.5, 5 and 10 m depth. (n = 3 for all species and depths except M. ferox at 1.5 m, n = 1). CORREDOR ET AL.: CARIBBEAN CORALS DEPTH UV SPECTRAL RESPONSE 825 Table 1. Effect of varying seawater salinity and pH on the wavelength of maximum absorbance of coral extracts (Porites astreoides). Methanol/tetraydrofuran extracts were evaporated to dryness and re-dissolved in seawater. Sample salinity was progressively lowered by dilution with distilled water. Sample pH was lowered by adding aliquots of a 10% HCl solution. Salinity (‰) 35 34 33 31 29 28 27 25 24 23 22 20 Wavelength (nm) 329.8 330.0 329.8 329.8 329.2 329.4 329.4 329.6 329.6 329.4 329.6 329.6 pH 7.64 7.63 7.50 7.24 6.93 Wavelength (nm) 330.1 330.3 329.7 329.9 329.4 Varying the ionic strength and pH of the seawater solutions of the P. astreoides extract had no significant effect on the absorption spectrum (Table 1). In contrast, MAA extracts for the most part exhibited substantial bathychromic absorption shifts in the MeOH/THF solvent relative to those re-dissolved in seawater (Table 2). We conclude that seawater adequately represents the intracellular milieu for assessment of wavelength-dependent absorptive capacity. HPLC revealed the presence of up to four distinct MAAs identified as mycosporineglycine, shinorine, palythine, and asterina 330 (Fig. 2). Asterina 330 was absent from A. cervicornis and M. ferox. Shinorine and palythine were absent from P. astreoides. Mycosporine-glycine was the prevalent MAA in P. astreoides. A. cervicornis contained three MAAs at all depths; asterina 330 was absent from all samples. P. astreoides tissue from 1.5 m contained the highest total quantity of MAAs (71 nmol mg protein−1). At the same depth, A. cervicornis had an intermediate total MAA concentration (25 nmol mg protein−1), while M. ferox had the lowest amount overall (10 nmol mg protein−1). All species examined exhibited a reduction of MAA content of approximately ten fold from 1.5 m to 10 m depth, with the largest decline observed in P. astreoides. Daily UV-doses at Table 2. Position (nm) of maximum absorbance for MeOH/THF coral extracts and for extracts re-dissolved in seawater. 1.5 m 5m 10 m SW Acropora cervicornis Porites astreoides Mycetophyllia ferox 322 326 332 324 no discernible peak 330 320 324 332 MeOH/THF Acropora cervicornis Porites astreoides Mycetophyllia ferox 332 330 336 326 320 336 320 322 338 BULLETIN OF MARINE SCIENCE, VOL. 67, NO. 2, 2000 826 Figure 2. Mean concentration of four MAAs identified in A. cervicornis, M. ferox and P. astreoides tissue from 1.5, 5 and 10 m depth. (n = 3 for each species at each depth except M. ferox at 1.5 m, n = 2). depth were computed using the GUV data and the mean Kd320 discussed above (0.70 m−1). A plot of individual MAA content as a function of the average daily UV dose (Fig. 3) reveals little variation in mycosporine-glycine content, but larger variation in the content of other MAAs. Horizontal colonies of M. ferox exposed to ambient light at 1.5 m contained the same three MAAs of A. cervicornis, however only trace quantities of shinorine were identified in vertically-oriented, partially shaded M. ferox samples (mean = 1.06 nmol mg protein−1) from the same depth. The quantity of MAAs was significantly different between 1.5 m samples (t-test, P = 0.001), while no differences existed between vertical, shaded 1.5 m samples and 10 m exposed colonies (t-test, P = 0.09). Table 3. Two-way ANOVA of the effect of species and depth on the total concentration of UV absorbing compounds. Species: Acropora cervicornis, Mycetophyllia ferox and Porites astreoides; depths: 1.5, 5 and 10 m. Source Species Depth Interaction Error Total DF 2 2 4 18 26 SS 0.004219 0.005005 0.002663 0.000348 0.012235 MS 0.002110 0.002502 0.000666 1.93Ε−05 F 109.3109 129.6580 P <0.01 <0.01 CORREDOR ET AL.: CARIBBEAN CORALS DEPTH UV SPECTRAL RESPONSE 827 Figure 3. MAA distribution as a function of average calculated in situ daily UV dose at 320 nm. The mean value (n = 5) for the diffuse attenuation coefficient (Kd320) of waters of Laurel reef was 0.70 m−1. Kd320 varied from a minimum of 0.5 m−1 to a maximum of 1.05 m−1. Average daily surface UV irradiance (280–400 nm) during the week of sampling was 0.41 J cm−2 d−1 for all samples except for the A. cervicornis collected at 1.5 m. The average daily UV dose at the time of sampling for this specimen was 0.35 J cm−2 d−1. 828 BULLETIN OF MARINE SCIENCE, VOL. 67, NO. 2, 2000 DISCUSSION Nineteen distinct MAAs have been identified in marine organisms (Dunlap and Shick, 1998). The corals we have characterized accumulate substantial quantities of only a limited number of these compounds. Our compound identifications are based on chromatographic elution sequence and UV absorption spectra and are not definitive given the lack of authenticated standards. Compound quantification is also tentative as molar absorptivities may vary from the published values cited above due to solvent effects. On this basis, mycosporine-glycine, shinorine and asterina 330 are the most abundant but palythine is also widespread and, in some instances, may be the most abundant. Two-factor analysis of variance comparing the total MAA concentration indicates that significant differences exist both among species and depths (Table 2). Our results thus confirm previous observations (Dunlap et al., 1986; Gleason 1993; Shick et al., 1995) regarding the inverse relationship between MAA concentration and depth over a varied range of species further strengthening the argument for a UV-photoprotective role of these compounds. The values we report for the green color morph of P. astreoides MAA content are significantly lower than those reported by Gleason (1993) for the reefs of St. Croix, U.S. Virgin Islands. Similarly, values for A. cervicornis are approximately three-fold lower than those reported for A. microphthalma; a congeneric Pacific species (Shick et al., 1995). While these discrepancies may be due to methodological differences in compound extraction and protein quantification, they may indeed reflect variations of physiological nature. Dunlap et al. (1986), for example, report a tendency for seasonal changes in total MAA content of A. formosa. Differences reported in the nature of the specific MAAs are only tentative as we lacked authenticated standards. Species of the genus Mycetophyllia are usually limited to deeper waters in Caribbean reefs (Colin, 1978). Accordingly, we tested the hypothesis that M. ferox might exhibit decreased UV photoprotection. MAA content of M. ferox was the lowest of the species examined being approximately one tenth of that of P. astreoides across the depth range examined. While we have demonstrated that M. ferox indeed contains MAAs and that the content varies with depth, its capacity for accumulation of these compounds appears to be limited. Previous studies of reef coral photoadaptation have demonstrated significant photosynthetic response (Zvalinskii et al., 1980) and adjustment of photosynthetic pigment content to total irradiance in the photosynthetically active range (Wethey and Porter, 1976). We here demonstrate that three widespread Caribbean species exhibit this capacity to varying degrees with reference to the content of UV-absorbing compounds. Our results further suggest that reef corals may be able to adjust their MAA content not only in terms of increasing their total UV absorption capacity but also in adjusting UV-absorbing compound suites to spectral quality of UV irradiation. Inhibition of diverse physiological functions in both plants and animals (Caldwell, 1977; Häder et al., 1995), including photosynthesis by corals (Lesser and Lewis, 1996) becomes apparent at about 320 nm and increases notably at lower wavelengths. Seawater selectively absorbs shorter wavelengths in such a manner that radiation at 320 nm can be attenuated 50 to 100 fold over a span of only 14.5 m (Baker and Smith, 1981). In order to overcome the deleterious effects of the shorter wavelength radiation close to the surface, photochromatic adaptation might be expected to cause shifts in the absorptivity of photoprotective compounds in this direction. Our results support this contention between species. A. cervicornis, and P. astreoides CORREDOR ET AL.: CARIBBEAN CORALS DEPTH UV SPECTRAL RESPONSE 829 exhibited hypsochromic displacement in their UV-absorption spectra relative to M. ferox, denoting greater capacity for absorption of the shorter, more energetic, and thus more harmful radiation. Individual species do not, however exhibit substantial wavelength maximum shifts with depth. As expected, those species with a wide depth range exhibited a large range of variation in MAA composition. In contrast, M. ferox, a stenobathic species, exhibits the lowest capacity for photoadaptation with restricted MAA suite composition. ACKNOWLEDGMENTS This work was supported by NASA grant #NCCW 0088. We acknowledge comments by M. Shick and an anonymous reviewer that contributed substantially to the quality of the manuscript. LITERATURE CITED Baker, K. S. and R. C. Smith. 1981. Spectral irradiance penetration in natural waters. Pages 233– 246 in J. Calkins, ed. The role of solar ultraviolet radiation in marine ecosystems. Plenum, New York. Caldwell, M. M. 1977. The effects of solar UV-B radiation (280–315 nm) on higher plants: implications of stratospheric ozone reduction. Pages 597–607 In Research in photobiology. Plenum, London. Chalker, B. E., W. C. Dunlap and J. K. Oliver. 1983. Bathymetric adaptations of reef building coral at Davies Reef, Great Barrier Reef, Australia. II. Light saturation curves for photosynthesis and respiration. J. Exp. Mar. Biol. Ecol. 73: 37–56. Colin, P. L. 1978. Caribbean reef invertebrates and plants. TFH Publications, Inc., Neptune City, New Jersey. 512 p. Dunlap, W. C. and B. E. Chalker. 1986. Identification and quantification of near-UV absorbing compounds (S-320) in a hermatypic scleractinian. Coral Reefs 5: 155-159. ____________, ___________ and J. K. Oliver. 1986. Bathymetric adaptations of reef building coral at Davies Reef, Great Barrier Reef, Australia. III. UV-B absorbing compounds. J. Exp. Mar. Biol. Ecol. 104: 239–248. ____________ and J. M. Shick. 1998. Ultraviolet radiation-absorbing mycosporine-like amino acids in coral ref organisms: A biochemical and environmental perspective. J. Phycol. 34: 418– 430. Gleason, D. F. 1993. Differential effects of ultraviolet radiation on green and brown morphs of the Caribbean coral Porites astreoides. Limnol. Oceanog. 38(7): 1452–1463. Görög, S. 1995. Ultraviolet-visible spectrophotometry in pharmaceutical analysis. CRC Press, Boca Raton, Florida. 391 p. Häder, D-P., R. C. Worrest, H. D. Kumar and R. C. Smith. 1995. Effects of solar ultraviolet radiation on aquatic ecosystems. Ambio 24: 174–180. Ito, S. and Y. Hirata. 1977. Isolation and structure of mycosporine-like amino acids from the zoanthid Palythoa tuberculosa. Tetrahedron Lett. 28: 2429–2430. Lesser, M. P. and S. Lewis. 1996. Action spectra for the effect of UV radiation on photosynthesis in the hermatypic coral Pocillopora damicornis. Mar. Ecol. Prog. Ser. 134: 171–177. Margalef, R. 1959. Pigmentos asimiladores extraídos de las colonias de celentéreos de los arrecifes de coral y su significado ecológico. Inv. Pesq. XV: 81–101. MacMunn, C. A. 1903. On the pigments of certain corals with a note on the pigment of an asteroid. The fauna and geography of the Maldives and Laccadive Archipelagoes 1: 184–190. Muszynski, F. Z., A. Bruckner, R. A. Armstrong, J. M. Morell and J. E. Corredor. 1998. Withincolony variations of UV absorption in a reef building coral. Bull. Mar. Sci. 63: 589–594 830 BULLETIN OF MARINE SCIENCE, VOL. 67, NO. 2, 2000 Shibata, K. 1969. Pigments and UV-absorbing substance in coral and a blue-green algae living in the Great Barrier Reef. Plant Cell Physiol. 10: 325–335. Shick, J. M., M. P. Lesser, W. C. Dunlap, W. R. Stochaj, B. E. Chalker and J. Wu Won. 1995. Depthdependent responses to solar ultraviolet radiation and oxidative stress in the zooxanthellate coral Acropora microphthalma. Mar. Biol. 122: 41–51. Takano, S., D. Uemura and Y. Hirata. 1978. Isolation and structure of a new amino acid, palythine, from the zoanthid Palythoa tuberculosa Tetrahedron Lett. 26: 2299–2300. Teai, T., J. H. Drollet, J.-P. Bianchini, A. Cambon and P. M. V. Martin. 1997. Widespread occurrence of mycosporine-like amino acid compounds in scleractinians from French Polynesia. Coral Reefs. 16: 169–176. Tsujino, I., K. Yabe and I. Sekekawa. 1980. Isolation and structure of a new amino acid, shinorine, from the red algae Chondrus yendoi Yamada et. Mikami. Bot. Mar. 23: 65–68. Wethey, D. S. and J. W. Porter. 1976. Sun and shade differences in productivity of reef corals. Nature 262: 281–282. Zvalinskii, V. I., V. A. Leletkin, E. A. Titlyanov and M. A. Shaposhnikova. 1980. Photosynthetic adaptation of corals to irradiance 2. Oxygen exchange. Photosynthetica 14: 422–430. DATE SUBMITTED: February 25, 1999. DATE ACCEPTED: May 12, 2000. ADDRESS: Department of Marine Sciences, P. O. Box 908, Lajas, Puerto Rico 00667-0908.
© Copyright 2026 Paperzz