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Author for correspondence: Laurence J. Clarke Tel: +612 4221 4961 Fax: +612 4221 4135 Email: email@example.com
• Studies of ultraviolet (UV) light-induced DNA damage in three Antarctic moss species have shown Ceratodon purpureus to be the most UV tolerant, despite containing lower concentrations of methanol-soluble UV-screening compounds than the co-occurring Bryum pseudotriquetrum.
• In this study, alkali extraction of cell wall-bound phenolics, combined with methanol extraction of soluble phenolics, was used to determine whether cell wall-bound UV screens explain the greater UV tolerance of C. purpureus.
• The combined pool of UV screens was similar in B. pseudotriquetrum and C. purpureus, but whilst B. pseudotriquetrum had almost equal concentrations of MeOH-soluble and alkali-extractable cell wall-bound UV-screening compounds, in C. purpureus the concentration of cell wall-bound screening compounds was six times higher than the concentration of MeOH-soluble UV screens. The Antarctic endemic Schistidium antarctici possessed half the combined pool of UV screens of the other species but, as in C. purpureus, these were predominantly cell wall bound. Confocal microscopy confirmed the localization of UV screens in each species.
• Greater investment in cell wall-bound UV screens offers C. purpureus a more spatially uniform, and potentially more effective, UV screen. Schistidium antarctici has the lowest UV-screening potential, indicating that this species may be disadvantaged under continuing springtime ozone depletion. Cell wall compounds have not previously been quantified in bryophytes but may be an important component of the UV defences of lower plants.
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Since the late 1970s, stratospheric ozone depletion has led to increased ultraviolet-B radiation (UV-BR; 280–315 nm) at the Earth's surface. Ozone depletion is most severe over the Antarctic in the austral spring (September–November), with the 2006 ozone hole being the largest ever recorded (Cracknell & Varotsos, 2007). As ozone screens UV-BR most effectively, ozone depletion leads to both an increase in the incident daily dose of ultraviolet-B (UV-B) as well as an increase in the ratio of UV-BR to photosynthetically active radiation (PAR) over Antarctica (Newsham et al., 2002; Newsham, 2003). The combined effects of springtime ozone depletion and the approach of the annual radiation peak at the summer solstice results in continental Antarctic vegetation being exposed to an extended period of high UV-BR. Because Antarctic vegetation has historically experienced some of the lowest levels of UV-BR on Earth, it has been hypothesized that it might show particular susceptibility to the elevated UV-BR resulting from ozone depletion. This has stimulated studies investigating the degree and mechanisms of UV tolerance in Antarctic plants.
Continental Antarctic vegetation is sparse and cryptogamic in nature, with mosses being the dominant plants. Three moss species (Bryum pseudotriquetrum, Ceratodon purpureus and Schistidium antarctici (formerly Grimmia antarctici)) co-occur in the Windmill Islands region near Casey station, East Antarctica. Bryum pseudotriquetrum and C. purpureus are both cosmopolitan moss species that occur in temperate regions as well as in the Antarctic, whereas S. antarctici is endemic to the Antarctic region. Previous studies have shown that S. antarctici is one of the few Antarctic mosses to show negative effects from current levels of UV radiation, with damage in the form of abnormal gametophyte morphology and loss of photosynthetic pigments apparent in UV-exposed plants (Robinson et al., 2005). Recent studies of UV-induced DNA damage have also shown that S. antarctici accumulates much higher concentrations of DNA photoproducts, under elevated UV-BR, than the two co-occurring cosmopolitan species (Leslie, 2003). Ceratodon purpureus is found in the most exposed, driest sites (Robinson et al., 2000; Wasley et al., 2006) and shows the highest UV tolerance, whilst B. pseudotriquetrum accumulates intermediate levels of photoproducts (Leslie, 2003). However, this relative susceptibility to UV damage is at odds with measurements of methanol-soluble UV-screening compounds from the three species because B. pseudotriquetrum contains approx. 2–4 times higher concentrations of such compounds than either C. purpureus or S. antarctici (Lovelock & Robinson, 2002; Dunn & Robinson, 2006). Given the difference in UV-screening compound content, the mechanism by which C. purpureus maintains such a high UV-tolerance compared with B. pseudotriquetrum is unclear.
Although many studies have quantified methanol (MeOH)-soluble UV-screening compounds in Antarctic plants, to date cell wall-bound UV-screening compounds have been examined in only two plants experiencing enhanced UV-BR as a result of Antarctic ozone depletion (Ruhland & Day, 2000; Ruhland et al., 2005). Ruhland & Day (2000) studied insoluble phenylpropanoids in Deschampsia antarctica and Colobanthus quitensis, the only vascular plants native to continental Antarctica, to test the hypothesis that cell wall-bound phenolics, such as ferulic acid, may constrain cell expansion, leading to the reduced leaf length observed under elevated UV-BR. A trend towards increased ferulic acid with increasing UV-B exposure was found in D. antarctica; however, the UV-screening capacity of cell wall-bound phenolics was not measured. Both species were found to have low epidermal transmittance of UV-BR, despite relatively low bulk-leaf concentrations of soluble UV-screening compounds, which the authors suggested may be a result of the high concentrations of cell wall-bound UV-screening compounds (Ruhland & Day, 2000). Lower concentrations of several soluble and cell wall-bound hydroxycinnamic acids were also found under reduced UV-BR in D. antarctica, but no effect of UV-BR on flavonoid concentrations was observed (Ruhland et al., 2005). Cell wall-bound UV-screening compounds were also measured in three species of the dwarf shrub Vaccinium at a site in north Sweden influenced by ozone depletion over the Arctic (Semerdjieva et al., 2000). The three species were shown to possess contrasting responses to enhanced UV-BR, with concentrations of methanol-soluble UV-screening compounds increasing in Vaccinium myrtillus and Vaccinium uliginosum, whereas the concentration of cell wall-bound UV-screening compounds increased in Vaccinium vitis-idaea (Semerdjieva et al., 2000). Cell wall-bound flavonoids were visualized microscopically in two moss species from central Finland, and methanol-soluble UV-screening compounds were shown to respond to seasonal changes in the radiation environment (Taipale & Huttunen, 2002). Cell wall-bound UV-screening compounds were not quantified in the latter study, but microscopic examination suggested no increase in cell wall-bound flavonoids in response to enhanced UV-BR (Taipale & Huttunen, 2002).
We used alkali extraction of cell wall-bound phenolics, in combination with methanol extraction of soluble phenolics, to determine whether cell wall-bound UV-screening compounds could explain the greater UV tolerance of C. purpureus compared with B. pseudotriquetrum and S. antarctici. To the best of our knowledge, this is the first study to quantify cell wall-bound UV-screening compounds in any moss species and the first to detect them in Antarctic mosses. As UV-BR is highest early in the summer season and decreases in late January (Dunn & Robinson, 2006), the concentration of UV-screening compounds was compared in samples collected early (November–December) and late (January–February) in the summer growing season to determine whether there is any association between the content of UV-screening compounds and the UV radiation environment. Confocal microscopy was also used to examine the localization of UV-screening compounds in each species. We hypothesized that C. purpureus would contain more cell wall-bound UV-screening compounds than the other two species.
Materials and Methods
Samples of the mosses B. pseudotriquetrum (Hedw.) Gaertn., C. purpureus (Hedw.) Brid. and S. antarctici (Cardot) Savicz-Ljubitskaya & Smirnova (formerly G. antarctici) were collected by Johanna Turnbull over the summer of 2002–2003 from a site within the Antarctic Specially Protected Area (ASPA) 135 (66°16.92′S, 110°32.36′E) near Casey Station in the Windmill Islands region, East Antarctica. Samples were stored on ice for 1–3 h after collection, after which the photosynthetically active shoot tips (3–5 mm) were removed in a walk-in freezer (−20°C) and stored at −80°C before analysis in 2007. Early season samples were collected between 9 November and 2 December 2002, and late season samples were collected between 16 January and 1 February 2003.
Radiation measurements for sampling days in the two collection periods, including UV-B (280–315 nm), total UV (290–400 nm) and total solar radiation (TSR), were obtained from Australian Radiation Protection and Nuclear Safety Agency (ARPANSA) sensors at Casey Station, as described in Dunn & Robinson (2006). The total UV sensor is not calibrated to collect the shortest UV-B wavelengths (280–290 nm); however, the amount of radiation below 290 nm that reaches the Earth's surface is negligible, particularly in the Antarctic. The TSR sensor was not calibrated in 2002–2003 and therefore the values for this parameter are approximate; however, measured changes in TSR over the season are robust. Ratios of radiation parameters (total UV : TSR and UV-B : TSR) were also calculated for each sampling day. As samples were typically collected during favourable weather, radiation measures were also averaged over the 10 d before sampling to remove bias and to obtain a better representation of the radiation environment.
Methanol extraction of soluble phenolics
Soluble phenolics were extracted from gametophyte tissue using a modified version of the method of Schnitzler et al. (1996). Samples were dried at 50°C to constant weight before extraction and then 20–50 mg of shoot tips from each species was frozen in liquid nitrogen and ground to a fine powder. Samples were extracted in 1 ml of MeOH for 1 h at room temperature in the dark, centrifuged (16 000 g for 15 min) and the supernatant was collected. The remaining cell debris was re-extracted three times with 0.5 ml of MeOH. The supernatants were pooled and made up to 3 ml with MeOH. The amount of MeOH used at each step was doubled for large samples to ensure complete extraction. Extracts were stored at 4°C over 1–2 nights before the spectrophotometric measurements were made. This length of storage time did not affect the results.
Alkali extraction of cell wall-bound phenolics
Cell wall-bound UV-screening compounds were extracted using the method of Semerdjieva et al. (2000). Cell debris remaining from the methanol extraction was incubated for 20 min each in 1 m NaCl, twice in 0.5% (w/v) sodium dodecyl sulphate, then twice in chloroform/methanol (1:1, v/v). After each incubation, extracts were centrifuged at 16 000 g for 5 min. The pellet was washed in acetone and air-dried at room temperature before use. A 10-mg sample of crude cell wall material was incubated in 1 ml of 1 m NaOH for 16 h in the dark (Strack et al., 1988). Samples were then centrifuged at 16 000 g for 15 min, and 0.7 ml of supernatant was mixed with 0.7 ml of 1.5 m formic acid and centrifuged for 5 min at 16 000 g. The resulting supernatant was used for spectrophotometric measurements.
Absorbance of methanol and cell wall-bound phenolic extracts in the region 250–400 nm was measured spectrophotometrically using a Shimadzu UV-1601 UV-visible spectrophotometer (Shimadzu, Sydney, Australia). Cell wall-bound phenolic extracts were blanked with distilled water, and methanol extracts were blanked with methanol. Concentrations of UV-B screening compounds were calculated as the area under the absorbance curve in the UV-B spectrum (AUC280–315) mg−1 dry weight of tissue according to Newsham (2003). Spectra were normalized to common absorbance peaks in the three species (268 and 259 nm for methanol and alkali extracts, respectively) to compare UV-screening compound composition.
Moss leaves of each species were mounted in water, and autofluorescence was detected in an emission window of 500–530 nm using an excitation wavelength of 488 nm on a Leica DMIRBE inverted microscope coupled to a Leica TCS SP confocal system (Leica Microsystems, Sydney, Australia). Samples were then stained with 0.5% (w/v) Naturstoffreagenz A (2-aminoethyl diphenylborate; Sigma-Aldrich, Sydney, Australia, Schnitzler et al., 1996) in 10 mm phosphate buffer (pH 6) containing 10% (w/v) sucrose and 2% (v/v) dimethyl sulfoxide, prepared immediately before use from a stock solution of 2.5% (w/v) Naturstoffreagenz A in ethanol (EtOH), and the fluorescence was detected as described at the start of this paragraph. Images were processed using tcs nt software (Leica Microsystems).
The effect of collection time on the values of radiation parameters, and the effect of species and collection time on the concentration of UV-screening compounds, was tested using one-way and two-way ANOVA, respectively, performed with jmp version 5.1 (SAS Inc., Cary, NC, USA). Radiation and UV-screening compound data were transformed where necessary to satisfy the assumptions of ANOVA. Post-hoc comparisons were made using Tukey–Kramer HSD tests.
Most values for radiation parameters were similar for sampling days in the early season and late season collection periods, with the exception of the 10-d mean UV-B : 10-d mean solar radiation (F1,10 = 10.5, P < 0.01) ratio, which was 36% higher in the early season collection period (Table 1). There was a similar, but not significant, trend for both the 10-d mean UV : 10-d mean solar radiation ratio and the daily mean UV-B : daily mean solar radiation ratio to be higher in the early season collection period.
Table 1. Radiation parameters for sampling days in the early season (9 November to 2 December 2002) and late season (16 January to 1 February 2003) collection periods at Casey station in the Windmill Islands region, East Antarctica
All radiation parameters are expressed in units of W m−2.
Error df = 10 in all analyses except ‘Daily mean UV-B’ and ‘Daily mean UV-B : daily mean solar’ where df = 9.UV, ultraviolet; UV-B, ultraviolet B.
Daily mean UV
Daily mean UV-B
Daily mean solar
10-d mean UV
10-d mean UV-B
10-d mean solar
Daily mean UV : daily mean solar
Daily mean UV-B : daily mean solar
10-d mean UV : 10-d mean solar
10-d mean UV-B : 10-d mean solar
The relative proportions of methanol-soluble and alkali-extractable cell wall-bound UV screening compounds differed for the three species. Bryum pseudotriquetrum possessed significantly higher levels of soluble UV-screening compounds than the other two species (13.3 ± 0.8 AUC280–315 mg−1, F5,37 = 71.9, P < 0.0001), 3.5-fold higher than C. purpureus and almost 9-fold higher than S. antarctici (Fig. 1a). Schistidium antarctici also possessed significantly lower concentrations of soluble UV-screening compounds than C. purpureus. Over the season, soluble UV-screening compounds increased (on a dry weight basis) by approx. 40% in C. purpureus. The apparent increase was not significant in the two-way ANOVA but was significant when the concentration of soluble UV-screening compounds for C. purpureus was analysed by one-way ANOVA (F1,14 = 5.9, P = 0.03). However, no significant difference was found between early season and late season material for the other two species.
In B. pseudotriquetrum, the concentrations of alkali-extractable cell wall-bound and soluble UV screening compounds were similar; by contrast, the concentrations of cell wall-bound UV screening compounds were up to nine times higher than the concentrations of soluble UV-screening compounds in C. purpureus and S. antarctici. Ceratodon purpureus contained significantly higher concentrations (on a dry weight basis) of cell wall-bound UV screening compounds (24 ± 2 AUC280–315 mg−1, Fig. 1b) than either B. pseudotriquetrum or S. antarctici (F5,36 = 9.7, P < 0.0001), which had similar concentrations of these compounds (13.8 ± 0.4 and 14 ± 1 AUC280–315 mg−1, respectively). There was no significant difference between the concentration of cell wall-bound UV-screening compounds in material collected early or late in the season for any species.
Combining the concentrations of MeOH-soluble and alkali-extractable cell wall-bound UV-screening compounds for each sample showed that B. pseudotriquetrum and C. purpureus have almost twice the UV-screening potential of S. antarctici (F5,35 = 14.21, P < 0.0001, Fig. 1c). Bryum pseudotriquetrum and C. purpureus had combined totals of 27.1 ± 0.8 and 28 ± 2 AUC280–315 mg−1, respectively, significantly more than S. antarctici (16 ± 1 AUC280–315 mg−1). There was no change in the combined pool of UV-screening compounds over the season for any species.
Inspection of the normalized spectra of MeOH-soluble phenolic extracts in the range 250–400 nm revealed qualitative differences in UV-screening compounds between the three moss species. In addition to a peak at 268 nm, common to all species, B. pseudotriquetrum showed a well-defined maximum at 340 nm (Fig. 2a). Ceratodon purpureus had a similar, but lower, peak shifted to 345 nm, whereas S.antarctici had a much less defined peak (c. 330 nm). Unlike the other two species, extracts from S. antarctici showed an increase in absorption with increasing wavelength above 355 nm. This is likely to reflect large amounts of chlorophyll, in particular chlorophyll a, which has an absorption maximum in MeOH near 420 nm with a shoulder extending into the UV-A region, in the extracts from this species. The spectra of the alkali-extractable cell wall-bound UV-screening compounds were similar between the three mosses, with absorption maxima at 259 nm in each species (Fig. 2b). The only substantial difference between the cell wall compound spectra was the presence of a shoulder at 350 nm in C. purpureus and S. antarctici that was absent in B. pseudotriquetrum.
Staining of leaves with Naturstoffreagenz A allowed the location of phenolic compounds to be visualized using confocal microscopy. These data confirmed the alternative UV-screening strategies of the three species. The leaves of B. pseudotriquetrum showed substantial amounts of both intracellular and cell wall-associated fluorescence (Fig. 3a), whereas the leaves of C. purpureus showed intense cell wall fluorescence with minimal staining of intracellular compounds (Fig. 3c). Cell walls of this species were still fluorescent after repeated methanol extraction. Like C. purpureus, fluorescence was associated more with the cell walls of S. antarctici than the cell contents; however, some intracellular fluorescence was also apparent (Fig. 3e). No species showed significant autofluorescence in the detection window (500–530 nm).
We found that the two cosmopolitan moss species present in the Windmill Islands region have alternative strategies for UV screening. Bryum pseudotriquetrum has equal proportions of MeOH-soluble and alkali-extractable cell wall-bound UV-screening compounds, whereas C. purpureus relies more strongly on MeOH-insoluble, alkali-extractable cell wall-bound UV-screening compounds (Fig. 1, note that salt-wash, sodium dodecyl sulphate-wash, chloroform/methanol-wash and acetone-wash fractions were disregarded). Although the Antarctic endemic S. antarctici also has a high ratio of cell wall-bound, alkali-extractable to MeOH-soluble UV screens, it only possesses half the combined pool of soluble and cell wall-bound UV-screens on a dry weight basis compared with the cosmopolitan species (Fig. 1). It is possible that UV screens other than the MeOH-soluble and alkali-extractable cell wall-bound compounds isolated could contribute to the total pool of UV-screening compounds in these species and similarly that some MeOH-soluble UV-screening compounds may be associated with the cell wall. However, the confocal microscopy images support the alternative UV-screening strategies, as suggested above (Fig. 3).
Previous studies of UV-induced DNA damage suggest that S. antarctici is the least UV-tolerant of the three moss species present in the Windmill Islands region, with B. pseudotriquetrum showing intermediate sensitivity and C. purpureus being the most UV tolerant (Leslie, 2003). Our results show that S. antarctici has the smallest pool of MeOH-soluble and alkali-extractable cell wall-bound UV-screening compounds, consistent with its ranking as the least UV-tolerant of the three moss species. Schistidium antarctici is negatively affected by current levels of ambient UV, with damage in the form of abnormal gametophyte morphology and chlorophyll bleaching apparent in UV-exposed plants (Robinson et al., 2005). These results support the hypothesis that this species might be at a disadvantage compared with the two cosmopolitan species under continuing springtime ozone depletion. We found no significant difference in the combined MeOH-soluble and alkali-extractable cell wall-bound UV-screening compound content between C. purpureus and B. pseudotriquetrum, and therefore these species would be expected to have similar degrees of UV tolerance. The greater UV tolerance of C. purpureus could arise from this species accumulating UV-screening compounds at the leaf surface, providing a more effective UV screen; however, the leaf blade in each of these moss species is only one cell thick (10–20 µm) and the small angle between leaf and stem and the tightly packed nature of Antarctic moss turfs (> 500 shoots cm−2, Wasley et al., 2006) makes it difficult to determine whether the abaxial or adaxial leaf surface would receive a higher UV flux. Confocal microscopy also suggests that the distribution of UV-screening compounds is uniform at the leaf level in these moss species. However, the confocal microscope image of B. pseudotriquetrum, the species with the highest fraction of soluble UV-screening compounds, shows that the intracellular UV-screening compounds are not equally distributed throughout the cell (Fig. 3a), but are possibly contained within the vacuoles, as is the case in many plant species (Hutzler et al., 1998; Cockell & Knowland, 1999; Meijkamp et al., 1999; Kolb & Pfündel, 2005). The cell wall-bound UV-screening compounds, by contrast, appear to be evenly distributed throughout the cell walls in each of the three species (Fig. 3). Cell wall-bound UV-screening compounds are likely to provide a more spatially uniform, and thus more effective, UV screen for the cell contents than intracellular UV-screening compounds. This is especially the case in mosses because the leaves are composed of only a single cell layer and thus UV-screening compounds in the vacuoles will not provide screening for lower cell layers, as is the case for the epidermal layer in vascular plants. The greater investment in cell wall-bound UV-screening compounds may explain the higher UV tolerance of C. purpureus compared with B. pseudotriquetrum, despite the combined UV-screening compound content being very similar in the two species. Post (1990) found higher concentrations of anthocyanins and carotenoids in Antarctic C. purpureus from high-light environments compared with low-light environments. It is possible that the antioxidant properties of anthocyanins, carotenoids and flavonoids could play a role in the tolerance of C. purpureus and B. pseudotriquetrum to multiple stressors, including UV-BR, by reducing oxidative damage (Grace, 2005; Smirnoff, 2005). Further work is needed to determine if intracellular compounds are more effective as antioxidants than those bound to the cell walls.
Differences in the absorption spectra of the methanol and alkali extracts between the three moss species indicate qualitative as well as quantitative differences in soluble and cell wall-bound UV-screening compounds (Fig. 2). The absorption spectra for MeOH-soluble UV-screening compounds differed between the three species, suggesting different compositions of soluble UV-screening compounds in these mosses. The peaks at c. 270 and 340 nm in these spectra suggest that flavonoid-type compounds may be present in these mosses, although other compounds also absorb in these regions (Harborne, 1989). Flavonoids have been previously identified in several species of the genus Bryum (e.g. Markham & Given, 1988; Webby et al., 1996), and in sporophytes, but not in gametophytes, of C. purpureus (Vandekerkhove, 1978); however, recent studies by our group suggest that flavonoids are also present in gametophytes of this species (S. A. Robinson & V. Chobot, unpublished data). Absorption spectra for alkali-extractable wall-bound UV-screening compounds were more similar between species, although B. pseudotriquetrum absorbed less in the UV-A region. The single absorption maximum in the spectrum of the alkali extract of B. pseudotriquetrum suggests that the cell walls of this species contain a relatively large proportion of simple phenolics compared to the other two species, which are less effective UV-screens than flavonoids (Harborne, 1989). The absorption spectra of the alkali-extractable cell wall-bound UV-screening compounds for this species are also similar to those observed in species of the dwarf shrub Vaccinium (Semerdjieva et al., 2000). Cell wall-bound UV-screening compounds may be more conserved across species than MeOH-soluble UV-screening compounds. Identification of the MeOH-soluble and cell wall-bound compounds involved in UV screening in these mosses and other plant species is needed to determine whether this is the case.
Our research suggests that cell wall-bound UV-screening compounds are an important component of the defence against UV radiation in all three moss species present in the Windmill Islands region. Field studies have shown that ambient or enhanced UV-BR rarely has an effect on photosynthesis in mosses (Caldwell et al., 2007). Cell wall-bound UV-screening compounds may explain the resilience of mosses to UV-BR, and moreover, such UV-screening compounds seem to be constitutive in these three species. The only seasonal difference in UV-screening compounds observed in this study was a greater concentration of MeOH-soluble UV-screening compounds in C. purpureus collected later in the growing season, whereas no change in alkali-extractable wall-bound UV screens was found in any species.
Although previous studies have shown the concentration of MeOH-soluble UV-screening compounds in B. pseudotriquetrum to be responsive to changes in the UV radiation environment (Dunn & Robinson, 2006), no change in the concentrations of soluble UV-screening compounds was found over the growing season for B. pseudotriquetrum in this study. We also found higher levels of MeOH-soluble UV-screening compounds in C. purpureus collected later in the growing season, even though UV-BR is typically higher earlier in the growing season under the influence of the ozone hole. Both results may be a consequence of the anomalously small ozone hole in the austral spring of 2002, which was both smaller in total area and broke up earlier in the season than in previous and subsequent years (Allen et al., 2003; Solomon, 2004). In fact, whereas the UV-BR was higher on average in November than January for the years 1997–2004, in 2002 the UV-BR was significantly lower in November than in January (J. D. Turnbull, unpublished). The relatively low UV-BR early in the season may not have been sufficient to induce UV-screening compound production in B. pseudotriquetrum to the extent observed in years with more extreme ozone-hole events. It should also be noted that the study by Dunn & Robinson (2006) was carried out over a much longer period of the growing season (November–March) than the present study (November–early February) and thus encompassed a larger range of UV radiation than the present study, regardless of the size of the ozone hole.
The greater investment in cell wall-bound UV-screening compounds offers C. purpureus a more spatially uniform and potentially more effective UV screen, and could explain the high UV tolerance of C. purpureus compared with B. pseudotriquetrum. The Antarctic endemic S. antarctici has only half the combined pool of MeOH-soluble and alkali-extractable cell wall-bound UV screens of the two cosmopolitan species, consistent with the hypothesis that this species may be disadvantaged under continuing springtime ozone depletion. Our research suggests that cell wall-bound compounds are an important component of the UV defences in mosses and deserve further investigation.
Funding for this research was provided through Australian Antarctic Science grant no. 2542. Johanna Turnbull collected moss samples. Some of the data used within this paper were obtained from the Australian Antarctic Data Centre (IDN Node AMD/AU), which is part of the Australian Antarctic Division (Commonwealth of Australia). The data are described in the metadata record ‘Daily broad-band ultra-violet radiation observations using biologically effective UVR detectors’ Roy, C. & Gies, P. (2001, updated 2006). Laurence Clarke would like to acknowledge funding from an Australian Postgraduate Award. We thank members of the Plant Ecophysiology Lab at the University of Wollongong for comments on the manuscript.