Interactive effects of ocean acidification and declining water quality on tropical seagrass physiology

Primary productivity is the conversion of inorganic carbon into structural and nonstructural carbon (growth and storage) and is thereby the basis of the ecosystem services provided by seagrass meadows. These services include provision of habitat, carbon sequestration, stabilisation and trapping of sediments as well as food for invertebrates, fish, and mega herbivores. Increased carbon dioxide (CO2) dissolved in seawater (ocean acidification, OA) can enable seagrass productivity to increase even though they also use HCO3 as an alternate form of dissolved inorganic carbon (DIC) However, productivity responses to increasing pCO2 might be affected by other environmental factors that influence metabolic processes, such as water temperature and local water quality. The lack of empirical evidence for interactive effects of OA and localized impacts (e.g. light, nutrients) hampers our ability to factor these into predictive models and into coastal management decision making processes. Therefore, in this thesis I aimed to investigate the physiological responses of tropical Great Barrier Reef (GBR) seagrass species to increasing pCO2 (simulating OA) temperature, and key water quality parameters. In an initial experiment (Chapter 2) productivity and growth responses of common tropical seagrass species, Cymodocea serrulata, Halodule uninervis and Thalassia hemprichii, to CO2 enrichment were quantified. The seagrasses were exposed for two weeks to pCO2 levels (442 1204 matm) approximating the range of end of century emission scenarios. Net productivity and carbon budgets (PG:R) significantly increased with a rise in pCO2 in all three species. The degree of productivity rise with pCO2 was similar across species. While increased productivity in H. uninervis and T. hemprichii resulted in faster growth from CO2 enrichment, this was not the case for C. serrulata. Varying carbon allocation strategies among species might have contributed to observed differences in growth responses and so internal carbon allocation was further explored in a later experiment (Chapter 5) When light availability is reduced from declining water quality (e.g. land run off) preference for utilisation of the DIC species (CO2 vs HCO3 and therefore response to increasing pCO2, might be affected. To test this, C. serrulata and H. uninervis were exposed to two DIC concentrations (447 and 1077 matm pCO2) and three light treatments (35, 100 and 380 mmol m 2 s 1) for two weeks (Chapter 3) DIC uptake mechanisms were separately examined by measuring net photosynthetic rates while subjecting C. serrulata and H. uninervis to changes in light and addition of bicarbonate (HCO3 use inhibitor (carbonic anhydrase inhibitor, acetazolamide) and TRIS buffer (pH 8.0) DIC enrichment stimulated maximum photosynthetic rates (Pmax) more in C. serrulata grown under lower light levels (36 60% increase) than for those in high light (4% increase) (DIC x light: P 0.049) This was due to C. serrulata's greater dependence on CO2 in low light. However, this increase due to DIC did not compensate for low light, as net productivity of DIC enriched plants at low light was 85 208 lower than non DIC enriched plants growing under high light. In contrast, photosynthetic responses in H. uninervis increased with higher light and were independent of the concentrations of the DIC substrates available. H. uninervis has more flexible HCO3 uptake pathways. Light availability strongly affected productivity and also influenced productivity responses to DIC enrichment, via both carbon fixation and acquisition processes. Nitrogen availability can limit productivity responses to OA, since nitrogenderived metabolites are required for carbon assimilation. In Chapter 4, the hypothesis that CO2 and nitrate enrichment can have additive effects on seagrass productivity and biomass was tested. Nitrogen uptake and assimilation, photosynthesis, growth, and carbon allocation responses of H. uninervis and T. hemprichii to OA scenarios (428, 734 and 1213 matm pCO2) under two nutrient levels (0.3 and 1.9 mM NO3 approximating average GBR flood plume levels) were measured. Net productivity (53 78 and growth (18 52 in H. uninervis increased with CO2 enrichment (P 0.05) but were not affected by nitrate enrichment. T. hemprichii did not show significant changes with pCO2 or nitrate by the end of the experiment (24 days) in net productivity and growth. There was no evidence that nitrogen demand increased with pCO2 enrichment in either species. Overall, nutrient increases to levels approximating flood plumes levels in the GBR only had small effects on seagrass metabolism, and high tissue nutrient concentrations (2.53 2.75 %N) suggest that only small responses occurred because they were not nutrient limited. Changes in ambient growth temperature can modulate seagrass response to OA by affecting assimilation and utilization of CO2. Yet the combined effects of temperature and CO2 enrichment on seagrass carbon metabolism are not known. In Chapter 5, C. serrulata and H. uninervis were exposed to three temperatures (20degC, 25degC and 30degC, spanning seasonal variation) and three target pCO2 levels (present day 353 485 matm; high 915 1102 matm; extreme 1658 2297 matm) for seven weeks. Net productivity, biomass allocation and enzyme activity as a proxy for carbon translocation (sucrosephosphate synthase SPS and sucrose synthase SS) were measured. Net productivity in C. serrulata and H. uninervis increased by 109 and 197 (P 0.001) over the 10oC rise (20 30oC) respectively. In addition, temperature rise stimulated the increase of aboveground biomass in C. serrulata (26 35 P 0.012) and H. uninervis (42 88 P 0.006) Differences in the allocation of fixed carbon in response to temperature were evident. At warmer temperatures (where net productivity was highest) C. serrulata exported more carbohydrates to its rhizomes, while H. uninervis increased shoot density. In comparison, responses to CO2 enrichment were limited to C. serrulata increasing above to below ground ratio (P 0.003) and H. uninervis increasing net productivity the least at 30oC (pCO2 x temperature: P 0.047) This study highlights that temperature exerts a much stronger control over carbon metabolism than CO2 enrichment in tropical seagrasses. In summary, the effects of OA on seagrass physiology varied with light availability and water temperature. Ocean acidification cannot fully compensate for productivity losses caused by reduced light. Nitrate fertilization did not enhance seagrass productivity responses to CO2 enrichment, but it might have indirect impacts encouraging the growth of algae, which can thrive in nutrient and CO2 enriched conditions. An overall analysis (Chapter 6) of results from all chapters suggests that nutrient status (leaf N content) might be a strong determinant of CO2 responses, as C. serrulata and H. uninervis increased productivity at high pCO2 when their tissue nutrient concentrations were elevated, but not at low tissue nutrient concentrations. Species specific responses to OA and environmental parameters were consistently demonstrated, warning against the generalisation of responses across seagrass species. Overall, seagrass productivity can increase under OA, which is likely to make them future "winners" (sensu. Fabricius et al 2011) among tropical marine habitats; however localised conditions will affect their response and many of these remain untested.