Inhibited growth in a photosymbiont-bearing foraminifer Marginopora vertebralis from the nearshore Great Barrier Reef, Australia

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The following supplement accompanies the article Inhibited growth in a photosymbiont-bearing foraminifer Marginopora vertebralis from the nearshore Great Barrier Reef, Australia Claire E. Reymond 1, *, S. Uthicke 2, John M. Pandolfi 1 1 Centre for Marine Science, Australian Research Council Centre of Excellence for Coral Reef Studies, School of Biological Sciences, University of Queensland, Brisbane, Queensland 4072, Australia 2 Australian Institute of Marine Science, PMB No. 3, Townsville, Queensland 4810, Australia *Email: c.reymond@uq.edu.au Marine Ecology Progress Series 435:97 109 (2011) Supplement 1. Here we provide a compilation of the water quality data known for the Whitsunday region and the inshore Great Barrier Reef, with additional statistical notes from the Kruskal-Wallis test and laboratory design for this study Table S1. Water quality parameters known for the Proserpine and O Connell rivers, Great Barrier Reef, Australia Site Flow conditions n suspended solids (mg l 1 ) Particulate filterable organic Ammonia Nitrate + nitrite (µg N l 1 ) Particulate filterable organic Proserpine a Event 5 4 160 60 150 50 271 Proserpine b Wet season Max 18 1060 85 38 220 807 Proserpine b Wet season Median 18 940 41 20 180 183 Proserpine a Median 1 28 744 138 606 582 8 16 130 50 80 15 65 Proserpine a Ambient 1 5.6 4520 300 4220 2 3670 548 1570 180 1390 1261 129 O Connell b Wet season Max 8 450 56 56 90 31 O Connell b Wet season Median 8 420 33 12 60 14 O Connell c Max 11 478 1270 600 949 694 47 538 211 155 77 27 50 O Connell c Median 11 104 1020 241 668 393 9 310 139 71 52 9 41 O Connell c Ambient 1 1.6 201 81 120 113 2 5 22 9 13 11 2 a Faithful (2003); b Mitchell et al. (1991); c Rohde et al. (2006) reactive 1

Table S2. Mean chlorophyll a, dissolved inorganic phosphate and dissolved inorganic nitrate values from inshore reefs in the Whitsunday Islands, the whole Great Barrier Reef (GBR) and flood plume values for the central GBR. Means are presented ±SE Location Distance from river (km) Chl a (µg l 1 ) PO 4 (µg l 1 ) NO 3 (µg l 1 ) North Repulse Island a 17.6 0.88 ± 0.18 0.20 ± 0.02 0.21 ± 0.07 Calf Island a 42.6 0.86 ± 0.16 0.20 ± 0.02 0.19 ± 0.04 Pine Island a 45.4 0.83 ± 0.13 0.19 ± 0.02 0.19 ± 0.04 Long Island a 50.9 1.07 ± 0.22 0.19 ± 0.01 0.18 ± 0.03 North Molle Island a 63.0 1.21 ± 0.25 0.20 ± 0.03 0.26 ± 0.06 Armit Island a 86.2 0.40 ± 0.05 0.19 ± 0.02 0.15 ± 0.02 Double Cone Island a 80.6 0.31 ± 0.03 0.17 ± 0.01 0.19 ± 0.02 Flood plume average for 4.6 14.3 GBR b Ambient (non-flood) 0.4 0.02 average for GBR c Central GBR c Inshore 0.4 3 0.3 Central GBR c Mid shelf 0.3 3 0.4 Central GBR c Outer shelf 0.3 3 0.6 a van Woesik et al. (1999); b Devlin et al. (2001); c Furnas (2003) 2

Table S3. Summary of water quality variables measured in the water column at the 5 field experiment sites in the Whitsunday Islands during the dry winter and wet summer. Chl a: chlorophyll a; DIN: dissolved inorganic ; DIP: dissolved inorganic ; PN: particulate ; POC: particulate organic carbon; PP: particulate ; TDN: total dissolved ; TDP: total dissolved ; TSS: total suspended solids. Values are means ± SE Deloraine Edward Double Cone Daydream Pine 2008 dry winter DIP (µmol l 1 ) 0.16 ± 0.01 0.13 ± 0.01 0.16 ± 0.02 0.17 ± 0.02 0.16 ± 0.04 DIN (µmol l ) 1 0.16 0.11 0.13 ± 0.03 0.22 ± 0.01 0.18 ± 0.04 PP (µmol l 1 ) 0.06 ± 0.00 0.05 ± 0.00 0.07 ± 0.00 0.10 ± 0.00 0.10 ± 0.00 PN (µmol l 1 ) 0.84 ± 0.02 1.00 ± 0.11 1.17 ± 0.04 1.07 ± 0.15 1.28 ± 0.04 TDP (µmol l 1 ) 0.18 ± 0.002 0.18 ± 0.015 0.39 ± 0.022 0.22 ± 0.026 0.17 ± 0.028 TDN (µmol l 1 ) 4.21 ± 0.29 5.00 ± 1.10 4.87 ± 0.01 4.92 ± 0.32 5.11 ± 0.32 POC (µmol l 1 ) 10.10 ± 1.35 14.31 ± 0.68 10.47 ± 0.99 13.91 ± 1.40 16.51 ± 2.82 TSS (mg l 1 ) 1.84 ± 0.02 1.84 ± 0.08 2.65 ± 0.09 1.76 ± 0.15 3.71 ± 0.75 Chl a (µg l 1 ) 0.34 ± 0.03 0.34 ± 0.01 0.35 ± 0.01 0.48 ± 0.01 0.46 ± 0.05 2009 wet summer DIP (µmol l 1 ) 0.10 ± 0.01 0.12 ± 0.01 0.11 ± 0.00 0.14 ± 0.02 0.17 ± 0.03 DIN (µmol l 1 ) 0.24 0.31 ± 0.12 0.39 ± 0.12 0.88 0.92 PP (µmol l 1 ) 0.07 ± 0.00 0.09 ± 0.01 0.13 ± 0.00 0.17 ± 0.00 0.33 ± 0.00 PN (µmol l 1 ) 1.22 ± 0.16 1.98 ± 0.98 1.46 ± 0.06 1.26 ± 0.05 2.02 ± 0.20 TDP (µmol l 1 ) 0.18 ± 0.00 0.18 ± 0.01 0.39 ± 0.02 0.22 ± 0.03 0.17 ± 0.03 TDN (µmol l 1 ) 9.82 ± 0.59 10.11 ± 2.83 6.81 ± 1.04 10.47 ± 0.00 10.04 ± 0.38 POC (µmol l 1 ) 13.70 ± 1.98 7.82 ± 0.29 17.63 ± 0.15 14.22 ± 0.14 23.59 ± 0.15 TSS (mg l 1 ) 0.78 ± 0.04 1.95 ± 0.01 3.14 ± 0.015 6.8 17.5 ± 0.08 Chl a (µg l 1 ) 0.73 ± 0.02 0.56 ± 0.04 1.29 ± 0.04 0.63 ± 0.04 0.72 ± 0.01 3

Table S4. Results (p-values) of Tukey s HSD post hoc pairwise comparisons following a Kruskal-Wallis non-parametric test (H 15 = 186.4881, p < 0.001, n = 309). Pairwise comparisons are based on ranking the 1-way ANOVA. DW: dry winter; WS: wet summer; DIN: dissolved inorganic ; DIP: dissolved inorganic phosphate; Ambient: ambient nutrient concentrations. Bold numbers indicate significant pairwise comparisons (p < 0.05) (1) (2) (3) (4) (5) (6) (7) (8) (9) (10) (11) (12) (13) (14) (15) (1) Deloraine DW (2) Edward DW 1.000 (3) Daydream DW 0.502 0.485 (4) Double Cone DW <0.001 <0.001 0.091 (5) Pine DW 0.002 0.002 1.000 1.000 (6) Deloraine WS 1.000 1.000 1.000 <0.001 0.020 (7) Edward WS 1.000 1.000 1.000 0.008 1.000 1.000 (8) Daydream WS 0.032 0.034 1.000 0.892 1.000 0.234 1.000 (9) Double Cone WS <0.001 <0.001 0.030 1.000 1.000 <0.001 0.002 0.361 (10) Pine WS <0.001 <0.001 0.020 1.000 1.000 <0.001 0.001 0.254 1.000 (11) Ambient 22 C 1.000 1.000 1.000 0.001 <0.001 1.000 1.000 1.000 <0.001 <0.001 (12) DIP 22 C <0.001 <0.001 0.805 1.000 1.000 <0.001 0.007 0.805 1.000 1.000 0.001 (13) DIN 22 C 0.001 0.001 1.000 1.000 1.000 0.011 1.000 1.000 1.000 1.000 1.000 1.000 (14) Ambient 28 C 1.000 1.000 1.000 0.036 1.000 1.000 1.000 1.000 0.012 0.008 1.000 0.031 1.000 (15) DIP 28 C <0.001 <0.001 0.028 1.000 0.299 <0.001 <0.001 0.028 1.000 1.000 0.001 1.000 0.473 0.001 (16) DIN 28 C <0.001 <0.001 1.000 1.000 1.000 <0.001 0.034 1.000 1.000 1.000 0.005 1.000 1.000 0.115 1.000 4

Fig. S1. Experimental setup of the laboratory trial testing the effects of temperature and nutrient concentration in the water on foraminiferal growth. A: Ambient seawater; N+: 2 µm addition of potassium nitrate (KNO 3 ); P+: 0.2 µm potassium dihydrogen phosphate (KH 2 PO 4 ). Circles represent 500 ml cylinders containing 5 Marginopora vertebralis each LITERATURE CITED Devlin MJ, Waterhouse J, Taylor J, Brodie J (2001) Flood plumes in the Great Barrier Reef: spatial and temporal patterns in composition and distribution. Great Barrier Reef Marine Park Authority, Townsville Faithful J (2003) Water quality in the Whitsunday Rivers catchments. James Cook University, Townsville Furnas MJ (2003) Catchments and corals: terrestrial runoff to the Great Barrier Reef. Australian Institute of Marine Science & CRC Reef Research Centre, Townsville Mitchell A, Rasmussen C, Blake S, Congdon R, Reghenzani J, Saffinga P, Sturmey H (1991) Nutrient concentrations and fluxes in north Queensland coastal rivers and streams. In: Yellowlees D (ed) Land use patterns and nutrient loading of the Great Barrier Reef region. James Cook University Press, Townsville, p 108 161 Rohde K, Masters B, Brodie J, Faithful J, Noble R, Carroll C (2006) Fresh and marine water quality in the Mackay Whitsunday region 2004/2005. Mackay Whitsunday Natural Resource Management Group, Mackay van Woesik R, Tomascik T, Blake S (1999) Coral assemblages and physico-chemical characteristics of the Whitsunday Islands: evidence of recent community changes. Mar Freshw Res 50:427 440 5