1 SUPPLEMENTARY MATERIAL: EXTENDED METHODS 2 Title: Warming alters food web-driven changes in the CO2 flux of experimental pond 3 ecosystems 4 Experimental design 5 Using a 2 x 2 x 2 factorial design we manipulated temperature (+3˚ C), nutrients 6 (nitrogen and phosphorus), and presence of predators (Gasterosteus aculeatus) to test their 7 interactive and individual effects on consumer biomass, primary producer biomass, and 8 dissolved CO2 concentrations. Experiments were performed in 40, well mixed, open-air, 9 experimental ponds (surface area = 2.16 m2) located at the Experimental Pond Facility at the 10 University of British Columbia, Vancouver, Canada. Mesocosms were filled with 1,136 L of 11 municipal water and left to de-chlorinate for one week prior to the assembly of food webs. 12 Experimental food webs were assembled by inoculating mesocosms with ~20 13 zooplankton taxa, ~ 50 phytoplankton taxa, and microbes from nearby ponds[1]. Zooplankton 14 and phytoplankton were collected from nearby ponds using 64 µm-mesh conical tow nets. 15 Additionally, 1 L of sediment containing eggs, spores, and microbes was added from nearby 16 ponds to aid in community assembly. Aquatic insects naturally dispersing from adjacent 17 freshwaters colonized the mesocosms throughout the experiment. Food webs were left for three 18 weeks before the addition of experimental treatments. 19 Mesocosms were randomly assigned one of eight treatments and replicated five times. 20 Temperature manipulations, hereafter referred to as warming treatments, were achieved by 21 warming ponds to 3.04˚ ± 0.05˚ C (mean ± s.e.) above ambient pond temperatures using 300 W 22 submersible water heaters (Hagen, Montréal, Québec, Canada). A 3˚ C increase in ambient 23 temperature falls within the range of predicted temperature projections for Northern Hemisphere 24 temperate zones over the next 100 years [2]. Temperatures of all mesocosms were monitored 25 using HOBO Pendant data loggers (Onset Computer Corp. Bourne, Massachusetts, USA) in 30 26 min intervals. Mean water temperatures during May sampling for warmed and ambient 27 mesocosms were 19.4 ± 0.3 and 16.1± 0.3˚ C. Mean water temperatures during October 28 sampling for warmed and ambient mesocosms were 17.6 ± 0.8˚ C and 14.3 ± 0.7˚C, 29 respectively. We manipulated nutrients through monthly additions of 264 µg of nitrogen/L (as 30 NaNO3) and 27 µg of phosphorus/L (as (KH2PO4), resulting in a N:P molar ratio of 22 [1]. These 31 nutrient additions represent the top end of a meso-eutrophic state for Canadian lakes[3]. Five, 32 Three-Spined Stickleback (2.8 individuals m-2 of surface water) of 52.4 ± 0.05 mm in standard 33 body length were added per tank as predator treatments. The open nature of the tanks allowed a 34 small amount (5-10 leaves over the study period) of terrestrial leaf litter to accumulate in the 35 tanks. Stickleback densities were within range of natural densities (< 1 individuals m-2 to > 25 36 individuals m-2[4,5]). In the event of death, Stickleback were removed from the tank and 37 replaced with a similar-sized fish. Stickleback were used because they are generalist predators 38 that are found throughout freshwater ecosystems in British Columbia and have been documented 39 to exert strong top-down effects on plankton and benthic macroinvertebrates [6]. 40 41 42 Organism Sampling Consumers, primary producers, and in situ CO2 concentrations were measured on two 43 dates during the 2010 growing season (May and October), starting 336 d after the 44 implementation of experimental treatments. We chose these sampling date for three reasons: 1) 45 May represents the beginning and October represents the end of the primary growing season for 46 phytoplankton[1], 2) this time-frame encompasses the periods of maximum macroinvertebrate 47 abundance (i.e. prior to summer emergence and after summer oviposition), and 3) the potential 48 for surface waters to freeze was very low. Phytoplankton biomass was measured with in vivo 49 fluorometry (Trilogy, Turner Designs, Sunnyvale, California, USA) using the concentration of 50 chlorophyll a in the water column. Periphyton biomass was determined fluorometrically from 51 algal growth collected from 25 mm2 unglazed tiles. Zooplankton were collected using 10 L, 52 depth-integrated zooplankton samples, filtered through a 64 µm-mesh sieve. Phytoplankton 53 biomass and periphyton biomass were added together to get total primary producer biomass. 54 Spatial variation of zooplankton biomass within the ponds was minimized by pooling samples 55 from multiple depths and locations within the tank [1]. Zooplankton were identified (usually to 56 genus), counted, and measured under a 10x magnification. Biomass of zooplankton was 57 estimated using length-mass regressions [1]. Benthic macro-invertebrates were sampled by 58 summing together organisms collected from the bottom and walls of the tank. Macro- 59 invertebrates on the bottom of the ponds were sampled with standard sweeps within a 0.02 m2 60 cylinder, in two areas of the pond. Macro-invertebrates inhabiting the walls of the ponds were 61 collected by sweeping two locations of the wall from the bottom of the pond to the water’s 62 surface using a 12 cm, 0.5 mm-mesh net. Macro-invertebrates were identified and measured, and 63 their biomass calculated using length-mass regressions [7]. Biomass of both benthic and pelagic 64 consumers (not including G. aculeatus) were combined to estimate total consumer biomass. 65 Biomass was converted to g C m-2 for all organism groups by dividing grams of carbon 66 per tank by the tank surface area. Grams of carbon were estimated by assuming a carbon biomass 67 to chlorophyll biomass ratio of 1:40 for phytoplankton [8,9], 1:50 for periphyton [10], and an 68 average carbon content of 48% of dry mass for zooplankton [11] and 51.8% of ash-free dry mass 69 for benthic invertebrates [12]. 70 71 Statistical analyses 72 Standard errors represented in the graphs for each of the fixed effects within the model were 73 approximated using the “predictSE.lme()” function in the “AICcmodavg” package in R 3.1.1 (R 74 Development Core Team, 2014). This function calculates predicted values based on fixed 75 effects, and standard errors are approximated from the linear mixed effects model using the delta 76 method [13]. Calculating standard errors from the LME model has the advantage that error 77 assigned to random effects has been accounted for in the estimates. Table S1: Percent contribution of different taxonomic classes/orders and genus/family and total biomass for each of the eight treatments: control (C), nutrient addition only (N), addition of a zooplanktivorous predator (P), 3o C increase in temperature (W), nutrient + fish addition (NP), nutrient + warming addition (NW), predator + warming addition (PW), and nutrient + predator + warming addition. Class/Order Benthic Invertebrates Coleoptera Coleoptera Coleoptera Diptera Diptera Diptera Diptera Diptera Ephemeroptera Ephemeroptera Hemiptera Hemiptera Hirudinea Gastropoda Gastropoda Gastropoda Odonata Odonata Odonata Oligochaeta Trichoptera Genus/Family C P N W NP NW PW NPW Agabinae Hydrophilidae Hydroporinae Chironomini Chaoborus Ceratopogonidae Tanypodinae Orthocladiinae Callibaetis Caenis Notonecta Corixidae 0.0 0.0 0.0 9.4 5.6 5.3 0.5 0.0 6.9 0.2 5.2 0.4 4.9 2.3 2.2 0.0 28.0 13.9 0.0 7.5 7.9 0.0 0.0 0.0 8.7 0.0 29.2 2.7 0.4 0.0 0.0 13.9 0.8 0.0 0.0 7.3 0.0 0.0 0.0 0.0 1.0 36.1 0.0 0.0 0.0 9.6 0.6 14.1 7.3 0.1 22.0 0.0 8.2 0.8 0.0 10.7 7.1 4.9 0.0 3.3 9.0 1.4 1.0 0.0 0.0 0.0 4.2 0.0 3.4 0.0 0.7 0.2 0.3 7.3 0.1 0.0 0.0 1.9 0.0 0.0 80.4 0.0 0.1 1.3 0.0 0.0 0.0 28.8 0.0 35.7 3.9 0.2 0.0 0.0 0.2 0.0 0.0 0.0 19.0 0.0 0.0 0.0 0.0 3.6 8.7 0.0 0.0 0.0 1.1 0.4 0.7 0.3 0.0 0.5 0.0 4.1 1.8 0.0 7.9 0.6 6.0 0.4 75.2 0.0 1.0 0.0 0.0 15.5 0.0 3.9 0.0 0.7 3.7 0.1 0.0 0.0 0.0 0.0 0.0 0.0 1.1 0.0 0.0 74.5 0.0 0.5 0.0 0.1 0.0 0.0 5.4 0.0 6.6 0.9 0.0 0.6 0.0 0.0 0.0 0.0 10.3 4.0 0.0 0.0 66.1 0.0 5.3 0.6 Physa Menetus Lymnaea Aeshna Libellulidae Ishnura Leptoceridae Table S1 continued Zooplankton Chydoridae Chydoridae Cladocera Cladocera Calanoida Cyclopoida Ostracoda Monogononta Eurotifera Monogononta Eurotatoria Sididae Alona Chydorus Ceriodaphnia Daphnia Brachionus Keratella Lecane Monostyla Diaphanosoma 1.4 35.1 9.4 26.4 3.5 1.7 2.4 0.0 19.1 0.0 1.1 0.0 0.7 16.3 0.0 0.3 2.0 0.1 2.5 0.0 77.5 0.0 0.6 0.0 0.4 12.3 0.3 21.3 10.9 0.4 5.5 0.0 48.6 0.0 0.1 0.2 0.4 1.4 2.4 60.0 5.8 2.8 0.7 8.4 13.5 0.0 0.0 4.6 0.3 1.2 0.0 1.9 84.4 0.6 3.2 0.0 5.9 0.0 2.6 0.0 0.5 0.0 35.8 0.0 9.8 3.1 2.7 0.2 29.6 0.0 0.2 18.1 0.4 0.0 0.1 9.8 4.2 0.9 30.8 0.1 49.8 0.0 0.0 3.7 2.3 0.0 11.1 0.0 2.3 1.4 3.8 0.0 50.0 0.0 22.3 Table S2: Mean (± s.e.) for total consumer biomass, total primary producer biomass and CO2 flux for our eight treatments: control (C), nutrient addition only (N), addition of a zooplanktivorous predator (P), 3o C increase in temperature (W), nutrient + fish addition (NP), nutrient + warming addition (NW), predator + warming addition (PW), and nutrient + predator + warming addition. Treatment C N P W NP NW PW NPW Consumer biomass (g C m-2) 0.12 (0.03) 0.37 (0.08) 0.04 (0.01) 0.21 (0.11) 0.12 (0.04) 0.75 (0.15) 0.15 (0.07) 0.22 (0.10) Primary biomass (g C m-2) 0.37 (0.04) 1.35 (0.17) 0.49 (0.06) 0.23 (0.03) 10.05 (3.21) 0.73 (0.10) 0.43 (0.06) 0.98 (0.16) CO2 flux (mg C m-2 d-1) 14.34 (8.17) -50.33 (15.17) -61.45 (12.34) 8.14 (10.02) -86.52 (11.47) 10.13 (10.88) 11.41 (9.18) -23.89 (7.75) References 1. Kratina, P., Greig, H. S., Thompson, P. L., Carvalho-Pereira, T. S. A. & Shurin, J. B. 2012 Warming modifies trophic cascades and eutrophication in experimental freshwater communities. Ecology 93, 1421–30. 2. Stocker, T. F. et al. 2013 Technical summary. In Climate Change 2013: The physical science basis. Contribution of working group I to the fifth assessment report of the International Panel on Climate Change. Cambridge United Kingdom and New York USA: Cambridge University Press. 3. 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