Jake Dittrich1, Kimberly Halsey2 BioResource Research 1, Department of Microbiology2 Oregon State University, Corvallis, Oregon Overview Introduction and Background Materials and Methods Results Discussion Conclusions Global Carbon Cycle •The world’s oceans are a major regulator of atmospheric carbon levels, sequestering up to a third of the anthropogenically produced carbon. The Marine Biological Pump Idealized schematic of the marine biological pump. Marine Net Primary Production Net Primary Production (NPP) Photosynthesis Accumulation of biomass Light Availability Nutrient Availability Nitrogen Nitrogen Limitation Much of the worlds oceans are nitrogen limited. Nitrogen limitation is predicted to increase. Decreasing mixed layer depth Nutrient cycling Seasonal phytoplankton blooms Biological pump Video credit NASA.gov/SeaWiFS Nitrogen limitation 30 10 0 Nitrate Nitrogen limitation effects NPP of cyanobacteria. Carbon cycling in the worlds oceans. Oceanic models of primary productivity. (mmol kg-1) 20 The Question No reasonably effective methods for measuring Net Primary Production (NPP) in the worlds oceans directly NPP = growth rate times cellular carbon. Chlorophyll a concentration (Chl) measured via remote satellite sensing. Chl then related to NPP through the Chl-specific carbon fixation rate (Pb) Carbon/Chl/Unit Time 12 10 6 Chl-specific carbon fixation NPP* Predicted 4 NPP* Alternative 8 2 0 0 0.2 0.4 0.6 0.8 Specific Growth rate (d-1) 1 Idealized schematic of the potential relationships between Pb and NPP*. Experimental Summary NPP* independent or dependent on nitrogen limited growth for Synechococcus WH8102. My research investigated the relationships between nitrogen limited specific growth rate, Chl-specific carbon fixation rates, and NPP*. Why Synechococcus WH8102? Motile Unknown No physical appendage 10-10 M nitrogen concentration Ubiquitous Second only to Prochlorococcus in abundance Synechococcus WH8102 cells are larger and grow faster Significant contributor to global marine primary production An Oligotrophic organism Nitrogen uptake A Little Bit of Scale Reference…… Synechococcus WH8102 Experimental Design 7 Chemostats 3 growth rates 0.2 day-1 0.5 day-1 1.0 day-1 Natural seawater Nitrogen limited 7 Generations Schematic of experimental setup for steady-state N-limited growth of Synechococcus WH8102. Chemostats Experimental Measurements Short term (20 min) 14 C uptake data. Pb Cellular Carbon and Nitrogen Elemental Analyzer Chlorophyll Concentration Spectrometry Steady-state N-limited cultures of Synechococcus WH8102 Statistical Analysis Linear regression, ANOVA Chl/ cell (femtograms/cell) Chlorophyll a per cell for Synechococcus WH8102 40 35 30 25 20 15 10 5 0 0 0.2 0.4 0.6 0.8 Specific growth rate (d-1) 1 1.2 Comparison of chlorophyll:carbon for three marine phytoplankton 35 30 Chl C-1 x 103 (µg µg-1) 25 20 Synechococcus WH8102 Dunaliella tertiolecta Thalassiosira weissflogiii 15 10 5 0 0 0.5 1 Specific Growth Rate (d-1) 1.5 Data for D. tertiolecta and T. weissflogi from Halsey et al. (2010); Halsey et al. (2013). Chl-specific production (µmol C (mg Chl*h)-1 Chlorophyll specific net primary production and carbon fixation for Synechococcus WH8102 350 300 250 200 150 100 NPP* 50 Pb 0 0 0.2 0.4 0.6 0.8 Specific Growth Rate (d-1) 1 C fixation (µmol C (mg Chl x h)-1 Photosynthesis irradiance curves for chl-specific 14C uptake data 350 300 250 200 150 100 0.2 50 0.5 1.0 0 0 500 1000 1500 Light intensity (µmol quanta m-2 x sec-1) 2000 Discussion Cyclic electron flow at Photosystem I Additional energy production Alternative forms of reduced nitrogen Unique form of motility Sodium Motive force Synechococcus WH8102 Chl cell-1 increased with increasing growth rate. Unique Motility Chl/ cell (femtograms/cell) Discussion 40 30 20 10 0 0 Nitrogen gradients 10-10 molar Sodium motive force Na+/H+ antiporters 0.5 1 Specific growth rate (d-1) Discussion Chl C-1 (µg µg-1) Chl:C strongly dependent on nitrogen limited PSI/PSII ΔChl:C growth rate for T. weissflogii 0.5 7.2 (0.86) D. tertiolecta 1 3.9 (0.74) Synechococcus WH8102 Synechococcus sp. 2 2.2 (0.25) PSI/PSII ratios 30 Previously studied organisms 20 10 0 0 Data for D. tertiolecta and T. weissflogi from Halsey et al. (2010); Halsey et al. (2013). 0.5 1 Specific Growth Rate (d-1) 1.5 Discussion Fast growth rate 1.0d-1 Slow growth rate 0.2d-1 Conclusions • Synechococcus WH8102 chl-specific net primary production is dependent on nitrogen limited growth rate. • Short term (20 min) chl-specific carbon fixation rates increased with increasing growth rate. • Pb cannot give estimates of NPP* • Pb, NPP* and growth rate, suggest a different strategy for carbon metabolism, pigment regulation, and photosynthetic energy utilization in Synechococcus WH8102. Cyclic electron flow at Photosystem I Uptake of alternative forms of reduced nitrogen Unique motility Acknowledgments Dr. Kimberly Halsey Dr. Michael Behrenfeld Dr. Peter Bottomley E.R. Jackman internship support program. Wanda Crannell Dr. Kate Field BioResources Research program Cyclic Flow PS II N/S reduction, direct utilization PS I Calvin cycle GAP PTOX Mehler TCA, OPP Storage Net growth