Significant year-round effect of small mixotrophic flagellates on bacterioplankton in an oligotrophic coastal system Speaker: Chen wei hung.

Slides:



Advertisements
Similar presentations
Physico-chemical and biological characteristics of the Blanes site.
Advertisements

Primary Production measurements over a daily cycle in Clark’s Cove Ayan Chaudhuri, Lin Zhang, Anne-Marie Brunner MAR640 – Global Marine Biogeochemistry.
Contents 7.2 Applications of Percentage in Banking and 7.3 Time-series Graphs 7.4 Interpreting and Analysing Data Collected 7.1 Arithmetic and Geometric.
Michael J. Brayton MD/DE/DC Water Science Center Hydrologic Controls on Nutrient and Pesticide Transport through a Small Agricultural Watershed, Morgan.
Methane and Nitrous Oxide distributions in natural waters around Taiwan Hsiao-Chun Tseng, Chen-Tung Arthur Chen, Ting-Yu Chen *, Hung-Ling Chen,Meng-Chia.
Chapter18 Determining and Interpreting Associations Among Variables.
Hawaii Ocean Time-series (HOT) program Marine Microplankton Ecology
Isolation of Viruses Infecting Marine Bacteria Jennifer Yan Mentors: Dr. Stephen Giovannoni Dr. Mike Schwalbach Giovannoni Lab Department of Microbiology.
Grazing and Trophic Transfer Sam Rankin BOT 437 May 21, 2009.
Organic Matter Metabolism in a Coastal Ocean Ecosystem Patricia Matrai Mike Sieracki Nicole Poulton Carlton Rauschenberg Bigelow Laboratory for Ocean Sciences.
VERSITET Mustafa Mantikci, Stiig Markager, Jørgen Hansen AARHUS UNIVERSITET DEPARTMENT OF BIOSCIENCE Liege, Belgium UNI The ratio of dark respiration to.
Properties of Gas in Water Oxygen Sources and Sinks Oxygen Distribution (space & time) Measuring Dissolved Oxygen Measuring 1º Production and Respiration.
RECYCLING IN THE BIOSPHERE Biogeochemical Cycles: 1. water cycle 2. carbon cycle 3. nitrogen cycle 4. phosphorus.
Zooplankton Fall Plankton Holoplankton Meroplankton Plankton Classification.
ABSTRACT In situ and modeled water-column primary production (PPeu) were determined from seasonally IMECOCAL surveys and satellite data off Baja.
IB 362 Lecture 12 Productivity and Food Webs.
Effect of viruses on bacteria-mediated C and Fe cycling M.G. Weinbauer CNRS-UPMC, UMR 7093 Villefranche-sur-mer.
Introduction Oithona similis is the most abundant copepod in the Gulf of Alaska, and is a dominant in many ecosystems from the poles to the sub-tropics.
Introduction Introduction Picophytoplankton, phytoplankton 3µm and smaller in size, are the dominant photosynthesizers in the ocean. Thus picophytoplankton.
Aqua Case Mussel culture area- Chalastra Thessaloniki Exercise Environmental Impacts of mussel farming o n water quality. Amalia Moriki, Sofia Galinou-Mitsoudi,
Seawater Seawater is a solution of about 96.5% water and 3.5% dissolved salts. The most abundant salt in seawater is sodium chloride (NaCl). Most elements.
Bacterial production and factors limiting bacterial production BIOSOPE project France Van Wambeke LMGEM, Marseille Villefranche-sur-Mer, presentation 27/01/2004.
Bacterial production and Microsystin in Lake Taihu GUANG GAO Nanjing Institute of Geography & Limnology, CAS
Correlation Between Groundwater Level And Altitude Variations in Land Subsidence Area of The Choshuichi Alluvial Fan, Taiwan Chieh-Hung Chen, Chung-Ho.
Review –Seasonal cycle –spatial variation Food web and microbial loop Eutrophic vs. Oligotrophic food webs Biological pump.
Fig. 5 showed the ratio of DON:DOP in the TS. Different slopes and their corresponding locations were marked with the same color. The average ratio of.
Hamilton, S. K Water quality and movement in agricultural landscapes. Pages in S. K. Hamilton, J. E. Doll, and G. P. Robertson, editors.
Trawling for cephalopods off the Portuguese coast —Fleet dynamics and landings composition Reporter :林信宏 Fisheries Research 92 (2008) 180–188 Tereza Fonseca.
Arrigo (2005) Marine Microorganisms and Global Nutrient Cycles Nature 437: Issues: Redfield stoichiometry Co-limitation N 2 -Fixation Anammox.
Vertical distribution of ontogenetically migrating copepods in the Western Subarctic Gyre T. Kobari 1, D. K. Steinberg 2, S. Wilson 2, K. Buesseler 3,
1. Which part of your paper should you create first? Graphical Results.
Backscattering Lab Julia Uitz Pauline Stephen Wayne Slade Eric Rehm.
Temporal and Spatial Variation of air-sea CO 2 Fluxes in the West Coast of Baja California, Mexico J. Martín Hernández-Ayón 1,Ruben Lara-Lara 2, Francisco.
Xosé Anxelu G. Morán 1, Laura Díaz-Pérez 1, Enrique Nogueira 1 and Antonio Bode 2 1 Instituto Español de Oceanografía (IEO), Xixón, Spain 2 Instituto Español.
Microbial Pathways in the Sea What is the relative importance of bacteria and viruses in regulating the flow of energy and the cycling of nutrients in.
Seasonal variations in mean water column temperatures in the northern GOA (obtained from IMS GLOBEC website ). The temperature.
PATTREN OF PRIMARY PRODUCTION
Assessing the Influence of Decadal Climate Variability and Climate Change on Snowpacks in the Pacific Northwest JISAO/SMA Climate Impacts Group and the.
Remotely sensed spatial dynamics of the Illex argentinus fishery, Southwest Atlantic Claire M. Waluda ∗, Huw J. Griffiths, Paul G. Rodhouse Fisheries Research.
Nutrient Response of the Ventura River to Drought Conditions in Southern California Al Leydecker 1 and Jessica Altstatt 2 ( 1 Bren School of Environmental.
1 Federal Research Centre for Fisheries Institute for Sea Fisheries, Hamburg Hans-Joachim Rätz Josep Lloret Institut de Ciències del Mar, Barcelona Long-term.
Introduction As part of a study investigating phytoplankton diversity and physiology in the Western Pacific Warm Pool, we measured group-specific rates.
“the oceanography of lakes” Study of the functional relationships and productivity of freshwater communities, as they are regulated by the dynamics of.
The Impact of Nutrients on Picophytoplankton Populations Along the Atlantic Coast Melinda Norris and Dr. Jessica Nolan Conclusions  The phytoplankton.
Growth Rates of Euphausiids in the Northern Gulf of Alaska in A.I. Pinchuk *, R.R. Hopcroft, K.O. Coyle Institute of Marine Science, University.
Nutrients in sea water Introduction Distribution of Phosphorus and seasonal variation Distribution of nitrogen compounds Distribution of silicates and.
Solute transport in sediments Physical properties Transport: Diffusion “Irrigation” Advection.
Predation rates. From a trophic point of view, microzooplankton plays a fundamental role as principal carrier of energy from the primary producers to.
Dr. Yan GAO Institute of Agricultural Resources and Environment Water Management and Resources Utilization Research Group.
Food web and microbial loop Eutrophic vs. Oligotrophic food webs
Food web and microbial loop Eutrophic vs. Oligotrophic food webs
Suggestions for getting an A
Table 1. Linkages between emissions of SO2 and NOx and important environmental issues From: Acidic Deposition in the Northeastern.
Marine Bacterioplankton Seasonal Succession Dynamics
Table S1: Chemical analysis and bacterial abundance of ice meltwater from EME and DLE Lee et al, Supporting Online Material.
J.C.A. CEPEDA-MORALES1 and G. GAXIOLA-CASTRO2 RESULTS AND DISCUSSION
The Extent of Orthorhombic Lipid Phases in the Stratum Corneum Determines the Barrier Efficiency of Human Skin In Vivo  Fabienne Damien, Mila Boncheva 
Precision and Variability in Bacterial Temperature Sensing
Noninvasive Molecular Monitoring in Multiple Myeloma Patients Using Cell-Free Tumor DNA  Giulia Biancon, Silvia Gimondi, Antonio Vendramin, Cristiana.
Biology of mixed layer Primary production
Food web and microbial loop Eutrophic vs. Oligotrophic food webs
Critical and Compensation Depths Spring bloom and seasonal cycle
Volume 111, Issue 2, Pages (July 2016)
Volume 5, Issue 3, Pages (May 2012)
Magnitude of mRNA fold change is best predictor of mRNA-to-protein correlation. Magnitude of mRNA fold change is best predictor of mRNA-to-protein correlation.
Relationship Between NO3 and Salinity:
Dmitrii V. Vavilin, Esa Tyystjärvi, Eva-Mari Aro  Biophysical Journal 
E. Chapman-McQuiston, X.L. Wu  Biophysical Journal 
Probing the Dynamics of Clot-Bound Thrombin at Venous Shear Rates
Presentation transcript:

Significant year-round effect of small mixotrophic flagellates on bacterioplankton in an oligotrophic coastal system Speaker: Chen wei hung

Introduction Many flagellated protists in marine and freshwater environments are capable of a mixotrophic mode of nutrition. Mixotrophy, defined here as the combination of photosynthesis and particle grazing (sensu Sanders 1991) Mixotrophic flagellates can be found in marine and freshwater systems at about 10 2 cell mL -1 to 10 3 cell mL -1 (Sanders 1991). Havskum and Riemann (1996) calculated that mixotrophs were responsible for up to 86% of the total bacterial grazing in some coastal environments FLB Bacteria This was done with grazing experiments using fluorescently labeled bacteria (FLB) during an annual cycle in the coastal northwest Mediterranean Sea.

Material and method Study area and sampling Chl a and nutrient concentrations Blanes Bay on the Catalan coast (NW Mediterranean 41°40'N 2°48'E ). The sampling site is placed at about 800 m offshore and has a sandy bottom at around 20-m depth Soluble reactive phosphorus (SRP), nitrate, nitrite, ammonia, and silica concentrations—Chl a concentration was determined fluorimetrically according to Yentsch and Menzel (1963).

Bacteria and FLB abundance Bacterial production 4,6-diamidino-2-phenylindole (DAPI) SYTO-13 (Molecular Probes) Flow cytometry Epifluorescence microscopy Heterotrophic bacterial production (BP) was estimated from the rate of protein synthesis determined by the incorporation of 3H leucine into trichloroacetic acid (TCA)-insoluble macromolecular material. Preparation of tracer FLB were prepared from a Brevundimonas diminuta (syn. Pseudomonas diminuta) strain obtained from the Spanish Type Culture Collection (Burjassot,Vale`ncia).

Short-term grazing experiments Water sample 100-μm inverse filtration 4.5 L culture chamber 3 – 4 h temperature light 4.5 L add FLB 10 ~ 30 % T 0 T L fixed with glutaraldehyde (2%) filter 0.6μm Long-term grazing experiments ExperimentControl Only FLB

Model to estimate community grazing rates GT : community grazing rate T : temperature HF : heterotrophic flagellate abundance (flag. ml -1 ) N : bacterial abundance (bac. ml -1 ) Vaque´ et al. (1994)

Results Surface-water temperature between 11 ℃ and 25 ℃ SRP concentration between0.12 and 0.24 μmol L -1 maximum concentrations beginning of winter and beginning of spring Chl a concentration Annual mean light intensity in the mixed layer was, on average 275 μmol m -2 s -1. Photoperiod Bacterial abundance 5.6 × 10 5 –1.4 × 10 6 cell mL -1

Fig. 2. Temporal fluctuation in abundance (a, b), specific grazing rate (c, d), and grazing effect (e, f) of the four flagellate categories analyzed. Bars represent SE. Grey shaded area represents temperature as shown in Fig. 1. Secondary y-axis in panels b, d, and f correspond to HF 5–20 μm. Abundance Specific grazing rate Grazing effect PF and HF abundances were higher at the beginning of winter and at the beginning of spring 3–5 μ m PF 0.2 ~ 2.1 bact. ind. -1 h -1 5–20 μm PF 0.5 ~ 3.6 bact. ind. -1 h -1 Seasonal patterns were not evident for PF. HF presented a noticeable seasonality, with higher grazing activity during the warmer months the four groups showed the same three peaks: one during the summer and two more at the beginning of winter and at the beginning of spring

Averaging the data obtained in the annual survey, the SGRs of PF were considerably lower than those of HF The smallest flagellates ( 5 μm) always had a greater effect on bacterioplankton than the larger ones. Flagellate abundances presented the opposite trend, thus resulting in very similar grazing effects of the groups

19-61% Fig. 4. The proportion of total flagellate bacterivory, expressed as a percentage, contributed by each of the four groups of flagellates (a) throughout the year and (b) as average annual values. 4-24%28-58%3-13% 50% PF HF

Fig. 5. (a–d) Relationship between the SGR of each flagellate category and SRP concentration. When significant, regression equation and Pearson’s correlation coefficient are shown. Bars represent SE.

Fig. 6. (a) Grazing effect on bacterioplankton assessed by FLB disappearance, FLB ingestion, and applying the Model 1 (Eq. 8) proposed by Vaque´ et al. (1994) based on temperature, bacterial abundance, and HF abundance. (b) Relationship between total flagellate bacterivory estimated by ingestion of FLB and using Eq. 8. Dashed line indicates 1 : 1 relationship. Fig. 7. Relationship between total bacterivory assessed by FLB disappearance and bacterial production estimated with a standard conversion factor (open circles) or with empirical CFs (solid circles). Dashed line indicates 1 : 1 relationship.

Discussion Bacterial losses and production BP and total grazing assessed by FLB disappearance were in the same range and were similar to values found in other oligotrophic marine environments (Vaque´ et al. 1994; del Giorgio et al. 1996). Virus-induced mortality ? However, results obtained by Weinbauer and Peduzzi (1995) and Guixa-Boixereu et al. (1999) indicate that bacterial mortality caused by viral lysis does not seem to be very relevant in the oligotrophic northwestern Mediterranean. Relative grazing effect of the different flagellate types Despite a lower grazing rate per individual, a high number of,5- μ m flagellates resulted in a significantly higher grazing effect than 5–20- μ m HF Havskum and Hansen (1997) found a considerable grazing effect of 10–20- μ m phagotrophic protists on nanoplankton, but not on picoplankton.

Table 1. Percentage of total protist bacterivory accounted for by mixotrophic flagellates in different environments.*

Seasonality of the effect of mixotrophs Factors controlling the ingestion rates of the flagellates The relative effect exerted by mixotrophic flagellates on the bacterial community was rather constant throughout the year. In light of these past studies, our results could not yield a global estimation of the grazing effect of mixotrophs because we did not perform measurements during a light : dark cycle. The significantly negative correlation between SRP concentration and SGR within both PF groups indicates a tendency toward a decrease of their ingestion rates at higher SRP concentrations. We did not find any relationship between grazing rates and bacterial abundance. The mixotrophic strategy may be successful when resources (e.g., light or nutrients) are limiting (Rothhaupt 1996). A seasonal pattern in feeding activity of HF was evident in our study SGRs and clearance rates were slightly significantly correlated with water temperature. HF PF

Thanks for your attention