VERSITET Mustafa Mantikci, Stiig Markager, Jørgen Hansen AARHUS UNIVERSITET DEPARTMENT OF BIOSCIENCE Liege, Belgium UNI The ratio of dark respiration to.

Slides:



Advertisements
Similar presentations
NCP ( mmol O 2 m -2 d -1 ) BP (mmol C m 2 d -1 ) NET ECOSYSTEM METABOLISM IN THE NW IBERIAN UPWELLING SYSTEM ON AN ANNUAL CYCLE C.G.Castro, Arbones B,
Advertisements

Long term mesozooplankton changes in coastal waters of North Spain Ricardo González-Gil F. González-Taboada, J. Höfer, R. Anadón University of Oviedo Department.
Zuchuan Li, Nicolas Cassar Division of Earth and Ocean Sciences Nicholas School of the Environment Duke University Estimation of Net Community Production.
A Recipe for Ocean Productivity, with Variations John Marra Lamont-Doherty Earth Observatory Palisades, NY USA.
JC068 Phytoplankton: Concentrations, Species, and Physiological Status UK-GEOTRACES: Ocean Micronutrient Cycles WP5: Biological responses and cycling of.
Assimilation Numbers?? Phytoplankton Absorption: a Strong Predictor of Primary Productivity in the Surface Ocean Or: Throw Away that Lab Fluorometer John.
IMPACTS OF DISSOLVED ORGANIC NITROGEN LOADING BY SUBMARINE GROUNDWATER DISCHARGE IN LITTLE LAGOON, AL JENNIFER ANDERS 1,2, BEHZAD MORTAZAVI 1,2, JUSTIN.
Environmental control on phytoplankton size-fractionated primary production in the tropical and subtropical Atlantic, Indian and Pacific oceans The 45.
Bacteria-Phytoplankton Competition Overview : Bacterial immobilization or remineralization of N. Competition between bacteria and phytoplankton for DIN.
WP12. Hindcast and scenario studies on coastal-shelf climate and ecosystem variability and change Why? (in addition to the call text) Need to relate “today’s”
Primary production and community structure response to deep seawater enrichment Karin Björkman, PhD OTEC/SWAC meeting 16 September 2011.
Water column structure and zooplankton distribution along Trevor Channel, Barkley Sound Andrew Hamilton.
Problem Description: Networked Aquatic Microbial Observing System (NAMOS) Problem Description: Networked Aquatic Microbial Observing System (NAMOS) Proposed.
Foodweb support for the threatened Delta smelt: Phytoplankton production within the low salinity zone Ulrika Lidström 1, Anne Slaughter 1, Risa Cohen 2,
Hawaii Ocean Time-series (HOT) program Marine Microplankton Ecology
MAREN MOLTKE LYNGSGAARD UNIVERSITY OF COPENHAGEN 1 Maren Moltke Lyngsgaard Marine biologist from Aarhus University PhD Project: Climate change impacts.
“The open ocean is a biological desert.”. Primary Production Global chlorophyll concentrations for Oct
OC211(OA211) Phytoplankton & Primary Production Dr Purdie SOC (566/18) LECTURE 6 Week 6 (i) Photosynthesis & Light (ii) Critical.
OSMOSIS Primary Production from Seagliders April-September 2013 Victoria Hemsley, Stuart Painter, Adrian Martin, Tim Smyth, Eleanor Frajka-Williams.
10 Productivity and Food Webs in the Sea Notes for Marine Biology: Function, Biodiversity, Ecology By Jeffrey S. Levinton ©Jeffrey S. Levinton 2001.
Organic Matter Metabolism in a Coastal Ocean Ecosystem Patricia Matrai Mike Sieracki Nicole Poulton Carlton Rauschenberg Bigelow Laboratory for Ocean Sciences.
Plankton and Productivity
Open Oceans: Pelagic Ecosystems II
Physical effects on plankton and productivity on the Faroe Plateau E. Gaard, B. Hansen, S. K. Eliasen and K. M. H. Larsen Faroese Fisheries Laboratory.
IB 362 Lecture 12 Productivity and Food Webs.
Trait-based representation of diatom diversity in a Plankton Functional Type model N. T ERSELEER 1, J. B RUGGEMAN 2, C. L ANCELOT 1 AND N. G YPENS 1 1.
SeaHARRE-3 : the third SeaWiFS HPLC Analysis Round Robin Exercise History 2 previous SeaHARRE exercises, coordinated by S. Hooker (NASA) and LOV:  1999:
Analysis of environmental variables and fouling organisms on an experimental artificial reef area of Daya Bay Chen haigang South China Sea Fisheries Institute,
SEASONAL CHANGES IN BENTHIC FLUXES AND NET ECOSYSTEM METABOLISM IN THE RIA DE VIGO (NW SPAIN) F. Alonso-Pérez, Carmen G. Castro, Zuñiga, D., B. Arbones.
Stratification on the Eastern Bering Sea Shelf, Revisited C. Ladd 1, G. Hunt 2, F. Mueter 3, C. Mordy 2, and P. Stabeno 1 1 Pacific Marine Environmental.
National Environmental Research Institute Denmark Temperature sensitivity of organic matter degradation Jørgen Bendtsen National Environmental Research.
Review –Seasonal cycle –spatial variation Food web and microbial loop Eutrophic vs. Oligotrophic food webs Biological pump.
From Ocean Sciences at the Bedford Institute of Oceanography Temperature – Salinity for the Northwest.
Backscattering Lab Julia Uitz Pauline Stephen Wayne Slade Eric Rehm.
45 th Liège Colloquium May 13 – 17, 2013 Fabian Große 1 *, Johannes Pätsch 2 and Jan O. Backhaus 2 1 Research Group Scientific Computing, Department of.
Biotic controls on microbial communities in estuarine and riverine habitats Trisha Pascal-Lopez Microbial Ecology Lab, Mentors: Rima Franklin, Ph.D, and.
Basin Scale Variability and Photoreactivity of Chromophoric Dissolved Organic Matter Jenna Robinson 1, Rob Upstill-Goddard 1 & Guenther Uher 1 : Carol.
Significant year-round effect of small mixotrophic flagellates on bacterioplankton in an oligotrophic coastal system Speaker: Chen wei hung.
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.
Sensing primary production from ocean color: Puzzle pieces and their status ZhongPing Lee University of Massachusetts Boston.
13-17 May th Liege Colloquium 1 Ocean Productivity: A Personal Perspective John Marra Brooklyn College, City University of New York.
1 Dynamics of nutrients in the Gdańsk Gulf; numerical simulations.
6 June 2011ACE workshop 1 Ocean Productivity: Concepts and Measurements John Marra Brooklyn College, CUNY.
*Minagawa M, Usui T, Miura Y, Nagao S, Irino T, Kudo I, and Suzuki K, Graduate School of Environmental Science, Hokkaido University, Sapporo ,
PATTREN OF PRIMARY PRODUCTION
Chapter 3 Part 2. Do Now 1) What is a thermocline 2) How does the graph look? (where are the axis and how are they labeled?) 3) What information do we.
Jamboree, October 19-22, 2015, Oostende, Belgium Nutrients in the Danish part of the North Sea EMODnet Chemistry Martin M. Larsen & Jonas K. Rømer, Aarhus.
THE FOOD WEB DO NOW: What do you think is the most important
Doney, 2006 Nature 444: Behrenfeld et al., 2006 Nature 444: The changing ocean – Labrador Sea Ecosystem perspective.
Potomac River Monitoring Programs R. Christian Jones and Donald P. Kelso Department of Environmental Science and Policy George Mason University.
Carbon-Based Net Primary Production and Phytoplankton Growth Rates from Ocean Color Measurements Toby K. Westberry 1, Mike J. Behrenfeld 1 Emmanuel Boss.
Phytoplankton seasonal dynamics in a Mediterranean coastal lagoon: emphasis on the picoeukaryote community JOURNAL OF PLANKTON RESEARCH VOLUME 27, NUMBER.
OEAS 604: Final Exam Tuesday, 8 December 8:30 – 11:30 pm Room 3200, Research Innovation Building I Exam is cumulative Questions similar to quizzes with.
The Impact of Nutrients on Picophytoplankton Populations Along the Atlantic Coast Melinda Norris and Dr. Jessica Nolan Conclusions  The phytoplankton.
Change Detection in Nutrients, Chlorophyll, Phytoplankton Composition and Primary Production Terry E. Whitledge and Sang H. Lee Institute of Marine Science,
Picoplankton Community Structure subarctic (K2) v.s. subtropical (Aloha similar) Nianzhi (George) Jiao,
Daoxun Sun Outline Background Data Technical details Result EOF of chlorophyll data Correlation with possible factors Summary.
Chapter 13 Biological Productivity and Energy Transfer
Food web and microbial loop Eutrophic vs. Oligotrophic food webs
Food web and microbial loop Eutrophic vs. Oligotrophic food webs
Meghan Hartwick, Cheryl Whistler, Erin Urquhart
Puget Sound Oceanography
Project coordinators: IOC-UNESCO & INGV
PHYTOPLANKTON GROWTH RATES AND CARBON BIOMASS FROM SPACE
NZOTS-STM and –SAM STM = Subtropical (macronutrient-limited); SAM = Subantarctic (micronutrient-limited) Moorings deployed October 2000-May 2012, ~3000.
Food web and microbial loop Eutrophic vs. Oligotrophic food webs
Department of Oceanography Sung-Chan Kang
Institute of Marine Science, University of Alaska Fairbanks
Typology and classification of coastal waters in Estonia
On Friday, Sep. 20 there is NO class/recitation.
Presentation transcript:

VERSITET Mustafa Mantikci, Stiig Markager, Jørgen Hansen AARHUS UNIVERSITET DEPARTMENT OF BIOSCIENCE Liege, Belgium UNI The ratio of dark respiration to maximum photosynthesis and seasonal variability in two marine coastal waters

VERSITET Mustafa Mantikci, Stiig Markager, Jørgen Hansen AARHUS UNIVERSITET DEPARTMENT OF BIOSCIENCE Liege, Belgium UNI Seasonal variations in respiration and relationships to production and temperature

You can’t know production without Respiration… John Marra, 2013

Who respires? Robinson & Williams,2005 >95% Community Respiration

Unknown Respiration BacteriaPhytoplankton Light Size fractionation-antibiotics

‘Global’ database of Respiration Robinson & Williams, %6% 14 C PP45 th Liege Colloquium Presentations

Great Belt North sea Baltic sea Roskilde fjord monthly sampling (12 total ) (1 m & 200µM) 24 CTD profiles in 2012 Study site

14 C samples (12 light + 2 dark) Dark Incubator 2 hours Linear Light Incubator 12h Respiration samples r 2 =0.997 Experimental setup

Results / CTD Profiles GBRF

Chlorophyll a GBRF

Community Respiration (CR) GBRF

P max - P max B GB RF

Q 10 Index r 2 = 0.38 r 2 = 0.32 r 2 = 0.72 r 2 = 0.88 GBRF Lomas et al., 2002

R / P max % indicator of the trophic balance of the plankton community (Irriarte et al., 1991) GB RF

% BR as a function of Chl-a GFF filtered (Sachia et al.,unpublished)

Photosynthetic parameters r 2 = 0.19 r 2 = 0.46 r 2 = 0.53 p< Webb et al, Markager et al., 1999

Bacterial abundance and POC r 2 = 0.45r 2 = 0.42

Respiration model r 2 = 0.83 p< 0.001

Take home messages Phytoplankton biomass and temperature are the main factors governing community respiration Bacteria become relatively more important in open coastal waters with lower phytoplankton biomass If you measure PP don’t forget to measure R Mustafa

NCP GB-mixed layer RF (gC m -2 y -1 )GBRF  PP  CR  NCP  NCP NCP 1 = GPP(PP) – CR (R a +R h ) NCP 2 = PP-R a light - R a dark -R h

Depth integration of PP and CR

Photosynthetic rates (mg C m 3 h -1 ) P est alpha P EKEK c P max =P est + c E Webb, Markager et al., 1999

Respiration rates (µmol O 2 L -1 h -1 ) oxy(y) t