JC068 Phytoplankton: Concentrations, Species, and Physiological Status UK-GEOTRACES: Ocean Micronutrient Cycles WP5: Biological responses and cycling of.

Slides:



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

PICODIV RED SEA ANALYSIS Some details of the area: i) continental shelf: 10 m from shore the seafloor drops sharply at station A the depth is 700 m. Can.

Vertical Distribution of Photosynthetic Pigments in Bamfield Inlet and Trevor Channel Ashlee Lillis Eosc 473.
First results of the NAOS project: Analysis of the interactions between mixed layer depth, nitrate and chlorophyll during a spring bloom event in the North-Western.
A Recipe for Ocean Productivity, with Variations John Marra Lamont-Doherty Earth Observatory Palisades, NY USA.
Mixed layer depth variability and phytoplankton phenology in the Mediterranean Sea H. Lavigne 1, F. D’Ortenzio 1, M. Ribera d’Alcalà 2, H. Claustre 1 1.Laboratoire.
IMPACTS OF DISSOLVED ORGANIC NITROGEN LOADING BY SUBMARINE GROUNDWATER DISCHARGE IN LITTLE LAGOON, AL JENNIFER ANDERS 1,2, BEHZAD MORTAZAVI 1,2, JUSTIN.
2014 NETCARE AMUNDSEN CRUISE Ocean-Atmosphere Interactions Michel Gosselin University of Quebec at Rimouski Maurice Levasseur Laval University Highly qualified.
Job opportunity Falkowski lab seeks aquarist/ undergraduate assistant for the coral lab! If interested, contact Frank Natale:
Problem Description: Networked Aquatic Microbial Observing System (NAMOS) Problem Description: Networked Aquatic Microbial Observing System (NAMOS) Proposed.
RU COOL Direct Broadcast Acquisitions L-band (1.2 meter antenna) United States NOAA POES AVHRR Product: 1km sea surface temperatures (SST), de-clouded.
Ocean Perturbation Experiment (OPEREX) CMORE Cruise, July 30 - August 14, 2008 Objective: To explore the potential and limitations of perturbation experiments.
Hawaii Ocean Time-series (HOT) program Marine Microplankton Ecology
Microbial Processes and Material Flow in Ocean Ecosystems.
“The open ocean is a biological desert.”. Primary Production Global chlorophyll concentrations for Oct
Ryan R. Rykaczewski -OSU Hatfield Marine Science Center Cooperative Institute for Marine Resources Studies -NOAA Geophysical Fluid Dynamics Laboratory.
Primary Production. Production: Formation of Organic Matter Autotrophic Organisms (Plants, algae and some bacteria) –Photosynthesis –Chemosynthesis CO.
Physical Controls on Phytoplankton Would you expect a fall bloom of phytoplankton? What would end it?
Monthly Composites of Sea Surface Temperature and Ocean Chlorophyll Concentrations These maps were created by Jennifer Bosch by averaging all the data.
Prof. Heidi Fuchs
2nd Reminder: Midterm 1 is this Friday February 1st Midterm 1 is 15% of your final grade Midterm 1 is 15% of your final grade It covers all lectures through.
Janelle Fleming Interdisciplinary Seminar September 16, 1998 The North Pacific Ocean event: A unique climate shift, natural decadal variability,
Open Oceans: Pelagic Ecosystems II
FIGURE 4.1 (a) Surface temperature (°C) of the oceans in winter (January, February, March north of the equator; July, August, September south of the equator)
State of the Oceans Portfolio Committee 13 February 2013.
Phytoplankton Bio-optics: Absorption, Pigments, Biomass Phytoplankton Bio-optics: Absorption, Pigments, Biomass Homework: Chapter 2 in your reader: C.
Phytoplankton: Nutrients and Growth. Outline Growth Nutrients Limitation Physiology Kinetics Redfield Ratio Critical Depth.
IB 362 Lecture 12 Productivity and Food Webs.
Remote Sensing & Satellite Research Group
Our Backyard Waterways: Predicting a Phytoplankton Bloom.
Review –Seasonal cycle –spatial variation Food web and microbial loop Eutrophic vs. Oligotrophic food webs Biological pump.
Prof. Heidi Fuchs Suggestions for getting an A How to deal with equations? –Don’t panic! –If you understand an equation, you.
The distribution of dissolved zinc in the South Atlantic as part of the UK GEOTRACES Programme UK GEOTRACES N. Wyatt 1, A. Milne 1, M. Woodward 2 G. Henderson.
Nature’s Density Column. Nature creates its own density column Example: The Bering Sea As you discovered in your experiment, when ice melts it forms a.
Ocean Color Products: The challenge of going from stocks to rates
Phytoplankton and nutrient dynamics in a vortex off Western Australia Paterson, H. L. 1, Waite, A. M. 1, Thompson, P. 2 1 The University of Western Australia,
International Workshop for GODAR WESTPAC Global Ocean Data Archeology and Rescue: Scientific Needs from the Carbon Cycle Study in the Ocean Toshiro Saino.
Marine Ecosystem Simulations in the Community Climate System Model
Doney, 2006 Nature 444: Behrenfeld et al., 2006 Nature 444: The changing ocean – Labrador Sea Ecosystem perspective.
ASSESSING BIODIVERSITY OF PHYTOPLANKTON COMMUNITIES FROM OPTICAL REMOTE SENSING Julia Uitz, Dariusz Stramski, and Rick A. Reynolds Scripps Institution.
Introduction As part of a study investigating phytoplankton diversity and physiology in the Western Pacific Warm Pool, we measured group-specific rates.
The Impact of Nutrients on Picophytoplankton Populations Along the Atlantic Coast Melinda Norris and Dr. Jessica Nolan Conclusions  The phytoplankton.
Coupling a Bio-Geo-Chemistry module to HYCOM within the NASA-GISS climate model Anastasia Romanou, Columbia U. and NASA-GISS Rainer Bleck, NASA-GISS Watson.
FIGURE 4.1 TALLEY Copyright © 2011 Elsevier Inc. All rights reserved (a) Surface temperature (°C) of the oceans in winter (January, February, March north.
Biology of mixed layer Primary production by Phytoplankton - small drifting organisms that photosynthesize Competition and limits on production Critical.
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
Primary Productivity.
Climate induced shifts in the phytoplankton community biomass
Primary Production and Satellite Remote Sensing
NASA’s Ocean Color Online Visualization and Analysis System
Time scales of physics vs. biology
Projected changes to the tropical Pacific Ocean
Projected changes to the tropical Pacific Ocean
SAB Chlorophyll Variability Local vs. Remote Forcing
Intro to Oceanography.
Climate change research in the Gulf of Alaska
NZOTS-STM and –SAM STM = Subtropical (macronutrient-limited); SAM = Subantarctic (micronutrient-limited) Moorings deployed October 2000-May 2012, ~3000.
The Chemical Connection Between Wind and Whales
Biology of mixed layer Primary production
Time scales of physics vs. biology
Food web and microbial loop Eutrophic vs. Oligotrophic food webs
Ocean Perturbation Experiment (OPEREX)
Projected changes to the tropical Pacific Ocean
Eutrophication indicators PSA & EUTRISK
Ocean Perturbation Experiment (OPEREX)
Projected changes to the tropical Pacific Ocean
Presentation transcript:

JC068 Phytoplankton: Concentrations, Species, and Physiological Status UK-GEOTRACES: Ocean Micronutrient Cycles WP5: Biological responses and cycling of micronutrients Tom Browning & Heather Bouman (Oxford) Mark Moore (NOCS)

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary NASA MODIS January 2012 SST Temperature (°C) Sea Surface Temperature JC068 CTD Temperature Depth (m) Temperature (°C) 30°S 40 °S 50°S 50°W 30 °W 10°W 10°E

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary Macronutrients Nitrate (µM) Phosphate (µM) Depth (m)

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary Chlorophyll Concentration (mg/m 3 ) NASA MODIS January 2012 Chlorophyll Phytoplankton Biomass JC068 Bottle Data: Chlorophyll Concentration Depth (m) Chlorophyll Concentration (mg/m 3 ) 30°S 40 °S 50°S 50°W 30 °W 10°W 10°E

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary JC068 D357 Chlorophyll Concentration (mg/m 3 ) Phytoplankton Biomass - Climatology NASA MODIS Chlorophyll, 9 km 2 resolution Month averaged

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary a ph (440)* (m 2 mg -1 ) Chlorophyll a-specific absorption at 440 nm: indicator of phytoplankton size Larger a ph (440)* = smaller cells Phytoplankton Absorption Samples run by Christian Utschig Depth (m)

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary Nanophytoplankton (2-20 µm) Picophytoplankton (0.2-2 µm) ProchlorococcusSynechococcus Total Bacteria Analytical Flow Cytometry Cell counts (cells/µL) Depth (m)

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary F v /F m : Thought to be influenced by phytoplankton species, light climate, micronutrients and macronutrients. F v /F m in JC068 transect, a signature of Fe limitation Phytoplankton Photophysiology F v /F m Depth (m)

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary ΔF v /F m = F v /F m Fe amended bottle – F v /F m Control bottle ControlFe addition (2 nM)Initial Immediate analysis24 hour incubation Fe incubation experiments

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary = Gough Island Two dominant regimes: 1) Subtropical Gyre type waters Low macronutrients Fe replete High irradiance (near surface) 2) AAC source waters High macronutrients Fe limited Possible light limitation

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary Chlorophyll Concentration (mg/m 3 ) Depth (m) A: Warmer, low macronutrients, stratified B: Colder, high macronutrients, deeper mixed layer Low surface chlorophyllHigher surface chlorophyll Dominated by smaller cellsDominated by large cells Fe repleteFe limited ABA Samples to be run: HPLC; microscopy; N-Fixers; DNA

Introduction Chlorophyll Cell Size Phytoplankton Types Fe Limitation Summary D357 Pre-bloom (leg 1) and bloom (leg 2) conditions Cause: shallowing of mixed layer = increased light Depressed mixed layer F v /F m = Fe limitation October – January: shift from Fe limited to macronutrient limited environment as bloom consumes macronutrients. 1 st LEG 2 nd LEG