Patterns of Zooplankton Diel Vertical Migration in the Global Ocean Devika Balachandran K. Allison Smith August 12, 2011.

Slides:



Advertisements
Similar presentations
Offer Curves and terms of trade
Advertisements

By: David Tafoya Student Mentor: Pat Kelly. The Biological Pump is the process in which CO2 fixed in photosynthesis is transferred to the interior of.
Eddy-driven changes in phytoplankton community composition and biogeochemical cycling in the Sargasso Sea NASA A regional eddy-resolving carbon cycle model.
Continuous Plankton Recorder Database: current uses and future directions Darren Stevens & Anthony J. Richardson Sir Alister Hardy Foundation for Ocean.
Examining Lake Michigan Spring Euphotic Depth (Z eu ) Anomalies utilizing 10 years of MODIS-Aqua data at 4 kilometer resolution James G. Acker NASA GES.
Marine Habitats and Communities. Main Concepts – Marine Habitats  Physical environment where community of organisms live is called a habitat.  Combination.
Abstract As part of the VERTIGO project (VERtical Transport In the Global Ocean) we used Thorium-234 ( 234 Th) as a natural proxy for particle export.
Mt. Hood Community College Market Enhancement Study Student Body.
Water column structure and zooplankton distribution along Trevor Channel, Barkley Sound Andrew Hamilton.
Lecture 16 Oxygen distributions and ocean ventilation Thermocline Ventilation and Deep Water Formation Oxygen Utilization rates.
Maps Displaying Spatial Data. Why do we need maps? To locate places on the surface of the earth.
Unit 3 Understanding Maps.
Questions How do different methods of calculating LAI compare? Does varying Leaf mass per area (LMA) with height affect LAI estimates? LAI can be calculated.
Topic 14 Density Driven Currents
An Investigation of the Effect of Turbidity on the Diel Vertical Migration of Zooplankton in the Chincoteague Bay, VA. James Bergenti, Department of Biology,
Graphing. a. Circle graph (also called pie chart) Used to show parts of a fixed whole. Usually parts are labeled as percents with the circle representing.
Plankton and Productivity
Open Oceans: Pelagic Ecosystems II
Rates of Summertime Biological Productivity in the Beaufort Gyre: A Comparison between the Record-Low Ice Conditions of August 2012 and Typical Conditions.
How to Use Project Nestwatch Your (hopefully) helpful guide to Project NestWatch.
Heat Transfer in Earth’s Oceans WOW!, 3 meters of ocean water can hold as much energy as all other Earth Systems combined!
INFLUENCE OF HYPOXIA ON THE ECOLOGY OF ZOOPLANKTIVOROUS AND BENTHIVOROUS FISHES IN LAKE ERIE’S CENTRAL BASIN. T.O. Höök1,2,*, S.A. Ludsin2, S.A. Pothoven3,
Prince William Sound Resurrection Bay Knight Island Passage Middleton Island The physical model is run in three dimensions and the data are used to drive.
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.
RA-228 AND RA-226 FROFILES FROM THE NORTHERN SOUTH CHINA SEA Hsiu-Chuan Lin, Yu-Chia Chung and Chi-Ju Lin Institute of Marine Geology and Chemistry, National.
Reviewing the Basics! SKILLS TO KNOW. Bellringer  TURN IN YOUR QUESTIONS AND MAP NOW.  In your own words, explain the difference between absolute and.
Jen Zhao, Levin Lab. Host Organization and Project Princeton University LevLab Stockholm Resilience Center Goal: Inform policy.
Maps Displaying Spatial Data. Why do we need maps? To locate places on the surface of the earth.
Vertical distribution of ontogenetically migrating copepods in the Western Subarctic Gyre T. Kobari 1, D. K. Steinberg 2, S. Wilson 2, K. Buesseler 3,
Effects of increased dissolved organic matter on zooplankton vertical distribution in a UV-transparent lake: Results from large-scale mesocosms Sandra.
Regents Exam Review August 2011 Part B-2 to D. Base your answers to questions 44 through 47 on the data table below and on your knowledge of biology.
Accessing and using event data in the classroom Michael Hubenthal, IRIS Educational Specialist.
ACUTAL Regents Do Now: As a person travels due west across New York State, the altitude of Polaris will ① decrease ② increase ③ remain the same.
A Survey of Diel-Vertical Migration of Freshwater Zooplankton at Pinchot Lake Eric Holtzapple Department of Biological Sciences, York College of Pennsylvania.
WOCE hydrographic Atlas, 1 As a result of the World Ocean Circulation Experiment (WOCE), a hydrographic survey of the world oceans occurred from
Reconstituting the Ocean: a tale from U.S. JGOFS Cyndy Chandler (MCG, WHOI) U.S. JGOFS Data Management Office and Ocean Carbon and Biogeochemistry Coordination.
Figure. Seasonally migrating copepods appeared at Station K2. We can identify two groups of the copepods by the life cycle. Red: surface spawning species,
Open Oceans: Pelagic Ecosystems III. Comparing the makeup of water and plankton Mean Elemental Ratios of N, and P Organisms: 16.0N / 1P Sea Water: 14.7N.
The Five Themes of Geography A Framework for Studying the World North Carolina Geographic Alliance PowerPoint Presentations 2007.
USA TIME ZONES and of the world. APHG TEST REVIEW MULTIPLE CHOICE PORTION- FRIDAY Part One ESSAY – THURSDAY. Essay is over Nature’s Inequalities reading.
Tracking the fate of carbon in the ocean using thorium-234 Ken Buesseler Dept. of Marine Chemistry and Geochemistry Woods Hole Oceanographic Institution.
Sentinel Lakes 2008 Zooplankton Update. Field Sampling MPCA staff collected 363 zooplankton samples. All 24 lakes were sampled monthly from April/May.
1 Dynamics of nutrients in the Gdańsk Gulf; numerical simulations.
1 | Program Name or Ancillary Texteere.energy.gov Water Power Peer Review Assessment of Energy Production Potential from Tidal Streams in the United States.
Today’s Goals Answer questions about homework and lecture 2 Understand what a query is Understand how to create simple queries using Microsoft Access 2007.
Great Lakes Environmental Research Laboratory Review – Ann Arbor, MI November 15-19, Click to edit Master text styles –Second level Third level.
Puget Sound Oceanography 2009 Course overview. Geology of Puget Sound Started from Pangaea Plate movement, subduction zones, volcanoes and valleys Glaciation.
Mapping Volcanoes 15 February What are volcanoes? What causes them to occur?
MEDFLUX: Use of Amino Acid Degradation Indices to Examine Exchange Between Sinking and Suspended Particles Cindy Lee, Zhanfei Liu, Stuart Wakeham & Rob.
Spatial Sense Map Package. Mercator Projection Miller Projection.
Interpreting the sedimentary record
Global Biogeochemical Cycles (2014) 28 Annual net community production and the biological carbon flux in the ocean Steven Emerson School of Oceanography,
A First Step into the Pelagia: Linking Bottom Water Hypoxia to the Vertical Distribution of Fishes on the Northwestern Gulf of Mexico Shelf Elliott Hazen,
Mesozooplankton component General objective: Quantitative assessment of its biomass and production and its impacts on phytoplankton stocks and vertical.
Food web and microbial loop Eutrophic vs. Oligotrophic food webs
Cases and controls A case is an individual with a disease, whose location can be represented by a point on the map (red dot). In this table we examine.
Theme 1: Biological uptake and trace element bioavailability
CHAPTER 1 LESSON 1 UNDERSTANDING MAPS.
Applying GIS to Santa Cruz Island:
Weeds & Weather: Local to Regional Daily Simulations
MAPPING THE EARTH.
Topographic Map Skills
Hydroacoustic estimates of plant (relative) density (dry g/m2) within cells 10 m wide by 1 m deep. [Nichols Lake Transect T450; 7/24/02] 15 foot depth.
Spatial and Temporal Variability of Zooplankton in the Northern Gulf of Mexico: Effects of Low Oxygen Bottom Waters Mike Roman, Dave Kimmel, Jamie Pierson,
Weeds & Weather: Local to Regional Daily Simulations
Ocean Water & Life.
A graphing calculator is required for some problems or parts of problems 2000.
Food web and microbial loop Eutrophic vs. Oligotrophic food webs
Diversity of Life – Activity 4 Molecules & Processes – 3
11:628:320 Dynamics of Marine Ecosystems 2019
Presentation transcript:

Patterns of Zooplankton Diel Vertical Migration in the Global Ocean Devika Balachandran K. Allison Smith August 12, 2011

What is DVM? Diel vertical migration is best defined as the vertical displacement of an individual or group of individuals, which occurs with diel periodicity (Huntley 1985) Tim e Depth (m)

Why is DVM important? Major component of the biological pump Biological pump

Questions to address What percent of zooplankton biomass leaves the euphotic zone during the day? To what depths do migrating species move during the day?

NOAA Database - Filter data manually and using R and Excel - Use ephemeris to flag data points as day or night (based on sun’s elevation) - Organize data with R and graph with Excel - Make maps plotting sites (longitude, latitude) using Generic Mapping Tools (GMT)

Sites used: Day and Night Values Close Together

What % of zooplankton biomass leaves the euphotic zone during the day? Results presented as ratio of Day/Night values – A ratio r 1 suggests that zooplankton are migrating into the euphotic zone during the day – If r < 1, % biomass leaving euphotic zone during the day = Ex: if r = , it appears as though 52.21% of the zooplankton biomass is leaving the euphotic zone during the day – If r > 1, % biomass entering euphotic zone during the day = Ex: if r = , it appears as though 42.65% of the zooplankton biomass is entering the euphotic zone during the day

- When considering values less than 1, results are comparable to values that have been presented in the literature % of all metazoan zooplankton biomass above 500 m perform migrations (Longhurst and Harrison, 1988) What % of zooplankton biomass leaves the euphotic zone during the day? - When all values are considered, results are not comparable to values presented in the literature - Most of the data was presented in counts (num/m 3 ), which is not the most accurate unit for zooplankton biomass

Emerging patterns?

Spatial distribution of values less than and greater than/equal to 1 < 1≥ 1 A ratio r <1 suggests that zooplankton are migrating out of the euphotic zone during the day, while an r ≥ 1 suggests that zooplankton are migrating into the euphotic zone during the day

Summary DVM is a component of export fluxes and should not be overlooked in nutrient flux calculations Studies that are specifically researching DVM show clearer DVM results than analysis of data from cruises not researching DVM – Perhaps due to methods (studies researching DVM more often report biomass in density or volume, while other cruises more often report biomass in counts, which does not represent biomass as accurately) It is not yet clear what global patterns of DVM are, but DVM appears to occur globally, so perhaps with more data, patterns may emerge

Future Studies More cruise data from the Atlantic Acquire more data from a variety of databases Analysis of acoustic data combined with tow data in order to find patterns