lesson 3: protecting ocean hotspots. lesson 3 presentation content engage explore explain elaborate...
TRANSCRIPT
Lesson 3: Protecting Ocean Hotspots
Lesson 3 Presentation Content
Engage
Explore
Explain
Elaborate
Evaluate
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Imagining the Seafloor
Identifying Seafloor Features
Upwelling and Phytoplankton
Marine Sanctuaries
Seafloor Features and Upwelling
Engage
Imagining the Seafloor
The ocean looks similar everywhere …
because we can’t see through the water
Pacific Ocean Atlantic Ocean
But the seafloor is full of features
Explore
Identifying Seafloor Features
Measuring the Seafloor
Mariana trench
Trenches are very deep areas of the ocean. The Mariana trench is the deepest known trench, with a depth of 10,910 m
Japantrench
Aleutiantrench
Exploring the SeafloorROV – Remotely Operated Vehicle
Alaskan shelf
Continental shelves are shallow (0 – 200 m deep) areas on the edges of continents and islands
Continental slopes are the steep “drop offs” between the continental shelf and the abyssal plain. The water depth ranges from 200 and 2,000 m
Bering Sea slope
Gulf of Alaskaslope
Continental Slope
The abyssal plain is the deep (2,000 m and deeper) and relatively flat seafloor making up most of the world’s oceans
Abyssal plain
Cortes – Tanner Bank
Banks are undersea hills, sitting on the continental shelf. They often reach very close to the surface
Cordell Bank
Cordell Bank
Image USGS
Emperor SeamountChain
Seamounts are volcanic mountains rising over 1,000 m above the seafloor, but always remaining under the waves. Sometimes they reach to 100 m from the surface
Volcanic Underwater Seamount
The stars and labels mark the three study sites, where albatross were tagged with transmitters.
• Grey shading indicates seafloor depth (m)
Shaded Contour Map of the North Pacific Seafloor
Albatross Nesting Colony
Kure Atoll Seabird Sanctuary
Tern Island, National Wildlife Refuge
Black-footed Albatross, kaʻupu, at Sea
Tagging Albatross over Cordell Bank
• Look at the map legend to find out what ocean depths this albatross flew over.
One albatross tagged over Cordell Bank, off California (see close-up)
• Black circles indicate where a bird was located at noon. Arrows show their path.
Explain
Upwelling and Phytoplankton
Microbes - microscopic organisms made up of a single cell (unicellular) or a cell cluster
Diatoms Cyanobacteria
Microbes Are the Most Abundant Organisms in the Ocean and form
the Base of the Marine Food Webs•These diatoms and other phytoplankton are tiny plant-like organisms.
• They produce sugar by photosynthesis using sunlight, carbon dioxide and nutrients.
The Wind Drives Coastal Upwelling
Central California Coast
Coastal Upwelling Fertilizes the Ocean
Central California
• Top-down view from a satellite shows the sea surface temperature off central California.
• Plumes of colder water (blue, 9 C or 42 F) upwell along the coast and mix with the warmer water offshore (red, 16 C or 60 F ).
Productive Water Looks Green
Green in the ocean indicates productive regions with abundant chlorophyll-containing phytoplankton.
Image Credit NASA
Albatross Food Chain
Image credits: Phytoplankton: NOAA MESA Project, Zooplankton: NOAA/D.Forcucci; NOAA Central Library/Charleston Bump Expedition 2003. NOAA Office of Ocean Exploration; Dr. George Sedberry, South Carolina DNR, Principal Investigator, Fish: NOAA, NEFSC, Squid: NOAA/MBARI 2006, Albatross: NOAA Corps/Lieutenant Elizabeth Crapo
Many marine birds and mammals come together to feed in productive areas of the ocean.
Elaborate
Marine Sanctuaries
Visit them online at http://sanctuaries.noaa.gov
Designing Marine SanctuariesSeveral marine sanctuaries protect seafloor features and the productive waters surrounding them, where many marine animals aggregate and thrive.
Cordell Bank
Sanctuaries Can Protect Seafloor Features
This map showsexisting sanctuariesoff central Californiaand the location of seamounts and banks(pink shading)
Where would you create an Albatross Sanctuary?
Map Hand-Outs for Printing
The following slides interpret the “Albatross Tracking and Bathymetry Maps” and provide material to stimulate discussion.
Commuting from the colony to a seamount
Use of the California shelf / slope and a visit to seamounts offshore
Foraging along the shelf / slope of the Aleutian Islands
Foraging along the shelf / slope of Japan
Use Agreement
Engage – Imagining the Seafloor 1. The ocean surface looks the same everywhere2. But the seafloor is full of features: Google Maps of
the Pacific Ocean and the Atlantic Ocean
Explore – Identifying Seafloor Features
1. Measuring the Seafloor2. Google Map of the Pacific Ocean3. Google Map of Trenches4. ROV Submersible5. Google Map of Continental Shelves6. Google Map of Continental Slopes7. 3D graphic of Continental Slope8. Google Map of Abyssal Plains9. Google Map of Banks10. 3D graphic of Cordell Bank11. Google Map of Seamounts12. 3D graphic of a volcanic seamount13. B&W Contour Map of Pacific Ocean Bathymetry14. Albatross Nesting Colony15. Photos of Kure Atoll and Tern Island where birds
were tagged16. Albatross At-Sea17. Photos of Tagging over Cordell Bank18. Handout Example: Cordell Bank Loop
Explain – Upwelling and Phytoplankton
1. Microbes are microscopic organisms2. Phytoplankton microbes photosynthesize3. The wind drives coastal upwelling4. Coastal upwelling fertilizes the ocean5. Productive water looks green6. Albatross Food Chain7. Whales and birds feed in productive areas
Elaborate – Marine Sanctuaries
1. Map of existing U.S. Marine Sanctuaries2. Designing Marine Sanctuaries3. Sanctuaries Can protect Seafloor Features4. Where Would You Create an Albatross Sanctuary?5. Information for Map Discussions 6. Map of Albatross Track: Kure Atoll Loop7. Map of Albatross Track: Cordell Bank Loop8. Map of Albatross Track: Kure Atoll to Alaska9. Map of Albatross Track: Kure Atoll to Japan
Lesson 3 Presentation Content