1. Test #2 Results by Next Week

2. Biological Productivity

3. Conditions for Life in the Sea Consider the main biochemical reaction for life in the sea, and on earth in general: 6H 2 O + 6CO 2 + energy + nutrients = C 6 H 12 O 6 + 6O 2 Focus on left side of equation What is in short supply in the sea and thus limits the amount of life in the ocean??

4. Absorbing Nutrients 6H 2 O + 6CO 2 + energy + nutrients = C 6 H 12 O 6 + 6O 2  Phytoplankton are base of the food chain  Most important primary producers of complex sugars and oxygen Lauderia sp.

5. Open Ocean Food Webs Barrie Kovish Vicki Fabry ARCOD@ims.uaf.edu Pacific Salmon Copepods Coccolithophores Pteropods

6. Sinking Organic Debris Present Ocean Food Web – Complex ecosystem interactions based on a low CO 2 ocean MicrobialRemineralization Primary Producers Zooplankton Food Web Upper Trophic Levels Seafloor community Provided by James Barry MBARI Ocean Food Web

7. Absorbing Nutrients  Nutrients absorbed by plants through diffusion across a semi-permeable membrane Lauderia sp.

8. Diffusion: molecules move from high to low concentrations

9. Which Nutrients are in Short Supply?  Nitrogen (N) as Nitrate NO 3 (-2)  Phosphorus (P) as Phosphate PO 4 (-2)  Silicon (Si) as Silicate SiO 4 (-2)

10. Phosphate and Nitrate in the Pacific

11. Silicate in the Pacific

12. Biolimiting Nutrients  N, P, and Si are exhausted first in Eq. surface waters during photosynthesis  Essential to the growth of phytoplankton  If these biolimiting nutrients increase in sea water, life increases  If these biolimiting nutrients decrease in sea water, life decreases  Where would you expect to find the highest biomass in the Pacific??

13. CZCS Global Primary Production

14. How Does Nutrient Distribution Compare w/ Dissolved Oxygen?

15. Dissolved O 2 Reverse of Nutrients  O 2 is high in the surface and mixed layer  O 2 decreases to a minimum at base of thermocline  O 2 then steadily increases with depth

16. Why is the Concentration of Oxygen High in the Mixed Layer?? Hint #1: How and where is oxygen produced in the sea??? 6H 2 O + 6CO 2 + energy + nutrients = C 6 H 12 O 6 + 6O 2 Hint #2: How can oxygen be mixed downward from the atmosphere into the ocean?

17. How is Oxygen Removed from the Thermocline & Slightly Below??

18. Dead and decaying organic matter sinks downward from surface waters  Rate of sinking decreases as it encounters the cold, dense water of the thermocline  Material decays (oxidizes) at the thermocline, which strips O 2 out of the water and returns nutrients to the sea  Cold, nutrient-rich water of the thermocline is returned to sunlit surface waters by way of upwelling

19. CZCS Global Primary Production

20. Marine Ecology

21. Basic Ecology  physical and chemical parameters affecting distribution and abundance  An ecosystem includes both the living (biotic) and non-living (abiotic) portions of the environment. –Examples include: salt marshes, estuaries, coral reefs, the North Pacific Gyre.

22. Classification of Organisms by Environment  horizontal: neritic | oceanic  vertical: –epipelagic (top) / euphotic (good) –mesopelagic (middle) / disphotic (low) –bathypelagic (deep) / aphotic (without) –abyssopelagic (“bottomless”)

23. Divisions of the Marine Environment Figure 9-1

24. Classification of Organisms by Lifestyle  Scientists have established another classification scheme to categorize biota on the basis of lifestyle. The major groups are: –plankton (floaters) –nekton (swimmers) –benthos (bottom dwellers)

25. Plankton  weak swimmers, drifters, unable to counteract currents. –Phytoplankton (plants) –Zooplankton (animals)

26. Nekton  active swimmers capable of counteracting currents. –Fish –Squids –Reptiles –Birds –Mammals

27. Distribution of Marine Lifestyles  16.7% of Earth’s animals are marine  2% inhabit pelagic environment (most of the oceans are cold and dark)  98% are benthic!

28. Benthos  Epiflora or epifauna live on the sea bottom.  Infauna live in the sea bottom.  Benthic plants - restricted to shallow waters (light)  Benthic animals occur everywhere from shallow depths to the deep sea.

29. Research Video Clips: “Live fast, die young...”

30. Hydrostatic Pressure  Pressure caused by the height of water.  Function of water height and water density  Pressure generally increases at a rate of 1 atm per 10 m of water. ( or 16 psi per 10 m depth)

31. Think You’re Under Pressure Now?

32. Hydrostatic Pressure (Cont.)  enormous in the deep sea yet animals live there.  Animals do not contain gases.  However, mesopelagic fish which have gas-filled swim bladders to help maintain neutral buoyancy –unable to move rapidly between depths –pressure change could cause bladder explode.

33. Oregon Coast Field Trip - Sat., May 30 th dusk.geo.orst.edu/oceans/field.html u Be here by 7:15 a.m. u 7:30 - Busses leave from Wilkinson lot u 8:30 - HMSC Visitor Center u 10:00- Travel to Seal Rock State Park u 10:30 - Seal Rock volcanic rocks and tide pools u 12:00 - Lunch at Seal Rock (bring your own) u 12:30ish - Return to Corvallis u Back by ~2:00

34. Required Field Trip Guide dusk.geo.orst.edu/oceans/field.html u Answers to bolded questions in guide –Turn assignment in to your TA –Due by 5:00 p.m., June 5th –This constitutes LAB 9