1. Water H 2 O, Sea Water and what it means to life in the ocean….

2. Figure 3.01 Hydrogen Bonds, Between water molecules Are weak, but IMPORTANT!

3. States of water Water occurs as solid, liquid & gas naturally No hydrogen bonds in water vapor Some molecules joined by hydrogen bonds in liquid – bonds break & reform All molecules rigidly bonded in solid

4. Figure 3.02

5. Heat and Water Adding heat makes molecules vibrate Heat energy is used to cause vibration AND to break hydrogen bonds

6. Heat and Water Ice melts at relatively high temperatures compared to similar substances –(O o C instead of –90 o C)

7. Water = Universal Solvent Good at dissolving salts (the solutes) Salts exist as separate ions in seawater Remember: Solvent dissolves, solutes are what gets dissolved!

8. Seawater Salts come from weathering of rock or outgassing from hydrothermal vents Sodium and Chloride account for 85% of the dissolved solids (solutes) in sea water. This makes it various degrees of SALINE: “total amount of salt dissolved in sea water”

9. Figure 3.05

11. SeaWater WHERE does the “salt” come from? And WHAT else is in the water?

14. Salinity The total amount of dissolved salts in seawater Measured in parts per thousand (ppt or o/oo) Average salinity of sea water is 35%

16. Density of (sea)water Density also affects the salinity of water Liquid water gets denser as the temperature decreases BUT ice is LESS dense than liquid water Increases with decreasing temperature Increases with increasing salinity

17. Temp. of ocean surface: cold = blue, warm = red Typical Ocean temp. range are 28-86 degrees F

18. Stratified Ocean (3 Layers) Salinity, Temperature and Density all effect ocean waters giving OCEAN GRADIENTS or stratified layers. Dense, cold water @ bottom Less dense, warmer water @ surface (floating on layer below)

19. 3 layered Ocean Surface “mixed” layer: 100-200 m thick Mid “intermediate” layer: 200-1500 m thick contains the main thermocline (transition zone between warm and cold top/bottom layers) Deep “bottom” layer: after 1500 m

20. Figure 3.17

21. Figure 3.25

22. Figure 3.21

23. Figure 3.15a

25. Water, salinity, light, pressure, depth How does this affect marine “life?”

26. Light in the ocean Transparency depends on what is suspended in the water Different colors penetrate to different depths

27. Figure 3.11

30. Pressure Water is heavier than air Pressure changes ( a lot!) w/ increased water depth 1 atm. of pressure = sea level (on land) but in ocean each 10 m of depth (33’) you add another atm. of pressure

31. Figure 3.13

32. Figure 3.14 Groupers swim bladder has expanded, due to pressure, thus stomach has Been forced through mouth!

33. Buoyancy Two deep-sea fishes on the deck of a ship after being hauled up from a depth of 800 m. Both fishes were seriously damaged and distorted by the rapid expansion of gases in their swim bladders as they were brought to the surface.

34. Buoyancy Fnft: A physoclistous swim bladder and associated blood vessels.

35. Life in the Ocean Deal with challenges that are unique to marine environment Must maintain suitable conditions inside the organism’s body

36. Diffusion & Osmosis Diffusion: movement of molecules from an area of HIGH concentration to an area of LOW concentration (things flow DOWNHILL) Osmosis: WATERS movement! The diffusion of water across a cell membrane. Water moves in opposite direction as solutes (“stuff” in water)

37. Osmosis More water molecule s Fewer water molecules water High to low concentration flow

38. Osmosis Watery environment Inside of the cell Plasma membrane

39. Osmosis solutes osmotic concentrationThe amount of all dissolved molecules, or solutes, in a solution is called the osmotic concentration. isotonicIf the number of solute molecules in two solutions is equal (the osmotic concentration is equal), the solution is isotonic. hypertonic hypotonicIf the two solutions have unequal osmotic concentrations, the solution with the higher concentrations of solutes is hypertonic; the solution with the lower concentration of solutes is hypotonic.

40. Isotonic Equal number of solute molecules No net movement of water molecules 1 2 1 2

41. Hypertonic and Hypotonic 1 2 1 3 HypertonicHypotonic More solutes; fewer water molecules Fewer solutes; more water molecules water

42. Images : Copyright © The McGraw-Hill Companies, Inc. More solutes; fewer water molecules Fewer solutes; more water molecules HypertonicHypotonic Tonicity is SOLUTES Only (not water)

43. hypotonic hypertonic Water always moves from hypotonic (fewer solutes) to hypertonic (more solutes) solutions. Images : Copyright © Pearson Education, Inc. HypertonicHypotonic 1 1 2 3

44. hypotonic hypertonic Water always moves from hypotonic (more water) to hypertonic (less water) solutions Images : Copyright © Pearson Education, Inc. HypertonicHypotonic 1 2 34 5 6 7 8 9 1010 1 1212 1313 1414 1515 1616 1717 1818 1919 2020 2121 2 1 2 3 4 5 6 7

45. Images : Copyright © The McGraw-Hill Companies, Inc. HypertonicIsotonicHypotonic

46. Figure 4.13b

47. Figure 4.13a More salt in cell, Water diffuses in to cell, it will swell and burst. HYPOTONIC (“o” = swell)

48. Figure 4.13c More salt outside cell,Water moves Out of cell, it will shrivel. HYPERTONIC (“e” = shrivel)

50. Osmosis in fish OSMOCONFORMERS: Internal concentration of ions CHANGES with changing environment around it (usually dealing with salt). Marine Inverts are like this (& hagfish). (Opposite) OSMOREGULATOR: control of internal concentrations. These are your vertebrates (from “Sharks”, fish, & up)!

51. Figure 4.14a Osmoregulator: Because salt conc. HIGHER outside the water will flow OUT & dehydrate fish. Instead fish will drink water (increasing salt) to increase water (& not urinate it out) & then pass excess salt out through gills to “balance” itself

52. Hawksbills’ “excrete” glands (near eyes) to get rid of excess salt osmoregulator

53. Temperature How does this effect marine organisms? It dictates where they live and metabolize

54. Temperature regions of the worlds oceans

55. Temperature Regulation Most marine animals are ectotherms (“cold- blooded”)

56. Temperature Regulation Most marine animals are ectotherms (“cold- blooded”) Mammals and birds are endotherms –Use fat, feathers for insulation

57. Temperature Most marine animals are adapted to living at a specific temperature –Temperature determines species ranges

58. New Topic Tides…

59. Tides Tide Tables Waves Weather (resultant)

60. Tides How do we calculate tides? Tide tables Semidiurnal Tides (in Northeast) Spring vs. Neap tides

66. Tides… …effect marine life too…

67. Low Tide…and offshore Thailand, Tsunami

68. Grunion

69. Waves

70. Orbits

71. Waves in a Bay

72. Hitting the shore