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Warm Up  What is salinity? The total amount of solid material dissolved in water The total amount of solid material dissolved in water  What is the difference.

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Presentation on theme: "Warm Up  What is salinity? The total amount of solid material dissolved in water The total amount of solid material dissolved in water  What is the difference."— Presentation transcript:

1 Warm Up  What is salinity? The total amount of solid material dissolved in water The total amount of solid material dissolved in water  What is the difference between a thermocline and a pycnocline? Thermocline- temp; pycnocline-density Thermocline- temp; pycnocline-density  What are the three different layers of the ocean? Mixed Zone, Transition Zone, Deep Zone Mixed Zone, Transition Zone, Deep Zone

2 The Diversity of Ocean Life Chapter 15, Section 2

3 Classification of Marine Organisms  Marine organisms can be classified according to where they live and how they move  Plankton include all organisms—algae, animals, and bacteria—that drift with ocean currents  Phytoplankton – the algae that undergo photosynthesis  Zooplankton – animal plankton  Nekton include all animals capable of moving independently of the ocean currents, by swimming or other means of propulsion  The term benthos describes organisms living on or in the ocean bottom

4 Plankton Phytoplankton Zooplankton

5 Nekton

6 Benthos

7  Give an example of a nekton.

8 Marine Life Zones  The distribution of marine organisms is affected by the chemistry, physics, and geology of the ocean  Three factors are used to divide the ocean into distinct marine life zones: the availability of sunlight, the distance from shore, and the water depth

9 Availability of Sun  Photic Zone – the upper part of the ocean into which sunlight penetrates  The clarity of seawater is affected by many factors, including the amount of plankton, suspended sediment, and decaying organic particles  The euphotic zone is the portion of the photic zone near the surface where light is strong enough for photosynthesis (usually no deeper than 100 meters)  Below the photic zone is the aphotic zone, where there is no sunlight

10 Distance from Shore  Intertidal Zone – the area where the land and ocean meet and overlap  The intertidal zone is a narrow strip of land which is alternately covered and uncovered between high and low tides  Neritic Zone – covers the gently sloping continental slope  The neritic zone is often shallow enough to put all of it in the photic zone, and is so rich with life that it supports 90% of the world’s commercial fisheries  Oceanic Zone – area beyond the continental shelf  Surface waters in the oceanic zone tend to not have many nutrients as they sink down to the deep ocean floor

11 Water Depth  Pelagic Zone – open ocean of any depth  Animals in the pelagic zone swim or float freely  Benthic Zone – includes any sea-bottom surface regardless of its distance from shore  The benthic zone is mostly inhabited by benthos organisms  Abyssal Zone – a subdivision of the benthic zone; includes the deep-ocean floor, such as abyssal plains  The abyssal zone is characterized by high water pressure, consistently low temperature, no sunlight, and sparse life

12 Marine Life Zones

13

14 Hydrothermal Vents  Seawater seeps into the ocean floor through crack in the crust  The water is super-heated and saturated with minerals, and escapes back into the ocean  The minerals precipitate out, giving the water the appearance of black smoke (black smokers)  At some vents water temperature of 100ºC or higher support communities of organisms found nowhere else in the world

15 Hydrothermal Vents

16 Assignment  Read Chapter 15, Section 2 (pg. 428-432)  Do Section 15.2 Assessment #1-7 (pg. 432)


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