2.2.2 abiotic factors in marine ecosystems

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2.2.2 Abiotic factors in Marine Ecosystems

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2.2.2 Abiotic factors in Marine Ecosystems. Marine Ecosystems. Limiting Factors. Too much or too little of a single physical factor can adversely affect the function of an organism. - PowerPoint PPT Presentation

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Page 1: 2.2.2 Abiotic factors in Marine Ecosystems

2.2.2 Abiotic factors in Marine Ecosystems

Page 2: 2.2.2 Abiotic factors in Marine Ecosystems

MARINE ECOSYSTEM

S

Page 3: 2.2.2 Abiotic factors in Marine Ecosystems

Limiting Factors Too much or too little of a single

physical factor can adversely affect the function of an organism.

Limiting factors are physical or biological necessities whose presence or absence in inappropriate amounts limits the normal action of the organism.

Page 4: 2.2.2 Abiotic factors in Marine Ecosystems

Light is needed for photosynthesis and vision.

Blue light penetrates deepest. Limited also by particles in the water.

Page 5: 2.2.2 Abiotic factors in Marine Ecosystems

Temperature influences the

metabolic rate, the rate

at which reactions proceed within an organism.

Page 6: 2.2.2 Abiotic factors in Marine Ecosystems

Most marine organisms are ECTOTHERMIC having an internal temperature that stays very close to that of their surroundings.

A few complex animals (mammals & birds) are ENDOTHERMIC, meaning they maintain a stable internal temperature.

Ocean temperature varies in both depth and latitude.

Ocean temperatures vary less than on land.

Page 7: 2.2.2 Abiotic factors in Marine Ecosystems

Salinity greatly affect cell membranes and protein structure.

Disrupts cells osmotic pressure. Varies because of rainfall, evaporation and

runoff from land.

Page 8: 2.2.2 Abiotic factors in Marine Ecosystems

Dissolved Gases are necessary for photosynthesis and respiration.

CO2 dissolves more easily in water than O2.

CO2 is more abundant in deep waters than surface water.

O2 decrease dramatically where light penetration decreases.

Page 9: 2.2.2 Abiotic factors in Marine Ecosystems
Page 10: 2.2.2 Abiotic factors in Marine Ecosystems

Pressure from the layers of water above. Increases with increasing depth. Pressure affects buoyancy (ability to

float). To counteract the mass of heavy muscles

and bone, many swimming fishes have gas-filled bladders.

Deep-sea fish don’t have gas bladders, but light bones and oily watery flesh.

Page 11: 2.2.2 Abiotic factors in Marine Ecosystems
Page 12: 2.2.2 Abiotic factors in Marine Ecosystems

Marine Zones Areas of homogeneous physical features. Usually based on light, temperature,

salinity, depth, latitude, behavior and/or water density.

Page 13: 2.2.2 Abiotic factors in Marine Ecosystems

By lightPhotic zone sunlit layer of water at the

ocean’s surface. Upper zone is called the Euphotic zone

and is where the rate of photosynthesis is high.

Lower zone is called Disphotic zone and is where organisms can see, but there is sufficient light for photosynthesis.

Aphotic zone where no light penetrates.

Page 14: 2.2.2 Abiotic factors in Marine Ecosystems
Page 15: 2.2.2 Abiotic factors in Marine Ecosystems

By LocationPelagic zone between water and ocean

bottom.a. Neritic zone = near shore over the continental shelf

Page 16: 2.2.2 Abiotic factors in Marine Ecosystems

b. Oceanic zone = deep-water beyond the continental shelf.

i. Epipelagic = photic zone of the ocean. ii. Mesopelagic = middle ocean waters. iii. Bathypelagic = ocean floor. iv. Abyssopelagic = deep-ocean trenches.

Page 17: 2.2.2 Abiotic factors in Marine Ecosystems
Page 18: 2.2.2 Abiotic factors in Marine Ecosystems

Classification of

Organisms

Page 19: 2.2.2 Abiotic factors in Marine Ecosystems
Page 20: 2.2.2 Abiotic factors in Marine Ecosystems
Page 21: 2.2.2 Abiotic factors in Marine Ecosystems