Marine Ecology Flashcards

0
Q

Why are mangrove forests difficult environments for organisms to live in?

A
  • Low oxygen
  • High and variable salinity
  • High temperature & water loss
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1
Q

What are mangrove forests?

A

Tropical, sheltered depositional coastal environments e.g. estuaries or inlets (but are not restricted to only estuaries). They are characterised by mangroves, the woody trees or shrubs adapted to saline environments.

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2
Q

What are the 4 key genera in mangrove forests?

A
Red Mangrove (Rhizophora)
White mangrove (Laguncularia)
Black mangrove (Avicennia)
Mangrove apple (Sonneratia)
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3
Q

What are the types of continental shelves?

A

a – Soft bottomed benthic

b – Seagrass beds

c – Hard bottomed benthic

d - Kelp forests

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4
Q

Discuss and contrast the physiological adaptations of (i) mesopelagic and (ii) deeper-zone organisms, relating to light.

A

Write l8rrr

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5
Q

Turtle Migrations

A

•Marine turtles spend most of their lives at sea, returning to land to lay eggs.
•Natal homing

•Research on nesting green turtles on Mayotte suggests turtles navigate using geomagnetic cues - Turtles were displaced, and satellite tracked. Longer homing paths when magnets put on head.

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6
Q

What is phenology?

A

Timing of life history events in organisms

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7
Q

Properties of water

A

Commonly found as liquid, gas and solid
Covalent
Polar
Hydrogen bonds - gives water unusually high melting and boiling point
Good solvent - dissolves more substances in greater quantities than any other liquid (salts, sugars, acids, and some gases)
Salts dissolve better at high temps
Gases dissolve better at low temps

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8
Q

Light penetration in water

A

Visible light attenuates with depth
Extreme wavelengths lost first: red and violet
Blue travels furthest down water column

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9
Q

Ocean depth profiles

A

Temperature: surface layer is warmest. Thermocline (colder with increasing depth) past surface layer to 1,000m. Constant temp in deep layer.
Density: surface layer has lowest density. Pycnocline (increased density with increasing depth) past surface layer to 1,000m. Constant density in deep layer.
Salinity: differs in intermediate and surface layer, constant in deep layer.

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10
Q

Seasonality in Ocean depth profiles

A

Summer: bigger difference between surface and deep temp. Surface is warmer
Autumn: surface water cools and becomes denser and sinks - downwelling. Displaces deeper water which then rises - overturn
Winter: this continues - water from deep and surface mixes.

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11
Q

Coriolis effect

A
Affects ocean circulation
Currents and winds are deflected:
To the RIGHT in the northern hemisphere
To the LEFT in the southern hemisphere 
By the Coriolis effect
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12
Q

Major gyres

A
North Pacific gyre
North Atlantic gyre
Indian Ocean gyre
South Pacific gyre
South Atlantic gyre
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