PHYSICAL CONDITIONS IN DEEP SEA ENVIRONMENTS Flashcards

1
Q

Are there strict ecological zones with altitude on land? Why?

A

No - boundaries between ecological zones vary with latitude, rainfall, prevailing wind, topography etc.

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2
Q

How much does pressure increase with 10m depth?

A

by ~1 atmosphere per 10m depth

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3
Q

Why do deep sea organisms not require structural adaptations at depths?

A

Internal and external pressures are equalised in most organism tissues (solids and liquids are largely incompressible)

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4
Q

Pressure can trap water on surfaces of unfolded proteins. What can this cause? How does the physiology of many taxa overcome this?

A

Prevents them folding into shape for correct enzyme function.
Many taxa use “chaperone” molecules (piezolytes) to remove water from unfolded proteins and promote correct folding.
Fish and decapod crustaceans use a molecule called TMAO.

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5
Q

How does fish and decapod tissue TMAO conc change with depth?
What effect does this have on depth distribution of teleost fish?

A

Increase.
With increasing TMAO, teleost fish become hypertonic to seawater by <9000 metres, limiting their depth distribution.

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6
Q

What is the piezothermal effect? What might this explain for vent fish and vent shrimp?

A

higher temperatures can enable tolerance of higher pressures
lower-than-expected-for-depth tissue TMAO in vent shrimp and fish

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7
Q

Why does lipid composition of cell membrane vary with depth in deep-sea taxa?

A

To maintain membrane fluidity under pressure

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8
Q

Calcite starts to dissolve below certain depths (CCD). How do trench amphipods overcome this?

A

Produce an aluminium hydroxide gel that coats their exoskeleton to protect its calcite mineral content from dissolving under pressure.

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9
Q

Why is their some slight adiabatic warming at great depths?

A

Due to slight incompressibility of water

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10
Q

What is water mass structure a consequence of? What concentration does it affect?

A

Thermohaline circulation
Deep-water oxygen concentration (& CCD)

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11
Q

What is the dysphotic and aphotic zone?

A
  • solar irradiance still present/detectable but insufficient for NET photosynthetic primary production
  • no (detectable) solar photon flux (but some other light sources still present e.g. bioluminescence, geochemistry, physics)
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