Lecture 1 Flashcards

1
Q

What are the three zones in aquatic environ meets?

A

Pelagic zone
Benthic zone
Littoral zone ( Rocky and non rocky)

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2
Q

What is the pelagic zone?

A

Open water eg. Overlying water inrivers/ open water in lakes • open ocean (not coastal regions)

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3
Q

What two type of organisms in habit the pelagic zone? Ts. e

A

Pelagic and nektonic

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4
Q

Where do planktonic organisms live?

A

In the pelagic zone/ open water

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5
Q

What are

Nektonic organisms?

A

Organisms that actively swim in the water column

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6
Q

What are Pelagic organisms?

A

Ones that float within the water column

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7
Q

Describe organisms in the benthic zone?

A

They dwell on the bottom of the water body, often in mud or on rocks

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8
Q

What are the two types of benthic organisms

A

Epifaunal , infaunal

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9
Q

What’s the difference between infaunal and epifaunal organisms

A

Ipifaunal-Living within the sediment the sediment or substrate

Epifaunal- living onto of the sediment or substrate

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10
Q

What is the difference between lotic and lentic waters?

A

Lotic-Running waters

Lentic- still waters

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11
Q

What is the density of 1cm cubed of water

A

1g

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12
Q

How does the viscosity of water benefit aquatic plants?i

A

The don’t need to put energy into building vascular tissues for stability
They can place more energy into reproductive processes,giving faster rates of reproduction in comparison to terrestrial plants

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13
Q

How does temperature relate to water stability?

A

Water has a high heat capacity at one calorie per gram, whereas waters is lower. This makes air temperatures more variable, and waters less- providing increased stability for organisms

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14
Q

When is water at its densest?

A

3.94 degrees Celsius
1ml equals 1g in freshwater
1ml equals 1.026g

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15
Q

Why is sea water denser that freshwater at 3.94 degrees Celsius?

A

The salt content

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16
Q

What temperatures do fresh and sea water freeze at?

A

Sea water:-2

Freshwater:0

17
Q

What is a homothermal environment

A

Organisms can exist anywhere within the water body due to effective mixing of the water column

18
Q

Explain the vertical structure of the water column in water bodies less than 3m in depth. Eg. Shallow seas, rivers,estuaries, coastal waters

A

The sun heats the water column, and convection occurs.

The water body is effectively mixed, forming a homothermal environment

19
Q

Explain the mixing regime in water bodies greater than 3m in depth

A

Warm water is heated by the sun and lighter than cold water. Mixing is ineffective, meaning that there’s no distribution of temperature throughout the water body and STRATIFICATION occurs

20
Q

What does the lake split into during stratification?

A

Epilimnion-the upper lake surface with warm water

Hypeolimnion-lower surface of the stratified system

21
Q

Why do organisms congregate at the thermocline?

A

Conditions in the epilimnion and hypo lim ion are too hot and cold respectively, and there’s high nutrient diffusion upwelling from the colder regions(nitrogen and phosphorous)

22
Q

What are the three main types of stratification?define them

A

Holomictic stratification- no stratifying occurs
Monomictic- stratifies once a year, in summer (eg deep lakes)
Amictic- system is permanently stratified

23
Q

Why is lots of biological activity concentrated at depths from the top to 200 m in oceans?

A

The epilmnion is at depths of 200m in oceans, so this doesn’t occur s above it (water at greater depths is hotter)

24
Q

Why is the thermocline the ideal position for food webs?

A

Nutrients up well from the hypolimnion