2.5 - Practicle Work Flashcards

1
Q

how can organism in an ecosystem be identified

A

Organisms in an ecosystem can be identified using a variety of tools including keys, comparison to herbarium / specimen collections, technologies and scientific expertise.

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2
Q

Define sampling strategies

A

Sampling strategies may be used to measure biotic and abiotic factors and their change in space, along an environmental gradient, over time, through succession or before and after a human impact, for example as part of an EIA.s

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3
Q

Why should measurements be repeated

A

Measurements should be repeated to increase reliability of data. The number of repetitions required depends on the factor being measured.

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4
Q

What are methods for estimating the biomas and energy trophies levels in a community

A

Methods for estimating the biomass and energy of trophic levels in a community include measurement of dry mass, controlled combustion and extrapolation from samples. Data from these methods can be used to construct ecological pyramids.

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5
Q

What are some methods for estimating the abundance of non motile organisms

A

Methods for estimating the abundance of non-motile organisms include the use of quadrats for making actual counts, measuring population density, percentage cover and percentage frequency.

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6
Q

What are direct and indirect methods for estimating the abundance of motile organisms

A

Direct and indirect methods for estimating the abundance of motile organisms can be described and evaluated. Direct methods include actual counts and sampling. Indirect methods include the use of capture-mark-recapture with the application of the Lincoln Index.

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7
Q

Define species richness

A

Species richness is the number of species in a community and is a useful comparative measure.

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8
Q

Define species diversity

A

Species diversity is a function of the number of species and their relative abundance and can be compared using an index. There are many versions of diversity indices but students are only expected to be able to apply and evaluate the result of the Simpson diversity index. Using its formula, the higher the result, the greater the species diversity. This indication of diversity is only useful when comparing two similar habitats or the same habitat over time.

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9
Q

Where should you collect data

A
  • quadrats and transects
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10
Q

What should you mesure when collecting data

A

Measuring abiotic factors
• Marine
• Freshwater
• Terrestrial • Measuring biotics
Biomass and productivity
• Catching small motile animals
• Terrestrial
• Aquatic
• Keys
Measuring abundance
• Lincoln Index
• Simpson diversity index

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11
Q

What must you do as you increase number of samples

A

As you increase the number of samples, plot the number of species found. When this number is stable, you have found all species in the area, so in figure 2.5.3, eight samples are enough.

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12
Q

How do you know what quadrant to use

A

If you increase the size of the quadrat (eg from side length 10 cm to 15 cm, 20 cm and so on) and plot the number of species found, when this number reaches a constant, that is the quadrat size to use.

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13
Q

What 2 ways should a quadrat be placed

A
  1. Random quadrats may be placed by throwing the quadrat over your shoulder but we do not recommend this as it could be both dangerous and not random - you may decide where to throw.
    The conventional method (figure 2.5.4) is to use random number tables:
    • Map out your study area.
    • Draw a grid over the study area.
    • Number each square.
    • Use a random number table to identify which squares you need to sample.
  2. Stratified random sampling is used when there is an obvious difference within an area to be sampled and two sets of samples are taken.
    This study area (figure 2.5.5) has two distinctly different vegetation types and three separate areas to be studied. Samples need to be taken in each area.
    • Deal with each area separately.
    • Draw a grid for each area.
    • Number the squares in each area (they can be the same numbers or different).
    • Use a random number table to identify which squares you need to sample in each area.
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14
Q

Define transect

A

A transect is a sample path/ line/strip along which you record the occurrence and/ or distribution of plants and animals in a particular study area.

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15
Q

When might you use a transect

A

You might use this to look at changes in organisms as a result of changes along an environmental gradient, eg zonation along a slope, a rocky shore or grassland to woodland, or to measure the change in species composition with increasing distance from a source of pollution. Transects are quick and relatively simple to conduct.

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16
Q

What are the 2 main types of transect

A
  1. Line transect: consists of a string or measuring tape which is laid out in the direction of the environmental gradient and species touching the string or tape are recorded.
  2. Belt transect: this is a strip of chosen width through the ecosystem.
    It is made by laying two parallel line transects, usually 0.5 or 1 metre apart, between which individuals are sampled.
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17
Q

What are the 2 ways transect lines can be

A
  1. In a continuous transect (line or belt transect) the whole line or belt is sampled.
  2. In an interrupted transect (line or belt) samples are taken at points along the line or belt. These points are usually taken at regular horizontal or vertical intervals. This is a form of systematic sampling.
    Quadrats are placed at intervals along the belt.
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18
Q

What 2 things should you do when measuring abiotic components of a system

A
  1. Describe and evaluate methods for measuring these.
  2. Describe and evaluate how to measure spatial and temporal variations in abiotic factors.
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19
Q

How can salinity be measured

A

The salinity can be determined by measuring the electrical conductivity or the density of the water.

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20
Q

How can temperature have a significant impact on some organisms

A

Temperature affects the metabolic rates of marine organisms: this is due to the fact that many are ectothermic (their body temperature is
about the same as the surrounding water). Lower temperatures = low metabolic rates. So changes in temperature caused by thermal pollution may have a significant impact on some organisms.

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21
Q

What affects salinity of oxygen in water

A

• Temperature: higher temperatures = lower concentrations of dissolved oxygen. Many marine organisms rely on dissolved oxygen for respiration hence changes in temperature will impact the marine ecosystem.
• Water pollution: this can cause low oxygen concentrations and thus problems for marine organisms.

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22
Q

How can disolved oxygen be measured

A

Dissolved oxygen can be measured using an oxygen-selective electrode connected to an electronic meter, datalogging, or by a Winkler titration.
(A series of chemicals is added to the water sample and dissolved oxygen in the water reacts with iodide ions to form a golden-brown precipitate.
Acid is then added to release iodine which can be measured, and is proportional to the amount of dissolved oxygen, which can then be calculated.) Oxygen-selective electrodes give quick results, but need to be well maintained and calibrated in order to give accurate results. The Winkler titration is more labour intensive.

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23
Q

How does wave action affect an ecosystem

A

Wave action is important in coastal zones where organisms live close to the water surface. Areas with high wave activity usually have high concentrations of dissolved oxygen. Typical examples are coral reefs and rocky coasts.

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24
Q

What is turbidity

A

High turbidity = cloudy water
Low turbidity = clear water
The turbidity is important because it limits the penetration of sunlight and thereby the depth at which photosynthesis can occur. Turbidity can be measured with optical instruments or by using a Secchi disc.

25
Q

How can turbidity be measured

A

A Secchi disc is a white or black-and-white disc attached to a graduated rope. The disc is heavy to ensure that the rope goes vertically down. The procedure is:
1. Slowly lower the disc until it disappears from view.
2. Read the depth from the graduated rope.
3. Slowly raise the disc until it is just visible again.
4. Read the depth from the graduated rope.
5. Calculate the average depth. This depth is known as the Secchi depth.
For reliable results a standard procedure should be followed:
• Always stand or always sit in the boat.
• Always wear your glasses or always work without them.
• Always work on the shady side of the boat.
This should be repeated in the same spot 3-5 times.

26
Q

What is flow velocity

A

This is the speed at which the water is moving and it determines which species can live in a certain area.

27
Q

What 3 things does flow velocity vary with

A
  1. Time: melt water in the spring gives high flow rates, summer drought low flow rates.
  2. Depth: Surface water may flow more slowly than that in the middle of the water column.
  3. Position in the river: Inside bend has shallow slower-moving water, outside bend has deeper fast-moving water.
28
Q

What are the 3 basic methods for measuring flow velocity

A
  1. Flow meter: These are generally expensive and can be unreliable as mixing water with electricity has its problems.
  2. Impellers: a simple mechanical device as shown in figure 2.5.7:
    a. The impeller is mounted on a graduated stick and the base placed on the floor of the river / stream. The height of the impeller can be adiusted and the velocity measured at different depths, BUT it can only be used in clear shallow water, as you must be able to see the impeller.
    b. The impeller is held at the end of the side arm and lowered into the water facing upstream.
    c. The impeller is released and the time it takes to travel the distance of the side arm is measured.
    d. Repeat 3-5 times for accurate results.
  3. Floats
    The easiest way to measure flow velocity is to measure the time a floating object takes to travel a certain distance. The floating object should preferably be partly submerged to reduce the effect of the wind. Oranges and grapefruits make suitable floats. This method gives the surface flow velocity only. The average flow velocity of a river can be estimated from the surface flow velocity by dividing the surface velocity by 1.25.
29
Q

What is ph and how can it be measured

A

pH values of freshwater range from moderately acidic to slightly basic, depending on surrounding soil, rock and vegetation. It can be measured with a pH meter or datalogging pH probe.
For temperature and dissolved oxygen see marine ecosystems

30
Q

What is air temp and how can it be measured

A

Temperature varies temporally and spatially and can be measured using simple liquid thermometers, min-max thermometers, or more complex (electronic) thermometers. The latter equipment can be used to measure temperature continuously during a longer time as can a data-logging temperature probe.

31
Q

what is light intensity and how should it be measured

A

This can be measured with electronic meters. The fact that light intensity varies with time (sunny period, clouds, time of the day, season) should be taken into account.

32
Q

How should you measure wind speed

A

A revolving cup anemometer consists of three cups that rotate in the wind. The number of rotations per time period is counted and converted to a wind speed. Revolving cup anemometers can be mounted permanently or hand-held.
• A ventimeter is a calibrated tube over which the wind passes. This reduces the pressure in the tube, which makes a pointer move. It is easy to use and inexpensive.
• By observation of the effect of the wind on objects. The observations are then related to the Beaufort Scale (a scale of wind speed from 0 to 12).

33
Q

How can rainfall be collected

A

Rainfall can be collected using a rain gauge. Some schools have an established weather station - in which case collecting rainfall data is easy.
Many schools will not have a weather station but rain gauges are very easy to make and there are plenty of websites that can give you advice on how to make your own. Once you have made your rain gauge:
1. Place your rain gauge in a suitable spot in the study area - somewhere away from the influence of buildings, trees and other obstacles that may affect rainfall.
2. Check rain gauge every 24 hours - at the same time every day. Pour rain into a graduated cylinder and record daily amount of rainfall.

34
Q

LOOK AT TABLE ON 133 ON HOW TO MEASURE SOIL

A
35
Q

How can you measure soil moisture

A

This is the amount of water in the soil. It can be measured by drying soil samples.
1. Place a sample of the soil in a crucible.
2. Weigh it and record the weight.
3. Dry the sample.
Drying can be done in a conventional drying oven or a microwave oven.
In a conventional oven:
• Set the oven to 105 °C; hot enough to dry the soil but not so hot as to burn off organic matter.
• Leave for 24 hours and weigh the sample, repeat this until its mass becomes constant. This takes several days. In a microwave oven:
• Place the sample in the microwave for 10 minutes.
• Weigh the sample, and return to the oven for 5 minutes - repeat until its mass becomes constant.
A minimum of 3-5 samples should be tested.

36
Q

What are the serval functions of the organic content of soil.

A

• Supplies nutrients to the soil.
• Holds water (like a sponge).
• Helps reduce compaction and crusting.
• Increases infiltration.

37
Q

How can the organic content be determined

A

Organic content can be determined by the loss on ignition (LOI) method.
1. Dry the sample as above.
2. Heat the soil at high temperatures of 500 to 1,000 °C for several hours.
3. Weigh the sample and repeat this until its mass becomes constant.

38
Q

How do you measure the mineral content and ph levels in soil

A

Mineral content and pH
There is a wide range of soil nutrients essential for a fertile soil. These are easy to measure through traditional soil testing kits or the ones available in many gardening centres.
Soil pH can also be measured using a soil testing kit or a pH probe.

39
Q

What questions do we need to observe when measuring biotic content

A

• Why is it as it is?
• What has changed recently?
• Why does this grow here and not there?
• What impact do more people walking here have?
So walk around your institution’s grounds or the local

40
Q

How do you measure biomass and productivity for low vegetation and grasses

A
  1. Place a suitably sized quadrat (see figure 2.5.2).
  2. Harvest all the above-ground vegetation in that area.
  3. Wash it to remove any insects.
  4. Dry it at about 60-70°C until it reaches a constant weight. Water content can vary enormously so all the water should be removed and the mass given as dry weight.
  5. For accurate results this should be repeated 3-5 times so that a mean per unit area can be obtained.
  6. The result can then be extrapolated to the total biomass of that species in the ecosystem.
41
Q

How do you measure the biomass and productivity of trees and bushes

A
  1. Select the tree or bush you which to test.
  2. Harvest the leaves from 3-5 branches.
  3. And repeat steps 3-6 in the above method.
42
Q

How do you measure productivity in a aquatic ecosystem

A
  1. Take two bottles filled with water from the ecosystem.
    a. One of the bottles is made of clear glass.
    b. The other is of dark glass or is covered to exclude light.
  2. Measure the oxygen concentration of the water by chemical titration
    (Winkler method) or an oxygen probe, and record it as mg oxygen per litre of water.
  3. Place equal amounts of plants of the same species into each of the bottles.
  4. Both bottles must be completely filled with water and capped. (No air should be present.)
  5. Allow to stand and incubate for several hours.
  6. Measure the oxygen levels in both bottles and compare with the original oxygen level of the water. The incubation can take place in the laboratory or outdoors in the ecosystem of investigation.
43
Q

How do you measure productivity in a terrestrial ecosystem

A
  1. Select three equally sized patches with similar vegetation (eg grass).
  2. The first patch (A) is harvested immediately and the biomass measured (see above).
  3. The second patch (B) is covered with black plastic (no photosynthesis, just respiration).
  4. The third patch (C) is just left as it is.
  5. After a suitable time period (depends on the season), patches B and
    C are harvested and the biomass measured (as above).
  6. Now GPP, NPP and R can be calculated (usually per m?).
44
Q

What is a typical secondary productivity experiment

A

In a typical experiment, a herbivore is fed with a known amount of food. The procedure is that the food and the herbivore(s) are weighed. After a suitable time period, the remaining food, the herbivore(s) and the feces are weighed.

45
Q

What is a pitfall trap

A

The pitfall trap is ideal for catching insects and other small crawling animals that cannot fly away (see figure 2.5.10). Insects can be attracted by decaying meat or sweet sugar solution (this must be covered so the insects do not fall in it and drown) and will fall into the trap.Several of these traps can be placed around the study area. They should be checked at regular intervals (every 6 hours) and the species and number of that species recorded.

46
Q

What are sweep nets

A

Sweep nets of various sizes can be swept through grasses at various heights in order to catch many insects.
These can then be emptied into a large clear container and the species and numbers recorded.

47
Q

What is tree beating

A

This method can find insects in tree branches. Simply place a catching tray beneath a tree branch and gently tap the branch. The tray will catch anything that falls from the tree and you can log the species and their numbers. Night-flying moths will be attracted to a light behind which a white sheet is hung and the moths settle on this for you to observe.Small insects and invertebrates can be caught with a pooter - a small jar with two tubes attached (see figure 2.5.13). You suck gently on one tube and the animal is pulled into the jar. You cannot swallow it as there is gauze at the end of the mouthpiece tube!

48
Q

What is kick sampling

A

The organisms of most interest will be the stream invertebrates and the most efficient way to catch them is through kick samples.
Kick sampling is another simple technique:
• Place the sweep net downstream from you.
• Shuffle your feet into the streambed for 30 seconds.
• Empty the contents of the net into a tray filled with stream water.
• Use a pipette to sort the various insects into small plastic cups and record your results.
• Repeat three times to ensure good results.
In aquatic systems, nets of various mesh sizes and net sizes can be used to catch plankton, small invertebrates or larger fish. These can be towed behind boats or held in running water. Simple plastic sieves are effective. Kick sampling loosens invertebrates, which drift into the net. Turning stones over is also effective. Some of these methods are destructive and kill the organisms.
You may think this is not acceptable but most do not harm the organisms caught and you should always return them to their habitats if at all possible.

49
Q

What is a key

A

Once you have collected the organisms, you may want to find out what they are called. A (biological) key is used to identify species. Ecologists make keys to specific groups of organisms, eg soil invertebrates in specific ecosystems, to help other interested people identify species. Keys come in two formats, a diagrammatic, dichotomous or ‘spider’ key and a paired statement key.
Look at examples of published keys. Diagram keys are useful but professionals use paired statement keys because printed descriptions are more exact than pictures. Both keys are used by starting at the top each time and following the lines or ‘go to’ numbers.

50
Q

How do you measure abundance

A

There are a number of ways of assessing plant species abundance:
• Density: mean number of plants per m?.
• Frequency: the percentage of the total quadrat number that the species was present in, may also be measured within the quadrat.
• Percentage cover: because plants spread out and grow percentage cover is often measured instead of individual numbers. This is an estimate of the coverage by each species and it sometimes helps if the quadrat is divided up for this. Species may overlap or lie in different storeys in a forest, so the percentage cover within a quadrat may be well over 100% or much less if there is bare ground. The percentage cover can be estimated either by comparing the sample area with figure 2.5.16 and then it can be graded on a scale from 0 to 5, or on the ACFOR scale by using figure 2.5.17.

51
Q

What is the Lincoln index

A

Capture, mark, release recapture

52
Q

How is the Lincoln index taken out

A
  1. Establish the study area.
  2. Capture a sample of the population. The actual method of capture will depend on the size of animals; you can take your pick from the methods discussed earlier.
  3. Mark each of the organisms captured and record how many you have marked: this must be done in a non-harmful way that does not expose them to higher predation levels than non-marked individuals.
    For example, dog whelks on a rocky shore or woodlice in a woodland can be marked with a spot of non-toxic subtle coloured paint (nothing bright).
  4. Release the captured individuals back into the environment and allow sufficient time to remix with the population.
  5. Take a second sample in the same way as the first: count the number of organisms captured in this sample and count how many of them are marked. At least 10% of the marked sample should be recaptured if this estimate is going to be fairly accurate.
53
Q

What assumptions should be made when carrying out the Lincoln index

A

• Mixing is complete, ie the marked individuals have spread throughout the population.
• Marks do not disappear.
• Marks are not harmful nor increase predation by making the individual more easily seen.
• It is equally easy to catch every individual.
• There are no immigration, emigration, births or deaths in the population between the times of sampling.
• Trapping the organisms does not affect their chances of being trapped a second time.

54
Q

State the Lincoln index formula

A

M2/n2 = n1/N

N= n1xn2/ms
Where
n1= number of animals first marked and released
n2= number of animals captured in the second sample
m2= number of marked animals in the second sample
N = Lincoln Index or total population (the figure you are after)

55
Q

Define species diversity

A

Species diversity is a function of the number of species and their relative abundance.

56
Q

What is the Simpson’s diversity index

A

Ecologists try to express diversity in a number. The higher the number, the greater the species diversity. This makes it possible to compare similar ecosystems or to see whether ecosystems are changing in time. The most common way to turn diversity into a number is by the Simpson diversity index.

57
Q

What does the Simpson’s diversity index describe

A

But be careful. The name ‘Simpson diversity index’ actually describes three related indices (Simpson’s Index, Simpson’s index of diversity and Simpson’s reciprocal index). Here we are using Simpson’s reciprocal index in which 1 is the lowest value (when there would be just one species) and a higher value means more diversity. The highest value is equal to the number of species in the sample. In the other indices, the value ranges from 0 to 1.

58
Q

State the Simpson’s diversity formula

A

D=n(n-1)/sigma N (n-1)

D = Simpson diversity index
N = total number of organisms of all species found
n = number of individuals of a particular species

59
Q

LOOK AT EXAMPLE PAGE 141

A