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Do Now
1. Define trophic level.
2. What are producers? Give an example.
3. What is a heterotrophic organism? Give an example.
4. What is pyramid of numbers?
5. Explain the difference between a pyramid of biomass and productivity. (Hint: think of the grocery store analogy)
6. Why are aquatic biomass pyramids typically inverted?
7. Why do you think food chains seldom have more than four trophic levels? (Why are the number of tertiary consumers relatively low in an ecosystem?)
Practice
• Complete the To Do activity on page 74 using graph paper
• Answer To Do questions (#1-3) on page 76
• On a piece of computer paper, construct three food chains (4 trophic levels), a food web, a pyramid of numbers, a pyramid of biomass, and a pyramid of productivity for one of the following ecosystems. You may need to research some information.
Warm-water ocean Temperate Forest Mountain
Arctic ocean JunglePrairie
Pond RiverDesert
Lake TundraSavannah
Practice Continued
Label the food chains and food web with the following:
Producer(s) = P
Primary consumer(s) = 1
Secondary consumer(s) = 2
Tertiary consumer(s) = 3
Herbivores = H
Carnivores = C
Omnivores = O
On your productivity pyramid, label the amount of energy available to each organism based on their trophic level
Need to research average total energy for the main producer in your ecosystem (For example: the total energy in a grassland producer was found to be 400 kJm-2 y-1)
Do Now
Study Ecosystem Structure. You have a quiz
today!
Abiotic Stations
Rotate through 5 stations as intro to abiotic factors
Station 1: Simulation on Temperature
Station 2 & Station 3: Reading Articles
Station 4 & Station 5: Watching Videos 10 min at each station. You will be directed
when to rotate. Use your time wisely. You must answer all
questions. You will be tested on this information.
2.2 Measuring Abiotic Components
OBJECTIVE 2.2
•Marine system – the sea, salt marshes, mangrove swamps and saline estuaries•Fresh water lakes and rivers•Terrestrial systems – land based
Three main types of ecosystem:
Marine System
Key Factors:•Salinity•Temperature•pH•Dissolved oxygen content (mg/L)•Wave Action
Temperature: Marine
Temperature probes (water, soil, air)
Determines the amount of oxygen which will dissolve in sea water which will become available to marine organisms
Affects metabolic rate
Surface waters warmer than deeper water which affects ocean currents
Dissolved Oxygen: Marine
Dissolved oxygen needed for respiration
O2 + C6H12O6 CO2 + H2O + ATP
Warmer water = less dissolved oxygen
Measured by using electrodes
Wave Action: Marine
Measured using a dynamometer which asses the force in waves
Wave action increases the amount of dissolved oxygen by mixing air with water
Coastal areas and coral reefs have high levels of dissolved oxygen
Fresh-Water Ecosystem
Key Factors:
•Turbidity •pH•Flow velocity•Temperature•Dissolved oxygen
Turbidity: Freshwater
Measure of cloudiness of water
Cloudy = high turbidity
Clear = low turbidity
Secchi disc is used to measure turbidity: lowered into the water until disappears from view
Depth reading is taken from the pole
Repeated for accuracy
Always be taken in the same light
Turbidity affects sunlight penetration which influences rate of photosynthesis
https://www.youtube.com/watch?v=yGJ5uV4jAPo
Flow Velocity: Freshwater
Observe surface water
Measure by taking the time for any floating object to pass a fixed distance between two marked points
Varies at different depths
More accurate using a flow-meter which is a calibrated propeller attached to a rod
Velocity determines which organisms can survive in flowing water
High velocity = plants and animals firmly anchored
Temperature/Dissolved Oxygen: Freshwater
Temperature affects the amount of dissolved oxygen in a lake or stream and the amount of oxygen which can remain dissolved
Warm water speeds up plant growth but increases the rate of decomposition reduces the water’s ability to hold oxygen
Minimum of 5 gm-3 oxygen is needed to support a balanced aquatic community
Water agitation (waterfalls) increases dissolved oxygen
pH: Marine and Freshwater
pH meter or probe
Cleaned between readings
Used at same depth.
Soil uses soil test kit – indicator added and compared to chart.
Terrestrial Ecosystems
Key Factors:
•Temperature•Light Intensity•Soil moisture content•Wind speed•Soil particle size•Soil mineral content•Slope•Drainage
Light Intensity: Terrestrial
Measured with a light meter
Intensity varies throughout the day
Dependent on cloud cover and season
Soil Moisture Content: Terrestrial
Measure by weighing soil samples before and after drying
Soil contains moisture and organic matter
Soil samples are heated to remove water
Samples weighed at intervals until a constant dry weight is reached
Wind Speed: Terrestrial
Measured with a digital anemometer
Cups on device revolve = rotations per unit time
Soil Particle Size: Terrestrial
Determines how much water soil can hold and how quickly the soil will drain
Passed through series of graduated sieves with different mesh sizes
Silt and clay are smaller
Soil Mineral Content: Terrestrial
Ratio of mineral to organic material present Organic content: plant and animal
residues in various stages of decay
Determines the soil’s ability hold water and its fertility
Measured by the loss-on-ignition (LOI) method Weighed soil samples are heated
organic matter is burnt off
Loss in mass is calculated once the sample has reached constant mass and no further change
Percentage weight lost gives a crude measure of the organic content of the soil
Slope: Terrestrial
Influences water runoff
Determines whether erosion is likely to be a problem
Drainage: Terrestrial
Too much or too littler water in soil can reduce plant growth
Drainage affected by soil type, humus content, and slope
Poor drainage = soil becomes water logged plants are unable to take up nutrients
Toxic compounds build up due to lack of oxygen (anaerobic conditions)
Slower to warm up in spring and summer inhibits germination and growth of seeds