Review 4.2 energy flow
Review 2.1 molecules to metabolism
Essential idea: Continued availability of carbon in ecosystems depends on carbon cycling.
If energy is continually entering and exiting ecosystems what about the raw building materials?
Exercise 1: Think-Pair-Share:
What are the building blocks of cells, organelles and molecules? What is the basic unit of matter?
Where do these units come from? How are they made?
Is there an infinite or finite number of them available on the planet do you think? Why?
A1: Estimation of carbon fluxes due to processes in the carbon cycle.
Guidance:
Carbon fluxes should be measured in gigatonnes.
Exercise 2: Answer these questions:
What is flux?
What materials tend to have fluxes?
If carbon is normally a solid, how does it have a flux?
What processes cause carbon to flux?
What is the relative size in gigatonnes of these processes?
Why is carbon flux measured in gigatonnes and why are they estimated and not measured directly? What does this do to the uncertainty in the measurements?
A2: Analysis of data from air monitoring stations to explain annual fluctuations.
NoS: Making accurate, quantitative measurements—it is important to obtain reliable data on the concentration of carbon dioxide and methane in the atmosphere. (3.1)
Exercise 3:
Describe the changes that you can see in the graph.
Explain the trends.
U1: Autotrophs convert carbon dioxide into carbohydrates and other carbon compounds.
U2: In aquatic ecosystems carbon is present as dissolved carbon dioxide and hydrogencarbonate ions.
U3: Carbon dioxide diffuses from the atmosphere or water into autotrophs.
U4: Carbon dioxide is produced by respiration and diffuses out of organisms into water or the atmosphere.
U5: Methane is produced from organic matter in anaerobic conditions by methanogenic archaeans and some diffuses into the atmosphere or accumulates in the ground.
U6: Methane is oxidized to carbon dioxide and water in the atmosphere.
U7: Peat forms when organic matter is not fully decomposed because of acidic and/or anaerobic conditions in waterlogged soils.
U8: Partially decomposed organic matter from past geological eras was converted either into coal or into oil and gas that accumulate in porous rocks.
U9: Carbon dioxide is produced by the combustion of biomass and fossilized organic matter.
U10: Animals such as reef-building corals and mollusca have hard parts that are composed of calcium carbonate and can become fossilized in limestone.
Exercise 4: Convert each of these understandings into a little diagram
S1: Construct a diagram of the carbon cycle.
Exercise 5: Connect each of your pictures together with arrows labelled as the processes that move carbon from one area to another