UNIT ____: Carbon Cycle                                 Name: ________________________

Essential Idea(s):

Continued availability of carbon in ecosystems depends on carbon cycling.

IB Assessment Statements and Class Objectives

4.1.U9:  Autotrophs and heterotrophs obtain inorganic nutrients from the abiotic environment.

4.1.U10:  The supply of inorganic nutrients is maintained by nutrient recycling.

4.3.A1:  Estimation of carbon fluxes due to processes in the carbon cycle.

4.3.U3:  Carbon dioxide diffuses from the atmosphere or water into autotrophs.

4.3.U1:  Autotrophs convert carbon dioxide into carbohydrates and other carbon compounds.

4.3.U4:  Carbon dioxide is produced by respiration and diffuse out of organisms into water or the atmosphere.

4.3.U5:  Methane is produced from organic matter in anaerobic conditions by methanogenic archaea and some diffuses into the atmosphere or accumulates in the ground.

4.3.U6:  Methane is oxidized to carbon dioxide and water in the atmosphere

4.3.U7:  Peat forms when organic matter is not fully decomposed because of acidic and/or anaerobic conditions in waterlogged soils.

4.3.U8:  Partially decomposed organic matter from past geological eras was converted either into coal or into oil and gas that accumulate in porous rocks.

4.3.U9:  Carbon dioxide is produced by combustion of biomass and fossilized organic matter.

4.3.A2:  Analysis of data from air monitoring stations to explain annual fluctuations.

4.3.U2:  In aquatic ecosystems carbon is present as dissolved carbon dioxide and hydrogen carbonate ions.

4.3.U10:  Animals such as reef-building corals and Mollusca have hard parts that are composed of calcium carbonate and can become fossilized in limestone.

4.3.S1:  Construct a diagram of the carbon cycle.

Nutrient Cycles

The Carbon Cycle

The carbon cycle is the biogeochemical cycle by which carbon is exchanged among the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere of the Earth. Carbon is the main element found in biological compounds as well as a major component of many minerals such as limestone.

Carbon moves between POOLS via eight FLUX processes.


Global carbon fluxes are estimated in gigatons of carbon per year

FLUX

PROCESS

DESCRIPTION

1

Photosynthesis*

2

Respiration

3

Decomposition

4

Diffusion

5

Lithification

6

Combustion

7

Fossilization

8

Feeding

Fossil Fuels

Combustion

                


Methanogenic Archaea

Methanogens are prokaryotic cells in the domain Archaea that produce methane as a byproduct of their anaerobic respiration.  Methane is oxidized in the atmosphere to form CO2 and H2O.

Prokaryotic cells:

Domain Archaea:

Methane:

Anaerobic respiration:

Oxidation:

Seasonal CO2 Fluctuations in the Northern Hemisphere

      J    F    M    A    M    J    J    A    S    O    N    D

CO2 in H2O

In plain water (neutral pH), dissolved calcium ions (Ca2+) will bond with the carbonate (CO32-) to form calcium carbonate which is used by marine animals to form shells.

               

OCEAN ACIDIFICATION:

With more CO2 diffusing into the water, the acidity of the solution increases and the solubility of calcium carbonate increases .  This dissolves the calcium carbonate in the solid shell into calcium ions and carbonate ions in the surrounding ocean water.