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Ch. 9. Aquatic ecosystems and Physiology: Energy Flow Productivity Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled with functional groups, measured as calories of energy, or moles of chemicals, biomass, or numbers.
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Ch. 9. Aquatic ecosystems and Physiology: Energy Flow Productivity Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Jan 04, 2016

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Page 1: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Ch. 9.Aquatic ecosystems

and Physiology:

Energy Flow Productivity Dissolved Oxygen

Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled with functional groups, measured as calories of energy, or moles of chemicals, biomass, or numbers.

Page 2: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Fig 1.14a. Energy flow model of Cedar Bog Lake, Minnesota (Lindeman 1942)

Page 3: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Food Web Model:

Boxes are filled with SPECIES.

Page 4: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Fig 1.14b. Energy flow model of Silver Springs, Florida (Odum 1971)

Page 5: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

PRIMARY PRODUCTIVITY: PHOTOSYNTHESIS

Fig. 9.4.

NPP = GPP – Respiration

Page 6: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

The world's ecosystems vary tremendously in productivity.

In terms of NPP per unit area, the most productive systems are estuaries, swamps and marshes, tropical rain forests, and temperate rain forests

To calcualte the total amount of NPP in the world, these values must be multiplied by the area that the various ecosystems occupy.

The most productive systems are open oceans, tropical rain forests, savannas, and tropical seasonal forests

http://www.globalchange.umich.edu/globalchange1.html

Page 7: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Horne and Goldman 1994

Page 8: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Horne and Goldman 1994

Page 9: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Kalff 2002

Page 10: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Horne and Goldman 1994

Page 11: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Importance of dissolved oxygen in aquatic systems

• Affect the distribution of aerobic heterotrophic life

• Impacts the solubility of phosphorus and other nutrients

• Influences redox potential (Ch. 10) and thus the solubility of redox-sensitive materials

• May be used to estimate ecosystem productivity

Page 12: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Photo-inhibition

Page 13: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Productivity may be measured in units of mgC volume-1 time-1

Because it takes two moles of O2 to fix 1 mole of C, productivity may also be measured in units of mgO2 volume-1 time-1

CO2 + H2O CH2O + O2

Ratio of moles of C to moles of oxygen = 12/32 = 0.375; i.o.w. 1 mg O2 produced = 0.375 mg C fixed

Examples of productivity measurement techniques:

Light - dark bottles

Diel cycles in oxygen levels

14C uptake

Page 14: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Lingeman and Ruardij, 1981

PN=PG-R

R

Page 15: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Kalff 2002

Page 16: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Kalff 2002

Page 17: Ch. 9. Aquatic ecosystems and Physiology: Energy Flow  Productivity  Dissolved Oxygen Fig. 9.1. Hypothetical Trophic Structure Model. Boxes are filled.

Kalff 2002