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Matter cycles • Organisms are reservoirs of these atoms, in various forms • Organisms are part of the cycling of these atoms, via various metabolic processes.

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Presentation on theme: "Matter cycles • Organisms are reservoirs of these atoms, in various forms • Organisms are part of the cycling of these atoms, via various metabolic processes."— Presentation transcript:

1 Matter cycles • Organisms are reservoirs of these atoms, in various forms • Organisms are part of the cycling of these atoms, via various metabolic processes

2 water cycle Reservoir: most locked in oceans; limited fresh water for life

3 water cycle Abiotic: evaporation, condensation, precipitation cycle
• transpiration – water moves through plants from roots to leaves, then to atmosphere; keeps plants upright • moved into organic molecules via photosynthesis • produced in respiration as sugars -> ATP

4 carbon cycle Reservoir: • CO2 in the atmosphere
(0.03% of atmospheric gases) • A greenhouse gas, blocking the escape of long wavelength terrestrial radiation • Increased CO2 is correlated with increased global temperatures

5 carbon Biotic: • C brought into ecosystem producers, as CO2, via photosynthesis • Transferred between organisms in feeding relationships and returned to abiotic reservoirs via respiration • Incomplete decomposition created organic C deposits - the non-renewable, CO2 releasing fuels of today Abiotic: • CO2 in atmosphere • oceans are CO2 sinks, but how much? H20 + CO2 -> carbonic acid

6 phosphorous Reservoir: locked in rocks & sediment

7 phosphorous Biotic: • Stored in organisms in cell membranes, ATP, nucleic acids • Low availability limits plant growth Abiotic: • continental rocks & sea floor sediments • slow release means limited availability in in soil

8 nitrogen Reservoir: N2 in atmosphere

9 nitrogen Biotic: • Used by organisms to construct proteins, nucleic acids Abiotic: • atmospheric form (N2) inaccessible to most organisms • little available in soil

10 nitrogen • or NH4+ ->N2 released to the atmosphere Denitrification
• Bacteria in legume roots turn N2 -> NH3 creating soil source of N for plants nitrogen-fixation 4 1 2 3 • In decomposition organically-bound N -> NH4+ ions ammonification • NH4+ -> nitrates/ nitrates in soil to be used by more plants nitrification

11 eutrophication • P, N are limiting factors for plant growth, therefore add to fertilizers • runoff introduces P, N to waterways, causing excessive plant growth, aka eutrophication • subsequent decomposition of plant mass robs water of oxygen, affecting fish and aquatic invertebrate populations

12 eutrophication


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