Nutrient Cycling and Chapter 19 Retention 11 Outline

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Nutrient Cycling and Chapter 19 Retention 11

Nutrient Cycling and Chapter 19 Retention 11

Outline n Nutrient Cycles q q q n Rates of Decomposition q q n

Outline n Nutrient Cycles q q q n Rates of Decomposition q q n n Phosphorus Nitrogen Carbon Terrestrial Aquatic Organisms and Nutrients Disturbance and Nutrients 22

Phosphorus Cycle n Global phosphorus cycle does not include substantial atmospheric pool. q Largest

Phosphorus Cycle n Global phosphorus cycle does not include substantial atmospheric pool. q Largest quantities found in mineral deposits and marine sediments. n q Much of this in forms not directly available to plants. Slowly released in terrestrial and aquatic ecosystems via weathering of rocks. 33

Phosphorus Cycle 44

Phosphorus Cycle 44

Nitrogen Cycle n Includes major atmospheric pool - N 2. q Only nitrogen fixers

Nitrogen Cycle n Includes major atmospheric pool - N 2. q Only nitrogen fixers can use atmospheric supply directly. n Energy-demanding process. q n N 2 reduced to ammonia (NH 3). Once N is fixed it is available to organisms. q Upon death of an organism, N can be released by fungi and bacteria during decomposition. 55

Nitrogen fixation Biological Nitrogen Fixation (BNF) occurs when atmospheric nitrogen is converted to ammonia

Nitrogen fixation Biological Nitrogen Fixation (BNF) occurs when atmospheric nitrogen is converted to ammonia by a pair of bacterial enzymes n. N 2 + 8 H+ + 8 e− + 16 ATP → 2 NH 3 + H 2 + 16 ADP + 16 Pi 66

Nitrogen Cycle Microbes Denitrification NO 3(nitrate) → NO 2 - → NO → N

Nitrogen Cycle Microbes Denitrification NO 3(nitrate) → NO 2 - → NO → N 2 gas 77

Carbon Cycle n Moves between organisms and atmosphere as a consequence of photosynthesis and

Carbon Cycle n Moves between organisms and atmosphere as a consequence of photosynthesis and respiration. q q In aquatic ecosystems, CO 2 must first dissolve into water before being used by primary producers. Although some C cycles rapidly, some remains sequestered in unavailable forms for long periods of time. 88

Carbon Cycle 99

Carbon Cycle 99

Rates of Decomposition n Rate at which nutrients are made available to primary producers

Rates of Decomposition n Rate at which nutrients are made available to primary producers is determined largely by rate of mineralization (organic to inorganic). q Occurs primarily during decomposition (breakdown of organic matter). n Rate in terrestrial systems is significantly influenced by temperature, moisture, and chemical compositions. 10 10

Fig. 19. 5 Decomposition in two Mediterranean woodland ecosystems Difference in annual rainfall due

Fig. 19. 5 Decomposition in two Mediterranean woodland ecosystems Difference in annual rainfall due to elevation Litter chemistry on rates of decomposition 11 11

Decomposition in Temperate Woodland Ecosystems n Gallardo and Merino found differences in mass loss

Decomposition in Temperate Woodland Ecosystems n Gallardo and Merino found differences in mass loss by the target species reflected differences in the physical and chemical characteristics of their leaves. 12 12

Fig. 19. 7 Inc. N and Dec. Lignin had Higher decomposition Inc lignin to

Fig. 19. 7 Inc. N and Dec. Lignin had Higher decomposition Inc lignin to nitrogen Loss less mass 13 13

Decomposition in Temperate Forest Ecosystems n Melillo et. al. used litter bags to study

Decomposition in Temperate Forest Ecosystems n Melillo et. al. used litter bags to study decomposition in temperate forests. q Found leaves with higher lignin: nitrogen ratios lost less mass. n Suggested higher N availability in soil might have contributed to higher decomposition rates. q Higher environmental temperatures may have also played a role. 14 14

Decomposition in Aquatic Ecosystems n Gessner and Chauvet found leaves with a higher lignin

Decomposition in Aquatic Ecosystems n Gessner and Chauvet found leaves with a higher lignin content decomposed at a slower rate. q n Higher lignin inhibits fungi colonization of leaves. Suberkropp and Chauvet found leaves degraded faster in streams with higher nitrate concentrations. 15 15

Decomposition in Aquatic Ecosystems 16 16

Decomposition in Aquatic Ecosystems 16 16

Animals and Nutrient Cycling in Terrestrial Ecosystems n n Huntley and Inouye found pocket

Animals and Nutrient Cycling in Terrestrial Ecosystems n n Huntley and Inouye found pocket gophers altered N cycle by bringing N-poor subsoil to the surface. Mac. Naughton found a positive relationship between grazing intensity and rate of turnover in plant biomass in Serengeti Plain. q Without grazing, nutrient cycling occurs more slowly through decomposition and feeding of small herbivores. 17 17

Animals and Nutrient Cycling in Terrestrial Ecosystems 18 18

Animals and Nutrient Cycling in Terrestrial Ecosystems 18 18

Plants and Ecosystem Nutrient Dynamics n Fynbos is a temperate shrub/woodland known for high

Plants and Ecosystem Nutrient Dynamics n Fynbos is a temperate shrub/woodland known for high plant diversity and low soil fertility. q n Two species of Acacia used to stabilize shifting sand dunes. Witkowski compared nutrient dynamics under canopy of native shrub and introduced acacia. q q Amount of litter was similar, but nutrient content was significantly different. Acacia - N fixer 19 19

Introduced Tree and Hawaiian Ecosystem n Vitousek and Walker found invading N-fixing tree Myrica

Introduced Tree and Hawaiian Ecosystem n Vitousek and Walker found invading N-fixing tree Myrica faya is altering N dynamics of Hawaiian ecosystems. q Introduced in late 1800’s as ornamental or medicinal plant, and later used for watershed reclamation. n Nitrogen fixation by Myrica large N input. q Leaves contain high N content. § High decomposition rate. 20 20

Disturbance and Nutrient Loss From the Hubbard Brook Forest n Vitousek studied effects of

Disturbance and Nutrient Loss From the Hubbard Brook Forest n Vitousek studied effects of disturbance and environmental conditions on N loss. q Trenching increased concentrations of nitrate in soil water up to 1, 000 x. n Nitrate losses are generally greatest at sites with rapid decomposition. q Uptake by vegetation is most important in ecosystems with fertile soils and warm, moist conditions. 21 21

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