plant ecology - chapter 14

31
Plant Ecology - Chapter 14 Ecosystem Processes

Upload: raymond-dickson

Post on 30-Dec-2015

64 views

Category:

Documents


2 download

DESCRIPTION

Plant Ecology - Chapter 14. Ecosystem Processes. Ecosystem Ecology. Focus on what regulates pools (quantities stored) and fluxes (flows) of materials and energy in abiotic and biotic components. Ecosystem Ecology. Turnover time - how rapidly does it move through the system - PowerPoint PPT Presentation

TRANSCRIPT

Page 1: Plant Ecology - Chapter 14

Plant Ecology - Chapter 14

Ecosystem Processes

Page 2: Plant Ecology - Chapter 14

Ecosystem Ecology

Focus on what regulates pools (quantities stored) and fluxes (flows) of materials and energy in abiotic and biotic components

Page 3: Plant Ecology - Chapter 14

Ecosystem Ecology

Turnover time - how rapidly does it move through the systemRetention time - how long does it reside in a component

Page 4: Plant Ecology - Chapter 14

Ecosystem Ecology

Pools, fluxes connected together into biogeochemical cyclesBiology, geology, chemistry interconnected

Page 5: Plant Ecology - Chapter 14

Ecosystem Ecology

Plants under the influence of some cycles, influence othersWater, oxygen, carbon, nitrogen, phosphorus, sulfur, potassium

Page 6: Plant Ecology - Chapter 14

Water Cycle

Page 7: Plant Ecology - Chapter 14

Water Cycle

Terrestrial plants are only living things to have significant effect on water cycleEvapotranspiration from plants can provide huge proportion of moisture in atmosphere - affect rainfall patterns

Page 8: Plant Ecology - Chapter 14

Water Cycle

Cutting rainforests can result in decreased evapotranspiration, decreased rainfall, increased air temperatures at ground surface

Page 9: Plant Ecology - Chapter 14

Water Cycle

Since plants intercept rainfall, reduce its impact on ground, removing vegetation can alter infiltration/runoff relations

Page 10: Plant Ecology - Chapter 14

Water Cycle

Even removing vegetation in semi-arid regions can reduce rainfall, increase soil temperatures, induce onset of desertification

Page 11: Plant Ecology - Chapter 14

Water CycleFlux differencesamong, within biomes

Page 12: Plant Ecology - Chapter 14

Water Cycle

Potential evapotranspiration (PET) - water lost via this process if water is freely available and plant cover is 100%Actual evapotranspiration (AET) - precipitation minus runoff and infiltrationPET>AET in dry climatesPET=AET in intact tropical rain forestsAET linked to productivity, decomposition

Page 13: Plant Ecology - Chapter 14

Carbon CyclePrimary productivity - rate oftransfer of inorganic C fromatmosphere into organic Cin plants via photosynthesis

Page 14: Plant Ecology - Chapter 14

Carbon Cycle

NPP -dry metric tons/ha/yr

Page 15: Plant Ecology - Chapter 14

ProductivityDifferent ecosystems -related to leaf biomass

Different forests - latitude,climate, elevation

Page 16: Plant Ecology - Chapter 14

Productivity

Page 17: Plant Ecology - Chapter 14

Estimating Productivity

Standing biomass after a growing seasonDrawbacks: destructive, and ignores belowground productivity (can be majority in some plants)

Page 18: Plant Ecology - Chapter 14

Estimating Productivity

Indirect measures: develop formulae for relating plant size changes to biomass changesAllometric relationships used by timber companies, forest ecologistsDrawback: formula needed for each species

Page 19: Plant Ecology - Chapter 14

Estimating Productivity

Indirect measures: use relation between productivity and AETFairly good estimates of productivity over broad range of climatesDrawback: poor predictor of productivity where precipitation and temperature are both high

Page 20: Plant Ecology - Chapter 14

Estimating Productivity

Remote sensing - use reflectance of light wavelengths by chlorophyll to estimate productivityNormalized difference vegetation index (NDVI) - good correlation between NDVI and NPP ground measurements

NDVI = NIR-VIS NIR+VIS

Page 21: Plant Ecology - Chapter 14

DecompositionDead stuff becomes soil organic matter, then viamineralization becomes inorganic nutrients, CO2,water, and energy

Page 22: Plant Ecology - Chapter 14

Decomposition- Saprophytic fungi are the major decomposers of dead leaves, plant litter- Bacteria also essential, but only in latter stages

Page 23: Plant Ecology - Chapter 14

Decomposition

Decomposition largely an aerobic process - very slow in waterlogged, cold soilsPhysical, chemical characteristics also affect rate of decomposition

Root decomposition ofsoft and hardwoods

Page 24: Plant Ecology - Chapter 14

Net Ecosystem Production

NEP is net accumulation of carbon per year by ecosystemPositive during growing season, negative during non-growing season

Page 25: Plant Ecology - Chapter 14

Net Ecosystem Production

Undisturbed ecosystems usually show small, positive accumulations of C each yearAccumulation of woody tissue in long-lived plants

Page 26: Plant Ecology - Chapter 14

Soil Carbon: Pools and Fluxes

Page 27: Plant Ecology - Chapter 14

Nitrogen & Productivity

Page 28: Plant Ecology - Chapter 14

Nitrogen Cycle- Rapid flux through living organisms- Large global pool with slow turnover

Page 29: Plant Ecology - Chapter 14

Phosphorus Cycle- Does not have major atmospheric pool like other cycles- Mostly recycled in organic form through other living organisms

Page 30: Plant Ecology - Chapter 14

Calcium Cycle

Sedimentary cycleNeeded by plants for chemical (growth, stress regulation), structural (support) rolesLargely lost in leaf fall - must be replaced each year

Page 31: Plant Ecology - Chapter 14

Calcium Cycle

Calcium depletion occurring in many forests todayAcid deposition displaces soil calcium, logging removes itDecreased growth, higher mortality (more susceptible to pathogens)