Transcript Document

Upcoming Seminars:
• EECB seminars – 4:00 Thurs in OSN 102
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Thurs Feb 5: Jed Sparks (Cornell) “Vegetation-level
process controls on troposhperic chemistry”
Geography seminar – 4:00 Wed in Mackay
Science 215.
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Wed Feb 4: Alan Taylor (Penn State) “presettlement
Forests, Fire Regimes, and Climatic Influences in the
Tahoe Basin”
Outline
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Radiation: heat, light, and photosynthesis
Energy budgets
Energy capture and dissipation
Photosynthesis: Calvin cycle, photorespiration
Alternative photosynthetic pathways
Carbon accumulation, ecological implications
Radiation (electromagnetic waves)
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Short wave (solar radiation) <4um wavelength
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UV 10-400nm (@ Earth’s surface 292-400)
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Potentially damaging to biological systems
Visible 400-700nm
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Near infrared 0.7-4.0um (and far red visible)
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Source of most energy for life on earth
“shade detector” pigment phytochrome absorbs 660nm and
730nm
Can cause inhibition of germination etc.
Long wave: far IR; heat.
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Heat is energy from objects (molecular motion).
Energy budgets
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Energy cannot be created or destroyed
Net=met+solar+thermal+conv+cond+LE+storage
Plants absorb PAR and reflect or transmit non-PAR
Use only a fraction of energy absorbed (2%); must
dissipate the rest
Angle of incidence determines energy intercepted.
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Paraheliotropic=leaf parallel to sun’s rays
Diaheliotropic=leaf perpendicular to sun’s rays
Sun VS shade leaves: different morphology
Albedo, laminar flow, reduced leaves
Energy effects
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Light or temperature mediated plant responses:
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Germination/seed dormancy (light)
Thermoperiodism (buds, seeds) temp differential induces
dormancy or activity
Dormancy – end of dormancy triggered by photoperiod or
temperature
Temperature stratification of seeds (hot or cold)
Physical rupture of seed coat (fire)
Energy capture: photosynthesis
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Leaves absorb light between 400 and 700nm
Energy is captured through an electron transfer
chain (“light reactions”)
Carbon dioxide is fixed into carbohydrate (“dark
reactions”) using energy captured in light
reactions
Calvin cycle (C3) prone to photorespiration (lightmediated release of CO2)
Level of photorespiration depends on CO2:O2
Electron transport
Calvin cycle
C4 Photosynthesis
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Means to concentrate CO2 and reduce
photorespiration. Requires energy (ATP) and
special anatomy (Kranz)
CO2 fixed in mesophyll cells to form a 4-carbon
acid (oxaloacetate)
C4 chain diffuses to bundle sheath cells,
releases CO2, C fixation occurs ‘normally’.
Higher light compensation point than C3, and
greater water use efficiency.
CAM Photosynthesis
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Temporally separates light and ‘dark’ reactions
Succulents
At night stomata open; plants fix CO2 to malic or
isocitric acid (4-carbon). Uses ATP.
Acid stored in large cell vacuole.
During day stomata close, CO2 released, and
fixed in “C3 type fixation”
Plants with this pathway are not always obligate
CAM – can switch to C3.
Environmental differences
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CO2 compensation lower for C4 than C3 (can
have higher stomatal resistance and still fix C)
Light saturation higher for C4 than C3 (reduced
photorespiration)
Light use efficiency highest for C4 monocots.
C4 uses energy; less efficient at lower light and
temperatures
Water stress: C4 more efficient than C3, CAM
can switch to C3 (less energy) when water
available
Ecological implications
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Timing of rainfall and nutrient availability affect
composition. How?
What are differences in radiation impacts in
forest VS rangeland?
What would effects of global climate change and
CO2 enrichment be?
How might plants with different photosynthetic
pathways be distributed?
Ecological implications
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Timing of rainfall and nutrient availability affect
composition. N availability affects photosynthetic
rates.
Herbivory and “overcompensation” – dependent
on N availability?
What are differences in radiation impacts in
forest VS rangeland?
What would effects of global climate change and
CO2 enrichment be?