Fundamental of Ecology Lec11 Carbon Cycles Hand2003

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  • 8/9/2019 Fundamental of Ecology Lec11 Carbon Cycles Hand2003

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    1.018/7.30J Fall 2003Fundamentals of Ecology

    Lecture 11 Carbon Cycle

    Bentley M. 2003. Synthetic trees could purify air. BBC.http://news.bbc.co.uk/2/hi/science/nature/2784227.stm. accessed 10/10/03

    Whitehouse D. 2003. Photosynthesis puzzle solved. BBC.http://news.bbc.co.uk/2/hi/science/nature/3174582.stm. accessed 10/10/03

    Global climate change articles (handed out last class)

    READINGS FOR NEXT LECTURE:

    Outline for today:

    I. Finish S cycle / Stable Isotope AnalysesII. Global Carbon Cycle

    A. C in the newsB. Global cycleC. Carbon and temperatureD. Ecological effects of increasing CO2

    The Global Carbon Cycle

    Burial

    0.1

    Ocean

    38,000

    92 90

    Atmospheric Pool

    750

    +3.2/yr

    Soils

    1500 Net destructionof vegetation

    0.90.9

    12060

    GP PRp

    60

    6

    Rivers

    0.8

    Land s

    560plant

    Reference: Schlesinger, 1997

    Pools (101 5 g C)Fluxes (1015g C/yr) Rocks

    81,000,000Fossil Fuels

    4000

    fossil fu elburning

    The Global Carbon Cycle

    Burial

    0.1

    Ocean

    38,000

    9092

    Atmospheric Pool

    Soils

    1500Pools (101 5 g C)Fluxes (1015g C/yr)

    Net destruction

    of vegetation

    Rocks

    81,000,000Fossil Fuels

    4000

    Rivers

    0.8

    12060

    GP PRp

    60

    6

    Land s

    560plant

    fossil fu elburning

    +3.2/yr

    750

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    Measured changes in CO2 dissolved on the surface of the Atlantic ocean.

    Adapted from: Schlesinger, 1997 (Figure 9.10)

    Adapted from Krebs, Fig. 28.13 Adapted from Krebs, Fig. 28.11Trees from Arizon, North Carolina and Italy

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    Concentration of CO2 at Mauna Loa Observatory Long-term variation in global temperatureIn Hawaii. Adapted from Krebs Fig 28.9. and atmospheric CO2 concentration

    determined from the Vostok Ice Core,Antarctica. Adapted from Krebs. Fig. 28.15

    Temperatures Relative to Millenial Average*. Adapted from Mann et.al., 1999

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    Its not just CO2

    Fuels,

    fertilizer,deforestation

    62300.20.31Nitrous

    oxide

    Wetlands,

    rice,livestock,

    fossil fuels

    122511.675Methane

    Foams,

    aerosols,solvents,

    refrigeration

    2515 00050.00225CFCs

    Fossil fuels,

    deforestation

    5710.4351Carbon

    dioxide

    Principal

    sources of

    gas

    Current

    GreenhouseContribution

    (%)

    Relative

    greenhouseefficiency

    (CO2 = 1)

    Annual

    ConcentrationIncrease

    (%)

    Atmospheric

    Concentration

    (ppm)Gas

    Fuels,

    fertilizer,deforestation

    62300.20.31Nitrous

    oxide

    Wetlands,

    rice,livestock,

    fossil fuels

    122511.675Methane

    Foams,

    aerosols,solvents,

    refrigeration

    2515 00050.00225CFCs

    Fossil fuels,

    deforestation

    5710.4351Carbon

    dioxide

    Principal

    sources of

    gas

    Current

    GreenhouseContribution

    (%)

    Relative

    greenhouseefficiency

    (CO2 = 1)

    Annual

    ConcentrationIncrease

    (%)

    Atmospheric

    Concentration

    (ppm)Gas

    Source: Schlesinger, 1997

    Effects of increased CO2 on Phytoplankton: Time variation of Larval weightRiebesell U., et. al. Reduced calcification of (adapted from Krebs Fig. 28.17)Marine phytoplankton in response to increasedAtmospheric CO2. Nature 407:364 (2000).

    Read:

    ZKA BISKUP, GET THE OCEANS SOME TUMS

    tudy questionsest C reservoirs and fluxes in the environment?

    g carbon likely to be?

    AGNIES

    Published on October 7, 2003, Boston Globe, Page C2 Col 2

    S What are the larg

    What do we mean by the missing carbon? Where is this missin

    How do temperate forests respond to elevated CO2 after 1-5 years? 30 years?

    How can stable isotopes be used to determine temperature 1000s of years ago?

    By what mechanism do oceans primarily absorb CO2?