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Published byDarnell Noblet Modified over 9 years ago
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Check In HW and Set Up 5 Yeast Dilutions
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Sentinel Species?
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Warwick E. Kerr
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Sentinels of Global Warming?
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Biogeochemical Cycles
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How do biogeochemical cycles reflect the 1 st law of thermodynamics?
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Nutrient Cycles Materials necessary to build tissues and carry out essential life functions Examples: Carbon, Phosphorus, Nitrogen
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HYDROLOGIC CYCLE Evaporation Condensation Powered by solar radiation
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Primary Productivity v. Rainfall
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Carbon Cycle Appx. 49,000 metric gigatons of carbon on Earth and in atmosphere 71% in ocean 22% fossilized 3% in dead matter 2% in live matter 1% in atmosphere
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Mutualism & The Carbon Cycle Photosynthesis “fixes” gaseous carbon (in form of CO 2 ) into a more stable form (glucose/C 6 H 12 O 6 ) Cellular Respiration releases carbon in form of CO 2
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A Precarious Balance CO 2 is only a small fragment of the atmosphere (0.04%) Less than 2% of the world’s CO 2 comes from burning fossil fuels YET, the carbon cycle is rapidly becoming unbalanced in its ability to absorb the increases in CO 2
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NITROGEN CYCLE 78% of atmosphere is DIATOMIC NITROGEN (N 2 ) N 2 is essentially useless to living organisms as the triple covalent bonds between nitrogen atoms make it chemically inert To “liberate” nitrogen it must be chemically reacted with other atoms
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ABIOTIC NITROGEN FIXATION High energy reactions like lightning and vulcanism can break the triple bonds of N 2 Liberated nitrogen reacts with oxygen to create Nitrate (NO 3 ) and Nitrite (NO 2 )
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BIOTIC NITROGEN FIXATION Rhizobium bacteria use the enzyme nitrogenase to break apart N2 in the absence of oxygen To isolate themselves from oxygen, Rhizobium live in nodules on legumes
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Phosphorus & Algal Blooms Excess phosphorus in aquatic ecosystems allows for algal populations to increase drastically by raising the carrying capacity However, biological oxygen demand becomes too high and system crashes
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