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Check In HW and Set Up 5 Yeast Dilutions. Sentinel Species?. Warwick E. Kerr. Sentinels of Global Warming?. Biogeochemical Cycles. How do biogeochemical cycles reflect the 1 st law of thermodynamics?. Nutrient Cycles.
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How do biogeochemical cycles reflect the 1st law of thermodynamics?
Nutrient Cycles • Materials necessary to build tissues and carry out essential life functions • Examples: Carbon, Phosphorus, Nitrogen
HYDROLOGIC CYCLE • Evaporation • Condensation • Powered by solar radiation
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
Mutualism & The Carbon Cycle • Photosynthesis “fixes” gaseous carbon (in form of CO2) into a more stable form (glucose/C6H12O6) • Cellular Respiration releases carbon in form of CO2
A Precarious Balance • CO2 is only a small fragment of the atmosphere (0.04%) • Less than 2% of the world’s CO2 comes from burning fossil fuels • YET, the carbon cycle is rapidly becoming unbalanced in its ability to absorb the increases in CO2
NITROGEN CYCLE • 78% of atmosphere is DIATOMIC NITROGEN (N2) • N2 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
ABIOTIC NITROGEN FIXATION • High energy reactions like lightning and vulcanism can break the triple bonds of N2 • Liberated nitrogen reacts with oxygen to create Nitrate (NO3) and Nitrite (NO2)
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
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