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Nitrogen and Phosphorus Cycles Martha E. Rosemeyer IES January 29, 2003 One of three dynamic processes of ecosystems Energy flow Nutrient cycles Succession Energy flows from the sun to entropy through a functioning food web Two types of nutrient cycles Volatile atmospheric reservior N, S Non-volatile No atmospheric reservior P, K, Ca, Mg all micronutrients Nitrogen cycle N2O N2 2 Nitrification 3 Gliessman, 1998 modified N Pool Size (Stocks) are relatively big Atmosphere g N 1021 Terrestrial biomass g N 1015 Soil organic matter g N 1015 Flows small Rate limiting steps with respect to getting N into terrestrial system: Via lightning (very small) Via Biological N Fixation natural legume crops Via Industrial fixation of fertilizer Via Fossil fuel burning What is biological nitrogen fixation (BNF)? Second most important biochemical reaction of ecosystem after photosynthesis to life on earth Involves the reduction of N from molecular state N2 to NH3 in which form it can be incorporated into an organic (C containing) molecular structure Involves microbes BNF Regardless of organism uses nitrogenase enzyme for to fix N2 to ammonia NH3 NH3 + org. acids amino acids proteins White clover, Trifolium repens “Trebol blanco” Temperate zone green manure crop seed Human-caused NF = or greater Natural terrestrial BNF BNF from crops 40 x 1012 g N fixed/yr Fertilizer industry 80 Fossil fuel burning 20 Total human-caused 144 BNF terrestrial ecosystems 100 Microbes: The Ancient Ones Responsible for all major processes on earth, including decomposition and photosynthesis and nutrient cycling Major cycles of Earth could continue without plants and animals Most microbes are beneficial! Most bacteria 99% cannot be cultured Therefore we know little about them! A ton of microscopic bacteria may be active in each acre of soil. Bacteria dot the surface of strands of fungal hyphae. --Soil Biology Primer Life on earth: starting with microbes First N fixed by lightning and meteor impact Formation of first amino acids and protein N-fixation early because N-limited environment in water Terrestrial system: P limited environment Mycorrhizal fungi have allowed plants to become terrestrial Nitrogen cycle:mediated by microbes = Microbial mediation 2 3 Gliessman 1998 modified P Cycle P is an important plant nutrient, anion Released from soil, taken up by plants and released to soil Green Rev ag is totally dependent on P rock P rock is basically a valuable, nonrenewable resource for agriculture some deposits contaminated with Cd, Pb, As 10% of the P which is applied to land is flushed way causing eutrophication of lakes Dead zone in Gulf of Mexico due to nutrients from Mississippi The phosphorus cycle = Microbial mediation mycorrhizae Gliessman 1998 P cycle Brady, 1999 Roots of Common Bean (Phaseolus vulgaris) from Costa Rica Mycorrhizal fungus stained blue Non mycorrhizal Components of association fungus + root = mycor + rhiza They are the rule, not the exception: Most of world’s vascular plants have association, except Brassicaceae (cabbage family) and a few other plant families Fungus: takes up water and P, receives CHO from plant Enables plants to live in low P, low water environments Mycorrhizae aid soil aggregation Mycorrhizal fungi link root cells to soil particles. In this photo, sand grains are bound to a root by hyphae from endophytes (fungi similar to mycorrhizae), and by polysaccharides secreted by the plant and the fungi. Credit: Jerry Barrow, USDA-ARS Jornada Experimental Range, Las Cruces, NM. Closing nutrient cycles Making the cycle circular The nutrient comes back to the “stock” or “pool” that it started with-- none is lost In a human time frame This is an important component of sustainability Chinese have used “night soil” for centuries to close nutrient cycle